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CANOD.pdfCity of Edmonds Critical Area Notice of Decision ritical Area F171—e#- Site ile#: Site Location: 3 4 �- S� Project Description: Owner: Permit Number: � 7d ► h 1 Parcel Number: S D ❑ Conditional Waiver. No critical area report is required for the project described above. 1. There will be no alteration of a Critical Area or its required buffer. 2. The proposal is an allowed activity pursuant to ECDC 23.40.220, 23.50.020, and/or 23.80.040. 3. The proposal is exempt pursuant to ECDC 23.40.230. ❑ Erosion Hazard. Project is within erosion hazard area. Applicant must prepare an erosion and sediment control plan in compliance with ECDC 18.30. ritical Area Report Required. The proposed project is within a critical area and/or, a critical area buffer and a critical area report is requiredry A critical area report has been submitted and evaluated for compliance with the following criteria pursuant to ECDC 23.40.160: 1. The proposal minimizes the impact on critical areas in accordance with ECDC 23.40.120, Mitigation sequencing; 2. The proposal does not pose an unreasonable threat to the public health, safety, or welfare on or off the development proposal site; 3. The proposal is consistent with the general purposes of this title and the public interest; 4. _� Any alterations permitted to the critical area are mitigated in accordance with ECDC 23.40.110, Mitigation requirements. 5. The proposal protects the critical area functions and values consistent with the best available science and results in no net loss of critical functions and values; and 6. The proposal is consistent with other applicable regulations and standards. ❑ Unfavorable Critical Area Decision. The proposed project is not exempt or does not adequately mitigate its impacts on critical areas and/or does not comply with the criteria in ECDC 23.40.160 and the provisions of the City of Edmonds critical area regulations. See attached findings of noncompliance. Favorable Critical Area Decision. The proposed project m described above and as shown on the attached site plan meets or is exempt from the criteria in ECDC 23,40, 10,0, Review Criteria, and complies with the applicable provisions of the City of Edmonds critical area regulations, Any subsequent changes to the proposal shall void this decision pending re -review of the proposal. Conditions. Critical Area specific condition(s) have been applied to the permit number referenced above. See referenced permit number for specific condition(s). Notice on Title. Critical area notice on title recorded under AFN 7-0 l -7 M I S Reviewer Signature Date Appeals: Any decision to approve, condition, or deny to development proposal or other activity based on the requirements of critical area rega lat ons may be appealed according to, and as part of, the appeal procedure, if any, for the permit or approval involved. Revised 11/29/2016 SHANNON �LSONJ. om GEOTECHNICAL AND ENVIRONMENTAL CONSULTANTS February 16, 2017 Ms. Taine Wilton Edmonds School District No. 15 20420 681h Avenue West Lynnwood, WA 98036 RE: RESPONSE TO PLAN REVIEW COMMENTS FOR PERMIT #BLD20161599, NEW MADRONA K-8 PROJECT, 9300 236T11 STREET SW, EDMONDS, WASHINGTON Dear Ms. Wilton: This letter presents our response to comments provided by the City of Edmonds Development Services Department in their letter dated February 3, 2017. The reviewer requested that we describe any impact to the slope west of the track and whether any mitigation will be needed for construction in that area. Currently, the slope to the west of the track and field (west slope) extends vertically down to the west approximately 30 to 40 feet at grades of 20 to 30 percent. It is densely wooded with mature trees and understory vegetation. Our reconnaissance of the west slope did not reveal any evidence of slope instability. Wetlands have been mapped along the west slope (Plan Sheet G-003) and are described within the Revised Wetland and Stream Delineation Report submitted on August 4, 2016. The wetlands within this area are described as being supported primarily from observed groundwater seeps. The existing stormwater drainage system within the track and field area discharges water onto the slope. The project design plans provided to us indicate there will be no significant construction on the slope or at the top of the slope. The slope will be protected from runoff and sedimentation during construction using a system of drainage swales, temporary stormwater collection/treatment, erosion -control fencing and a chain link fence installed along the top of slope. Improvements to the track and field stormwater drainage system will include abandoning the existing discharge pipes and replacing them with a system that conveys water away from the 400 NORTH 34TH STREET, SUITE 100 P.O. BOX 300303 SEATTLE, WASHINGTON 98103-6636 206-632-8020 FAX: 206-695-6777 www.shannonwilson.com 21-1-22082-004 Ms. Taine Wilton SHANNON 6WILSON, INC. Edmonds School District No. 15 February 16, 2017 Page 2 of 2 slope. The proposed construction within the track and field area will not impose additional surcharges to the slope as no additional soils will be placed along the top of slope. In our opinion, the west slope is currently in a stable condition and no mitigation measures are required to maintain stability during or after construction. If you have any questions regarding the findings presented herein, please contact me at (206) 695-6875. Sincerely, SHANNON & WILSON, INC. Martin W. Page, PE, LEG Vice President Geotechnical Engineer KJW:MWP/kjw 21-1-22082-004-LlhvpAkn 21-1-22082-004 Geotechnical Engineering Report New Madrona K-8 Project 9300236 th Street SW Edmonds, Washington October 31, 2016 Excellence. Innovation. Service. Value. Since 1954. Submitted To: Ms. Taine Wilton Oli1pC 10 R S C 0 Edmonds School District #15 2042068 th Avenue West y� Lynnwood, Washington 98036 By: Shannon & Wilson, Inc. RECEIVED400 N 34th Street, Suite 100 Seattle, Washington 98103 ,.) 2016 21-1-22082-004 TABLE OF CONTENTS SHANNON WILSON, INC. Page 1.0 SITE AND PROJECT DESCRIPTION ....... ....... ........ ........ ........ ..............................1 2.0 SITE CONDITIONS.....................................................,.. ,..,.,...,,,.,.,,., .,...,,,.,,.,.,,.,...,,.....,....2 2.1 Regional Geology.......................................................... ..,.,.... , ..,,.,., 2 2.2 Regional Seismicity....................................................................................................2 3.0 SUBSURFACE EXPLORATION.... ,,. ..,,,,. ,,. ,,.., ....__ ..... ...........................3 4.0 FIELD INFILTRATION TESTING, .......,. „.... .,...... ....... ., .......,............,...,...,..4 5.0 LABORATORY TESTING .......... —...................................... ............M., .. ,.,....,..,..,..,....5 6,0 SUBSURFACE CONDITIONS....... ..... ....... ... ........ .... .......... ...5 ....... ....... .... ........ ..... ........... .... . 6.1 Site Geology and Subsurface Conditions...................................................................5 6.1.1 Subsurface Conditions at Proposed Building..............................................5 6.1.2 Subsurface Conditions at Proposed Parking Lots and Driveways...............6 6.2 Hydrogeologic Conditions ........................................... ..,,..,.. ..,,,... ...,..., ,..,.,...,6 7.0 ENGINEERING STUDIES AND RECOMMENDATIONS................................................6 7.1 General .................................. ........................... ......... .................. .....................6 7.2 Foundation Design............................................................... ............ ................ .......... 7 7.3 Seismic Design.............................................................. 7.4 Lateral Earth Pressures and Retaining Walls.............................................................8 7.5 Lateral Resistance ......................................... ..... _,..... ..,,....... ....... ,.,....,,..,................. 9 7.6 Slope Stability............................................................... ...,., ,..,..,,, ...........,..........9 7.7 Pavement Design..........................................................___.,....,.,.,....,,,,...,,.,,....,10 7.7.1 Traffic Load ................................. ................. ...........,................. ,,,,.,,,,10 7.7.2 Subgrade Conditions..................................................................................10 7.8 Non -Porous Pavement Section Recommendations..................................................10 7.9 Porous Pavement Section Recommendations..........................................................11 7.9.1 Grass Grid Pavers .......................____ .. ........ ................., ......,.. .........11 7.9.2 Pervious Hot Mix Asphalt (HMA) and Concrete......................................11 7.10 Pawei cut Sect as Near Steep Sl?e.12 7.11 Frost $e,t „ n; �c a�"" . ................ ..........12 ��.. q 8.0 G�EOTECHN1 A�a �� .... ........ VOR"ItE '� O� ��A;".................13 8.1 Earth rk �, �s fit o ......... ,. .................13 8.2 Pervious Pavement Materials........... ................... .............. ........ ,., ,.,,_..,14 8.3 Construction and Maintenance Considerations for Pervious Pavement ,,..,,„„.,,.,,..,14 8.4 Temporary and Permanent Excavation Slopes.........................................................15 8.5 Erosion Control ....................................................,.,,,..,,,,,..... „ ........ ...,........... ,,..16 21-1-22082-004-R1fdocx/wp/Bm 1 21-1-22082-004 TABLE OF CONTENTS (cont.) SHANNON 6WILSON, INC. Page 8.6 Construction Drainage.............................................................................................16 8.7 Subsurface Drainage ... ............ .................. .................. ....................... ..............16 8.8 Utilities .......................................... ., ....,.... ..,..,............................................... ,......16 8.9 Wet Weather Earthwork...........................................................................................17 8.10 Plans Review and Construction Observation ....................... ..........-- ........ —..,,..--18 9.0 LIMITATIONS .............................. ...... .......................................... .........., ........, ,..,.... ,.18 10.0 REFERENCES.............................................................................. .... ... .............— ...20 TABLES 1 Recommended Minimum Parking Lot and Driveway Section Thicknesses .........11 2 Recommended Minimum Porous Pavement Section Thicknesses ........................11 3 Imported Backfill Specifications Based on 2016 Washington State Department of Transportation Standard Specifications.........................................13 FIGURES 1 Vicinity Map 2 Site and Exploration Plan 3 Typical Rockery Detail 4 Measured Water Level, Pilot Infiltration Test, Test Pit PIT -1 5 Measured Water Level, Pilot Infiltration Test, Test Pit PIT -2 6 Measured Water Level, Pilot Infiltration Test, Test Pit PIT -3 APPENDICES A Subsurface Explorations B Laboratory Test Results C Analytical Laboratory Test Results D Important Information About Your Geotechnical/Environmental Report 21-1-22082-004-R1f.docx/wp/Um 11 21-1-22082-004 SIM4NON WILSON, INC. GEOTECHNICAL ENGINEERING REPORT NEW MADRONA K-8 PROJECT 9300236 T11 STREET SW EDMONDS, WASHINGTON 1.0 SITE AND PROJECT DESCRIPTION The Edmonds School District No. 15 plans to construct a new Madrona K-8 School on the south side of the property at 9300 236' Street SW in Edmonds, Washington, as shown in the Vicinity Map (Figure 1). The property contains the existing Madrona K-8 School and is bounded by 236th Street to the north, residential developments on the east and south sides, and the former Woodway Elementary School on the west. The site has a number of distinct surface features including a parking lot on the northwest side, track and large open field area on the southwest side, and a baseball field on the southeast side. There is a densely wooded ravine area along the east side of the property and a densely wooded slope on the west side of the property that slopes down to the former Woodway Elementary School. The purpose of this study is to finalize our geotechnical recommendations with data from additional subsurface explorations and testing to aid in the final design of the proposed structure. Geotechnical recommendations were provided previously in a preliminary geotechnical engineering report submitted on August 6, 2015. Our scope of services for the design phase included drilling and sampling 12 geotechnical borings and excavating 5 test pits. However, one of the proposed drilling locations was changed to a test pit exploration for a total of 11 geotechnical borings and 6 test pits. The proposed drilling location was changed to a test pit due to the close proximity to subsurface utilities and access issues. Locations of the subsurface explorations were selected to coincide with the planned location of the proposed building and associated facilities. Descriptions of the subsurface exploration activities are discussed further in Section 3.0. The results of our pilot infiltration testing (PIT) are discussed in Section 4.0. This report presents updated geotechnical engineering recommendations to incorporate the additional subsurface information gathered from the new explorations and information provided by the design team. We have'included recommendations for pavement design and a discussion of buffer and setback distances when adjacent to steep slopes and other geologic hazard areas. The results of the soil fertility testing are also provided to aid the design team in evaluating the suitability of on-site topsoil for use in landscaping. 21-1-22082-004-R1f docx/wp/llm 21-1-22082-004 2.0 SITE CONDITIONS 2.1 Regional Geology AMON 6W11130N,IIID The site is located in Edmonds, Washington, which is within a region known as the Puget Lowland. The Puget Lowland is a structural depression bordered by the Olympic and Cascade Mountain ranges that is generally within about 500 feet of sea level. The geology of the area has been influenced by repeated cycles of glaciation, which worked to fill the lowland to significant depths with a complex sequence of glacial and nonglacial deposits. The most recent glacier to impact the area, the Vashon Stade of the Fraser Glaciation, overrode the area with up to 3,000 feet of ice in some locations. Following the last glaciations, the erosion of some of the glacially overridden soil deposits, as well as local deposition and human placement of additional soil deposits, have further complicated the local geology (Troost and Booth, 2008). The project site itself is situated on a ridge underlain by Quaternary Vashon till (Qvt) that was observed at relatively shallow depths during the current subsurface investigation. This geologic unit was found to be a very dense, gray to gray -brown deposit consisting of silty sand with variable gravel, cobble, and some boulder content. Other explorations performed on the site (Shannon & Wilson, Inc. [Shannon & Wilson], 2016) encountered deposits of Quaternary Vashon advanced glacial outwash (Qva) at depths of approximately 40 to 50 feet below ground surface (bgs). This geologic unit is characterized by dense to very dense sands and gravels with variable amounts of silt. Qva is typically less compact and more pervious than Qvt. Geologic maps of the Snohomish County region indicate that the contact between the glacial till and advanced outwash material is on the slope on the west side of the property. The Qva at the site may be underlain by pre-Vashon interglacial and glacial soils, predominantly fluvial. 2.2 Regional Seismicity The Puget Sound Lowland is located in the fore arc of the Cascadia Subduction Zone. The seismicity of the region is largely derived from the subduction of the Juan de Fuca Plate beneath the North American Plate. The convergence of these two plates results in a number of generally east -west -trending faults, as well as basin and uplift regions (Troost and Booth, 2008). The seismic hazard of the region comes from three major sources, a major subduction type events, deep intraplate events (such as the 2001 Nisqually earthquake), and earthquakes due to rupture of shallow crustal faults. The site itself is located a reasonable distance from subduction and intraslab sources, and as a result, the more local, crustal faults are believed to drive the seismic hazard for the site. The closest known potentially active fault to the site is the South Whidbey Island Fault (SWIF). The 21-1-22082-004-R1 f docx/wp/Um 21-1-22082-004 2 SWIF is a shallow, strike -slip fault that is believed to be capable of producing a magnitude 7.5 event, which could impose significant seismic demands on structures at the site. 3.0 SUBSURFACE EXPLORATION Previously, we completed subsurface explorations as a part of a preliminary geotechnical engineering study to aid in the selection of the proposed building location. Previous explorations consisting of 16 test pits on the southern half of the property were completed on June 24, 2015. Logs of the previous subsurface explorations are included in Appendix A. Recent subsurface explorations consisted of test pits and geotechnical borings completed between Monday, July 25, 2016, and Friday, July 29, 2016. Holocene Drilling (Holocene), under subcontract to Shannon & Wilson, completed a total of 11 geotechnical borings with the use of a track -mounted Diedrich D-50 drill rig. Holocene used the hollow -stem auger drilling method to complete the borings to depths ranging from 15.5 to 16.5 feet bgs. Holocene collected samples on approximate 2.5 -foot intervals with the use of the Standard Penetration Test. Once the geotechnical borings were completed, Holocene backfilled the holes with bentonite to within approximately 1 to 2 feet bgs. Borings that were drilled in the asphalt parking area were patched with concrete. Clearcreek Contractors (Clearcreek), under subcontract to Shannon & Wilson, completed a total of six test pits to depths ranging from 4 to 10 feet with the use of a rubber -tired John Deere 310SJ backhoe. Three of the test pits were used to characterize infiltration within the near - surface soils. Infiltration testing within the near -surface soils is discussed below in Section 4.0. Following the excavations and testing, Clearcreek backfilled the test pits with the excavated material and tamped the material down using the excavator bucket in approximately 1 -foot -thick lifts. Once Clearcreek had completed backfilling the test pits, they rolled the surface for further compaction and replaced the grass layer where it was possible to salvage. The explorations were located throughout the site as shown in the Site and Exploration Plan, Figure 2. Test pits designated with a PIT were the ones in which we performed the in situ infiltration tectinu/PTTc_ while the tect nits decinnated with a TP were not need fnr in citli ---- -- ---a - ---1 • • ----- ---- ---- r- -- -a--- -- .. ---- -- -- • • --- ___ _ —_-- --- --- ___» infiltration testing. During the exploration process, the soil and groundwater conditions were observed by an engineer or a geologist from our office. Soil samples were collected and transported to our Seattle laboratory for analysis and testing. Logs of the explorations are presented in Appendix A. 21-1-22082-004-R1 f docx/wp/Ilm 21-1-22082-004 3 S511 MMON MILSON, IING The geotechnical boring and test pit locations provided in Figure 2 are approximate, being based on hand measurements from site features, and surface elevations shown in the logs are estimated from a topographic survey of the site prepared by PACE Engineers, Inc. 4.0 FIELD INFILTRATION TESTING We performed small-scale PITs within three of the six test pits excavated during the current subsurface explorations. The PIT test pits were designated as PIT -1 through PIT -3, and the locations are shown in the Site and Exploration Plan, Figure 2. All three of the infiltration tests were performed on July 28, 2016. These test pits were over excavated following the PITs on July 29, 2016. Details of the three tests are presented below and are summarized in the PIT data plots (Figures 4 through 6). The PIT -1 test pit bottom during the PIT was approximately 3.8 feet bgs, or about Elevation 440.7 feet. The tested soil unit was fill, consisting of reworked glacial till. After the water flow was terminated, the test pit drained completely overnight. No free water was present below the PIT test depth when we overexcavated it on July 29, 2016. A plot of the PIT -1 test data is presented as Figure 4. The observed (short-term) infiltration rate was approximately 0.80 inch per hour, based on the last hour of the constant head period. If these soils represented the subgrade beneath a bioretention feature constructed with imported bioretention soil, the City of Edmonds (City) will require the application of a correction factor of 2 due to the test being performed during the dry season. This would result in a design (long-term) infiltration rate of 0.4 inch per hour. The PIT -2 test pit bottom during the PIT was approximately 3.3 feet bgs, or about Elevation 452.7 feet. The tested soil unit was glacial till, with a short-term infiltration rate of 0.13 inch per hour, based on the falling head data collected after the water flow into the test pit was terminated. Applying the correction factor would result in a design infiltration of 0.06 inch per hour. The test pit failed to drain completely overnight and this soil is considered to be a hydraulic restriction to infiltration, due to its low infiltration rate. A plot of the PIT -2 test data is presented as Figure 5. The PIT -3 test pit bottom during the PIT was approximately 2.9 feet bgs, or about Elevation 447.1 feet. The tested soil unit was glacial till, with a short-term infiltration rate of 0.07 inch per hour based on the falling head data collected after the water flow into the test pit was terminated. Applying the correction factor would result in a design infiltration rate of 0.03 inch per hour. The test pit failed to drain completely overnight and this soil is considered to be a hydraulic 21-1-22082-004-Rlfdocx/wp/llm 21-1-22082-004 4 restriction to infiltration due to its low infiltration rate. A plot of the PIT -3 test data is presented as Figure 6. If a shallow well were installed in the vicinity and read during the wet season, no correction factor would be required, provided groundwater is at least 3 feet below the bottom of the facility,. 5.0 LABORATORY TESTING Laboratory testing was conducted on several soil samples collected from the test pit explorations to assist in classification and characterization of the subsurface soils. The laboratory tests included natural moisture content determination and grain size analysis. The natural moisture contents are indicated on the test pit logs in Appendix A. The results of the grain size analyses are presented in Appendix B. Most of the grain size tests were sieve analyses. Combined sieve and hydrometer tests were performed on two samples (from B-4 at 5 feet deep [about Elevation 440 feet] and from B-5 at 7.5 feet deep [about Elevation 439.5 feet]) so that the U.S. Department of Agriculture (USDA) texture could be identified. Both samples are considered to be "sandy loam," based on the USDA textural system. Based on our discussions with the City, the short-term infiltration rate for these soils is 1 inch per hour. Since the explorations were completed during the dry season, a seasonal correction factor of 2 is required, resulting in a design infiltration rate of 0.5 inch per hour. This assumes that these soils represent the subgrade beneath bioretention features with imported bioretention soil. In order to characterize the existing topsoil within the upper and lower field, we submitted two samples to Spectra Laboratories (Spectra) in Poulsbo, Washington. The samples were tested for soil fertility and the results with recommendations from Spectra are included in Appendix C. 6.0 SUBSURFACE CONDITIONS 6.1 Site Geology and Subsurface Conditions Intact glacial till soils were encountered in all but one of the explorations performed under the current scope of work. The test pit PIT -1 did not encounter intact glacial till, but did encounter weathered till at a depth of approximately 7 feet bgs. 6.1.1 Subsurface Conditions at Proposed Building Explorations performed within or near the proposed building footprint on the existing upper play field in the southeast corner of the site indicate that this area is underlain by a thin layer of topsoil followed by layers of fill, weathered or reworked glacial till, and intact glacial 21-1-22082-004-R1 f docx/wp/Hm 21-1-22082-004 5 Q,,,,AINNON WILSON, IING till. Borings B-7, B-9, B-10, and B-12 indicate that there is a layer of fill soils at depths ranging from 4.5 to 7 feet bgs. Fill soils consisted of medium dense to very dense, silty sand to silty sand with gravel. Intact very dense glacial till underlying the building footprint was encountered at depths ranging from approximately 1 to 7 feet bgs. 6.1.2 Subsurface Conditions at Proposed Parking Lots and Driveways Explorations performed within the parking areas west of the existing school building and north of the track indicated that fill soils overlying the glacial till are present at depths ranging from 7 to 9.5 feet bgs. Borings and test pits on the north and east sides of the existing building also encountered fill soils at depths ranging from 4.5 to 6 feet bgs. Intact, very dense glacial till was found to underlie the fill soils. 6.2 Hydrogeologic Conditions Groundwater was not encountered in the recent shallow soil borings and test pits, all of which were performed during the dry season. Moist to wet layers were observed below about 15 feet in borings B-2, B-3, and B-5, and below about 12 feet in boring B-9, which may indicate the presence of perched groundwater. Subsurface explorations performed previously onsite as part of our hydrogeologic study (Shannon & Wilson, 2016) identified a regional groundwater aquifer at the site at about 180 feet deep and between approximate Elevations 276.3 to 277.2 feet. Perched groundwater zones were also encountered during the previous hydrogeologic explorations at depths ranging from 8.5 to 11 feet bgs (Shannon & Wilson, 2016). Note that groundwater is not expected to be encountered during excavations for the new school building. We understand that the project stormwater management system will consist of a series of shallow bioretention swales combined with underground injection control (UIQ wells. The results of our recent hydrogeological testing and analysis are presented in a separate report (Shannon & Wilson, 2016). Please refer to this report for design recommendations regarding UIC construction and infiltration rates. 7.0 ENGINEERING STUDIES AND RECOMMENDATIONS 7.1 General Based on the observations made during the subsurface exploration program and information reviewed for the project, we expect the glacial till material will provide good support for conventional spread footing foundations with minimal settlements. 21-1-22082-004-R1 £docx/wp/Hm 21-1-22082-004 6 ,,,,1ANNOIN 6W11,,,,,,SON, IIIA The following subsections provide detailed recommendations on the following topics: • Foundation design • Seismic design ® Lateral earth pressures • Lateral resistance • Slope stability • Pavement design 7.2 Foundation Design The subsurface explorations encountered undisturbed, very dense, native glacial till soils across the entire site. Spread footings founded in the dense, native till material may be designed with an allowable bearing pressure of 10,000 pounds per square foot (psf). Spread footings that are founded in compacted structural backfill placed above the glacial till may be designed for an allowable bearing capacity of 4,000 psf. These allowable bearing values may be increased by one-third for transient seismic loading. Any fill material that is to be reused should be evaluated by a geotechnical engineer to see if they are suitable for use. Use of on-site fill material is discussed in Section 8.1. Based on the subsurface conditions, isolated overexcavation could be required due to the presence of some existing fill within the building footprints. As an alternative to overexcavation of fill material encountered at footing subgrade elevations, in situ densification of the fill could be accomplished with the use of heavy vibratory compaction equipment (i.e., excavator -mounted "ho-pac"). Footing subgrades should be observed by a qualified geotechnical engineer or geologist. If the native glacial till material or compacted structural backfill is used as the foundation bearing soils, it is anticipated that any settlement that occurs will be essentially instantaneous as the load is applied during construction. If the footings are designed for the bearing pressures noted above, then the total footing settlements will be less than '/z inch. Differential settlements would be about one-half of the total settlement. However, if the entire structure is founded on the glnoinl till then differential settlements .vo',:ld he :ns.gruficant. 7.3 Seismic Design The seismic design of the structure should be in accordance with the International Code Council, Inc. 2015 International Building Code (IBC) (International Code Council, Inc., 2014). The IBC design criteria are based on a target risk of structural collapse of 1 percent in 50 years. The soil 21-1-22082-004-xff:aocx/wpnkn 21-1-22082-004 7 °°ANMON &WILSON, ING profile is assessed by assigning a site class definition. It is our opinion that based on the soil classification, i.e., very dense, the site can be classified as Site Class C. Seismic inputs are the short -period maximum spectra acceleration, Ss, and spectral acceleration at a period of one second, Si. Using the map provided in the IBC, which corresponds to Site Class B sites, the mapped values of Ss and S1 are approximately 1.262 and 0.493g, respectively. The site coefficients for the given spectral acceleration values and site class C are 1.0 and 1.31 for Fa and F, respectively. Seismic hazards such as liquefaction and fault rupture are not present at the project site. 7.4 Lateral Earth Pressures and Retaining Walls Lateral earth pressures will act on portions of the building as well as on retaining walls. The magnitude and distribution of these lateral pressures will depend on many factors, including, but not limited to, the type of backfill, the method of backfill placement, level of backfill compaction, slope of backfill, drainage, and characteristics of the wall itself. If the wall is allowed to move at least 0.001 times the wall height, the wall is considered flexible and active earth pressures can be used. If the wall is considered to be inflexible then at -rest earth pressures must be used. The active and at -rest earth pressures, evaluated using an equivalent fluid unit weight, are estimated to be on the order of 30 and 50 pounds per cubic feet (pcf), respectively. The values given above assume a permanent wall structure, the ground surface behind the wall is level, and that proper drainage is installed to prevent the buildup of pore water pressure behind the wall. The total earth pressures should be analyzed for seismic loading conditions using a dynamic load increment equal to a percentage of the static earth force. The percentage load increase for seismic condition was developed to be consistent with a pseudo -static analysis using the Mononobe-Okabe equation for lateral earth pressures (Kramer, 1996) and a horizontal seismic coefficient of 0.2. The load increase for seismic conditions is recommended to be a uniformly distributed load equal to 8H, where H is the height of the wall. Note the seismic coefficient is not equal to the peak ground acceleration (PGA) expected to be encountered at the site in a design event. The PGA is experienced only a few times within the record of earthquake shaking, and the actual earthquake ground motion is cyclic in nature, not static. Values of the seismic coefficient are thus typically one-third to one-half the value of the PGA that may be experienced at the site during a design level event. We understand that rockery walls may be installed. Rock walls have been used in numerous locations around Puget Sound area primarily to provide erosion protection to cuts in stable 21-1-22082-004-R1f docx/wp/Hm 21-1-22082-004 8 SNANNON 6WILw IIIA materials. Rockeries have also been used to retain fill slopes; however, this practice is not as prevalent. In our opinion, rockeries could be used to retain cut slopes made in dense to very dense native soil that are less than 6 feet high. Rockeries should be constructed in accordance with the recommendations shown in Figure 3. Rockeries could be used to retain fill slopes provided they are 5 feet high or less, or if they are reinforced. If used with a reinforced slope, the rockery would form a facade or erosion protection facing on an otherwise stable slope. Rockeries that are used to retain fill slopes that are 5 feet high or less should be built in accordance with the recommendations shown in Figure 3. We recommend that the fill be built out beyond the planned wall location and then cut back. With this procedure, the fill can be fully compacted, as compared with the difficulty of compacting the edge of a fill slope. 7.5 Lateral Resistance Footings may resist lateral loads using a combination of base friction and passive pressure against the buried or embedded portion of the footings and buried wall. We recommend that base sliding resistance be determined using an allowable coefficient of friction of 0.7 for a concrete foundation founded on on-site glacial till or compacted structural fill. Passive earth pressures can be evaluated using an equivalent unit weight of 400 pcf. This value includes a factor of safety of 1.5. 7.6 Slope Stability The slope along the eastern perimeter of the property is mapped as a critical area by the City due to the steepness of the slope and the presence of wetlands. We recommend that the Madrona K-8 school footprint be set back at least 10 feet from the top of slope. While we did not observe active landsliding on this slope, the Edmonds Community Development Code requires that buildings or other structures constructed near an environmentally critical area maintain a setback of 15 feet from the edge of the critical area which in this case is the top of the slope (Edmonds, Wash., 2016). However, the code also allows for setbacks to be determined by a Geotechnical Engineering Report. In our opinion, after review of the subsurface conditions and the current condition of the slope, a setback of 10 feet would not cause an increased potential for landslides or surficial soil instability on the steep slope. In our opinion, buried utilities within this setback distance are acceptable and will not be at risk due to slope instability. We understand that dead or diseased tree removal is planned along the east, west, and south perimeter of the property near the top of the slopes. We made a site visit on September 20, 2016, 21-1-22082-004-R1 f docx/wp/11m 21-1-22082-004 9 IIII°° IIS WILSON, [ING to observe the slope areas where tree removal is planned. In our opinion, the planned tree removal will not cause instability of the slope and the trees may be felled and chipped in-place. 7.7 Pavement Design Pavement analyses were conducted using the American Association of State Highway and Transportation Officials (AASHTO) method for flexible and rigid pavement design (AASHTO, 1993). The AASHTO method is a widely used empirical design procedure for the design of flexible and rigid pavement structures. It considers strength of the base course materials, traffic stresses, and the strength of the pavement subgrade. The pavement design life is assumed to be 20 years. 7.7.1 Traffic Load Average daily traffic counts, including delivery trucks, school buses, and occasional heavy vehicles such as fire trucks, were based on assumed conditions for similar projects. Assumed traffic volumes were then converted into equivalent single -axle loads by using equivalent load factors. We assume that there will not be a significant increase in traffic at this location, but did include a 1 percent growth factor in the design life traffic counts for our analysis. 7.7.2 Subgrade Conditions The subgrade conditions at the proposed pavement locations are medium dense, silty sand to silty sand with gravel fill suitable for pavement support. If loose or soft subgrade is observed during construction, we recommend that it be removed and replaced with at least 1 foot of compacted structural fill. A Resilient Modulus, MR, of 15,000 pounds per square inch is recommended for pavement design where existing medium dense fill and newly placed compacted structural fill are present. 7.8 Non -Porous Pavement Section Recommendations For support of the proposed parking and driveway areas we propose pavement section thicknesses shown in Table 1 below. Recommendations have been separated into lightly loaded and heavily loaded pavement sections. Lightly loaded pavement sections are assumed to be those that are utilized primarily by car and other passenger vehicle traffic. Heavily loaded pavement sections are assumed to be those that are utilized by heavy vehicles such as buses, delivery, and fire trucks. 21-1-22082-004-R1fdocx/wp/1lm 21-1-22082-004 10 X1111°°ANNON INWIlLSO , INC TABLE 1 RECOMMENDED MINIMUM PARKING LOT AND DRIVEWAY SECTION THICKNESSES Base course should correspond to crushed surfacing in accordance with the Washington State Department of Transportation (WSDOT) Standard Specifications (WSDOT, 2016). Placement, compaction, and material specification for crushed surfacing is discussed in Section 8.1 of this report. 7.9 Porous Pavement Section Recommendations 7.9.1 Grass Grid Pavers Grass grid pavers will be a proprietary product and should be designed in accordance with the manufacturer's recommendations. For design of the porous pavement sections, we recommend that the compacted subgrade be assumed to have a California Bearing Ratio of approximately 20. 7.9.2 Pervious Hot Mix Asphalt (HMA) and Concrete As we understand, porous pavement sections consisting of pervious HMA or concrete underlain by an underdrain are being considered within the fire lane to collect surface drainage. Pervious pavement consists of porous asphalt or concrete overlying a stone bed. For support of the proposed fire lane areas, we propose porous pavement section thicknesses shown in Table 2 below. TABLE 2 RECOMMENDED MINIMUM POROUS PAVEMENT SECTION THICKNESSES 21-1-22082-004-R1f docx/wp/Um 21-1-22082-004 11 SHANNON IIIA ING Please note that porous asphalt is susceptible to considerable wear due to heavy vehicle loading especially in vehicle turning areas. Rutting due to surface abrasion is known to occur between the wheel and the pavement during breaking and turning. Also note that pervious concrete pavement is sensitive to the means and methods used in mix design and placement. We recommend following the American Concrete Institute (ACI) Specification for Pervious Concrete Pavement, ACI 522.1-13 for design and installation practices of porous concrete pavement systems (ACI, 2013). This specification covers materials, preparation, forming, placing, finishing, jointing, curing, and quality control of pervious concrete pavement. Provisions governing testing, evaluation, and acceptance of pervious concrete pavement are included. Pervious concrete pavement will require annual cleaning to maintain its infiltration function. We recommend vacuum cleaning once or twice a year (depending on conditions) with a regenerative sweeper and pressure washing as needed. 7.10 Pavement Sections Near Steep Slopes Pavements constructed near the steep slopes on the east and west perimeters of the property should have the same minimum pavement sections shown above in Table 1. Subsurface conditions encountered in the explorations indicate that the site is underlain by glacial till at relatively shallow depths, so slope stability is not an issue with regard to pavement construction. 7.11 Frost Susceptibility Frost -susceptible soil is regarded as having greater than 3 percent finer that 0.02 millimeter (mm). Soil with a fines content not exceeding 7 percent passing the No. 200 sieve, based on the minus %-inch fraction, can normally be expected to have 3 percent or less finer than 0.02 mm. The current subsurface explorations indicate the subgrade soil has an average fines content of about 30 percent, which should be considered frost -susceptible. The measured frost depth during cold winters of 1949 and 1950 was about 15 inches near Edmonds, Washington. In accordance with the WSDOT Pavement Policy (WSDOT, 2015), pavement can be designed for frost protection by providing a pavement section that is equal to or thicker than half of the anticipated frost depth. The pavement section includes pavement and non -frost susceptible base course. In our opinion, the minimum recommended pavement sections presented in Table 1 above should provide adequate frost protection. 21-1-22082-004-R1f docx/wp/Hm 21-1-22082-004 12 I�- M IIIY 6WILSON, ING 8.0 GEOTECHNICAL CONSTRUCTION RECOMMENDATIONS 8.1 Earthwork and Use of On-site Soils Fill placed beneath structures such as floor slabs, pavements, sidewalks, or backfill against footings should be structural fill. Structural fill should be placed and compacted upon native soil surfaces observed during construction by a geotechnical engineer or the engineer's representative. The fill soils encountered onsite generally contain sufficient fines to make them moisture -sensitive. In our opinion, on-site soils may be difficult to place and compact to adequate relative compaction levels, particularly during wet weather or in wet conditions. The on-site glacial till soils may be used as structural fill material provided the following conditions are met: • The soil is free from organics, debris, or other deleterious material. • The water content of the on-site soil at the time of compaction is close to its optimum as determined by a Modified Proctor Test (ASTM International [ASTM], 2012). • On-site soils used for fills and backfills that become wet and unstable after placement should be removed and replaced with suitable material. • Stockpiled on-site soils are protected when rainfall is anticipated in accordance with Section 2-09.3(1)E (WSDOT, 2016). If on-site soil becomes too difficult to compact or construction site space limitations prevent stockpiling, we recommend using imported, granular, structural backfill. Imported backfill should meet gradation requirements of the WSDOT Standard Specifications (WSDOT, 2016). Table 3 provides material specifications for various backfill applications. On-site soil not suitable for structural backfill could be used as backfill within landscaped areas. TABLE 3 IMPORTED BACKFILL SPECIFICATIONS BASED ON 2016 WASHINGTON STATE DEPARTMENT OF TRANSPORTATION STANDARD SPECIFICATIONS Structural fill should be placed in horizontal, uniform lifts and compacted to a dense and unyielding condition, and to at least 95 percent of the Modified Proctor maximum dry density (ASTM D1557 [ASTM, 2012]). Subgrades to receive structural fill should be dense and unyielding and should be evaluated by the geotechnical engineer prior to the placement of fill. 21-1-22082-004-R1faocx/wp/1lm 21-1-22082-004 13 SHANNOIN 6WILSON,11611 Preparation of subgrades should be in accordance with Section 2-06 of the WSDOT Standard Specifications (WSDOT, 2016). In general, the thickness of soil layers before compaction should not exceed 10 inches for heavy equipment compactors or 6 inches for hand -operated mechanical compactors. The most appropriate lift thickness should be determined in the field using the Contractor's selected equipment and fill, and verified with in situ soil density testing (nuclear gauge methods). All compacted surfaces should be sloped to drain to prevent ponding. Structural fill placement operations should be observed and evaluated by an experienced geotechnical engineer or technician. 8.2 Pervious Pavement Materials We recommend the following material specifications for pervious pavement: Porous Bituminous Asphalt. The bituminous surface course shall be a bituminous mix of 6 percent by weight dry aggregate. Porous asphalt uses the same mixing and application equipment as for conventional asphalt. A neat asphalt binder modified with an elastomeric polymer is recommended. The polymer modified asphalt binder shall be heat and storage stable. Aggregate shall be minimum 90 percent crushed material and have a recommended gradation of: U.S. Standard Sieve Size Percent Passing 1/2 (12.5 millimeter [mm]) 100 % (9.5 mm) 92 to 98 4 (4.75 mm) 34 to 40 8 (2.36 mm) 14 to 20 16 (1.18 mm) 7 to 13 30 (0.60 mm) 0 to 4 200 (0.075 mm) 0 to 2 Stone Bed. Stone bed course aggregate shall be a crushed, %- to 1 -inch uniformly graded coarse aggregate conforming to AASHTO size number 67 (or equivalent). Stone bed aggregate shall be placed immediately after approval of subgrade preparation. Clean (washed) stone bed aggregate should be in maximum 8 -inch lifts. Each layer shall be compacted to a dense condition with a smooth drum roller. 8.3 Construction and Maintenance Considerations for Pervious Pavement Pervious pavement is susceptible to damage and clogging during construction and afterward. We recommend that the construction be undertaken in such a way as to prevent: 21-1-22082-004-R1f docx/wp/Ucn 21-1-22082-004 14 °°1ANNON 6WILS01% ING • Compaction of Subgrade: If the existing subgrade under the stone bed is to be used for infiltration, then the subgrade shall not be compacted or subject to excessive construction equipment traffic prior to stone bed placement. ■ Contamination of Stone Bed and Pervious Pavement with Sediment and Fines: Control of sediment is critical and rigorous installation and maintenance of erosion and sediment control measures is required to prevent sediment deposition on the pavement surface or within the stone bed. Staging, construction practices, and erosion and sediment control must all be taken into consideration when using pervious pavements. Due to the nature of construction sites, pervious pavement and other infiltration measures should be installed at the end of the construction period. All pervious pavement installations must have a backup method for water to enter the stone storage bed in the event that the pavement fails or is altered. In uncurbed lots, this backup drainage may consist of an unpaved 2 -foot -wide stone edge drain connected directly to the bed between the wheel stop. In curbed lots, inlets with 12 -inch sediment traps may be required at low spots. Backup drainage elements will ensure the functionality of the infiltration system if the pervious pavement is compromised. These systems should be designed by the project civil engineer. 8.4 Temporary and Permanent Excavation Slopes Safe temporary excavations are the responsibility of the Contractor and depend on the actual site conditions at the time of construction. Temporary cuts are the responsibility of the Contractor and should comply with applicable Occupational Safety and Health Administration (OSHA) and Washington Industrial Safety and Health Administration Standards. For trench safety purposes, the fill material at the site should be considered as OSHA "Class C" material, which requires side slopes no steeper than 1.5 Horizontal to 1 Vertical (1.5H: IV). Cut slopes during construction, particularly during wet weather, should be compacted to achieve a dense surface and covered with plastic sheeting to reduce erosion. All traffic and/or construction equipment loads should be set back from the edge of the cut slopes a minimum of 5 feet. Excavated material, stockpiles of construction materials, and equipment should not be placed closer to the edge of any excavation than the depth of the excavation, unless the excavation is shored and such materials are accounted for as a surcharge load on the shoring system. Permanent slopes excavated in dense native soils should be no steeper than 1.5H:1 V. We recommend that permanent slopes in on-site fill materials be no steeper than 2H: IV. 21-1-22082-004-x1f aocx/wp/Bm 21-1-22082-004 15 IIS°°1ANNON WILSON, INC. 8.5 Erosion Control Erosion control for the site will include the Best Management Practices incorporated in the civil design drawings and may incorporate the following recommendations: • Limit exposed cut slopes. • Route surface water through temporary drainage channels around and away from exposed slopes. • Use silt fences, straw, and temporary sedimentation ponds to collect and hold eroded material on the site. al Seed or plant vegetation on exposed areas where work is completed and no buildings are proposed. 0 Retain existing vegetation to the greatest possible extent. 8.6 Construction Drainage Even during dry weather, we recommend that site drainage measures be incorporated into the project construction. Perched water in the excavations (if present) and surface runoff can be controlled during construction by careful grading practices. Typically, these include the construction of shallow perimeter ditches or low earthen berms, and the use of temporary sumps to collect runoff and prevent water from damaging slopes and exposed subgrades. All collected water should be directed, under control, to a positive and permanent discharge system. The site will need to be graded at all times to facilitate drainage and minimize the ponding of water. 8.7 Subsurface Drainage We recommend installing a subdrain system along the outside of the perimeter footings to prevent pooling of stormwater against the building foundations. The subdrain system should consist of a perforated or slotted, 4 -inch (minimum) -diameter plastic pipe bedded in %-inch to No. 8 size washed pea gravel. Where a perforated or slotted drain pipe from a subdrain system connects into a tightline, we recommend that a low permeability concrete collar or dam be placed along the first 2 feet of the tightline to force all water into the tightline. Cleanouts should be provided at convenient locations along all drain lines, such as at the building corners. 8.8 Utilities In general, utilities at the site can be installed within the existing site soils, provided they are not underlain by extremely loose, soft, or organic materials. Maintaining safe utility excavations is 21-1-22082-004-R1f docx/wp/11m 21-1-22082-004 16 SFUNNON WLSON, IING the responsibility of the Contractor. Conventional excavation equipment can be used to excavate the soils. The utility trenches should be backfilled as noted in Section 8.1. We recommend utilities placed under the roadway have a minimum cover of 2 feet from the crown of the pipes or conduits to the top of the pavement subgrade. Catch basins, utility vaults, and other structures installed flush with the pavement should be designed and constructed to transfer wheel loads to the base of the structure. 8.9 Wet Weather Earthwork In the project area, wet weather generally begins about mid-October and continues through about May, although rainy periods may occur at any time of the year. Therefore, it would be advisable to schedule earthwork during the dry weather months of June through mid-October. Most of the soils at the site contain sufficient fines to produce an unstable mixture when wet. Such soils are highly susceptible to changes in water content, and may become muddy, unstable, and difficult to compact if their moisture content significantly exceeds the optimum. Performing earthwork during dry weather would reduce these problems and costs associated with rainwater, trafficability, and handling of wet soil. However, should wet weather/wet condition earthwork be unavoidable, the following recommendations are provided: Earthwork should be accomplished in small sections to minimize exposure to wet conditions. That is, each section should be small enough such that the removal of unsuitable soils and the placement and compaction of clean structural fill can be accomplished on the same day. If there is to be traffic over the exposed subgrade, the subgrade should be protected with a compacted layer (generally 8 inches or more) of clean crushed rock. Fill material should consist of clean, well -graded granular soil, of which not more than 5 percent by dry weight passes the No. 200 mesh sieve, based on wet sieving the fraction passing the 3/4 -inch mesh sieve. The fines should be non -plastic. The ground surface in the construction area should be sloped and sealed with a smooth -drum roller to promote the rapid runoff of precipitation, to prevent surface water from flowing into excavations, and to prevent ponding of water. 01 No soil should be left uncompacted and exposed to moisture. A smooth -drum vibratory roller, or equivalent, should be used to seal the ground surface. Soils which become too wet for compaction should be removed and replaced with clean granular soil. Excavation and placement of structural fill material should be observed on a full-time basis by a geotechnical engineer or his/her representative, experienced in wet -weather earthwork, to determine that all work is being accomplished in accordance with the project plans and specifications, and our recommendations. 21-1-22082-004-R1f docx/wp/Uw 21-1-22082-004 17 Illi°°LANNON WILSON, II . Covering of work areas, soil stockpiles, or slopes with plastic; sloping, ditching, and installing sumps; dewatering; and other measures should be employed, as necessary, to permit proper completion of the work. Bales of straw and/or geotextile silt fences should be aptly located to control soil movement and erosion. Grading and earthwork should not be accomplished during periods of heavy, continuous rainfall. 8.10 Plans Review and Construction Observation We recommend that Shannon & Wilson be retained to review those portions of the plans and specifications that pertain to the geotechnical aspects of the project to determine if they are consistent with our recommendations. We also recommend that we be retained to observe the geotechnical aspects of construction, particularly the pavement and shallow footing subgrade preparation, drainage installation, and earthwork (structural fill placement and compaction). This observation would allow us to witness the subsurface conditions as they are exposed during construction and to determine that the work is accomplished in accordance with our recommendations. 9.0 LIMITATIONS This report was prepared for the exclusive use of the Edmonds School District No. 15 for specific application to the design of the Madrona K-8 School project at this site as it relates to the geotechnical aspects discussed in this report. The data and report should be provided to prospective contractors and/or the Contractor for factual information only. Our judgments, conclusions, and interpretations presented in the report should not be construed as a warranty of subsurface conditions and should not be relied upon by prospective contractors. Construction period observation by our firm is necessary to confirm recommendations and interpretations made in this report. The analyses, conclusions, and recommendations presented in this report were prepared in accordance with generally accepted professional geotechnical engineering principles and practice in this area at this time. No other warranty, either express or implied, is made. The analyses, conclusions, and recommendations contained in this report are based on site conditions as they existed during our site visits and explorations, and further assume that the explorations are representative of the subsurface conditions throughout the site; i.e., the subsurface conditions everywhere are not significantly different from those disclosed by the explorations. If subsurface conditions different from those described in this report are observed 21-1-22082-004-R1£docx/wp/Um 21-1-22082-004 18 SHANNON WILSON, INC. or appear to be present during construction, we should be advised at once so that we can review these conditions and reconsider our recommendations, where necessary. If there is a substantial lapse of time between the submission of this report and the start of work at the site, or if conditions have changed because of natural causes or construction operations at or adjacent to the site, we recommend that this report be reviewed to determine the applicability of the conclusions and recommendations, considering the changed conditions and time lapse. Unanticipated soil conditions are commonly encountered and cannot be fully determined by merely taking soil samples or completing test pits. Such unexpected conditions frequently require that additional expenditures be made to attain a properly constructed project. Therefore, some contingency fund is recommended to accommodate such potential extra costs. Shannon & Wilson has prepared the enclosed Appendix D, "Important Information About Your Geotechnical/Environmental Proposal," to assist you and others in understanding the use and limitations of our proposals. SHANNON & WILSON, INC. Kevin Wood Geotechnical Staff KJW:MWP/kjw Martin W. Page, PE, LEG Vice President C'rantPrlhniral Pnrrinaar T PPT) AP TIRTATM 21-1-22082-004-R] Vwp/Ikn 21-1-22082-004 19 SHANNON 6WILSON, INC. 10.0 REFERENCES American Association of State Highway and Transportation Officials (AASHTO), 1993, AASHTO guide for design of pavement structures, Washington, D.C., AASHTO, 2 v. American Concrete Institute (ACI), 2013, Specification for pervious concrete pavement (ACI 522.1): Farmington Hills, Mich., American Concrete Institute, ACI 522.1-13, 7 p. ASTM International (ASTM), 2012, Standard test methods for laboratory compaction characteristics of soil using modified effort (56,000 ft-lbf/ft3 (2,700 kN-m/m3)), D1557 - 12e1: West Conshohocken, Pa., ASTM International, Annual book of standards, v. 04.08, soil and rock (I): D420 - D5876, 14 p., available: www.astm.org. Edmonds, Wash., 2016, Natural resources: Edmonds, Wash., Edmonds City Code and Development Code Title 23, available: http:L/www.codeoblisliin .coin/WA Fdmonds/. International Code Council, Inc., 2014, International building code 2015: Country Club Hills, Ill., International Code Council, Inc., 700 p. Kramer, S.L., 1996, Geotechnical earthquake engineering: Upper Saddle River, N.J., Prentice Hall, 653 p. Shannon & Wilson, Inc. (Shannon & Wilson), 2016, Hydrogeologic report, new Madrona K-8 project, Edmonds, Washington: Report prepared by Shannon & Wilson, Inc., Seattle, Wash., 21-1-22082-003, for Edmonds School District No. 15, Edmonds, Wash., November. Troost, K.G., and Booth, D.B., 2008, Geology of Seattle and the Seattle area, Washington, in Baum, R.L., Godt, J.W. and Highland, L.M., eds., Landslides and Engineering Geology of the Seattle, Washington, Area: Geologic Society of America Reviews in Engineering Geology XX, p. 1-35. Washington State Department of Transportation (WSDOT), 2015, WSDOT Pavement Policy: Olympia, Washington, WSDOT, 131 p., available: htt://www.wsdot,.wa. ov/NWrdonl res/L,F9AAC9E-6323-4BO9-A3D1- DD2E2C905D02/0/WSDOTPavemeiatPolic June2015. df Washington Department of Transportation (WSDOT), 2016, Standard specifications for road, bridge, and municipal construction: Olympia, Wash., WSDOT, Manual M 41-10, 1 v., January, available: litlp://www.wsdot,wa.gov/Publications/Manuals/M41-10.htm. 21-1-22082-004-R1£docx/wp/llm 21-1-22082-004 20 co -rename: J:�[l Iv UUU4V--Vd—V4 rig z - — r—awg �.aYOUI: i YWI U- I U ­U 1� Login: 7 /.J 1�u dvl� 12 I –. TP -13% LEGEND B-1 Boring Designation and Approximate Location PIV Test Pit Designation and Approximate Location (2016) TP -1 F PIT -3 and Approximate Location TP -1 % Previous Test Pit Designation and P-2 F Approximate Location (2015) 12 I –. TP -13% LEGEND B-1 Boring Designation and Approximate Location TP -1 F Test Pit Designation and Approximate Location (2016) Infiltration Test Pit Designation PIT -3 and Approximate Location TP -1 % Previous Test Pit Designation and Approximate Location (2015) 0 100 200 Scale in Feet NOTE Figure adapted from client file, Topo and Survey, dwg, received 10-3-16. T 0 N 0 0 H = 6 Ft. Max. 4 16" Min. Width 4 for Top Rock _VIII Ditch Drain to Appropriate Outlets 8" Compacted Native or Imported Soil (Impervious Surface Layer) Stable Excavation Slope in Very Dense Native Soil (Contractor's Responsibility) Opening Chinked with 2 to 4 -inch Quarry Spalls v \ Very Dense Undisturbed Native Soil Backfill All loose soil at rockery foundation subgrade should be overexcavated down to medium dense to very dense soil and replaced with compacted backfill as described above. The excavation shall be kept free of water. The prepared foundation subgrade shall be evaluated by a soils engineer prior to placement of rock. MINIMUM WEIGHT OF ROCK Rock shall be sound and have a minimum density of 160 pounds per cubic foot. Not to Scale 6" Diameter Slotted Pipe Bedded in washed 3/8" to No.8 sieve size pea gravel (6" cover around pipe), sloped to drain and connected by tightline to storm drain outfall or other appropriate outlets. No fabric around pipe. Maximum slot width is 1/8". Clean, well -graded sand and gravel or ° crushed rock, 2 -inch maximum size, 40 to 60% gravel, less than 5% fines (passing Medium 12�� Min. #200 sieve). Fines shall be non -plastic. dense to - Ve Dense rY AAs'. ' �" . yr Compact in 4" lifts with minimum of 4 Native Soil 6wa " Min. `^ coverages by hand -operated tamper. Compact to at least 92% of Modified H/3 Min. Width Proctor maximum dry density (ASTM �- —� for Base Rock D-1557). Backfill and rock placement should be built up together. All loose soil at rockery foundation subgrade should be overexcavated down to medium dense to very dense soil and replaced with compacted backfill as described above. The excavation shall be kept free of water. The prepared foundation subgrade shall be evaluated by a soils engineer prior to placement of rock. MINIMUM WEIGHT OF ROCK Rock shall be sound and have a minimum density of 160 pounds per cubic foot. Not to Scale 6" Diameter Slotted Pipe Bedded in washed 3/8" to No.8 sieve size pea gravel (6" cover around pipe), sloped to drain and connected by tightline to storm drain outfall or other appropriate outlets. No fabric around pipe. Maximum slot width is 1/8". (WdJ) o;e�tl MON polnseeIN QO 1l CO UP ,I: M N O O O O O O O O O C) CD N 00 (q 14: N O O O O O (190=0 Goold M 3sal;o w0110e anogy 1019H Ja;eM L 9. fR O N 00 N a a v a� rn Ur 7 N N H EL MdO) 9189 mogul painseaW ap ti c0 Un q: M N �- O O O O O O O O O O (190=0 JooI=1id 1sal;o Wo11O8 anogy 1019H Ja;eM t CL c6 O N N O (L N F d U) m CA LL 7 N H d N v W N __ .. _ as J 0 N _ �Y WH Q v N oo t o vas D a?m� 0 � E WLi W Z cfl 3 .c o �o 00= C9 3-0 �- o 7 tD - " W) c - Z W N O N q W J v a, > af0i aD ....._ � i O v O O. O N c a _ a> m 0 -^ G N O) C 0_ 00 a0 N Y O-� - a) v . O a) .+ +L cu r 4)> D 7 C C - O C.0 Nca L a) a3 N f - a N .••. p O C N a7 0 C N a) N C d L a) 3 WM ti O Orr N a7 W . ID co _ _ o cn +r 3 aG-Z,FL o 0) `mom 46 -----Cc aoo 0 (L) o p"L"'>N :03c O +�O (n O .I-- � O CL— N Nz a N a) O O N 2 C 00 . -. C r... Lp C CD N O N "I� a N o C C f fa Z N O 'ca .. O :3 � a c . 0 E-.. O, NL c0 0 ca - >% > ca E>3E.2mccOiL .,....µ ...... .... ...e,.... ..�, ..... ,..,. .. .�._,..,. _ ,. ... .. ,............. ..� ._.-- --- ........ �.,., OQ a0tX'=' 'zEo)���`ia -.. a0 0) C) N'x (D ccga(D a)Oti O` 3tor- 0cc _ ..... .,. .... p I -T •- COI) o _.. _L._ _ O o a o mcn 3 ac = m v >y3E~�� _. . ., ........ _ c o m a) .. c- O� ° m 3 O — a) L N CC C O � _ .. _......,. o .O N 4 N O �_.. a). - — E.� ac ca o .m. .�.. _ . _ C NOt-OOOO-y ` M .0.. C y L ..... .,,....._ _.. _,,.._ .. ...... _,�:., ' .. ....,.. ........,.. .,...� ..... fa CL 0 U CL 0 SD NQ N O N E c O — O H '- m 7-j-- wNO ° aoaoomN �:N , W L O a) O U °Q MH 3 w O 0 Z. r cD N .- a0 CO N O O O O O (190=0 JooI=1id 1sal;o Wo11O8 anogy 1019H Ja;eM t CL c6 O N N O (L N F d U) m CA LL 7 N H d (WdJ) 84e1:1 m011ul peinseeyy cq ll*� U M N O O O O O O O O 0 0 v cV r a0 c0 't N O O O O (199=0 Goold M Isal;o wo:408 anogV 1019H J91BM t a c2 0 N N m O a M H d co N 7 0I I1 N N H FL APPENDIX A SUBSURFACE EXPLORATIONS SHANNON N, INC. 21-1-22082-004 Shannon & Wilson, Inc. (S&W), uses a soil identification system modified from the Unified Soil Classification System (USCS). Elements of the USCS and other definitions are provided on this and the following pages. Soil descriptions are based on visual -manual procedures (ASTM D2488) and laboratory testing procedures (ASTM D2487), if performed. S&W INORGANIC SOIL CONSTITUENT DEFINITIONS 2 FINE-GRAINED SOILS COARSE-GRAINED SOILS CONSTITUENT (50% or more fines)' .... -n tless_than 50%fines)' Fine Lean Clay, Medium Major aj Elastic ic Silt Sand or Grave GRAVEL tiOla Fine Modifying (Secondary) 30% or more More than 12% Precedes major coarse-grained:. fine-grained: 3 constituent Sandy or Gravellya Silty or Clayey COHESIVE SOILS 15% to 30%-mmm - 5% to m N, SPT, RELATIVE coarse-grained: fine-grained: Minor with Sand or with Silt or Follows major with Grave14 , —�--- with Ola 3 ------- constituent 30% or more total Medium dense 4-8 Medium stiff coarse-grained and' 15% or more of a 8-15 Stiff lesser coarse- second coarse- 15-30 Very stiff grained constituent grained constituent: > 30 Hard is 15% or more: with Sand or with Sand or with Gravels with Gravel e "All percentages are by weight of total specimen passing a 3 -inch sieve 2The order of terms is: Modifying Major with Minor tetermn ned based on behavior, 4DetermMad based on which constituent comprises a larger percentage RWhichever Is the lesser constituent. MOISTURE CONTENT TERMS Dry Absence of moisture, dusty, dry to the touch Moist Damp but no visible water Wet Visible free water, from below water table STANDARD PENETRATION TEST (SPT) SPECIFICATIONS Hammer: 140 pounds with a 30 -inch free fall. Rope on 6- to 10-inch-diam. cathead 2-1/4 rope turns, > 100 rpm NOTE: If automatic hammers are used, blow counts shown on boring logs should be adjusted to account for efficiency of hammer. Sampler: 10 to 30 inches long Shoe I.D. = 1.375 inches Barrel I.D. = 1.5 inches Barrel O.D. = 2 inches N -Value: Sum blow counts for second and third 6 -inch increments. Refusal: 50 blows for 6 inches or less; 10 blows for 0 inches. NOTE. Penetration resistances (N -values) shown on boring logs are as recorded in the field and have not been corrected for hammer efficiency, overburden, or other factors. PARTICLE SIZE DEFINITIONS DESCRIPTION SIEVE NUMBER AND/OR APPROXIMATE SIZE FINES < #200 (0.075 mm = 0.003 in.) SAND... ..........-. ............._.......................m.................................................... �........... Fine #200 to #40 (0.075 to 0.4 mm; 0.003 to 0.02 in.) Medium #40 to #10 (0.4 to 2 mm; 0.02 to 0.08 in.) Coarse #10 to #4 (2 to 4.75 mm; 0.08 to 0.187 in.) GRAVEL Silica SandI� Fine #4 to 3/4 in. (4.75 to 19 mm; 0.187 to 0.75 in.) Coarse 3/4 to 3 in. (19 to 76 mm) COBBLES 3 to 12 in. (76 to 305 mm) BOULDERS > 12 in. (305 mm) RELATIVE DENSITY / CONSISTENCY COHESIONLESS SOILS COHESIVE SOILS N, SPT, RELATIVE N, SPT, RELATIVE BLOWS/FT. DENSITY BLOWS/FT. CONSISTENCY. < 2 Very soft <4 Very loose 4-10 Loose 2-4 Soft 10-30 Medium dense 4-8 Medium stiff 30-50 Dense 8-15 Stiff > 50 Very dense 15-30 Very stiff > 30 Hard PERCENTAGES TERMS 1.2 Trace BentoniteSurface Cement Grout M"µ"": Cement Seal .� �, Bentonite Grout M Asphalt or Cap 15 to 25% Bentonite Chips Slough Mostly Silica SandI� q ..., �.....,� Inclinometer or Non -perforated Casing Perforated or ............... Screened Casing°°°° 'l Vibrating Wire Piezometer PERCENTAGES TERMS 1.2 Trace < 5% .............................................Few.................................��................. �...�����................��....�5..to 10%.............................................. Little 15 to 25% Some.................... .............._...... 30 to 45%..................................... Mostly 50 to 100% 'Gravel, sand, and fines estimated by mass. Other constituents, such as organics, cobbles, and boulders, estimated by volume. 2Reprinted, with permission, from ASTM D2488 - 09a Standard Practice for Description and Identification of Soils (Visual -Manual Procedure), copyright ASTM International, 100 Barr Harbor Drive, West Conshohocken, PA 19428. A copy of the complete standard may be obtained from ASTM International, www.astm.org. 351 /0///qn//I�/�G,i//d/, /dIQ�// /,1 ////%/l///,//flI lfi/rA�U„'/dill Nh O/G,(„dl,�N f✓/-/li. Y��f ,,'//,/i l�/%O�f MAJOR DIVISIONS GRt7UP/GRAPHICSYMa0L TYPICAL IDENTIFICATIONS GW Well -Graded Gravel; Well -Graded b Gravel with Sand Gravel (less than5% fines) GP Pooriy Graded Gravel; Poorly Graded Gravels b «, Gravat wrtfa Sand (more than 50%., of coarse fon racdo 4 saineed SiltyGoraCllayey GM Silty Gravel; Silty Gravel with Sand vel COARSE- (mor nes) han 12/o GC Clayey Gravel; Clayey Gravel with GRAINED Sand' SOILS (mora than 50% retained on tlos SW Well -Graded Sand; Well -Graded Sand 200 sieve) Sand .. u with Gravel (less than 5% tines) SP Poorly Graded sand; Poorly Graded Sands Sand with Gravel (50% or mora of , coarse fraction passessat�ee No. 4 v) Silty r SM Silty Sand; Silty Sand with Gravel Clayand Mara (more f2%. tines) Sc �” Clayey Sand; Clayey Sand with Gravel ML Silt; Silt with Sand or Gravel; Sandy or Gravelly Silt Inorganic Silts and Clays (liquid limit less CIL Lean Clay; Lean Clay with Sand or Gravel; Sandy or Gravelly Lean Clay than 50) Organic Silt or Clay„ Organic Silt or FINE-GRAINED Organic OL Clay with Sand or Gravel; Sandy or SOILS Gravelly Organic Silt or Clay (50% or more paasses tho No.ECH Elastic Silt; Elastic Silt with Sand or 200 sieve) Gravel; Sandy or Gravelly Elastic Silt Inorganic Silts and Clays Fat Clay; Fat Clay with Sand or (liquid limit 50 or Gravel; Sandy or Gravelly Fat Clay more) OH �, Organic Silt or Cla ; Organic Silt or Clay Sand or gravel; Sandy or Organic with Gravelly Organic Silt or Clay HIGHLY- Primarily organic matter, dark in PT Peat or other highly organic soils (see ORGANIC SOILS color, and organic odor„ ASTM D4427) NOTE: No. 4 size = 4.75 mm = 0.187 in.; No. 200 size = 0.075 mm = 0.003 in. NOTES 1. Dual symbols (symbols separated by a hyphen, Le., SP -SM; Sand' with Silt) are used for soils with between 5% and 12% fines or when the liquid limit and plasticity index values plot to the CL -ML area of the plasticity, chart. Graphics shown on the logs for these soil types are a combination of the two graphic symbols (e.g., SP and SM). Borderline symbols (symbols separated by a slash, i.e., CUML, Lean Clay to Silt, SP-SWSM„ Sand with Silt to Silty Sand) indicate that the soil properties are close to the defining boundary between two groups. Poorly Graded Narrow range of grain sizes present or, within ATD At Time of Drilling singular: bed. the range of grain sizes present, one or more Alternating layers of varying material or Diam. Diameter sizes are missing (Gap Graded). Meets Fissured Elev. Elevation with little resistance.. criteria in ASTM 032487, if tested. Fracture planes appear polished or glossy; sometimes striated. Well-Graded Full range and even distribution of grain sizes ft. Feet breakdown. present. Meets criteria in ASTM D2487, if Inclusion of small pockets of different FeO Iron Oxide tested. Homogeneous gal. Gallons EN ' Horiz. Horizontal HSA Hollow Stem Auger Weak Crumbles or breaks with handling or slight I.D. Inside Diameter I pressure. Moderate Crumbles or breaks with considerable finger in. Inches pressure. lbs. Pounds Strong WIII not crumble or break with finger MgO Magnesium Oxide ssu , 01 ACTC mm Millimeter MnO Manganese Oxide APPROX. NA Not Applicable or Not Available DESCRIPTION PLASITICITY VISUAL-MANUAL CRITERIA INDEX NP Nonplastic .P .. ...._...... _ .. ..--...... .. lP N1 E.. O.D. Outside Diameter Nonplastic A 1/8 In. thread cannot be rolledOW Observation Well Low at any water content. A thread can barely be rolled and 4 to 10 pcf Pounds per Cubic Foot a lump cannot be formed when PID Photo-Ionization Detector drier than the plastic limit. PMT Pressuremeter Test Medium A thread Is easy to roll and not 10 to 20 ppm Parts per Million much time is required to reach the plastic limit. The thread psi Pounds per Square Inch cannot be terolled after reaching PVC Polyvinyl Chloride the plastic limit. A lump crumbles when drier than the rpm Rotations per Minute plastic limit. SPT Standard Penetration Test High It takes considerable time rolling > 20 USCS Unified Soil Classification System and kneading to reach the plastic limit. A thread can be rerolled qu Unconfined Compressive Strength several times after reaching the VWP Vibrating Wire Piezometer plastic limit. A lump can be Vert. Vertical formed without crumbling when drier than the lastio limit. WOH Weight of Hammer WOR Weight of Rods ONA S Wt. Weight Mottled Irregular g lar patches of different colors. Bioturbated Soildisturbance or mixing by plants or animals. Diamict Nonsorted sediment; sand and gravel in silt and/or clay matrix. Cuttings Material brought to surface by drilling. Slough Material that caved from sides of ptorehole. Sheared Disturbed texture, mix of strengths. Angular Sharp edges and unpolished planar surfaces, Subangular Similar to angular, but with rounded edges. Subrounded Nearly planar sides with well-rounded edges. Rounded Smoothly curved sides with no edges. Flat Width/thickness ratio > 3. Elongated Length/width ratio > 3. Interbedded Alternating layers of varying material or calor with layers at least 1/4 -inch thick; singular: bed. Laminated Alternating layers of varying material or color with layers less than 1/4 -Inch thick; singular: lamination. Fissured Breaks along definite planes or fractures with little resistance.. Slickensided Fracture planes appear polished or glossy; sometimes striated. Blocky Cohesive soil that can be broken down into small' angular lumps that resist further breakdown. Lensed Inclusion of small pockets of different soils, such as small lenses of sand scattered through a mass of clay, Homogeneous Same color and appearance throughout. 'Reprinted, with permission, from ASTM D2488 - 09a Standard Practice for Description and Identification of Sails (Visual -Manual Procedure), copyright ASTM international, 100 Barr Harbor Drive, West Conshohocken, PA 19428. A copy of the complete standard may be obtained from ASTM International, www.astm.org. ZAdapted, with permission, from ASTM D2488 - 09a Standard Practice for Description and Identification of Soils (Visual -Manual Procedure), copyright ASTM International, 100 Barr Harbor Drive, West Conshohocken, PA 19428. A www.asim.org. Geotechnical Report New Madrona K-8 Project Edmonds, Washington SOIL DESCRIPTION AND LOG KEY October 2016 21-1-22082-004 SHANNON & WILSON, INC. Geotechnical and Envlronrnental Consultants Total Depth: 16.5 ft. Northing: .............. ---- - Drilling Method: Hollow Stem ...... AugerHole Diam.: 6 in.­­-.....---- Top Elevation: - -.449 ft. Easting: .... . . Drilling Company: _Holocene Qd#ing­1­,­.....--- Rod Diam.: --------------- 2.-.inch '.. Vert. Datum: NA VD 88 Station: .............. .. Drill Rig Equipment: ...Diedrich.-D-50 Hammer Type: .... ....... . ...... ... Horiz. Datum: Offset: Other Comments: . ... .... .... . . ...... . . ....... . . . . . . . ........ - ... . .............. ......... SOIL DESCRIPTION � 75 U) -0 tt� PENETRATION RESISTANCE (blows/foot) Refer to the report text tier a proper understanding, of the Z -0 'a :5 A Hammer Wt. & Drop: 1bs130 inches subsurface materials and drilling methods. The stratificationE E 2 lines indicated below represent the approximate boundaries 0) 0 W U) (9 between material types, and the transition may be gradual. 0 20 40 60 isphalt 0.4 Dense, red-brown, Silty Sand with Gravel (SM); moist; fine, subrounded to subangular gravel; fine to coarse sand; nonplastic fines; 2 few organics. — Topsoil/Weathered Glacial Till 4 — - - ------ . ..... . . . . . ......... . . . . .... . Very dense, gray-brown, Silty Sand with 4.5 Gravel (SM); moist; fine, subrounded to angular gravel; fine to coarse sand; nonplastic 2 6 . . ...... . . fines; diamict. Glacial Till 3t. 8 . . ................ 7 710T, T. rn 10 . ... .... . . . . . ......... 41 it 0 z 12 5 5014'o 14 Moist to wet below about 15 feet. 6 16 "1 . ...... - - - ------- 16.5 BOTTOM OF BORING COMPLETED 7/26/2016 18 --- ---- 0 20 40 60 LEGEND 0 % Fines (<0.075mm) Sample Not Recovered 0 %Water Content 2.0" O.D. Split Spoon Sample Geotechnical Report New Madrona K-8 Project NOTES Edmonds, Washington 1. Refer to KEY for explanation of symbols, codes, abbreviations and definitions. 2. Groundwater level, if indicated above, is for the date specified and may vary. 3. USCS designation is based on visual-manual classification and selected lab testing. LOG OF BORING B-2 cw W September 2016 21-1-22082-004 SHANNON & WILSON, INC.2 FIG. A- GooWchnical and: EnvWonrnental Consultants REV 3 - Approved for S I ubmittal Total Depth: 15;9..ft. Northing: _____-----,----""-Drilling Method: Hollow Stem Auqer Hole Diam.: 6 in. - . Stem -- — - - - ---------- Top Elevation: -447.5ft. Easting: ..... Drilling Company: Holocene Drilling,, Rod Diam.: 2 -inch Vert. Datum: 1111,,NAVD88_.__ Station: ........ . .... ............ . . ..... ... . ---- Drill Rig Equipment: Diedrich D-50 Hammer Type:, ... .......... Horiz. Datum! ......... . Offset: Other Comments: SOIL DESCRIPTION PENETRATION RESISTANCE (blows/foot) � Refer to the raport text for a proper understanding of the E CL CU A A Hammer Wt.& Drop: I 101k��00iqqhes­ subsurface nwtorials and drilling methods. The stratification CL , E 2 cl lines indicated below represent the approximate boundaries a) U) Cc U) (9 between material types, and the transition may be gradual. 0 20 40 60 _,Asphalt0.4. ............ . . . ............. . . ............ - ---------- ------ Dense, gray -brown, Silty Sand with Gravel (SM); moist; fine to coarse, subrounded to subangular gravel; fine to coarse sand-, 2 nonplastic fines; diamict. y. Weathered Glacial Till 4 — ------- .......... . ... . .... .... . ........ . - - --------- Very dense, gray -brown, Silty Sand (SM) to 4.5 -T- - Silty Sand with Gravel (SM); moist; fine, X. subrounded to subangular gravel; fine to 3% 2 50/6"1 6 -7 coarse sand; nonplastic fines; diamict. Glacial Till Diamict pockets from 7.5 to 9 feet. 0 8- . . . ........ .. - ---- - — ----------- 3-1 01 A Z '0 ........... . . . . . — ---------- ... . .......... . 1 4 :X 1- 0' O z 12 ------ �50/6` 14 Moist to wet below about 15 feet. BOTTOM OF BORIN - G ------ --- - 15.9 16 -------- ...... __7 COMPLETED 7/26/2016 Q: 18 ............... LEGEND 0 20 40 60 Sample Not Recovered 0 % Fines (<0.075mm) 2.0" O.D. Split Spoon Sample 0 %Water Content J Geotechnical Report New Madrona K-8 Project NOTES Edmonds, Washington 1. Refer to KEY for explanation of symbols, codes, abbreviations and definitions. 2. Groundwater level, if indicated above, is for the date specified and may vary. 3. USCS designation is based on visual -manual classification and selected lab testing. ca LOG OF BORING B-3 lu September 2016 21-1-22082-004 SHANNON & WILSON, INC. FIG. A-3 I Geotochn[cal and Environmental Consultants REV 3 - Approved for Submittal REV 3 - Approved for Submittal Total Depth: 15 .8 ft. Northing: . ... ...... . . ... ...... Drilling Method: Hollow Stem A Hole Diam.: 6 in. ... ....... Top Elevation: �ft__ Easting: . . . ............... Drilling Company: --- - inch_____..__ Holocene„ Rod Diam.: 2 -inch Vert. Datum: NAVQ 88 Station: -­-------- . ...... ... ... Drill Rig Equipment: Diedrich D•56 Hammer Type: . ............. . ............ . ..... . Horiz. Datum: Offset: . . .... - ------ Other Comments: -------- . . ... .. ......... . ... . . ...... . ..... ...... ...... ....... SOIL DESCRIPTION o Cni v PENETRATION RESISTANCE (blowsifoot) Rotor to the report text for a proper understanding of the E CL :3 -6 A Hammer Wt.& Drop: _14,Q'1,bs�1'30_1nch.es.. subsurface matertals and drilling methods, Thes1ratificationCL > 1 E 2 EL (D lines indicated below represent the approximate boundaries a) 0 U) co between material types, and the transition maybe gradual. 20 40 60 ,asphalt. ........... . . . . . . . --- --------- - - ---- 0.4 Medium dense, brown, Silty Sand (SM) to Silty Sand with Gravel (SM); moist; fine to coarse, subrounded to angular gravel; fine to coarse 2 sand; nonplastic fines; trace to few organics; trace diamict pockets below about 7 feet. Fill 4 . . . . ...... 2 6 . . .... 'T. 8 . . ......... .. .. . . 3 . . . . ............ . ..... Sand Very dense, gray -brown, Silty Sand (SM) to 95 10- Siltro y Sand with Gravel (SM); moist; fine, subrounded to subangular gravel; fine to 4 coarse sand; nonplastic fines; diamict. Glacial Till 12 . .. ........ 5 78h :f 14- . . ........ . . . 2018"6 BOTTOM OF BORING 15.8 161 . ..... . ................ . . . . . ...... COMPLETED 7/26/2016 W 18 — . . . ........ . . . QD 0 20 40 60 LEGEND 0 % Fines (<0.075mm) Sample Not Recovered %Water Content 0 !9 2.0" O.D. Split spoon Sample Geotechnical Report New Madrona K-8 Project Edmonds, Washington NOTES 1. Refer to KEY for explanation of symbols, codes, abbreviations and definitions. 2. Groundwater level, if indicated above, is for the date specified and may vary. 3. USCS designation is based on visual -manual classification and selected lab testing. LOG OF BORING B-4 W September 2016 21-1-22082-004 SHANNON 4 WILSON, INC. FIG. A-4 I I Gede0n[call and Environmental Consultants REV 3 - Approved for Submittal Total Depth: 15.9 ft. Northing:__ Drilling Method: AqgK_,", Hole Diam.: 6 in. Hollow Stqm - -------- — -.111- -111 Top Elevation: 455 ft. Easting: . ................ Drilling Company: Holocene p ng Rod Diam.: 2 -inch . .... . _ ........... Vert. Datum: NAVD 88 Station: Drill Rig Equipment: '-D.i.edr.i.ch­Q-,50 111-111111111-- Hammer Type: ...... . .... . Horiz. Datum: Offset: . . .......... . Other Comments: ­­ .. . . .. ..... .. ............ . . . .. ...... . ...... SOIL DESCRIPTION -6 Cn 4= PENETRATION RESISTANCE (blowstfoot) Refer to the report text for a proper understanding of ttraa — E A Hammer Wt. & Drop:140 lbs 30.fijqq4_ subsurface matertals and drifting irpelhods. The stratiflaotion CL E lines indicated below represent the approximate boundaries 0 cn cc U) (.9 between material types, and the fronsillon may be gradual. 20 40 60 Medium dense to very dense, gray -brown, Silty Sand with Gravel (SM); moist; fine, subrounded to subangular gravel; fine to coarse sand; nonplastic fines; diamict. 2 —7— Weathered Glacial Till X �T 4- I T 2 6 8 . . . . ......... 3 ..........9.0 Very dense, gray -brown, Silty Sand with Gravel (SM); moist; fine, subrounded to 10 . . ........... . . . . . . . ....... angular gravel; fine to coarse sand; nonplastic fines; diamict. 4 1 68/11"0 Glacial Till Y z 12 711". ------ --- X..", 5 4110k 14 . .... ..... 6 — ---------- . .. ........ . BOTTOM OF BORING 15.9 16 COMPLETED 7/25/2016 8 18 . . .... - . . . ........... 0 20 40 60 LEGEND 0 %Fines (<0.075mm) Sample Not Recovered 0 %Water Content 2.0" O.D. Split Spoon Sample Geotechnical Report New Madrona K-8 Project Edmonds, Washington NOTES and definitions. 1. Refer to KEY for explanation of symbols, codes, abbreviations 2. Groundwater level, if indicated above, is for the date specified and may vary. maW 3. USCS designation is based on visual -manual classification and selected lab testing. LOG OF BORING B-6 0 September 2016 21-1-22082-004 0 SHANNON & WILSON, INC. FIG. A-6 Geotechnical and Environmental Consultants REV 3 - Approved for Submittal Total Depth: 15.9 ft Northing Drilling Method: Hollow Slam Auper Hole Diam 6 in. Top Elevation 4,54 ft. Easting Drilling Company: IlolocenPAriiliti Rod Diam 2 -inch Vert. Datum: /VA'V 1 88 Station: Drill Rig Equipment: _.._Diedrich D-50 Hammer Type _ .._._._._ Horiz. Datum _ „ Offset: Other Comments: SOIL DESCRIPTION ct� o y u PENETRATION RESISTANCE (blows/foot) Pieter to :the report text for a proper understanding of t/ro stobsurface materiels and driPMng methods. The stratification t n .0a E E � � r o n A Hammer Wt. &Drop: 140,Ibs / 30 inches ...... lines indicated below represent the approxirnale boundaries. (a (7 between rnotedal types, and the transition may be gradual. l] 0 20 ...., .. __..M ,,.° .. 0.2 40 60 Medium dense, brown, Silty Sand (SM); moist; few fine, subrounded to subangular gravel; :. - fine to coarse sand; nonplastic to low plasticity 2 fines; diamict; trace organics. — Topsoil/Weathered Glacial Till 7 4 Very dense, gray -brown, Silty Sand with Gravel (SM); moist; fine to coarse, subrounded 2=*t�;" to subangular gravel; fine to coarse sand; nonplastic fines. 6 Glacial Till L* Oi .... c °c m c 4�m H 10 50141' C w r a Z 12 14 - - Trace pockets of poorly graded sand with silt x . below abo.ut 15— f._e.__et. 15.9 +: 6 ° �tl - ------ _....... 116- BOTTOM OF BORING COMPLETED 712612016 m18 _ ..... _..m. 3 Y LEGEND 0 20 40 60 * Sample Not Recovered O % Fines (<0.075mm) �a I 2.0" O.D. Split Spoon Sample 0 % Water Content t� Geotechnical Report New Madrona K-8 Project NOTES Edmonds, Washington 1. Refer to KEY for explanation of symbols, codes, abbreviations and definitions. 2. Groundwater level, if indicated above, is for the date specified and may vary. 3. USCS designation is based on visual -manual classification and selected lab testing. LOG OF BORING B-7 au September 2016 21-1-22082-004 SHANNON & WILSON, INC. FIG. A-7 Gaoten:0rnlcal and Environmental Consultants REV 3 - Approved for Submittal Total Depth: 15.9.E ......,, Northing _ Drilling Method: Hollow Stem Auner Hole Diam.: _ ___ 6 to To Elevation: 456 ft Eastin —_ P 9� Drillin Company: 9 P Y H_ olocene,wDrflling Rod Diam. 2 inch Vert. Datum: NAVD 88 Station: 9 Equipment: Drill Ri E ui ment Diednch 5th....... Hammer Type Horiz. Datum: _ Offset: _ .... Other Comments: .. SOIL DESCRIPTION cr� 5 -0 PENETRATION RESISTANCE (blowsifoot) Rotor to the report taxi for a,proper understanding of Me I- Mn C a)� ♦Hammer Wt. &Drop: , 149„lbs Inches,,,,,, subsurface materials and drilling naelhod& The stratification a j, E 2 n fines Indicated below represent tho approximate boundaries f/) fn 0 fa) between material types, and the transition may be gradual. 0 20 40 60 I sp t lt, .. 0.2 Very dense, gray-brown, Silty Sand with Gravel (SM); moist; fine to coarse, subrounded to angular gravel; fine to coarse sand;'. 2 '­-__. . , - ........ nonplastic fines; diamict. Glacial Till 4 2 5015", 6— — 3 -]$ c 5014". D m c 0 O 10 4 N 5013” O m Z 12 — - - Gray below about 12 feet. .� 5012u; 14 6 Y _.... . ,----- .....----- �.. _. J .... -.BOTTOM OF BORING 15.8 �. 16 ...... 5014" COMPLETED 7/25/2016 18 3 Y 0 20 40 80 LEGEND 0 % Fines (<0.075mm) Sample Not Recovered • S m • %Water Content I 2.9'0.D. Split Spoon Sample a tv Geotechnical Report z I' New Madrona K-8 Project Edmonds, Washington NOTE 1. Refer to KEY for explanation of symbols, codes, abbreviations and definitions. 2. Groundwater level, if indicated above, is for the date specified and may vary. 3. USCS designation is based on visual-manual classification and selected lab testing. N LOG OF BORING B-8 September 2016 21-1-22082-004 SHANNON &WILSON, INC. FIG. A-8 C ttechNeal and Environmental Consultants REV 3 - Approved for Submittal Total Depth: 5 ft Northin 1456 DrillingMethod: Hollow Stern Auger Hole Diam.: fi In Top Elevation: ft.__.._ Easting Drilling Company: Holccerter Drllitng„ Rod Diam.: 2 inch Vert. Datum: NAVD 88 ,., Station: ... „. Drill Rig Equipment: Diedrich Hammer Type. Horiz. Datum Offset: ..... ... Other Comments: ........ SOIL DESCRIPTIONo a� v cH PENETRATION RESISTANCE (blows/foot) Rotor to the report text for a proper uroderstantding of the subsurfar.°o materiels and drilling rnetlrods. The stratificaldczn t a M E n E «( t a ♦Hammer Wt. & Drop: w 14 l 5 d 30 inches, tines Indicated belowrepresent the approximate boundariesN U) N o C. N between material types, and the transition may be gradual. 0 to 0 Topsoil. 20 40 60 __....... .. .. ....-- 0.5 .. Dense to very dense, brown and gray, Silty Sand with Gravel (SM); dry to moist; fine to coarse, subrounded to angular gravel; fine to 2 coarse sand; nonplastic fines; trace organics; diamict pockets. Fill/Weathered Glacial Till 4 2 7t). Very dense _. .......... "......---.... ry gray -brown, Silty Sand with 7.0 ' Gravel nded osubang�la gravel;) finne e to coarse sand 3 c 8 nonplastic fines; diamict. o Glacial Till:t Q10' .. t 40 m 62 - Fewoorl of ockets p poorly graded, fine to z 12...._. - ... medium sand with silt pockets below about 50/4" 12 feet; moist to wet from about 12 to 14 .... feet. 14 — Y.. Z — .......". OM OF BORING F' BOTTOM 15.5 w ! s= Al COMPLETED 7/25/2016 16 CO Z, 18 3 Y I LEGEND 0 20 40 60 Sample Not Recovered 0 % Fines (<0.075mm) I 2.0" O.D. Split Spoon Sample 0 % Water Content r� J Geotechnical Report New Madrona K-8 Project � NOTES Edmonds, Washington 1. Refer to KEY for explanation of symbols, codes, abbreviations and definitions. a 2. Groundwater level, if indicated above, is for the date specified and may vary. �w 3. USCS designation is based on visual -manual classification and selected lab testing. LOG OF BORING B-9 ua September 2016 21-1-22082-004 SHANNON & WILSON, INC. FIG. A-9 Csotech nIcal and Environmental Consultants REV 3 - Approved for Submittal Total Depth: 15.8 Northing: Drilling Method: Hollow Stem.Au.qer Hole Diam.: Top Elevation: 454.5 ft. Easting: ... . ......... . ......... . . Drilling Company: Holocene Rod Diam.: 2 -inch Vert. Datum: NAVD 88 Station: Drill Rig Equipment: _-_Diedrich„D 5il. . ......... Hammer Type:__ Horiz. Datum: Offset: . . . . . .......... Other Comments: . .. . . ........ . . . . ...... ........ .---- ................ ... ........ ........... . . - SOIL DESCRIPTION 0 a) PENETRATION RESISTANCE (blows/foot) Refer to the roi)ort text for a proper understanding of the E CL C: D• CU n A Hammer Wt. & Drop: 140 lbs I;IQ-frlq�99 subsurface materials and drilling methods. 7he stratification CL >1 E C) - 3: lines Indicated bolow represerif the approximate boundaries a) U) U) CcC7 0 between material types, and the transition may be gradual, 0 20 40 60 ............. "I'll”, Topsoil. ... . . ...... 0.5 Medium dense, brown, Silty Sand(SM); dry to moist; few fine, subrounded to subangular gravel; fine to medium sand; nonplastic fines; 2 . . ............... . . . ..... . ...... . diamict pockets; trace organics. T Fill 4 Roots at about 5 feet. 2 6 . . . ..... . ...... . . . ......... . . ..... . ...... Very dense, gray -brown, Silty Sand with 7.0 Gravel (SM); moist; fine to coarse, subrou nded : 8 to angular gravel; fine to coarse sand; 3 -a nonplastic fines; diamict. Glacial Till Mottled orange and gray -brown with pockets 10 7 . . . . ...... of iron oxide staining from 7 to 9 feet. 4 5011 12 V 5 50/3% 6 14— 5014" BOTTOM OF BORING 15.8 16 . . .......... -7- COMPLETED 7/25/2016 181 0 20 40 60 LEGEND 0 % Fines (<0.075rnm) Sample Not Recovered 0 %Water Content 2.0" O.D. Split Spoon Sample 2 cz Geotechnical Report New Madrona K-8 Project Edmonds, Washington NOTES 1. Refer to KEY for explanation of symbols, codes, abbreviations and definitions. 2. Groundwater level, if indicated above, is for the date specified and may vary. 3. USCS designation is based on visual -manual classification and selected lab testing. LOG OF BORING B-10 as September 2016 21-1-22082-004 SHANNON &WILSON, INC. I FIG. A-10 I Geatechnical and Environmental Consultants REV 3 - Approved for Submittal Total Depth:„m4 ft Northing: ___ Drilling Method: Hollow Stern Atl5�t Hole Diam.: 6 in. Elevation: 4 1 Eastin 9 Drilling Company: n : 9 P Y Holocene Drllldn Rod Diam : 2 -inch N� Vert. Vert. Datum: NA VD 1-11 D 88 . Station: Drill Ri E ui menta Drednch D at? Hammer T e – G P Honz. Datum .. Offset: Other Comments: SOIL DESCRIPTION o U) „ PENETRATION RESISTANCE (blows/foot) Refer to the report text for a proper understanding of the satasaadeco rnnterlats acrd driillr�g methods. The stratificattrn s n n E °� t o a Hammer Wt. Drop: 1401bs /30 inches ......... linesbetypes, �c present the approximate boundaries IndIl a) U) Cc� � (1)ige material and the transition may be gradual, 0 20 40 6n -�..—..........�. 0.5 Dense, gray -brown, Silty Sand with Gravel (SM); moist; fine, subrounded to subangular gravel; fine to coarse sand; nonplastic fines; 2 diamict. Weathered Glacial Till 1 AL,–. 4 Very dense, gray -brown, Silty Sand (SM) to Silty Sand with Gravel (SM), moist; fine, subrounded to subangular gravel; fine to z 8i11^"^ coarse sand; nonplastic fines; diamict. ., 6 .. Glacial Till 3 c 8621 1,. C J 10 4�m m 50WIA 0 12 -- .rc a•.5t)/�F 6 14 ° . 11, s 16 ” ........... .: $6f a". BOTTOM OF BORING 16.4 .. Cn COMPLETED 7/25/2016 ' 18 3 , Y, LEGEND 0 20 40 60 Sample Not Recovered O % Fines (<0.075mm) I 2.0" O.D. Split Spoon Sample 0 %Water Content U J Geotechnical Report New Madrona K-8 Project RNOTES Edmonds, Washington 1. Refer to KEY for explanation of symbols, codes, abbreviations and definitions. 2. Groundwater level, if indicated above, is for the date specified and may vary. W 3. USCS designation is based on visual -manual classification and selected lab testing. LOG OF BORING B-1 1 September 2016 21-1-22082-004 SHANNON 8 WILSON, INC. FIG. A-11 Dookoctun�cal and Environmental Consultants REV 3 - Approved for Submittal Total Depth: 16.3 R. Northing: ----------- Drilling Method: Hollow tern Aygeir Hole Diam.: 61x1.-_..... Top Elevation -456 ft . Easting: . ...... . . .. I — - Drilling Company: _Yq19q Rod Diam.: . ........... 21 -Inch . . ........... Vert. Datum: NAVO 88 Station: Drill Rig Equipment: _D.ie01chD-.50__.. Hammer Type: Horiz. Datum: Offset: I --- - ------ . ............ . Other Comments: .. . . .......... — --- - . . . .............. . ....... SOIL DESCRIPTION o o � PENETRATION RESISTANCE (blowsilfoot) Refer to the report text for a proper understanding of the r_ CL E :3 A Hammer Wt. & Drop: subsurface materials and drilling mallwds. The stratificallon CL >� E 0 lines indicated below represent the approximate boundaries (D ca U) Co U) between material types, and the transition may be gradual. 0 20 40 60 Topsoil. . . . . . . . . ........ . . . . . ....... 0.5 Medium dense, brown, Silty Sand with Gravel X. (SM); dry to moist; fine, subrounded to subangular gravel; fine to medium sand; 2 7— nonplastic fines; trace organics. Fill T ...... .... . 4 - - — ------- - . ........ ........ . . . . . ..... ..... . .... . ...... Very dense, gray -brown, Silty Sand with 4.5 Ts Gravel (SM); moist; fine, subrounded to subangular gravel; fine to coarse sand; t 2 6 . ........... nonplastic fines; diamict.. X. . . .... ....... Glacial Till Trace organics from about 4.5 to 8.5 feet. 8 . .. .... ..... -501601 10 . .......... . . ...... 4 501,5% 12 . ........ .. S 50t2% 14 6 16 -1-1: . . . . ........... . . . .. ------- -- - ----------- BOTTOM OF BORING 16.3 COMPLETED 7/25/2016 18 0 20 40 6C LEGEND 0 % Fines (<0.075mm) Sample Not Recovered 0 %Water Content 2.0" O.D. Split Spoon Sample Geotechnical Report New Madrona K-8 Project NOTES Edmonds, Washington 1. Refer to KEY for explanation of symbols, codes, abbreviations and definitions. 2. Groundwater level, if indicated above, is for the date specified and may vary. 3. USCS designation is based on visual -manual classification and selected lab testing. LOG OF BORING B-12 September 2016 21-1-22082-004 SHANNON &VVILSON, INC. I FIG. A-12 GootechnIcal 8rW Environ that. Consultants 3- r LL cLO oCL a 0CL w CL Q� c o m ami" .. �, . U � " f0 co . , , ,. . , . , O� �, ,. . r .. . . . , O NIDm CNl n CO CO "w., ✓✓ . . . , . . . , 00 d) V O R^ , , . �. . , .. Lii FLj F ., CLCo �. Y .�•✓ 1 cc,,) V, �� , , I N 'O Z Nca _ N O L) L) m m.� seldweg ch ch JaleM % _�..� o anus au._���.._ P q0 oN n... P}j! 0 a� c , C4 ooa�irn �U� m o m(6 Eos Ci m Z. O N G �� C0+% �N X a o y 3 E E U n� CV _O .� -0 7 f6 LL H N N 'a o�yJ'D�N OE o ac 1 = F- w O` off Z (D ° U C LJJ ❑ J N c c it, w n c`? O a H LL O _ y 4c--- mcc T, Ucn ��a�a ca �m O o -omoC,) a rw�e u�iC40= 0 y a y C • c . _ c ° co cc C E` Vi V> U N ao 3 0 d M o °� =,cam mm °' roti Z!,;Z -0Z' 7 lB ,� O d N Zo ~ O N� C Oa) E aC�- j C N O O C�� 3� O)C 'O OCV CD cc �. � o Z'�Mv H w aoao ZW W C i�z��$ y Z a N N r _ h O O df0 (0 �6 � a O y 7� �O�pp� Cha LL.O sr O O U= 0 7 C .Sg N (V N C c H �� coli > 300 v m m� �� nn 0 � Now 0 CO� a_a- N FIG. A-1 N Cc tai L oca c, x p x OL Q o LU N > . , co O 'Nt E LL< o 4D I „ w o �,.... (0CD �.. N N c N �, . , ti Llj f` ` O Z .r , Q, _ O arm. �� �Eocn, �. o CO` Y �� o. oo� ��. .. LL o Q o,_ D N ca p N m °oOo » Li C� - N q 0 N N O Z LUco i 0 U) . .. " . . . _.... __ �� ...._..,...�..�_ _.m..... C). ..�.. saldweg H H CD U jualuoo.._ ..............._........ Ja}eM % ., . � l em ............ .,,...� _ __.. ....... � .. �__w � �m�...---..m_ pun p panaasgp auoN y a y C • c . _ c ° co cc C E` Vi V> U N ao 3 0 d M o °� =,cam mm °' roti Z!,;Z -0Z' 7 lB ,� O d N Zo ~ O N� C Oa) E aC�- j C N O O C�� 3� O)C 'O OCV CD cc �. � o Z'�Mv H w aoao ZW W C i�z��$ y Z a N N r _ h O O df0 (0 �6 � a O y 7� �O�pp� Cha LL.O sr O O U= 0 7 C .Sg N (V N C c H �� coli > 300 v m m� �� nn 0 � Now 0 CO� a_a- N FIG. A-1 N a Q occ > c. ����:.'.'�, , . . E :...� ::.::: v cu 00 Z Cl) } LL cu CD co Cb N N. 0 W 2 <a C, ca f Q. 1 Oco f NCo. 00 N ca „ i ., . . . N 0 'v W fa T N.. Zco W 0^ V/ 3 r o of �..�imii .........mm�� 00 T T saldWeS Ch ;uaJuo0 ....... ._......._. Ja1eM % Ja}eM P 3 )ON punoa� N `m o> o 'n o 3E 3a�°io �rn y� 3 ° 'i {.7 V Z. LL�.:.� ZO - �� C C 2�c� �ONDo tq y �' >. U O N V 3 - va)a.0 C M N 7 d E a E Cl)Au co 0 ` a°i of c as y cooa H U N a) w� aLz 3 T _ j U C Z .. E j d �s W W E-0 LZ - — Baa a o CU CL -0 r�M LL O cn O a a) � o U l m E2 m �'ta m c— rn T O` cl m y mcn 0 o »� _ o—. CD colo — E i co a3 U m C H N 0 0 8� COO FIG. A-16 N, . . . . . . Q o E wLL . 00 1 o U I'd N , N . o Z CD O 0_ � .. f . . , N 00,. N (6 co . , , , N a w N N H t w ui '^ LL N„_. . D ........ _ �� co 00o C14 seldweg Cb JuajuoC) JejeM punoaE) auoN E LL Z ai Cl 0 �� _3 H aID u > 2 rna� > cn cc q �c U� a" >0 . h w� z m rn n ° �" J ,50. 8� � 3 OL to N 0 y .o 0 4 C R3 N LL O Q ^ ` Q> I I1 V H .,V S%S,. ILIA.. w`9' ", F- L � FIG. A-17 N C (0 a c 0 O LL CL 19t W v c c0 0 to > Q o W CC O U o0 Z c O OLL cu c J -0 c ccT O Lo E a co p CD W N N 0 C N (6 U (n 2 W Q cc N E r N CD W O O OND c O o N CO 0 Z N i r i N O U O Z 0 Yco .. O CL o "1=1 'qjd9Cj CN seldWeS 9 ..., .. .., ..... .......... juajuoo JajeM % r� .......-. . Ja}eM ..... punojE) panjasgp auoN t o w i CL Z rovo �42 E nO C7 2 _ a 'i a o� ° >, = z�W U w Q, C c Prov c: 0.2 1--p 3 CD c 6 . z J_ M +_.. 3 C7 O o � o'110 �3 mm 0 J 0 CL Jfq EE- >A (N FIG. A-19 1=1 q4 ad saldweS o o � N Cl) JaIeM % ori p paAjesgp auON pole jE) CC3 3 C7 -0 o cq E 4 a -01 -1 N3O 3-. F- c >. c o 5 F- 0 o C/) D ° cn 4) wN ( LV ~ o caai�o 3a o LL c'`�° 6C9 0 O J 0 m o" �' c a) m CL Z.-' c � O xo co ai=� a i° y '0a C7 LU co -� O OD_"a 0- � o m—_ 0 v �D_C�iLL ani cco= i�H c m � i FIG. A-20 O cao C0 U) co � ao .r v O ) LL H U ca � M U ca L O co) Cfl a o W two N _ C N 0N CO V `O U)ca 2 Q CL) 10 c a) E .. A? a o w C) 0 o i ca w N N r O N O C) Z Y m O O a .. - __, . .. .�_ ...... - �... O N.... .._ -- N co O CD N 1=1 q4 ad saldweS o o � cn Cl) JaIeM % ori p paAjesgp auON pole jE) o � � 3 M N � p y. w z d 3 C7 -0 o cq E 4 O -01 -1 N3O 3-. F- >. c o 5 F- o C/) D ° cn 4) wN ( LV ~ w caai�o 3a o coim� ca c'`�° 6C9 0 O J 0 m o" �' c a) m CL Z.-' c � O O co ai=� a � i y '0a C7 Cf) co -� O OD_"a 0- � o m—_ 0 J�� CCCC7H �D_C�iLL ani cco= i�H FIG. A-20 seldweg jualuoo Ja;eM % Jolem .�...�.�.�. puna CL H �E a o w` N 02 H Z, 0 O N� O J --.-.-.-. ........ o o ...... _....... T r peAjesgp auON m a) o a c m L N SCO o C olztc wE a� T �acu rn m C a m o c c w 7 0 ;- O� N O � co p U O N E _N 0_ �� Z O o m o o C N 0 a m 0.4- O a� (D ` (D c a� v 7 -o C) vOi i �aai 7. :3 O J�� NH �D,C7E >coH T LL CL LO O xxO T W C (d C O (D W ( c O Z C U `C N U) LL >>w > U o (04 p U c T co O v (p o E p N W c�0 N p N i (O U fA 2 LLJ Q m N O T a) LL o w 0 ONDc ° v� o N N >m > N T N O O U Z o U O of --3 a o seldweg jualuoo Ja;eM % Jolem .�...�.�.�. puna CL H �E a o w` N 02 H Z, 0 O N� O J --.-.-.-. ........ o o ...... _....... T r peAjesgp auON m a) o a c m L 3U a SCO o olztc wE a� �N �acu rn m C a m o c c w 7 0 ;- O� N O � co p U O N E �� Z O o m o o C N 0 a m 0.4- O a� (D ` (D c a� v 7 -o C) vOi i �aai 7. :3 m J�� NH �D,C7E >coH T FIG. A-21 N C (a a c 0 o u w LO c m m o LU � c o ao Z c co L) `C N OLL_. H m O c c. o A m Lo E v C) W m N C N 0 N c6 U p fA _ Q C o ++ a o w o � 04 o 2 (0 m N N w N, r N v o � Z m O O a o O C%4 ._ .. .__ .. ..... O N. 00 saldweg Chq ua uoo 0 J91BM % 4 �....... Ja;eM panuasgo auoN punao ip aoca cN .'+u N ca co E 0 CO E 0=. H o F �� c �o a) a'EH U _.. a c o� m76 WW c v co v 3C7 z w O c�— aim L 24z cc _ rn� = m o (n z c=_ Z'c_ 0 N Q 0 Oa 0 0 0 N •► = M N ca — L Jc/5 E 2 1— D i co l— FIG. A-22 N C cc � a c 0 12 o LL CL Iq o v c m o cn > CDCOn w c o o mCj) LL Q � O v�N*" ca o LO E v, co p o W N is �. N p C N (6 U fA 2 LL (D C, C c :a E. W o w a C) alloc ° o NCa 0 Z N r N O U O Z W N 0 d O `4�daa Ocq . _ .... .........,..... �.. .. O ... .. (V.. saldweS 9 .. ...... .......... ... ....... ,,,...... co ......... }ua;uoO N _.r. Ja}eM % L6 �. Jelem punojE) pa/uasgp auoN r W) u w IL 2 OA O U c > a 0 W ZgW U U) c C(a cm (,u O! H p 3 C7 c ZB LL O 3 (a — a> >y Ui O N O NMI O O CL J� Ei— 7 N FIG. A-23 C: N 30 cu c 0 0 22 �a z 0 0 a x a) co M!� "0 LL C) C) LO uj ca cc r- (D C,) c (a 0 a. 0 ip Q. 0 cLt" .0 --,d ca > 0 (D 0O w 00 w US cc U) LL 0 Q. E 0 cc Mn CO LO C) C\l E W C*4 cD --.r o 0 c 0 L4 0 W (D C) 9 I A LU co 04 CO 0 C-4 04 C 0 " -0 CC (D 04 04 w 0 Z 0 0 w -me (D I I CO CL- R,� -- . - 11-1 .. .... ........ . ....... .... . . ....... . ... O 04 'T CO co C) 04 1=1,ql aa FIG. A-24 30 cu C -0 0 22 �a z 0 -0 a) co M!� "0 (D p ca cc r- (D C,) a. cz C3) Q. 0 cLt" .0 --,d U) 0 C0 M) 04 E (D a) 0)- , L- -a C/) w (D o '0 o 0 r s - (D 0 6 Q. E An 0 cn - cc a0 ca z 0 0 io CL —oj C/) a cu �0- a) 2 .0 C/) EM (D 2 c >.0 F FIG. A-24 N cc a c 0 O w x `o w a c m O CD } cn > o m w o OD Z c a> Oy H cn LL cc Um c O vi J c cu O cA E o CO p C) W N _ N O C N (O U (n 2 LLJ Q u a) Nt p aci E �- a C> w tZ o cu Noc o n 0 a) NCCN r N O O U � Z oY co o a o _.........._ ....... o _,_,_..... N �... ...C.0 OD o — CN sajdweg 9 ...... __ ;ua;uo� ....... ...... -- Ja;eM % r-4� _..... Ja;eM .. ..---- panuasgp _------- -"",.... ............ auON ...-. ....... _.------- .. punoaE) .. ..... w ........................... ..-....... . ......... _�........ ami _oCD_ ° N a U' �' co = c: ca CO co v H Z ca ,�+ U ` O J E a d > co 2(D c 3 a) a -� — v N c rn O O e c cm 2 v c:c o MC,) +. w 0 z� W �� Z�� o o'° H o �, "� c Cc -: Cl) Q) � a; o 0) a) 70 m 75 — ZE LL O J O rna.o Hca _ vro:E EC�c�u(„ c� oc`o mcq U) Na vi w C7 1AA11� 0 o ccoA o n. J E 2� ai oa2— O Z'� �_ J c>M >y3EP FIG- A-25 N t0 a c 0 c`o o } w w LO v in > a� a� ? w Cl) O a) co Z c O w cuQ U O vi J c �N Ccu O Lo to Co O W N yp N p N C Co V p fA 2 W Q N D c aD E. � aD O w a N O O` Ncu w N r N O U O � U Z m O O a .-1-----o -- — - N ..............m.m m ................... r r co 00 O N saldweS 9 aM o ... ......._ N _............ -- - .................. �ue/u.... Li J819M pan.iasgp auoN punaE) t3 0 CL 014, HZ a i. .0 Uc. 0 I� w U"a U. zi J —0 o 5 o 4-7 0 7C) O O 3 �0- Com' a �= J (7) FIG. A-26 N fC a c O li in �x v v c m in ca aa) W c Cl)O U op Z c a� O CO � c O w c O An co Ln E p o W N N O C N V fA 2 W Q N p c N � c- N O W �. d N cc C co N M O Z N N O U O L U Z O a o oN Co....................................... ...... r � saldweg 1 0 jualuoo LO JejeM % ui Ja�eM ............................................. ............... -------------- ----------------------- - - peAjesgp auoN punas CD � c LZ O� o An CO ~O Z = ° � E CL a ma m � c 08N W c m E OMS w oroo �C7 U) N O�^+N' Q �' " p 0 o� C — >c," LFIGLA-27 N C (C � a c 0 T CL LL co, � w v o a� co o w a) 00 Z O Cl) LL cu U CQ N O vi c" cca o cn E w C0 o o w N O C CO U O cn _ W QN 0 c N N O W d 04 c O C O N O Z N r N 1 U O Z C) Y O a ...__ o •�� `4�dad �...... - o N __ _......... _..._. o o ........... r 04 soldweg o u ;uoo ------- C9 ...— ------------ o poAjesgp OuoN una� unojE a� a c c ca Z is O a Z 3 ca o� .0 (; E . -� O N o c JE F_ a �c� -0 Cc— �Cc— U C;) v) 4--; c1°n E2 � W z� W w .•• -Q o � c o E o 3a o ° a� a � ��v) o �, �•o m0 o F- Z LL o o T. — (D ma E N=_ 3 cA m �= v Q Ca CL r- 0H UH Q JAI) CC 2�C7LL icn J ,.. ., FIG. A-28 N C N T a c 0 o ti X N LOW v c m o cc a� o fA cW o co LD w U LL ca Q � c U O � c cc o co E a co p NW N O C N CO V C/) 2 W Q O � � T CD LLI O cc c °No o 2 NCc W N T N U Z w 3N 0 ) a- o . .o ... _ N _ ..... .. o - to 00 N T T saidweg ............... 9 JuaJuoo ... ... -- ..... 0 ial1M % 6 . ,a jem — ... punojo panuasgo auoN z; r Z '. 01 H E a 2 a of ad U � c Oz= W w o Lo0 Z 8 LL alM20 o 0 y� U)CJ C!� {rg o "IG, A-29 N C (d � Ll c 0 o LLm CD v c Nca O fA c o W v OD Z c O N LL cc O vi J O C d,N C cc µ. O LO _N Cfl O W N N p N C (O U p fA 2 W Q (D � c N � U) .r O O W d ODc O 2 NCU> >N N N F O U O � Z Y O a O ............�.�- ... ........ �_. •1=1 `uldea 0... ..—_.. - .� -_ r saldweS o U) ;ua}uoa . .... ............... ........_, xajeM % cd -- ......... �a�eM panjasgp auoN punoj!D � a 2 3� �� o E Z IL Z's 0- z O ° � �3� � �� 0 X30 c 3 H F- � o� �Co CD Z's Lu "W ~ cA W cmEo 3v0 cap rn� cm DC7 z LL J o DC7 Z'�C [2 EO`" c N 0 N o N= Q O MMMMIN` C) p O H C O (0 H O O�= (2 C7 lL O J FIG. A-30 N (u a c 0 m o w Cl x 't LOLU a c N ai (n > =o 00 v Z ccfl O ) U) LL U1 3:O c -0 c ;g o un E T co p C) w N cc - N O C N CO V `0 fA 2 W o = a) CD w a C) 00 o N CU 0 Z N r N V o Z ao �� `4�daa ........ C) _ __.. N ........... co 0 N saldweg 9 cn }ua}. ..... — ------------ _ . It Ja}eM % L6 ........ ........ �a�eM ............ .....m... ..... . ... .__�........ ........._...... ..........................� ........... punoj0 p an.as QO uoN ch 'oo �v —. o 2 0 0 O �2 3-: Z -i E a a O (� � -0 U CL CTO cc m'm ZW OO w 3C�c do Z ~ .. d�0 of X3`00 cam_ p �3 �Ml� rama 0 o�o 0 i° E � aim= 05 � CV c0 a c 0 m o LL CL 00w c ca:Ll o :r ca CD CD CD cn o W o ao Z `C O w H cc Q c M O cca o co E cn co o a O W N coo N p N C CO V `p (n 2 Qcc a)c (, o w a occ N c o 2 t N 0 O Z N r r N O V p U Z m O (q O a o O _ ..�.....N_ --..... . -- ..... - _� .. ...... �p O N r seldweg o Jua}uo0 CR JeleM co �....,.. ......_. .- --- ....— ......r�.. Ja}eM panjasgp auoN punas — ....-........... ...._ MA..... m o ' �+ao� m CO iq c2 0- p o ff° CL � 3� a 3 2 r n. c 2 co a� -D c � La ` o o� U m E W w z- LL Q cm m — E a) $ tl7 cn O= N 0- N p�= N c�0 FIG. A-32 L N IC a c 0 o w CL 19t `n w v c ca o cn > o m CO c O W U co Z C N p fn LL W �: C U JO N C r9 N f0 O EQ N (O _LO C) W N N N p C N CC U LO cq 2 W Q c N qt O r N C:) w a o cuONDc o N O 0 Z N r i N V O U Z Y O 0 a o �� y... }daa O N .. .�. � ...._._.. � ......... ..... � O � . ,..., N r r saldweS 9 ....... .......... „ ua uo0 L .. _..... JoleM .....--- ,... JajeM _. .................. .. ............. _ .... ..... ....... .. .. ...... punojE) panjasgp auoN IL avow a Z, 0 .o .- 0- ZO ��o° �E O c � E a �> a o Ql) cc � c.� �a�Q > �o Z O" H � 223 Cc 3C!c ZZ,B U. J �`_M t0 — Com. N O w 0 X3+-;0 o c .0 a o .'■, O Jct EH _ >coh LFIGL-A-33 N C N � a c 0 cm `o LLCL 00C v c N ° UA > N N a c o W ao cOi O m U) LL Q :�: O vi O Lo to CO o W N N _ N p C N Cfl V `O U) 2 LLI ca N C, N O C:) W o d � c O o N N ° Z N o U U Z o a o CD -co o.... soldweg �_....., jua}uoo ------ --CV ...... w. JaleM % ui ---- —.. _..... ............... panuasgp auoN Puri as m c Z' 3v m _tea — >3 c (D c ca -� :3 CL o c � 'D6C a �� �Cl) rn co :-: °a w N Z2 W uvi W ° c 6 E °° Co c 3 rn � v� aS Ur`'0 ~ Z LL o o 2 12 (D CO) cOn co ° CO)=co O E= (' O °o °oa c �aC cc 0 mZ gv� °� ani m o= >� °H FIG. A-34 APPENDIX B LABORATORY TEST RESULTS SHANNON 6WILSSON, INC. 21-1-22082-004 S WHOM EIII SHANNON 6WIL SON, INC. Preliminary Hydrogeologic Report New Madrona K-8 Project GRAIN SIZE DISTRIBUTION PLOT BORING B-3 'a N N O O N m O N N N SHANNON & WILSON, INC. • 400 NORTH 34TH STREET - SUITE 100 - SEATTLE, WASHINGTON - 98103 - MAIN (206) 632-8020 • FAX (206) 695-6777 Gravel Sand Fines Coarse Fine Coarse Medium Fine m Silt .. _.... _ Clay S¢e _........ .-. Mesh Opening in Inches .............. ._ �. Mesh Openings per Inch, U.S. Standard Grain Size in Millimeters a ^ O O 00 o Oa 00 O ro Ory O^ 00 00 0• o• o• M ry O� 00 00 00 o• o 0 00 o ^o do �o �o �o 0 0 0 0 100 tlr 90 65 N,20 76... .. �.. .26 70 l ,,, , , .. ,,, , + e 0,. , . 30 35 W 60 CD CD 5 f 45 n N 'sG1 C ... - iI - O 50 0) LL 45 55 40. 4,,,. 64 d .. �._..65 W 5 _.. ..... ._. ^ ,. ,. 30, 70 25 75 '. zo �_ .• �.�. �e... . N �� 6 a 15 .. . � I� .... _ ... �ti,. ... .. ". 86 1 0 .: 90 5 _. i 9 -- 95 0 R 100 +" 0'0 O b Grain Size (MM) Sample Depth USCSp USCS Gravel Sand Fines <20pm,<2pm WC Tested Review ASTM Identification (ft) Symbol Group Name % % % % % % By By Std. �! B-3, S-3' 7.5 SM Silty Sand 11 55 34 8.7 AKV JFL C136 Test specimen did not meet minimum mass recommendations. 'a N N O O N m O N N N SHANNON & WILSON, INC. • 400 NORTH 34TH STREET - SUITE 100 - SEATTLE, WASHINGTON - 98103 - MAIN (206) 632-8020 • FAX (206) 695-6777 U 0 c� J_ �1 IL IL q N W O N N N N N NS NON �IION, INC 7N Preliminary Hydrogeologic Report New Madrona K-8 Project GRAIN SIZE DISTRIBUTION PLOT BORING B-4 Test specimen did not meet minimum mass recommendations SHANNON & WILSON, INC. • 400 NORTH 34TH STREET • SUITE 100 • SEATTLE, WASHINGTON • 98103 - MAIN (206) 632-8020 • FAX (206) 6955.6777 V rn N m O N N N O 00 N M ORION mill SHANNION WILSON, INC. FN eliminary Hydrogeologic Report ew Madrona K-8 Project GRAIN SIZE DISTRIBUTION PLOT BORING B-5 Gravel Sand Fines _w . ..�. m ......._ .. -- la -S-e Coarse .... Fine Coarse Medium Fine Silt C_... Mesh Opening in Inches Mesh Openings per Inch, U.S. Standard Grain Size in Millimeters Sample Depth I USCp USCS Gravel Sand Fines <20pm <2pm WC Tested Review ASTM Identification (ft) Symbol Group Name % % % % % % By By Std. * B-5, S-3' 7.5 SM Silty Sand 14 54 32 22 8 15.0 AKV JFL D422 * B-5, S-6' 15.0 SM Silty Sand with Gravel 15 52 33 10.0 AKV JFL C136 ' Test specimen did not meet minimum mass recommendations. N SHANNON & WILSON, INC. • 400 NORTH 34TH STREET • SUITE 100 - SEATTLE, WASHINGTON - 98103 • MAIN (206) 632-8020 • FAX (206) 695-6777 I a C7 N m O N N N N VIM ow SHANNON WILSON, INC. Preliminary Hydrogeologic Report New Madrona K-8 Project Edmonds, Washington GRAIN SIZE DISTRIBUTION PLOT BORING B-11 Gravel Sand CFines �.__._�,w................. Coarse Fine Coarse 1 Medium Fine Silt Cla S¢e Mesh Openinq in per Millimeters Inches Mesh Openings Inch, U.S. Standard Grain Size in p Millimeters Sample Depth USCS USCS Gravel Sand Fines <20pm <2Nm WC Tested Review ASGroTM Identification (ft) Symbol Group Name o� o� o� o� % % By By Std. OB -11, S-11' 5.0 SM I Silty Sand 13 53 34 8.1 AKV JFL C136 1 Test specimen did not meet minimum mass recommendations. SHANNON & WILSON, INC. • 400 NORTH 34TH STREET • SUITE 100 • SEATTLE, WASHINGTON • 98103 • MAIN (206) 632-8020 • FAX (206) 695-6777 1 New5.5111 SHANNON WILSON, Preliminary Hydrogeologic Report New Madrona K-8 Project Edmonds, Washington I rn N m O N N N a K GRAIN SIZE DISTRIBUTION PLOT TEST PIT PITT -1 Gravel Sand Fines Coarse .. ....._. _.. ._-.....� 6...- . .......... Fine Coarse Medium_ Fine _ Silt Clay-S¢e Mesh Opening in Inches .._... Mesh Openings per Inch, U.S. Standard Grain Size in Millimetersmmmm • � g p It, o 0 a op e a ,a a oo& ooa o0o tory db .� o o _0 0 0 _. ,6 10 15 20 25 55 35 CD 40 N K 45o O 50 55 Q 0o N 65 M 70 75 80 85 so 95 100 Grain Size (mm) Sample Depth Group USCS Cobbles Gravel Sand Fines < 20pm < 2pm WC Tested Review ASTM Identification (ft) Symbol Group Name %2 % % % % % % By By Std. PIT -1, S-1 3.0 SM Silty Sand with Gravel 15 56 29 5.7 AKV JFL C136 PIT -1, S-6' 7.0 SM Silty Sand with Gravel and Cobbles 13 28 51 21 13.9 AKV JFL C136 ' Test specimen did not meet minimum mass recommendations. 1 Cobble percentages are calculated using the pre -removal, oven -dried mass of the total specimen. USCS Group Symbol, Soil Classirication Group Name, Gravel %, Sand %, Fines %; <0.02mm %, <2um%, Cu, and Cc values are calculated from particles smaller than 76.2mm (3 inches) only, per ASTM D2487. SHANNON & WILSON, INC. - 400 NORTH 34TH STREET - SUITE 100 • SEATTLE, WASHINGTON • 98103 • MAIN (206) 632-8020 • FAX (206) 695-6777 IIIA SHANNON WILSON, INC. Preliminary Hydrogeologic Report New Madrona K-8 Project GRAIN SIZE DISTRIBUTION PLOT TEST PIT TP -1 F I Gravel Sand Fines Coarse Fine Coarse Medium Fine �. Silt ClaSize .wm Mesh Opening in Inches Mesh Openings per Inch, U.S. Standard Grain Size in Millimeters p 0\ �y ^4110P ^O 0 00 OP o0 Ory O 000 000 ooa o00 411 00 100 ry0 �O 00 ^O O' O' o' O' O' O' O' o' o' W o' 0 V r _. 95 _ 5 90 10 '95 die „„ VVV r ,,. �.,,� � ppi C B., {{ .15 20 76 � ( 26- 703e V ti "r ,... - - ... .. �.... ._. .. 35 CO) N Ei0 .. CD CD 45 n 50 � (L ._ c45 - 55v U d 4e 50 N 35 65 co 30 9 _ ._. r ..Ye 25 ...�� .. Rkk �, t .... I r ",." •75 20 .. ..... ( ,... .� .. 60 1090 J 95 100 0 Grain Size (mm) Sample Depth USCSGro USCS Gravel Sandn3l 20pm < 2Nm WC Tested Review ASTM Identification (ft) Symbol Group Name % %% % % By By Std. m 0 TP -1 F, S-1' 7.0 SM Silty Sand 13 55 7.5 AKV JFL C136 rn ' Test specimen did not meet minimum mass recommendations. N N SHANNON & WILSON, INC. - 400 NORTH 34TH STREET - SUITE 100 - SEATTLE, WASHINGTON - 98103 - MAIN (206) 632-8020 • FAX (206) 695-6777 T .L a. a 0 N m O N N N M O O N W O N N N `111 IF Iran MONO SHANNON WILSON, INC. Preliminary Hydrogeologic Report New Madrona K-8 Project Edmonds, Washington GRAIN SIZE DISTRIBUTION PLOT TEST PIT TP -2F Gravel _ Sand Fines Coarse Fine I Coarse mm Mediummmmmm.. I Fine m Silt mmm mm Clay -Size . �m--M e Mesh Opening in Inches I Mesh Openings per Inch, U.S. StandardGrain Size in Millimeters �a \Y 0 M p �. 0 0 0� 4 orO op oh o`� W p• O' O' oorO ooa oo`� oon 1^ OW O' W O' W o0 O'0 100 Gravel Sand Fines < 20Nm o/ < 2pm WC Tested Review ASTM Identification (ft) Symbol Group Name % % % % % 4 By r TP -2F, S-1 6.0 SM Silty Sand with Gravel 29 5 L13 7.3 AKV JFL C136 10 15 20 7'S _. li - `� i _ S I. 2� Cr 35 M . .. I .... .. °,,. .. . �.. .. .. CD CD �411 ry I� . { f � 45 o n 'O _ _ s ,. ... , . ,,,, O rr0 0) LL i�. c 45pNNV ,pQ 56 a- 4) 40450 (( ppj 0) N 65 ,5. „ �. — 30 .. _ ......... ., _.. V „.. a ........ I _.� N 70 . 75 ..i 1, 80 15 r f V 85 i C .. 10 _ - �. 4 90I o �y p lrN' 'l5' 1p JS' ,00 ��� t7" 6, Grain Size (mm) Test specimen did not meet minimum mass recommendations. SHANNON & WILSON, INC. • 400 NORTH 34TH STREET - SUITE 100 • SEATTLE, WASHINGTON • 98103 • MAIN (206) 632-8020 • FAX (206) 695-6777 Sample Depth USCSS USCS Gravel Sand Fines < 20Nm o/ < 2pm WC Tested Review ASTM Identification (ft) Symbol Group Name % % % % % By By Std. TP -2F, S-1 6.0 SM Silty Sand with Gravel 29 58 L13 7.3 AKV JFL C136 Test specimen did not meet minimum mass recommendations. SHANNON & WILSON, INC. • 400 NORTH 34TH STREET - SUITE 100 • SEATTLE, WASHINGTON • 98103 • MAIN (206) 632-8020 • FAX (206) 695-6777 SHANMON&WIl,,,,SON, INC. APPENDIX C ANALYTICAL LABORATORY TEST RESULTS 21-1-22082-004 VIA t»sluau��v�arr��a SPECTRA Laboratories - -.) ,..Where experience matters 26276 Twelve Trees Lane, Suite C e Poulsbo, WA 98370 a (360) 779-5141 a Fax(360)779-5150 a www.spectra-lab.com August 15, 2016 Shannon & Wilson, Inc. 400 N. 34h Street, Suite 100 Seattle, WA 98125 Project: Madrona K-8 Sample Date: 7/29/16 pH 1:2 soil to vwl Phosphorus &ay ppm Potassium NH4QAc ppm Calcium NH4QAc mW100 g Magnesium NH4QAc meq/100 g Sodium NH4QAc meq/100 g SMP Buffer Index` Organic Matter LOI % by Wt Nitrate -Nitrogen KCI ppm Sol Salts 1:2 961:weter dS/m &O ,qu," PAP -Accredited 2014 Lab Work Order #: 161057 Sample Received: 8/1/16 Sample ID: SF -1 Lab No.: 161057-01 . e YI4 ilii ' Illa�j� r r Q Low Medium High NA- Not analyzed All analyses performed on air-dried soil passed through a 2 mm sieve. Soil Fertility Levels The soil sample submitted from your site was found to have the following general nutrient levels: pH Phosphorus (P) Potassium (K) Calcium Magnesium Nitrate -Nitrogen EC (Sol Salts) Neutral High Low Low Medium Low Salinity Negligible 6.6-7.3 40-100 ppm <150 ppm <5 meq/1008 0.5-2.5 meq/100g <10 ppm <0.4 dS/m 1 SPEcr rRA Laboratories'- Kits4p re experience matters .... ,.�,.m.-.. _........ n� a...98370 ,®, .,360 779-51.41..... Fax ... p 26276 Twelve Trees Lane Suite C Poulsbo, WA F �- (6) (360) 779-5150 • ........e www.spectra-lab.com Project: Madrona K-8 Sample Date: 7/29/16 pH 1:2 soil to vial Phosphorus Bray ppm Potassium NH40A,c ppm Calcium NH40Ac meq/100 g Magnesium NH40Ac nxgl00 g Sodium NH40Ac meq/100 g SMP Buffer Index* Organic Matter L01 % by wt Nitrate -Nitrogen KCI ppm sib+ sails 1:2 soiimmer d5Wm Lab Work Order #: 161057 Sample Received: 8/1/16 Sample ID: SF -2 Lab No.: 161057-02 NA- Not analyzed All analyses performed on air-dried soil passed through a 2 mm sieve. Soil Fertility Levels The soil sample submitted from your site was found to have the following general nutrient levels: PH Moderately Acid 5.2-6.0 Phosphorus (P) Medium 20-40 ppm Potassium (K) Low <150 ppm Calcium Low <5 meq/100g Magnesium Low <0.5 meq/100g Nitrate -Nitrogen Low <10 ppm EC (Sol Salts) Salinity Negligible <0.4 dS/m 2 . A A oda SPECTRA Laboratories - , f ...Where experience matters 26276 Twelve Trees Lane, Suite C - Poulsbo, WA 98370 - (360) 779-5141 - Fax(360)779-5150 - www.spectra-lab.com Project: Madrona K-8 Lab Work Order #: 161057 Sample Date: 7/29/16 Sample Received: 8/1/16 Recommendation: SF 1: The pH of this area is best suited for turf, vegetable gardens and bedding plants (>6.0). The use of sulfate -containing fertilizers will tend to make the soil more acid with continuous use, and will make the soil pH better suited to our native plants, or the pH can be adjusted downward by broadcasting 2 lbs of finely ground elemental sulfur or 6 lbs of iron sulfate per 1000 sq ft, soil for every 1/2 to 1 pH unit decrease desired. Repeat this application every 3 months until the desired amount of sulfur has been added. (Iron sulfate works faster.) A pH requirement sheet has been included to help you decide if the pH needs to be adjusted to meet your needs. The calcium and magnesium levels are low, but in an acceptable ratio to one another. Increase both by incorporating 50 lbs of gypsum and 20 lbs of Epsom salts per 1000 sq ft of soil. The macronutrient levels of nitrogen, phosphorus and potassium are all low. Incorporate a complete fertilizer such as 10 lbs of 10-20-20 plus 12 lbs of 0-0-60 per 1000 sq ft. The goal should be approximately 1 lbs of actual nitrogen, 2 lbs of P205 and 9 lbs of K20 per 1000 sq ft. SF 2: The pH of this soil is closer to that needed for native plants, but still acceptable for turf. The pH can be lowered further as stated above for natives. The buffer pH indicates that liming is not needed, but the calcium and magnesium levels are low. Increase as stated above. The macronutrient levels are low. Incorporate a complete fertilizer such as 10 lbs of 10-20-20 plus 71bs of 0-0-60 per 1000 sq ft. The goal should be approximately 1 lbs of actual nitrogen, 21bs of P205 and 61bs of K20 per 1000 sq ft. Both areas: The soluble salts and sodium content are low indicating that excess salts have not built up to a level that will harm plants. The organic matter is low in SF -1 and borderline in SF -2. Adding 2-4 inches of compost or other top -dressing will be of benefit. More nitrogen may need to be added periodically during the growing season (April, July and late October -November) at the rate of one lb actual nitrogen per 1000 sq ft of soil (for example, 5 lbs of 21-0-0) if a rapid growth is desired. The reuse of grass clippings produced from a mulching mower can take the place of one of the nitrogen applications for turf during the growing season or a good grade of compost or manure can be substituted for one of the fertilizer applications. Spread 1/4 inch deep over the soil, compost will supply nutrients and increase the organic matter content of any soil, which in turn will boost nutrient and water -holding capacity. For turf maintenance, Washington State University studies have shown that grass uses N:P:K in the ratio of 3:1:2 and it is helpful to use a fertilizer with that ratio of N:P:K in future applications. For ongoing maintenance of woody ornamentals, once a year in the spring they can be fertilized lightly (5 lbs per 1000 sq ft) with a complete fertilizer such as 10-20-20. Thank you for the opportunity to help you prepare healthy landscape. Nancy Parrott Laboratory Supervisor WDOE Accreditation #C594 This report is issued solely for the person or company to whom it is addressed. This laboratory accepts responsibility only for the due performance of analysis according to industry accepted practice. Spectra Laboratories - Kitsap or its employees are not responsible for consequential damages in any ldnd or in any amount. A= 03 pue Hd :IIoS 6V� ,.: =IVY 1001 JO NdVY :w10 I aJ I 1 a bW c �.y a snoaoydsoyd lelol NXI d-ajeydsoydoyrJO N-eluowwy N-SM)IN HdlIAI4�A d _, seat SS/LL S/11 SSI SOl sP!IoS � � (Hdlla� O V 110) IOS V43H W .�. 000 0090 001' tIosd) spslo ,V m �. C uZ OS!N Ovy no BH �p �s21 88s6a cog q3 Zli6VOSIN6ff Qd_ u b I d N W 8y aS BH Qd A0 PO e9 sb'�s elaW V210L1 ,r �� � W m c t + i. sJaule;u00 jo jagwnN °�'w, d CL ws;u con ton &^ rIN, 73 „ o T E CL o V oar ro m m q �* _J7 0 f ;; to . q o Sz CL v ❑ - a CL c ca V Rn1) m9' a�� n °f I ; o g 12q N a 1 71, of 0 m� . o h O O c E FITV v > of c .1: R s N .y (D r_4 ,P" ' d S, U 1134+ E m m ID,CO co E C E CL me� a N Gl �^ dy p a aEi LE' o o F �— to0 El SHANINOWSWLSOKINC, APPENDIX D IMPORTANT INFORMATION ABOUT YOUR GEOTECHNICAL/ENVIRONMENTAL REPORT 21-1-22082-004 SHANNON $ WILSON, INC. Attachment to and part of Report 21-1-22082-004 Geotechnical and Environmental Consultants Date: October 31, 2016 To: Ms. Taine Wilton Edmonds School District #15 IMPORTANT INFORMATION ABOUT YOUR GEOTECHNICAL/ENVIRONMENTAL REPORT CONSULTING SERVICES ARE PERFORMED FOR SPECIFIC PURPOSES AND FOR SPECIFIC CLIENTS. Consultants prepare reports to meet the specific needs of specific individuals. A report prepared for a civil engineer may not be adequate for a construction contractor or even another civil engineer. Unless indicated otherwise, your consultant prepared your report expressly for you and expressly for the purposes you indicated. No one other than you should apply this report for its intended purpose without first conferring with the consultant. No party should apply this report for any purpose other than that originally contemplated without first conferring with the consultant. THE CONSULTANT'S REPORT IS BASED ON PROJECT -SPECIFIC FACTORS. A geotechnical/environmental report is based on a subsurface exploration plan designed to consider a unique set of project -specific factors. Depending on the project, these may include: the general nature of the structure and property involved; its size and configuration; its historical use and practice; the location of the structure on the site and its orientation; other improvements such as access roads, parking lots, and underground utilities; and the additional risk created by scope -of -service limitations imposed by the client. To help avoid costly problems, ask the consultant to evaluate how any factors that change subsequent to the date of the report may affect the recommendations. Unless your consultant indicates otherwise, your report should not be used: (1) when the nature of the proposed project is changed (for example, if an office building will be erected instead of a parking garage, or if a refrigerated warehouse will be built instead of an unrefrigerated one, or chemicals are discovered on or near the site); (2) when the size, elevation, or configuration of the proposed project is altered; (3) when the location or orientation of the proposed project is modified; (4) when there is a change of ownership; or (5) for application to an adjacent site. Consultants cannot accept responsibility for problems that may occur if they are not consulted after factors which were considered in the development of the report have changed. SUBSURFACE CONDITIONS CAN CHANGE. Subsurface conditions may be affected as a result of natural processes or human activity. Because a geotechnical/environmental report is based on conditions that existed at the time of subsurface exploration, construction decisions should not be based on a report whose adequacy may have been affected by time. Ask the consultant to advise if additional tests are desirable before construction starts; for example, groundwater conditions commonly vary seasonally. Construction operations at or adjacent to the site and natural events such as floods, earthquakes, or groundwater fluctuations may also affect subsurface conditions and, thus, the continuing adequacy of a geotechnical/environmental report. The consultant should be kept apprised of any such events, and should be consulted to determine if additional tests are necessary. MOST RECOMMENDATIONS ARE PROFESSIONAL JUDGMENTS. Site exploration and testing identifies actual surface and subsurface conditions only at those points where samples are taken. The data were extrapolated by your consultant, who then applied judgment to render an opinion about overall subsurface conditions. The actual interface between materials may be far more gradual or abrupt than your report indicates. Actual conditions in areas not sampled may differ from those predicted in your report. While nothing can be done to prevent such situations, you and your consultant can work together to help reduce their impacts. Retaining your consultant to observe subsurface construction operations can be particularly beneficial in this respect. Page 1 oft 1/2016 A REPORT'S CONCLUSIONS ARE PRELIMINARY. The conclusions contained in your consultant's report are preliminary because they must be based on the assumption that conditions revealed through selective exploratory sampling are indicative of actual conditions throughout a site. Actual subsurface conditions can be discerned only during earthwork; therefore, you should retain your consultant to observe actual conditions and to provide conclusions. Only the consultant who prepared the report is fully familiar with the background information needed to determine whether or not the report's recommendations based on those conclusions are valid and whether or not the contractor is abiding by applicable recommendations. The consultant who developed your report cannot assume responsibility or liability for the adequacy of the report's recommendations if another party is retained to observe construction. THE CONSULTANT'S REPORT IS SUBJECT TO MISINTERPRETATION. Costly problems can occur when other design professionals develop their plans based on misinterpretation of a geotechnical/environmental report. To help avoid these problems, the consultant should be retained to work with other project design professionals to explain relevant geotechnical, geological, hydrogeological, and environmental findings, and to review the adequacy of their plans and specifications relative to these issues. BORING LOGS AND/OR MONITORING WELL DATA SHOULD NOT BE SEPARATED FROM THE REPORT. Final boring logs developed by the consultant are based upon interpretation of field logs (assembled by site personnel), field test results, and laboratory and/or office evaluation of field samples and data. Only final boring logs and data are customarily included in geotechnical/environmental reports. These final logs should not, under any circumstances, be redrawn for inclusion in architectural or other design drawings, because drafters may commit errors or omissions in the transfer process. To reduce the likelihood of boring log or monitoring well misinterpretation, contractors should be given ready access to the complete geotechnical engineering/environmental report prepared or authorized for their use. If access is provided only to the report prepared for you, you should advise contractors of the report's limitations, assuming that a contractor was not one of the specific persons for whom the report was prepared, and that developing construction cost estimates was not one of the specific purposes for which it was prepared. While a contractor may gain important knowledge from a report prepared for another party, the contractor should discuss the report with your consultant and perform the additional or alternative work believed necessary to obtain the data specifically appropriate for construction cost estimating purposes. Some clients hold the mistaken impression that simply disclaiming responsibility for the accuracy of subsurface information always insulates them from attendant liability. Providing the best available information to contractors helps prevent costly construction problems and the adversarial attitudes that aggravate them to a disproportionate scale. READ RESPONSIBILITY CLAUSES CLOSELY. Because geotechnical/environmental engineering is based extensively on judgment and opinion, it is far less exact than other design disciplines. This situation has resulted in wholly unwarranted claims being lodged against consultants. To help prevent this problem, consultants have developed a number of clauses for use in their contracts, reports, and other documents. These responsibility clauses are not exculpatory clauses designed to transfer the consultant's liabilities to other parties; rather, they are definitive clauses that identify where the consultant's responsibilities begin and end. Their use helps all parties involved recognize their individual responsibilities and take appropriate action. Some of these definitive clauses are likely to appear in your report, and you are encouraged to read them closely. Your consultant will be pleased to give full and frank answers to your questions. The preceding paragraphs are based on information provided by the ASFE/Association of Engineering Firms Practicing in the Geosciences, Silver Spring, Maryland Page 2 of 2 1/2016 Wetland Buffer Averaging and Enhancement Plan New Madrona K-8 Project Edmonds, Washington Excellence. Innovation. Service. Value. Since 1954. September 20, 2016 Submitted To: Ms. Taine Wilton Edmonds School District #15 20420 68th Avenue West Lynnwood, Washington 98036 By: Shannon & Wilson, Inc. 400 N 34th Street, Suite 100 Seattle, Washington 98103 21-1-22082-006 01 TABLE OF CONTENTS Page 1.0 PURPOSE..... .......................................... ........................... ......... ..............................1 2.0 INTRODUCTION ........... ............ ........... .......,.,...... ,.............. .. . ,.,,,.....,,,................ ,.....,1 3.0 WETLAND BUFFER AVERAGING ..................................... ......................... ...........2 3.1 Edmonds Community Development Code (ECDC) Requirements .........................,..2 3.2 Existing Wetland B Buffer Condition and Functions................................................2 3.3 Wetland B Buffer Averaging Strategy.......................................................................3 4.0 WETLAND BUFFER ENHANCEMENT ................................. ---- ................................ ,.,4 4.1 Wetland Buffer Enhancement Plan ............................... , ..,..,............... .,..,..,..4 4.2 Wetland Buffer Enhancement Sequence ....................... ........ -- ....,.............,..5 4.3 Maintenance .......................... ........................... ............................. — - .., ............6 4.4 Monitoring Plan........................,......,...,,............,.....--- ... ..................... ......,......6 4.5 Performance Standards ...................... ..—,,..... -.................... ...................... .,..,..,...8 5.0 CLOSURE .................... ............................................. .................. ...............................8 6.0 REFERENCES-- .................. .....,.. ..............,.., ......., ......,..,................,. ,,....,,...........10 TABLE 1 Vegetation Performance Standards ................... ..---.............. .............. . ,,,.,......8 FIGURES 1 Vicinity Map 2 Wetland Buffer Averaging Plan 3 Wetland Buffer Enhancement Plan APPENDICES A Wetland Buffer Enhancement Area Photos B Important Information About Your Wetland Delineation/Mitigation and/or Stream Classification Report ...... ....... _.. ._.......... 21-1-22082-006-xI f/wp/lkn 21-1-22082-006 1 S1 ANNON 6WILS01% INN WETLAND BUFFER AVERAGING AND ENHANCEMENT PLAN NEW MADRONA K-8 PROJECT EDMONDS, WASHINGTON 1.0 PURPOSE Shannon & Wilson, Inc. (Shannon & Wilson) was contracted by the City of Edmonds School District (District) No. 15 to assist with the wetland buffer averaging and enhancement strategy associated with a site wetland, Wetland B, identified by Shannon & Wilson on the New Madrona K-8 project site in Edmonds, Washington (Figure 1). This plan was prepared for the exclusive use of the Edmonds School District and their representatives for the purpose of complying with the Edmonds Community Development Code (ECDC), which regulates activities within wetland buffers. 2.0 INTRODUCTION The District plans to construct a new Madrona K-8 school on the south side of the approximately 40 -acre property, located at 9300 236th Street SW (Snohomish County tax parcel 27033600404600). The project is located within Section 36 of Township 27 N, Range 4 E, Willamette Meridian. The property is dissected by two steeply sloped wooded areas running in north -south alignments; one is a ravine located along the eastern property boundary and the other is a forested incline located near the middle of the property. The existing Madrona Elementary School is located in the northeast corner of the property and the former Woodway Elementary School is located in the opposite southwest corner of the property. Recreational areas including a track and baseball field, and soccer fields are located in the southeast and northwest corners of the property. The areas surrounding the property consist primarily of residential development. A wetland and stream delineation completed in July 2015 identified three wetlands (Wetlands A, B, and C) on the project site. Wetland delineation findings are described in the Revised Wetland and Stream Delineation Report for the New Madrona K-8 Project (Shannon & Wilson, 2016). The current design for the new school is constrained by the property's steep slopes and would unavoidably extend into a portion of the standard buffer for Wetland B. This plan describes the Wetland B buffer averaging strategy and also describes proposed Wetland B buffer enhancements that would complement the wetland buffer averaging strategy. 21-1-22082-006-R] Vwp/flm 21-1-22082-006 OCHANNON 8WH..,1330N, ENG 3.0 WETLAND BUFFER AVERAGING 3.1 Edmonds Community Development Code (ECDC) Requirements The City regulates wetland buffers under Chapter 23.50 of the ECDC (City, 2016). Wetland B is a Category III depressional wetland (Shannon & Wilson, 2016). The City requires a 60 -foot standard buffer width around Category III wetlands (ECDC 23.50.040(F)(1). Under ECDC 23.50(G)(3), the City allows for wetland buffer averaging with wetland buffer enhancement if the following requirements are met: The buffer averaging and enhancement plan provides evidence that wetland functions and values will be: — Increased or retained through plan implementation for those wetlands where existing buffer vegetation is generally intact; or — Increased through plan implementation for those wetlands where existing buffer vegetation is inadequate to protect the functions and values of the wetland. The wetland contains variations in sensitivity due to existing physical characteristics or the character of the buffer varies in slope, soils, or vegetation, and the wetland would benefit from a wider buffer in places and would not be adversely impacted by a narrower buffer in other places; 01 The total area contained in the buffer area, or the total buffer area existing on a subject parcel for wetlands extending off-site, after averaging is no less than that which would be contained within a standard buffer; and ■ The buffer width at any single location is not reduced by more than 25 percent to less than 50 percent of the standard buffer width.1 The following sections of the plan demonstrate how the Wetland B buffer averaging and enhancement strategy meets these criteria. 3.2 Existing Wetland B Buffer Condition and Functions The standard buffer associated with Wetland B is primarily located in the forested ravine located along the eastern property boundary, and a portion of the wetland buffer extends beyond the steep slopes of the ravine and into playfield south of the existing school. A chain link fence is located at the top of the slope at the edge of the play field. Most of the Wetland B buffer is densely vegetated, with the exception of several areas in the ravine adjacent to the wetland's ` As shown on the City's ECDC website. Communication with the City has clarified the sentence to mean, "The buffer width at any single location is not reduced by more than 25 percent of the standard buffer width." 21-1-22082-006-Rlflwp/lkn 21-1-22082-006 2 3HANNON Illllm eastern boundary and the playfield area. The wetland buffer's vegetation within the ravine is generally dominated by a forested strata of western red cedar (Thuja plicata), big leaf maple (Acer macrophyllum), and Douglas fir (Pseudotsuga menziesii), a shrub strata of salal (Gaultheria shallon), Oregon grape (Mahonia nervosa), English laurel (Prunus laurocerasus), and Indian plum (Oemleria cerasiformis); and a ground cover of sword fern (Polystichum munitum). The vegetation, in combination with the topographic variation in the ravine, visually screen and reduce noise in the wetland from the surrounding residential developments and school. The vegetation also has the potential to provide wildlife habitat to passerine birds and small mammals and slow surface water flow through the area. The portion of Wetland B buffer that extends beyond the steep slopes and into the playfield is comprised of lawn and due to its vegetation and proximity to school activities, provides minimal wildlife habitat, water quality function, or screening. Several unimproved footpaths are located in and around the Wetland B buffer. The paths are part of a large trail system located throughout the project area. The paths provide educational opportunities to students and the community and are part of an orienteering course. Chapter 23.50.040.G.5.c.i of the ECDC allows walkways and trails within wetland buffer and the project does not plan on removing the paths. Based on the site survey, there are two existing stormwater outfalls located in the Wetland B buffer. One outfall, an 8 -inch metal pipe, is located in the field and will continue to be used to discharge stormwater following project construction. However, as part of the project, the site's stormwater treatment prior to reaching the outfall will be updated to meet current standards. Additionally, the area around the 8 -inch outfall has been scoured by the discharge. To prevent further erosion and sedimentation, the project will install quarry spalls underlain by geotextile fabric, which will not require vegetation removal. The second outfall, a 10 -inch polyvinyl chloride pipe, has not been identified in the field and may be buried or dysfunctional. 3.3 Wetland B Buffer Averaging Strategy The project proposes to average the Wetland B buffer width where improvements associated with the new school design would unavoidably impact the wetland buffer, mainly at the top of the steep slope and in the play field area. This strategy would involve reducing the standard wetland buffer width to no less than 45 feet (25 percent of the standard 60 -foot buffer width) in the locations closest to the new school design, which would be a reduction of 3,835 square feet, and extending the wetland buffer by 3,835 square feet at its northern boundary (Figure 2). 21-1-22082-006-R1 flwp/Um 21-1-22082-006 3 SI-IANNON 8WILE33014,INC Given the variation in wetland buffer condition between the ravine and play field area, the wetland would benefit from a greater wetland buffer width where dense vegetation is present to the north and would not be adversely affected by a reduction in buffer width to the west, at the top of the steep slope, and in the existing play field area. Section 23.50.40.1-1.3 of the ECDC includes a requirement for the installation of permanent fencing at the wetland buffer boundary when buffer averaging is implemented as part of a development proposal, and also states that the director may waive this requirement (City, 2016). The majority of the Wetland B buffer boundary is located on densely vegetated steep slopes, largely negating the need for a fence. Additionally, the few available access points to the wetland buffer are used to support the education opportunities described above in Section 3.2. For these reasons, fencing is not part of the wetland buffer averaging plan and we recommend that this requirement be waived. 4.0 WETLAND BUFFER ENHANCEMENT 4.1 Wetland Buffer Enhancement Plan A wetland buffer enhancement plan has been developed to meet the City's criteria for wetland buffer averaging, as described above in Section 3.1. The proposed enhancements are meant to compliment the averaging strategy as well as offset the removal of two 10 -inch red alder (Alnus rubra) trees at the top of the slope within the western wetland buffer boundary. The project arborist identified the two hazard trees as diseased and has recommended them for removal. The trees will be cut off at or near the ground surface, leaving the root ball intact and avoiding earth disturbance. The proposed enhancement plan consists of dense plantings of native shrub and fern species in the currently bare areas adjacent to the eastern wetland boundary. These areas were selected because although they are shaded by a forest of Western red cedar they have limited shrub and ground cover and are in a part of the buffer that would most benefit from the enhancements (Photos 1 and 2). Our wetland buffer enhancement will provide greater vegetation structure and wildlife habitat and will improve screening for the wetland. To provide continuity and to increase the planting success, the plant species selected for the enhancement area include native species already thriving in the wetland buffer and surrounding area (Figure 3). These species have also been used successfully in similar wetland buffer planting projects. The wetland buffer enhancement plan includes removal of existing patches of English holly (Ilex aquifolium) from the planting areas (See Section 4.2 below and planting note 2 on Figure 3). 21-1-22082-006-R1flwp/Hm 21-1-22082-006 4 SHANNOIN 6WLSON,ING The wetland buffer enhancement plan also includes placing large woody debris (LWD) around the outer borders of the planting areas to discourage disturbance and to provide insect, passerine bird, and small mammal habitat (Figure 3). In total, the wetland buffer enhancement area is approximately 1,380 square feet. The proposed wetland buffer enhancement plan will increase wetland and wetland buffer function and value in an area where existing buffer vegetation is inadequate by providing the following ecological benefits: Increased woody species at the wetland boundary will help contribute woody debris and other organic material to the wetland; Invasive species will be replaced by native species in the planting areas; Native woody vegetation will provide wildlife habitat, forage, and cover for birds and small mammals; and 0: Increased vegetation in the planting areas will filter pollutants in surface water runoff through capturing of mobilized sediment, phytoextraction, transpiration, and soil microbial interactions. 4.2 Wetland Buffer Enhancement Sequence The sequence below summarizes the steps that should be taken to implement the wetland buffer enhancement plan. Additional detail can be found in the Planting Notes section of Figure 3. A. A wetland biologist will re -flag or stake the eastern wetland B boundary in the vicinity of the enhancement areas prior to the start of enhancement work. B. Install erosion control Best Management Practices (BMPs) and protect existing native woody vegetation in and adjacent to the planting areas. Earth disturbance should be minimized to the extent possible to avoid damaging existing tree roots in the area. C. Remove existing non-native invasive species such as English holly (Ilex aquifolium) from the planting areas using a combination of hand pulling, cutting, and application of triclopyr or similar, depending on size of individuals. Relocate existing downed woody debris within the site to locations outside of the enhancement areas, to be replaced and reoriented following plant installation. D. Place LWD along the boundaries of the enhancement areas. LWD must be at least 12 inches in diameter. Existing downed woody debris that was removed from the site prior to planting may be used in this delineation, if size criteria is met. E. Procure plants and store properly. Biologist shall review plant material and plant layout prior to planting. Install plants by hand in the planting areas in natural, random clusters. Planting should occur between September 15 and January 15 to take advantage of cool temperatures and precipitation. 21-1-22082-006-R1flwpAkn 21-1-22082-006 5 0SHAMON &WILSON, I F. Mix 3 inches of compost into soil at plant pits and hand -dig circular plant pits. Take care to avoid cutting through existing native tree roots. Backfill with native soil/compost mix. G. Water plants thoroughly after planting to avoid capillary stress. H. Mulch the wetland buffer enhancement areas with 4 to 6 inches of wood chips to discourage weed establishment. I. Remove construction debris. Remove BMPs after site is stabilized. 4.3 Maintenance The contractor will be responsible for maintenance of the enhancement areas for the first year following installation. The District will be responsible for maintenance of the enhancement area for the remaining four years of the monitoring period (see Section 4.4). Maintenance will include watering during the first dry season following planting, weeding around base of installed plants, pruning, replacing plants to meet survival requirements (see Section 4.5), removing all classes of noxious weeds (see Washington State Noxious Weeds List, Washington Administrative Code 16-750-005), and implementing any other measures needed to ensure plant survival. All proposed maintenance shall be reviewed by the biologist. Water shall be provided to installed plants during the dry season (June 1 through October 15) for the first year after plant installation to enhance plant survival and establishment. Water should be applied at a rate of one inch of water, once per week. 4.4 Monitoring Plan Monitoring shall be conducted in years 1, 3, and 5 following installation of the enhancement areas (ECDC 23.40). Below we have outlined proposed monitoring methods, success criteria, and reporting schedule. Monitoring will be conducted by a qualified biologist and will consist of documenting plant mortality in the first year after installation and estimating plant cover thereafter. Monitoring will also include identifying maintenance needs as they relate to plant survival and weed control. Monitoring will be conducted soon after installation to document baseline conditions and in years 1, 3, and 5 to assess whether the site is meeting the success criteria in Section 4.5. A. Baseline Documentation. Within 30 days of completion of the vegetation enhancement installation, the site will be visited to document the as -built condition. The final plant count by species will be verified, and any approved departures from the plan will be mapped and recorded. Recommendations for correcting any unauthorized plan deviations will be included in a Baseline Monitoring Report. Permanent photo points will be established during the as -built site visit to provide a 21-1-22082-006-R1 flwp/Um 21-1-22082-006 6 record of the entire monitoring area. These points will be noted on the map and baseline photos included in the report. B. Vegetation Monitoring. Year 1: Each installed plant will be assessed and counted, and its condition recorded. Invasive species cover will be visually estimated. Years 3 and 5: Total percent cover of native shrub and fern/ground cover species and percent cover of invasive species will be visually estimated. Native volunteer species may be counted in the cover assessment. — All vegetation monitoring shall occur between May 15 and September 30 (prior to leaf drop), unless otherwise specified. — Photos of the vegetation enhancement shall be taken from consistent locations established during baseline monitoring. The monitoring reports will include: A. Reports. Monitoring reports shall be submitted to the City December 31 of each reporting year (baseline and years 1, 3, and 5). Monitoring reports will include the following description/data: 1. Site plan and location map. 2. History of project, including date of plant installation, current year of monitoring, and restatement of performance standards. 3. Plant survival and/or cover and vigor of the installed vegetation, in the context of assessing achievement of performance standards. 4. Observed wildlife, including amphibians and birds. 5. Assessment of nuisance/exotic biota and recommendations for management. 6. Color photographs taken from permanent photo points established during the as - built visit. 7. Summary of maintenance and contingency measures proposed for the next season and completed for the past season. B. Deficiencies. Any deficiency discovered during any monitoring or inspection visit must be corrected within 60 days. C. Contingency Plan. If any monitoring report reveals that the enhancement plan has failed in whole or in part, and if that failure is beyond the scope of routine maintenance, a Contingency Plan shall be prepared and submitted. The Contingency Plan may range in complexity from a list of plants substituted to cross-sections of proposed engineered structures. Once approved, contingency measures may be installed and will replace the approved wetland buffer enhancement plan. 21 -1 -22082 -006 -RI Vwp/Um 21-1-22082-006 7 IIID "SII Ml SON, III14C, 4.5 Performance Standards Plant survival and cover standards are established to measure enhancement plan success. The proposed performance standards are summarized in Table 1. TABLE 1 VEGETATION PERFORMANCE STANDARDS Notes: * Includes native plants in that category that are naturally recruiting. ** Applies to all exotic invasive species. If weed cover exceeds 10 % during vegetation monitoring, this performance standard can be met by removing weeds within 60 days of vegetation monitoring. 100 percent (%) survival criteria shall be met by replacing all mortalities the first year after planting. > = greater than or equal to 5.0 CLOSURE This report has been prepared for specific application to the New Madrona K-8 project. This report has been developed in a manner consistent with the level of care and skill normally exercised by members of the environmental science profession currently practicing under similar conditions in the area. The wetland buffer averaging and enhancement approach presented in this report incorporates professional opinions based on interpretation of information currently available to us, and was completed within the operational scope, budget, and schedule constraints of this project. No warranty, express or implied, is made. This report was prepared for the exclusive use of the District and its representatives. We have prepared Appendix B, "Important Information About Your Wetland Delineation/Mitigation 21-1-22082-006-R1 ftp/Um 21-1-22082-006 8 SHANNON WILSON, INC. Report and/or Stream Classification Report," to assist you and others in understanding the use and limitations of our reports. SHANNON & WILSON, INC. Samh C, Corbin, PPS Senior Biologist -Scientist SCC:KLW/scc 21-1-22082-006-Rlflwpflkn 21-1-22082-006 9 6.0 REFERENCES Edmonds, Wash., 2016, Wetlands: Edmonds, Wash., City Code and Development Code Title 23.50, available: http://www.codepublishing.com/WA/Edmonds/. Shannon & Wilson, Inc., (Shannon & Wilson), 2016, Revised wetland and stream delineation report for new Madrona K-8 project, City of Edmonds, Washington: Report prepared by Shannon & Wilson, Inc., Seattle, Wash., 21-1-22082-002, for City of Edmonds School District, Edmonds, Wash., August, 94 p. 21-1-22082-006-Rl f/wp/Ua 21-1-22082-006 10 ♦ • • Proj I` ---�LocatlIn Seattle Or 41 �i pir VAI r k✓ if m � )" e g r % 19 1 le��i d r r A �/ W'j��LJVIII JI JVV /: �r, 1 ta ' ' 11,1,r / 6238th St SW r �1 �— , " „ r 240th Lakc Balling • a r , '� 11 205th St 'p, o m qtr LO N 0 2,000 4,000 Go I CD —-.--.. 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Z0N0LL 22RzW=OQ0 s22JOp.W azWX z0i2 Z z¢4N0Wwil=pQzFmza, FLLawwzOompWwWmW1 gNa°x Na9gG "WHz=O=,Wr�3 j� ZmN�=Q rW �NOS m2W 2NNJOCaW �HOp2=oaQ4J= g_QOq6 CW ZO aaoW30Jdr ZIt CL NmNoOa0 amw WE 3a8 0maoJa wz Uzz oz Hog I IL CL r M R V N 16 C C21 `^A w C C N WyOo FC W wLL (33 H ivj O�w a jSN�sWy QQUx W J�J� W SFi �iN O O N LL Sr,' 'Z' <O C Jy -�ryTy y,, YAC ry r 'NN�I�M -a OI.n7MLM:W0n MW'U9IAU8Wa3UBUUgl9�MMMgl919-N } f� w C7 as O_ _ F C C21 `^A w C C N WyOo FC W wLL (33 H ivj O�w a jSN�sWy QQUx W J�J� W SFi �iN O O N LL Sr,' 'Z' <O C Jy -�ryTy y,, YAC ry r 'NN�I�M -a OI.n7MLM:W0n MW'U9IAU8Wa3UBUUgl9�MMMgl919-N ,,,,LANNON MILSON, INC. APPENDIX A WETLAND BUFFER ENHANCEMENT AREA PHOTOS 21-1-22082-006 SHANNON &WILSON, INC. Photo 1: A portion of buffer enhancement area 1, viewing northeast, taken on September 12, 2016. Photo 2: A portion of buffer enhancement area 2, with Wetland B shown on the left, viewing north, taken on September 12, 2016. 21-1-22082-006-R1 f-AA/wpAkn 21-1-22082-006 APPENDIX B IMPORTANT INFORMATION ABOUT YOUR WETLAND DELINEATION/MITIGATION AND/OR STREAM CLASSIFICATION REPORT 21-1-22082-006 SHANNON & WILSON, INC. Attachment to and part of Report 21-1-22082-006 Geotechnical and Environmental Consultants Date: September 20, 2016 To: Ms. Taine Wilton ._....._.........._..........� Edmonds School District #15 IMPORTANT INFORMATION ABOUT YOUR WETLAND DELINEATIONNITIGATION AND/OR STREAM CLASSIFICATION REPORT A WETLAND/STREAM REPORT IS BASED ON PROJECT -SPECIFIC FACTORS. Wetland delineation/mitigation and stream classification reports are based on a unique set of project -specific factors. These typically include the general nature of the project and property involved, its size, and its configuration; historical use and practice; the location of the project on the site and its orientation; and the level of additional risk the client assumed by virtue of limitations imposed upon the exploratory program. The jurisdiction of any particular wetland/stream is determined by the regulatory authority(s) issuing the permit(s). As a result, one or more agencies will have jurisdiction over a particular wetland or stream with sometimes confusing regulations. It is necessary to involve a consultant who understands which agency(s) has jurisdiction over a particular wetland/stream and what the agency(s) permitting requirements are for that wetland/stream. To help reduce or avoid potential costly problems, have the consultant determine how any factors or regulations (which can change subsequent to the report) may affect the recommendations. Unless your consultant indicates otherwise, your report should not be used: ► If the size or configuration of the proposed project is altered. ► If the location or orientation of the proposed project is modified. ► If there is a change of ownership. ► For application to an adjacent site. ► For construction at an adjacent site or on site. ► Following floods, earthquakes, or other acts of nature. Wetland/stream consultants cannot accept responsibility for problems that may develop if they are not consulted after factors considered in their reports have changed. Therefore, it is incumbent upon you to notify your consultant of any factors that may have changed prior to submission of our final report. Wetland boundaries identified and stream classifications made by Shannon & Wilson are considered preliminary until validated by the U.S. Army Corps of Engineers (Corps) and/or the local jurisdictional agency. Validation by the regulating agency(s) provides a certification, usually written, that the wetland boundaries verified are the boundaries that will be regulated by the agency(s) until a specified date, or until the regulations are modified, and that the stream has been properly classified. Only the regulating agency(s) can provide this certification. MOST WETLAND/STREAM "FINDINGS" ARE PROFESSIONAL ESTIMATES. Site exploration identifies wetland/stream conditions at only those points where samples are taken and when they are taken, but the physical means of obtaining data preclude the determination of precise conditions. Consequently, the information obtained is intended to be sufficiently accurate for design, but is subject to interpretation. Additionally, data derived through sampling and subsequent laboratory testing are extrapolated by the consultant who then renders an opinion about overall conditions, the likely reaction to proposed construction activity, and/or appropriate design. Even under optimal circumstances, actual conditions may differ from those thought to exist because no consultant, no matter how qualified, and no exploration program, no matter how comprehensive, can reveal what is hidden by earth, rock, and time. Nothing can be done to prevent the unanticipated, but steps can be taken to help reduce their impacts. For this reason, most experienced owners retain their consultants through the construction or wetland mitigation/stream classification stage to identify variances, to conduct additional evaluations that may be needed, and to recommend solutions to problems encountered on site. Page 1 of 2 1/2016 WETLAND/STREAM CONDITIONS CAN CHANGE. Since natural systems are dynamic systems affected by both natural processes and human activities, changes in wetland boundaries and stream conditions may be expected. Therefore, delineated wetland boundaries and stream classifications cannot remain valid for an indefinite period of time. The Corps typically recognizes the validity of wetland delineations for a period of five years after completion. Some city and county agencies recognize the validity of wetland delineations for a period of two years. If a period of years have passed since the wetland/stream report was completed, the owner is advised to have the consultant reexamine the wetland/stream to determine if the classification is still accurate. Construction operations at or adjacent to the site and natural events such as floods, earthquakes, or water fluctuations may also affect conditions and, thus, the continuing adequacy of the wetland/stream report. The consultant should be kept apprised of any such events and should be consulted to determine if additional evaluation is necessary. THE WETLAND/STREAM REPORT IS SUBJECT TO MISINTERPRETATION. Costly problems can occur when plans are developed based on misinterpretation of a wetland/stream report. To help avoid these problems; the consultant should be retained to work with other appropriate professionals to explain relevant wetland, stream, geological, and other findings, and to review the adequacy of plans and specifications relative to these issues. DATA FORMS SHOULD NOT BE SEPARATED FROM THE REPORT. Final data forms are developed by the consultant based on interpretation of field sheets (assembled by site personnel) and laboratory evaluation of field samples. Only final data forms customarily are included in a report. These data forms should not, under any circumstances, be drawn for inclusion in other drawings because drafters may commit errors or omissions in the transfer process. Although photographic reproduction eliminates this problem, it does nothing to reduce the possibility of misinterpreting the forms. When this occurs, delays, disputes, and unanticipated costs are frequently the result. To reduce the likelihood of data form misinterpretation, contractors, engineers, and planners should be given ready access to the complete report. Those who do not provide such access may proceed under the mistaken impression that simply disclaiming responsibility for the accuracy of information always insulates them from attendant liability. Providing the best available information to contractors, engineers, and planners helps prevent costly problems and the adversarial attitudes that aggravate them to a disproportionate scale. READ RESPONSIBILITY CLAUSES CLOSELY. Because a wetland delineation/stream classification is based extensively on judgment and opinion, it is far less exact than other design disciplines. This situation has resulted in wholly unwarranted claims being lodged against consultants. To help prevent this problem, consultants have developed a number of clauses for use in written transmittals. These are not exculpatory clauses designed to foist the consultant's liabilities onto someone else; rather, they are definitive clauses that identify where the consultant's responsibilities begin and end. Their use helps all parties involved recognize their individual responsibilities and take appropriate action. Some of these definitive clauses are likely to appear in your report, and you are encouraged to read them closely. Your consultant will be pleased to give full and frank answers to your questions. THERE MAY BE OTHER STEPS YOU CAN TAKE TO REDUCE RISK. Your consultant will be pleased to discuss other techniques or designs that can be employed to mitigate the risk of delays and to provide a variety of alternatives that may be beneficial to your project. Contact your consultant for further information. Page 2 of 2 1/2016 Revised Wetland and Stream Delineation Report New Madrona K-8 Project City of Edmonds, Washington GEOTECHNICAL AND E Excellence. Innovation. Service. Value, Since 1954. CITY COPY RECEIVED BUILIANG Revised August 4, 2016 Submitted To: Ms. Taine Wilton Edmonds School District #15 20420 68th Avenue West Lynnwood, Washington 98036 By: Shannon & Wilson, Inc. 400 N 34th Street, Suite 100 Seattle, Washington 98103 21-1-22082-002 °°LANNON MUSON, VIII, TABLE OF CONTENTS Page 1.0 INTRODUCTION ... ....................................... ...,......... ......,...,...., .. .,......,.... ....„,...............1 2.0 SITE DESCRIPTION ....... —...., ............ ......... ..,................ ................. ,......,...............1 3.0 METHODS......,.w...,.......,.,„.„ ............................... ................... ........................................2 4.0 DOCUMENT REVIEW .......... , ..............— ..— ....................... ....... ......— .........,..,.........3 5.0 WETLAND DELINEATION........ ......... — .............................,,......-......., ..............,..........3 5.1 Wetland A ........................ .......... ..................... ......... ... ......... .................., ..,,....,,..,3 5.2 Wetland B .................. ..........................., ................,........., ..........,....,.., .,......,....4 5.3 Wetland C .................. ............ .............................. ....--- ..... ....... 5 5.4 Uplands., ...........--- ................ ......,..., ,............... ........ ........,,................ ............ 6 6.0 REGULATIONS...�................................., ......,.............................. .....,............ ,......,,....6 6.1 Federal Regulations ............ ......... ................... .................. . .............................6 6.2 State Regulations ................. ........................,....... ,.......... ,.........,.....,......,..7 6.3 City of Edmonds (City) ....................................................... .................. .............8 6.3.1 Wetlands Regulations ................ .................. .......... ...,..... , ... .........8 6.3.2 Other Critical Areas......... ............................... ................ .., ....................10 7.0 CLOSURE... .............. ........ ,.......... ,........,...........,.....,.................. ....— ...... . ........,.........11 8.0 REFERENCES ...................................................................................... ...................1.2 TABLES 1 Wetland Impact Compensatory Mitigation Ratios..................................................7 2 Required Measures to Minimize Impacts (ECDC 23.50.040(F)(2) .........................8 FIGURES 1 Vicinity Map 2 Wetland Delineation Map 21-1-22082-002-R1 f-rev/wp/lk 21-1-22082-002 SHANNON L O,ilii i3O`, The property is well used by local residents for recreation. During our site visits, we observed many people walking dogs in trail systems located throughout the sloped wooded areas as well, as many joggers on the track. A series of catch basin grates were observed along the inside of the track. The survey performed for the property shows that these storm drains, along with storm drain from the existing Madrona Elementary School, discharge to the top of the steep wooded slope in the middle of the property. The survey also identifies storm drain discharges to the top of the wooded ravine located on the eastern property boundary. 3.0 METHODS Shannon & Wilson conducted the wetland delineation fieldwork on July 6 and 7, 2015. Potential wetlands were identified using methods described in the Corps Wetlands Delineation Manual (U.S. Army Corps of Engineers [Corps] Waterways Experiment Station, 1987) and the Regional Supplement to the Corps of Engineers Wetland Delineation Manual: Western Mountains, Valleys, and Coast Region (Corps Engineer Research and Development Center, 2010). Potential wetland areas were determined using the triple -parameter approach, which considers vegetation types, soil conditions, and hydrologic conditions. For an area to be considered wetland, it must display each of the following: (a) dominant plant species that are considered hydrophytic by the accepted classification indicators, (b) soils that are considered hydric under federal definition, and (c) indications of wetland hydrology, in accordance with the federal definition. Appendix A provides a detailed description of methodology used. Typically, the OHWM of streams are delineated following the guidance within Ecology's technical report Determining the Ordinary High Water Mark on Streams in Washington State (Ecology, 2010). However, no onsite streams were observed; therefore, no OHWM delineations occurred. Identified wetlands were delineated by using pink "wetland boundary" flagging and pink pin flags. Data point locations were marked with orange flagging and orange pin flags. 21-1-22082-002-R1f-rev/wp/1k 21-1-22082-002 2 dliANNON OWL' S011% INC 4.0 DOCUMENT REVIEW Prior to conducting fieldwork, we reviewed the following background information: ■ U.S. Department of Agriculture (USDA) Natural Resources Conservation Service (MRCS) Web Soil Survey interactive mapping system ■ U.S. Fish and Wildlife Service (USFWS) National Wetland Inventory (NWI) Wetlands Mapper interactive mapping system Washington Department of Fish and Wildlife (WDFW) SalmonScape mapping system WDFW PHS on the Web interactive mapping system The NRCS web soil survey identifies the site soils as Alderwood gravelly, sandy loam; 15 to 30 percent slopes; Alderwood-Urban land complex; 2 to 8 percent slopes; and 8 to 15 percent slopes (USDA, 2015). These soil series are identified as non -hydric, however they may contain areas of hydric inclusions. Neither the NWI map, the WDFW SalmonScape application, nor the WDFW PHS on the Web application identify streams, wetlands, or other fish and wildlife habitat conservation areas on the property (USFWS, 2015 and WDFW, 2015 and 2016). 5.0 WETLAND DELINEATION Three wetlands (identified as Wetland A, B, and C) were delineated in the project area (Figure 2). Descriptions of the wetland and adjoining uplands follow. Vegetation is described below by common name, with the scientific name and indicator status in parentheses for the first use. Soils are described with the associated Munsell® Color Charts color. Wetlands were characterized according to the updated 2014 version of the "Washington State Wetland Rating System for Western Washington" (Ecology, 2014) as required by the City, Corps, and Ecology (see Appendix B for Wetland Determination Data Forms and Appendix C for Wetland Rating Forms). 5.1 Wetland A Wetland A (approximately 0.02 acre) was delineated on the steep, wooded slope located in the middle of the property, approximately 100 feet downgradient from a storm drain outfall identified on the survey. A trail system on the slope allows human and pet access to the wetland. Wetland A is classified as a palustrine scrub -shrub wetland according to the Cowardin classification and is a slope wetland according to hydrogeomorphic classification. 21-1-22082-002-R1 f-rev/wp/1k 21-1-22082-002 3 6HANNOY 6WLSON,IIT Dominant vegetation in Wetland A includes a shrub strata of salmonberry (Rubus spectabilis, FAC), English laurel (Prunus laurocerasus, NI), mountain ash (Sorbus sitchensis, FAC), as well as an emergent strata of lady fern (Athyrium cyclosorum, FAC) (see Appendix B, Data Sheet DP -7). Soil in Wetland A is generally characterized by a surface horizon of black (IOYR 2/1) loam extending to 5 inches below ground surface (bgs), underlain by a grayish brown (IOYR 5/2) sand with dark yellowish brown (IOYR 4/6) redoximorphic concentrations in the matrix. Soil observed in Wetland A meets the depleted below dark surface (A11) and depleted matrix (F3) hydric soil indicators. During the site visit, groundwater seeps were observed in Wetland A. Hydrology in Wetland A is likely predominantly supported by natural groundwater seeps. Although surface water flow may contribute to the wetland's hydrology during and after rainfall, surface flow is not expected to be a significant contribution to the wetland's hydrology. No evidence of surface water inputs, such as channelized flow, were observed during the fieldwork. Water in the data pit was observed at 11.5 inches bgs and the soil was saturated to the surface. Wetland A was rated according to Ecology's 2014 wetland rating manual (Ecology, 2014). Wetland A is rated as a Category IV wetland (Appendix Q. 5.2 Wetland B Wetland B (approximately 0.4 acre) was delineated within the wooded ravine located on the eastern property boundary. A network of walking paths run adjacent to and through parts of the wetland. Wetland B is classified as a palustrine forested wetland according to the Cowardin classification and as a depressional wetland according to the hydrogeomorphic classification. Dominant vegetation in Wetland B includes a forested strata of western red cedar (Thuja plicata, FAC) and red alder (Alnus rubra, FAC), as well as an emergent strata of slough sedge (Carex obnupta, OBL), yellow -flag iris (Iris pseudocorus, OBL), and reed canarygrass (Phalaris arundinacea, FACW) (see Appendix B, Data Sheet DP -3). Soil in Wetland B is generally characterized by a black (IOYR 2/1) silt loam extending to 4 inches bgs underlain by a very dark gray (IOYR 3/1) silt loam with gray (IOYR 6/1) depletions and dark yellowish brown (IOYR 4/6) and grayish brown (IOYR 5/2) redoximorphic concentrations extending to 17 inches bgs, underlain by a very dark gray (IOYR 3/1) silt loam extending to 18 inches bgs, underlain by a very dark gray (IOYR 3/1) silt loam with gray (IOYR 6/1) depletions and dark yellowish brown (IOYR 4/6) and grayish brown (IOYR 5/2) 21-1-22082-002-Rl&rev/wp/]k 21-1-22082-002 4 SWUY140114 WIL,; IN, IIVIING redoximorphic concentrations extending to at least 20 inches bgs. The redoximorphic and depletions observed in the soil below 4 inches bgs appeared blocky and mixed up within the matrix suggesting that the soil may have been disturbed in the past. Soils observed in Wetland B meet the redox dark surface (F6) hydric soil indicator. Wetland B is located downgradient of the storm drain outlets associated with the existing Madrona Elementary School and the play fields. Drainage patterns were observed upgradient of Wetland B in the ravine. While these areas showed indication of past surface water flow, they were not dominated by hydric vegetation and did not meet wetland hydric soil indicators. Hydrology in Wetland B is likely predominantly supported by surface flow from the surrounding ravine, the storm drain inputs from the school, and a seasonally high groundwater table. Wetland B was rated according to Ecology's 2014 wetland rating manual (Ecology, 2014), Wetland B is rated as a Category III wetland (Appendix Q. 5.3 Wetland C Wetland C (approximately 0.1 acre) was delineated south of Wetland A along the steep wooded slope located in the middle of the property. A trail system on the slope allows human and pet access to the wetland. Wetland C is classified as a palustrine emergent wetland according to the Cowardin classification and as a slope wetland according to hydrogeomorphic classification. Dominant vegetation in Wetland C includes a shrub strata of western red cedar, an emergent strata of lady fern, and creeping nightshade (Solanum dulcamara, FAC) (see Appendix B, Data Sheet DP -6). Soil in Wetland C is generally characterized by a black (IOYR 2/1) loam, underlain by a grayish brown (IOYR 5/2), gravelly, loamy sand with dark yellowish brown (IOYR 4/4) redoximorphic concentrations in the matrix extending to at least 14 inches bgs. Soils observed in Wetland C meet the depleted below dark surface (Al 1) and the depleted matrix (173) hydric soil indicators. During the site visit, groundwater seeps were observed throughout Wetland C. Wetland C is likely predominantly supported by natural groundwater seeps. Although surface water flow may contribute to the wetland's hydrology during rainfall, surface flow is not expected to be a significant contribution to the wetland's hydrology. . No evidence of surface water inputs to the wetland were observed during the fieldwork. Soil in the data pit was saturated to the surface. Wetland C was rated according to Ecology's 2014 wetland rating manual (Ecology, 2014), Wetland C is rated as a Category 1-V wetland (Appendix Q. 21-1-22082-002-R1 f-rev/wp/lk 21-1-22082-002 5 SHANNON WLSON,VIII G 5.4 Uplands Uplands observed on the project site consist predominantly of developed school structures and recreational facilities as well as portions of the wooded slope and. The play fields are dominated by a variety of grasses, dandelion (Taraxacum officinale, facultative upland [FACU]), hairy cat's ear (Hypochaeris radicata, FACU), and clover (Trifolium repens, facultative [FAC]). The wooded areas are dominated by western red cedar, Douglas -fir (Pseudotsuga menziesii, FACU), hemlock (Tsuga heterophylla, FACU), red elderberry (Sambucus racemosa, FACU), holly (Ilex aquifolium, FACU), English laurel, sword fern (Polystichum munitum, FACU), and English ivy (Hedera helix, FACU) (see Appendix B, Data Sheets DP -1, DP -2, DP -4, and DP -5). Upland soils on the property generally consisted of a surface horizon comprised of dark yellowish brown (IOYR 3/4) to black (5YR 2.5/1) loam in the upper 2 to 5 inches bgs, underlain by dark yellowish brown (IOYR 3/4 and 4/4) to light olive brown (2.5Y 5/3) loamy sand to silt loam extending to at least 16 inches bgs. In areas closer to the wetland boundaries, redoximorphic concentrations were observed below 5 inches. However, the soil profiles in these areas do not meet wetland hydric soil indicators. No saturation was observed in the upland soils although surface drainage patterns were observed in the ravine and below storm drain outfalls on the western slope. 6.0 REGULATIONS Several local, state, and federal regulations apply to development proposals in and/or near wetlands and streams. A summary of applicable regulatory implications is given below. 6.1 Federal Regulations The Corps' review process under Section 404 of the Clean Water Act (CWA) is required for projects involving discharges of dredges or fill materials into waters of the United States, including non -isolated wetlands and streams. We did not observe a hydrologic surface connection between the onsite wetlands and a Water of the U.S. Therefore, the Corps may consider the onsite wetlands to be isolated and not subject to the CWA. However, this determination would need to be made by the Corps through a "Jurisdictional Determination." If the Corps takes jurisdiction over the site wetlands, impacts to the wetlands would require compensatory wetland mitigation. The Corps, in cooperation with Ecology, has developed guidance for conducting wetland mitigation in western Washington (Ecology and others, 2006). For unavoidable impacts to Category III and Category IV wetlands, the Corps and Ecology 21-1-22082-002-R1 f-rev/wp/1k 21-1-22082-002 6 %S31-1ANNONW11,,,,. SON, INC. recommend the on-site and in-kind permittee -responsible mitigation ratios shown in Table 1 based on area (area of mitigation: area of wetland impact.) TABLE 1 WETLAND IMPACT COMPENSATORY MITIGATION RATIOS 6.2 State Regulations Ecology has been authorized to implement Section 401 of the CWA for Water Quality Certification in Washington for most projects that require Corps permits under CWA Section 404. Typically, projects requiring a CWA Section 404 permit also require a CWA Section 401 Water Quality Certification. If the onsite wetlands are determined to be isolated, the project would not require a Section 401 Water Quality Certification. The purpose of the 401 certification process is to ensure that federally permitted or federally funded activities comply with the federal CWA, state water quality laws, and any other applicable state laws. Some general requirements for Section 401, if it is required, include pollution spill prevention and response measures, disposal of excavated or dredged material in upland areas, use of fill material that does not compromise water quality, clear identification of construction boundaries, and provision for site access to the permitting agency for inspection. If the Corps does not take jurisdiction over the onsite wetlands under the CWA, Ecology still has regulatory authority to protect isolated wetlands under the State Water Pollution Control Act (Chapter 90.48 Revised Code of Washington). Ecology would perform an administrative review of the project and would issue an Administrative Order for unavoidable impacts to isolated wetlands. 21-1-22082-002-R1 f-rev/wp/1k 21-1-22082-002 7 6.3 City of Edmonds (City) 6.3.1 Wetlands Regulations The City regulates wetlands and wetland buffers under Chapter 23.50 of the Edmonds Community Development Code (ECDC) (City, 2016).2 Based on our field observations and using the 2014 Wetland Rating System for Western Washington, Wetlands A and C are Category IV wetlands and Wetland B is a Category III wetland (Appendix Q. The City requires a 60 -foot standard buffer around Category III wetlands and a 40 -foot standard buffer around Category IV wetlands, with implementation of the following minimization measures when applicable (Table 2 and Figure 2) (ECDC 23.50.040(F)(1-2)). TABLE 2 REQUIRED MEASURES TO MINMINIZE IMPACTS (ECDC 23.50.040(F)(2)) IA I w^I o e77777777771 ilr d:easur s i'` itis i 'log Lights Direct lights away from wetland. Noise 0 Locate activity that generates noise away from wetland. • If warranted, enhance existing buffer with native vegetation plantings adjacent to noise source immediately adjacent to the outer wetland buffer. Toxic runoff w Route all new, untreated runoff away from wetland while ensuring wetland is not dewatered. Establish covenants limiting use of pesticides within 150 feet of wetlands. • Apply integrated pest management. .... Stormwater runoff ................. ......._ __WWWW • Retrofit stormwater detention and treatment for roads and existing adjacent development. Prevent channelized flow from lawns that directly enters the buffer. Use Low Impact Development (LID) techniques (per Puget Sound Action Team �.-.....WW publication on LID techniques). Change in water ........ ...... __ ................ Infiltrate or treat, detain, and disperse into buffer new runoff from impervious surfaces regime and new lawns. Pets and human • Use privacy fencing OR plant dense vegetation to delineate buffer edge and to disturbance discourage disturbance using vegetation appropriate for the ecoregion. • Place wetland and its buffer in a separate tract or protect with a conservation easement. Dust Use best management practices to control dust. Disruption of corridors I * Maintain connections to offsite areas that are undisturbed. or connections • Restore corridors or connections to offsite habitats by replanting. 2 The Edmonds City Council adopted revisions to these regulations in May 2016, so all code references below are taken from the track changes version of the code provided in the Council's agenda packet. Accordingly, there remain some typographical errors in that version with respect to section numbering. 21-1-22082-002-R1 f-rev/wp/& 21-1-22082_002 8 � l'„°IIID YNO VL,,,SON, MING In accordance with ECDC 23.50.040(F)(2), the City may require increased buffer widths on a case-by-case basis when a larger buffer is necessary to protect wetland functions and values. The City bases this determination on the following criteria: A larger buffer is needed to protect other critical areas; ■ The buffer or adjacent uplands has a slope greater than 15 percent or is susceptible to erosion and standard erosion control measures will not prevent adverse impacts to the wetland; ■ The buffer area has minimal vegetative cover. In lieu of increasing the buffer width where existing buffer vegetation is inadequate to protect the wetland functions and values, development and implementation of a wetland buffer enhancement plan may substitute. The wetland and/or buffer is occupied by a federally listed threatened or endangered species, a bald eagle nest, a great blue heron rookery, or a species of local importance; and it is determined by the director that an increased buffer width is necessary to protect the species. ECDC 23.50.040(G) allows for buffer reduction only when existing buffer vegetation is inadequate; the buffers of the existing wetlands are primarily densely vegetated with a mix of native tree and shrub species so this provision may not be applicable. Based on our understanding of the current development proposal, there may be some small areas of existing buffer that are lawn and ballfields that would be impacted. Under ECDC 23.50(G)(3), the City allows for buffer averaging with buffer enhancement if the following requirements are met: ■ The buffer averaging and enhancement plan provides evidence that wetland functions and values will be: — Increased or retained through plan implementation for those wetlands where existing buffer vegetation is generally intact; or — Increased through plan implantation for those wetlands where existing buffer vegetation is inadequate to protect the functions and values of the wetland. • The wetland contains variations in sensitivity due to existing physical characteristics or the character of the buffer varies in slope, soils, or vegetation, and the wetland would benefit from a wider buffer in places and would not be adversely impacted by a narrower buffer in other places; • The total area contained in the buffer area, or the total buffer area existing on a subject parcel for wetlands extending off-site, after averaging is no less than that which would be contained within a standard buffer; and 21-1-22082-002-R1 f-rev/wp/]k 21-1-22082-002 9 ■ The buffer width at any single location is not reduced by more than twenty-five percent (25%) of the standard o buffer width. However, wetland buffer averaging that also modifies the erosion hazard area and/or its buffer would not be allowed by the ECDC without a geotechnical analysis and demonstration that the wetland buffer averaging and erosion or landslide hazard area buffer modification would not adversely impact the wetlands. Wetland buffer reduction through buffer enhancement may also be allowed if buffer averaging is not feasible on site (ECDC 23.50.040(G)(4)). ECDC 23.50.040(G)(8) describes potential permitted uses within wetland buffers, including conservation and restoration activities, passive recreation (such as trails), and stormwater management facilities. The proposed development of a new school and fire access road are not allowed uses within wetland buffers. If buffer averaging or reduction with enhancement is not sufficient to address the need for placement of structures, then a variance and additional buffer mitigation would be required. 6.3.2 Other Critical Areas The City regulates critical areas including wetlands (addressed in Section 6.3.1), fish and wildlife habitat conservation areas, geologically hazardous areas, critical aquifer recharge areas, frequently flooded areas, and shorelines under ECDC Title 23 Natural Resources. Fish and wildlife habitat conservation areas include streams, state priority habitats and areas associated with state priority species, and federally designated threatened or endangered species, among others. The site investigation and document reviews did not identify any streams or other fish and wildlife habitat conservation areas on site or within 225 feet. This scope of services did not include professional assessment of other regulated critical areas. However, some observations about potential geologically hazardous areas is warranted given the affect this critical area can have on site development, particularly when it overlaps with wetlands and wetland buffers. Based on soils mapping, available topographic information, and the 0iiLy 's Uefi111t1Vll0 of gcVivgicaiiy liazarUVus areas (El^..Dl^_. 2J.OV .V2V), rile pi'eseilce of erosion and/or landslide hazard areas on the eastern and western sides of the property at or near Wetlands A, B, and C and their buffers seems likely. A geotechnical report would be required to establish the appropriate building setback and buffer from the top and toe of any erosion or landslide hazards. An additional analysis would be required to alter the hazard area, the minimum building setback and any required buffer (ECDC 23.80.070(A)(1-2)). A hazards analysis must demonstrate the following: 21-1-22082-002-R1 f-rev/wp/1k 21-1-22082-002 10 SHANNON &WILSON, INC. • The alteration will not increase surface water discharge or sedimentation to adjacent properties beyond predevelopment conditions, • The alteration will not decrease slope stability on adjacent properties, and • Such alterations will not adversely impact other critical areas (ECDC 23.80.070(A)(3)). Shannon & Wilson will be providing the necessary geotechnical analyses under a separate scope of work. 7.0 CLOSURE The findings and conclusions documented in this report have been prepared for specific application to this project, and have been developed in a manner consistent with that level of care and skill normally exercised by members of the environmental science profession currently practicing under similar conditions in the area, and in accordance with the terms and conditions set forth in our agreement. The conclusions and recommendations presented in this report are professional opinions based on interpretation of information currently available to us, and are made within the operational scope, budget, and schedule constraints of this project. No warranty, express or implied, is made. Shannon & Wilson has prepared Appendix D, "Important Information About Your Wetland Delineation/Mitigation and/or Stream Classification Report," to assist you and others in understanding the use and limitations of our reports. SHANNON & WILSON, INC. 44� '"` Sarah orbin, PWS Senior Biologist SCC:PCJ:AJS:MWP:KLW/scc 21-1-22082-002-R1 f-revhvp/1k 21-1-22082-002 11 8.0 REFERENCES City of Edmonds (Edmonds), 2016, City of Edmonds City Code Chapter 23.50 Wetlands: Edmonds, Wash., May 2016. U.S. Department of Agriculture (USDA), Natural Resources Conservation Service, 2015, Web soil survey. Available: http://websoilsurvey.sc.egov.usda.gov/App/HomePage.htm. Accessed: August 2015. U.S. Army Corps of Engineers (Corps) Waterways Experiment Station, 1987, Corps of Engineers wetlands delineation manual: Vicksburg, Miss., U.S. Army Corps of Engineers Waterways Experiment Station, Wetlands Research Program Technical Report Y-87-1, 143 p., available: http://www.wli.nres.usda.gov/delineation/. U.S. Army Corps of Engineers (Corps) Engineer Research and Development Center, 2010, Regional supplement to the Corps of Engineers wetland delineation manual: western mountains, valleys, and coast region (version 2.0): Vicksburg, Miss., U.S. Army Corps of Engineers Engineer Research and Development Center, Final report ERDC/EL TR -10-3, 152 p. U.S. Fish and Wildlife Service (USFWS), 2015, Web map service: FWS—Wetlands_WMS: U.S. Fish and Wildlife Service. Open geographical information systems consortium version: 1.3. Available: http://www.fws.gov/wetlands/Data/WebMapServices. Accessed: August 2015. Washington State Department of (Ecology), U.S. Army Corps of Engineers Seattle District, and U.S. Environmental Protection Agency Region 10, 2006, Wetland Mitigation in Washington State — Part 1: Agency Policies and Guidance (Version 1): Olympia, Wash, Washington State Department of Ecology, Publication no. 06-06-11a. Washington State Department of Ecology (Ecology), 2010, Determining the ordinary high water mark on streams in Washington State, second review draft: Lacey, Wash., Washington State Department of Ecology, Publication no. 08-06-001. Washington State Department of Ecology (Ecology), 2014, Washington State wetland rating system for western Washington: Olympia, Wash., Washington State Department of Ecology, Publication no. 14-06-029, 126 p. Washington State Department of Fish and Wildlife (WDFW), 2015, SalmonScape mapping application, accessed July 2015, available: ht� a ms.wdfw.wa. g,ovlsali�nonsca e/ana .html Washington State Department of Fish and Wildlife (WDFW), 2016, PHS on the Web mapping application, accessed March 2016, available: ht�l/ p s,wdfw.wa.gov/phsolitheweb/ 21-1-22082-002-R1 f-rev/wp/lk 21-1-22082-002 12 0 200 4nn Scale in Feet LEGEND Data Point and Designation Wetland Boundary Wetland Buffer NOTE Map adapted from aerial imagery provided by Google Earth Pro, reproduced by permission granted by Google Earth Tm Mapping Service. APPENDIX A WETLAND DELINEATION METHODOLOGY N 6WLSON,I 21-1-22082-002 APPENDIX A WETLAND DELINEATION METHODOLOGY TABLE OF CONTENTS Page A.1 WETLAND VEGETATION.......................................................................................... A-1 A.2 HYDRIC SOILS ............................................. ...................,.................................... A-3 A.3 WETLAND HYDROLOGY .......................... ........ .................. ........ ................ A-3 A.4 DISCLAIMER....................................................................... __............... ................. A-4 A.5 REFERENCES ........................... ........................... ....... ...---..............,... A-4 A-1 Definitions of Plant Indicator Status....... ..__.. ....,.... ............ ........ A-2 AppoudixA'Methodology (Westem Mens) Dec 2012/ A -i 21-1-22082-002 APPENDIX A WETLAND DELINEATION METHODOLOGY The triple -parameter approach, as required in the Washington State Department of Ecology's (Ecology's) 1997 Washington State Wetlands Identification and Delineation Manual, the United States Army Corps of Engineers' (the Corps') 1987 Corps of Engineers Wetland Delineation Manual, and the Corps' 2010 Regional Supplement to the Corps of Engineers Wetland Delineation Manual: Western Mountains, Valleys, and Coast Region (Version 2.0) was used to identify and delineate the wetlands on the site described in this report: The triple -parameter approach requires that vegetation, soils, and hydrology are each evaluated to determine the presence or absence of wetlands. An area is considered to be a wetland if each of the following is met: (a) dominant hydrophytic vegetation is present in the area, (b) the soils in the area are hydric, and (c) the necessary hydrologic conditions within the area are met. A determination of wetland presence was made by conducting a Routine Delineation. Corresponding upland and wetland plots were recorded to characterize surface and subsurface conditions and more accurately determine the boundaries of on-site wetlands. A.1 WETLAND VEGETATION Hydrophytic plants are plant species specially adapted for saturated and/or anaerobic conditions. These species can be found in areas where there is a significant duration and frequency of inundation, which produces permanently or periodically saturated soils. Hydrophytic species, due to morphological, physiological, and reproductive adaptations, have the ability to grow, effectively compete, reproduce, and thrive in anaerobic soil. Indicators of hydrophytic vegetation are based on the wetland indicator status of plant species on the national wetland plant list (Lichvar, 2012). Plants are categorized as Obligate (OBL), Facultative Wetland (FACW), Facultative (FAC), Facultative Upland (FACU), or Upland (UPL). Species in the facultative categories (FACW, FAC, and FACU) are recognized as occurring in both wetlands and non - wetlands to varying degrees. Most wetlands are dominated mainly by species rated as OBL, FACW, or FAC (Table A-1). AppendixA_Methodology (Western Mtns)Dec 2012/ 21-1-22082-002 A-1 TABLE A-1 PLANT INDICATOR STATUS GROUPS Plant Indicator Status Categories Obligate Wetland (OBL) — Plants that almost always occur in wetlands. Facultative Wetland FACW Plants that usually occur ( ) — y �in wetlands, but may occur in non -wetlands. ..... ........ . (...... e FAC)...._� — FacultativPlants that occur in wetlands or non -wetlands. Facultative Upland (FACU) — Plants that usually occur in non -wetlands, but may occur in wetlands. _. ._....... ._....... Obligate Upland (UPL) — Plants that almost never occur in wetlands. (Lichvar, 2012) The approximate percentage of absolute cover for each of the different plant species occurring within the tree, sapling/shrub, woody vine, and herbaceous strata was determined. Trees within a 30 -foot radius; sapling/shrubs and woody vines within a 15 -foot radius; and herbaceous species within a 5 -foot radius of each data point were identified and noted. However, where site conditions merited it, the dimensions of the tree, sapling/shrub, woody vine, and herbaceous strata were modified. The dominance test is the primary hydrophytic vegetation indicator and it is used in all wetland delineations. Dominant plant species are considered to be those that, when cumulatively totaled in descending order of absolute percent cover, exceed 50 percent of the total absolute cover for each vegetative stratum. Any additional species individually representing 20 percent or greater of the total absolute cover for each vegetative strata are also considered dominant. Hydrophytic vegetation is considered to be present when greater than 50 percent of the dominant plant species within the area had an indicator status of OBL, FACW, or FAC. If a plant community does not meet the dominance test in areas where hydric soils and wetland hydrology are present, vegetation is reevaluated using the prevalence index, plant morphological adaptations for living in wetlands, and/or abundance of bryophytes (e.g., mosses) adapted to living in wetlands. The prevalence index is a weighted average that takes into account the abundance of all plant species within the sampling area to determine if hydrophytic vegetation is more or less prevalent. Using the prevalence index, all plants within the sampling area are grouped by wetland indicator status and absolute percent cover is summed for each group. Total cover for each indicator status group is weighted by the following multipliers: OBL=1, FACW=2, FAC=3, FACU=4, UPL=5. The prevalence index is calculated by dividing the sum of the weighted totals by the sum of total cover in the sampling area. A prevalence index of 3.0 or less indicates that hydrophytic vegetation is present. AppendixA_Methodology(WestemMWs)Dec 2012/ 21-1-22082-002 A-2 A.2 HYDRIC SOILS Hydric soils are defined as soils that formed under conditions of saturation, flooding, or ponding long enough during the growing season to develop anaerobic conditions in the upper part (USDA SCS, 1994). Repeated periods of saturation and inundation for more than a few days, in combination with soil microbial activity, causes depletion in oxygen (anaerobic conditions) and results in delayed decomposition of organic matter and reduction of iron, manganese, and sulfur elements. As a result of these processes, most hydric soils develop distinctive characteristics observable in the field during both wet and dry periods. (USDA MRCS, 2010). These characteristics may be exhibited as an accumulation of organic matter; bluish -gray, green -gray, or low chroma and high value soil colors; mottling or other concentrations of iron and manganese; and/or hydrogen sulfide odor similar to a rotten egg smell. The USDA Natural Resources Conservation Service (MRCS) has developed official hydric soil indicators as summarized in Field Indicators of Hydric Soils in the United States (USDA NRCS, 2010). These indicators were developed to assist in delineation of hydric soils and are based predominantly on hydric soils near the margins of wetlands. Some hydric soils, including soils within the wettest parts of wetlands, may lack any of the approved hydric soil indicators. If a hydric soil indicator is present, the soil is determined to be hydric. If no hydric soil indicator is present, additional site information is used to assess whether the soil meets the definition of hydric soil. Identification of hydric soils was aided through observation of surface hydrologic characteristics and indicators of wetland hydrology (e.g., drainage patterns). Soil characteristics were observation at several data points, placed both inside and outside the wetland. Holes were dug with a shovel to the depth needed to document an indicator or to confirm the absence of hydric soil indicators. Soil organic content was estimated visually and texturally. Soil colors were examined in the field immediately after sampling. Dry soils were moistened. Soil colors were determined through analysis of the hue, value, and chroma best represented in the Munsell® Soil Color Chart. A.3 WETLAND HYDROLOGY Wetland hydrology is determined by observable evidence that inundation or soil saturation have occurred during a significant portion of the growing season repeatedly over a period of years so that wet condition have been sufficient to produce wetland vegetation and hydric soils. Wetland hydrology indicators give evidence of a continuing wetland hydrologic regime. Wetland hydrology criteria were considered to be satisfied if it appeared that wetland hydrology was AppendixA_Methodology (Westem Mtns) Dec 2012/ A-3 21-1-2.2082-002 present for at least 5 to 12.5 percent (12 to 31 days) of the growing season. The growing season in western Washington is typically considered to be from March 1 to October 31 (244 days). However, the growing season is considered to have begun when: (a) evidence of plant growth has begun on two non -evergreen vascular plants, and (b) the soil reaches a temperature of 41 degrees Fahrenheit at 12 inches. The Seattle District Corps of Engineers requires 14 consecutive days of inundation or saturation for a wetland hydrology to be considered present. Wetland hydrology was evaluated by direct visual observation of surface inundation or soil saturation in data plots. The area near each data point was examined for indicators of wetland hydrology. Wetland hydrology indicators are categorized as primary or secondary based on their estimated reliability. Wetland hydrology was considered present if there was evidence of one primary indicator or at least two secondary indicators. Some primary indicators include surface water, a shallow water table or saturated soils observed within 12 inches of the surface, dried watermarks, drift lines, sediment deposits, water -stained leaves, and algal mat/crust. Some secondary indicators include a water table within 12 to 24 inches of the surface during the dry season; drainage patterns; a landscape position in a depression, drainage, or fringe of a water body; and a shallow restrictive layer capable of perching water within 12 inches of the surface. A.4 DISCLAIMER This methodology was prepared for reference use only and is not intended to replace Ecology's 1997 Washington State Wetlands Identification and Delineation Manual, the 1987 Corps of Engineers Wetland Delineation Manual, or the Corps' 2010 Regional Supplement to the Corps of Engineers Wetland Delineation Manual: Western Mountains, Valleys, and Coast Region (Version 2.0). A.5 REFERENCES Munsell Color, 1992, Munsell soil color charts: Newburgh, N.Y., Macbeth Division of Kollmorgen Instruments Corporation, 1 v. Lichvar, R. W., 2012, The national wetland plant list: U. S. Army Corps of Engineers Engineer Research and Development Center, Report ERDCC/CRREL TR -12-11, 224 p., available: http://rsgisias.crrel.usace.anny.mil/NWPL/doc/proc 2012/ERDC-CRREL TR -12-11 NWPL 2012.pdf. AppendixA_Methodology(WestemMtw)Dec 2012/ 21-1-22082-002 A-4 U.S. Army Corps of Engineers Engineer Research and Development Center, 2010, Regional supplement to the Corps of Engineers wetlands delineation manual: western mountains, valleys and coast region, Version 2.0: Vicksburg, Miss., U. S. Army Corps of Engineers Engineer Research and Development Center, Report ERDC/EL TR -10-3, 153 p. U.S. Army Corps of Engineers Waterways Experiment Station, 1987, Corps of Engineers wetlands delineation manual: Vicksburg, Miss., U.S. Army Corps of Engineers Waterways Experiment Station, Wetlands Research Program Technical Report Y-87-1, 143 p., available: http://www.wli.nres.usda.gov/delineation/. U.S. Department of Agriculture (USDA) Soil Conservation Service (SCS), 1994, Changes in hydric soils of the United States: Washington, D.C., Office of the Federal Register, FR 59 (133): 35680-35681, July 13. U.S. Department of Agriculture (USDA) Natural Resources Conservation Services (MRCS), 2010, Field indicators of hydric soils in the United States, Version 7. 0, L.M. Vasilas, G.W. Hurt, and C.V. Noble (eds.), USDA, NRCS, in cooperation with the National Technical Committee for Hydric Soils. Washington State Department of Ecology, 1997, Washington state wetlands identification and delineation manual: Olympia, Wash., Washington State Department of Ecology, Report 96-94. AppendixA_Methodology (Western Mtns) Dec 2012/ 21-1-22082-002 A-5 HN, I APPENDIX B WETLAND DETERMINATION DATA FORMS - WESTERN MOUNTAINS, VALLEYS, AND COAST REGION 21-1-22082-002 WETLAND DETERMINATION DATA FORM – Western Mountains, Valleys, and Coast Region v Pro ecUSlte: i Cltyl'ounN"° �r dSamPling Date: AI Stale sanP I0 Point: fi .. Investlgator(a): t � �� 1 t S rcN:goat ToRang® wnship, Landform (hillslope, terrace, etc. Local (concave convex, none): ��4„ Slope (%)"..L;." Subregion (LRR): Let Long: Datong"_ Soil Map Unit Name: .. ... NWI classl(Jcalion ........ � Are climatic f hydrologic condlitons on The site typical for this time of year? Yes� °� No � (If no, explain in Remarks.) Are Vegetation , Soil , or Hydrology significantly disturbed? Are "Normal Circumstances" present r Yes Nc Are V etaiion .Soil . of Hydrology naturally problematic? (If resdad. explain any answers inRemarks.) SUMMARY OF FINDINGS – Attach site map Showing sampling point locations, transects, Important features, etc. Hydrophytic Vegetation Present? Yrs -�. Nor Hydric Soil Freaenl? Yes filo Is the Sampled Area within a Wetland? Yen No Wetland Hydrology Present? Yes No VEGETATION – Use scientific names of plants. Absolute Dom, inant Indicator (Plol Site _ J ° l- 4 o r i Total Cover (Plot ixe:„, 3, 4.— Tot—at Cover H � � (I t 2.rt,wi 4 — - www_..., 7. o Al 9. ta. 11. 00 = Total Cone: !v Vine *° (Plot ) t � 2_ ,= Total Cover % Bare Ground in Herb Stratum d��r��"i y. � �'�� m;,� �.•4� ��..�,l�N�'�p'a„e �t,�Ndi r�r,�p�i� Dominain o Test Worl(sheal Number of Dominant Spode$ That Aron OBL, FAC01, or p'AC: ( } Total Number of Dominant�rl Species Across All Strata!w. (ft) Percent of Dominant Species a( That Are DBL, FACW, or FAC. Total % Cover of:hw - L species xi. FACW species x 2 + FAC species x 3 FACU species X4. UPL species Column Totals: (A) ) .. (B) Prevalence Index = B/A= Hydrophytle Vagatallon lodloaiorsw _ 1 - Rapid Test for Hydrophytic Vegetation 2 - Dominanoe Test is >60% _ 3 - Prevalence Index Is s3.0' _ 4 - Mor°pbotogical Adaptations' (Provide supporting data in RenI or on a separate shoot) _ 5-'iVetlsnd Non -Vascular Plants' _ Problematic Hydrophytle Vegetation' (Explain) ' indicators of hydric soll and wetland hydrology must be present, unless disturbed or problematic, Hydroystlytic Vootation Present? Yea -��,.. ,,_. No ... US Army Corps of Engineers Westem Mountains, Valleys. and Coast – Version 2.0 SOIL W — Water -Stained Leaves (89) (except — Water-Shilned Leaves (BB) (MLRA 1, 2, Sampling Paint-, P(0fJlQD0%CFI IV (OpSerbo to the depth needed to documoilt the Indicator or conifirrij if fn�Tl . . ....... Depth Saturation (A3) — Sall Crust (1311) — Drainage Patterns (810) Water Marks (1311) — Aquatic Invertebrates (1313) — Dry -Season Water Table (C2) Sediment Deposits (B2: — Hydrogen Sultda Odor (Cl) — Saturation Visible on Aerial Imagery (C9) Delft Deposits (1213) Oxidized Rhizospheras along Living Roots (C3) , SAW Grains, .')(qaj08 ed or Cooled ........ . . Hydric Soil lndlcatorw. (Applicable to all LRRs, unless otherwise noted.) Indicators for Problematic Hydric Salle: HIsInsal (Al) Sandy Redox (S6) — 2 orin Muck (Al D) Hisbc Enipeclon (A2) Stripped Matrix (S6) — Red Parent Material (TF2) ..,•••.. Black Histic (A3) Loamy Mucky Mineral (FI) (except MLRA 1) — Very Shallow Dark Surface (TF12) — I-lydrogen Sulfide (A4) Loamy Gleyed Matrix (F2) Other (Explain in Remarks) — Depleted Below Dark Surface (Ail) ­ Depleted Matrix (173) — Thick Dark Surface (Al 2) — Redox Dark Surface (176) 31ndlcators of hydrophyfic vegetation and — Sandy Mucky Mineral (Si) Depleted Dark Surface (F7) welland hydrology must be present, — Sandy Glayed Matrix (S4) _K661101" �mayor Redox Depressions (178) unless disturbed or problarnatic. (lf Present). Type, Depth (irtzher.): Hydric Soil Present? Yee No f, Ilk L I �j HYDROLOGY PrflmSurFaca Water (Ai) — Water -Stained Leaves (89) (except — Water-Shilned Leaves (BB) (MLRA 1, 2, High Water Table (A2) MLRA 1, 2, 4A, and 4131 4A and 40) Saturation (A3) — Sall Crust (1311) — Drainage Patterns (810) Water Marks (1311) — Aquatic Invertebrates (1313) — Dry -Season Water Table (C2) Sediment Deposits (B2: — Hydrogen Sultda Odor (Cl) — Saturation Visible on Aerial Imagery (C9) Delft Deposits (1213) Oxidized Rhizospheras along Living Roots (C3) _ Geornorphlc Position (132) Algal Mat or Crust (84) Presence of Reduced Iran (C4) — Shallow Aquilard (D3) Iron Deposits (B5) Recent Iron Reduction in Tilled Sails (C6) — FAC -Neutral Test (135) Surface Soil Cracks (198) Stunted or Stressed Plants (Di) (LRR A, — Raised Ant Mounds (DG) (LRK A) Inundation Visible on Aerial Imagery (B7) Other (Explain in Remarks) — Frost -Heave Hummocks (07) SP21601y Vege(aled Concave Surface (138) Surface Water Present? Water Table Present? Saturation Presard? Yes ­ No Vie„ Depth (Inches): Y03 — No Depth (inches): -- ­ Yes — No, Depth (Inches): � Welland Hydrology Present? Yes _ No gauge, al aortal ptiolos, previous inspection J 4. US Army Corps of Engineers Western Mountains, Valleys, and Coast –Version 2.0 1NETI.AND DETERMINATION DATA FORM - Western Mountains, Valleys, and Coast Region ,w _ v h+ �'p,m ; I 1 ,11 ��JaLV" f—I' e I " ssi Clll Icoun ' i td'"bit ow � t + S YmpRNntt Da ProecUSlte: ' Appllcantowner i��1 � ,�� r wl � r t .tip^ t tit late t � �� ad wpllatg� Pglnt .m �" ' "° lnvesti alio's . .. �•.�tc'.): olion, Township, Range:Landform (hillslope, t®rrate, ��, l ��n,�,,�_.,� Local relief (concave, convex, no e}: Slope (%): Subregion (LRR)-. ,,tl" � Lai. � "ng:,„ alum Sall Map Unit Name: co NWI classification: � 4`^.� 't Are cllmallo I hydrologic conditions an Melte typical for this We of year? Yes No (If no, explain In Remarks.) Are Vegetation , Soil or Hydrology significantly disturbed? Are "Norrnal Circumstances" present? Yes No Are Vegetation , $oail or Hydrology naturally problematic? (If needed, explain any answers in Remarks.) SUMMARY OF FINDINGS - Attach site map showing sampling point locations, transects, important features, etc. Hydrophytic Vegetation Present? Hydric Sail Present? Welland Hydrology Present? 'yes, No "Iris .� No 'yes No VEGETATION -Ilse scientific naMes of plaints. Is the Sampled Area rrlthin a Wetland? (�W .r'rl {Plot size; ", ) nosoiu)ra Laor�nan¢ mowamr l"ireera a ll? lie 1. ._�.a2. I (� t" iPM^t0i Ns _ _n C i 10 3. FA 4 Total Cover � i {,Ptrtt Sita � 1• �.I t �""��,� rlc � �r �rw a 'Na�'k� '� r" m.. � "�ri ,-..�. f '.. u 4. tau rR f" 5• .. _.. ., .,,., __ .., _. — = Total Cover —fturf (Plot size: ) 1. ,000 °I i0l i (A u; )wj,,rc 2.w� 3. 't t' t.. 4. 5_ tdl�� d"° I •x FAr B. 7_ t3- 10. . 1 ")° m- 1 Total Cover lriv Vlrte Str {Plot size 2e lP l % Bare Ground In Herb Stratum Yes ,," x2a No x3= x4 x5 Dominance Testworksrteet; Number of Dominent Species That Are OBL, FACW, or FAC, Total Number of Dominant Species Across All Strata; Percent of Dominant Species That Are DBL, FACW, or FAC DBL species FACW species FAC species FACU species UPL species Column Totals: x 1, = ,," x2a x3= x4 x5 Index -B/A= �1P .- Provalanoe 0 hit—lo Vetatiott indlcatarsh 1 - Rapid Test for HydrophyUc Vegetation _ 2 - Dominance Test Is >50% _ 3 - Prevalence Index Is s3,0' 4 - Morphological Adaptations' (Provide supporting data in Remarks or on a separate sheet) _ 5 - Welland Non -Vascular Plants' _ Problematic Hydrophytic Vegetation' (Explain) 'indicators of hydric soil and wetland hydrology must be present, unless disturbed or problematic. Hydrophytic , / Vagatatlon �J Present? Yes No US Army Corps of Engineers Western Mountains, Valleys, and Coast — Version 2.0 SOIL Sampling Point" Profile Description: (Describe to the depth needed to dci.6 rant the Indicator or confirm the a %ionco of Indicalom.) Dep – C Chea] xatu Redox Feresa� � Surface Water (Al) _ Water-Stalned Leaves (69) (except _ Water-Slalned Leaves (B9) (MLIZA 1, 2, _ High Water Table (A2) MLRA 1, 2.4A, and 46) A � IIS. T �Mdld rr t C onrcowtralio. MO"�tl ? )r t xi f r tt (l Nwc, CC rr rr w r�r oadeti S�ar� w 6 kacaflonPL- oLninwNhA il,'x, Ykar. Hydric Soil Indicators: (Applicable to all LRRs, unless otherwise noted. -- H drlc SoIW _ Histosol (Al) - _ Sandy Redox (SS) _ 2 cm Mucic (A10) — Hislic Eplpedon (A2) _ Stripped Matrix (S8) Red Parent Material (72) _ Black Histic (A3) _ Loamy Mucky Mineral (F1) (except MLRA 1) ,.._, Very Shallow Dark Surface (TF 12) Hydrogen Sulfide (A4) _ Loamy Gleyed Matrix (F2) — Other (Explain in Raaxarks) _ Depleted Below park Surface (A11) Depleted Matrix (F3) _ Stunted or Stressed Plants (D1) (LRRA) Thick Dark Surface (Al 2) Redox Dark Surface (F6) 'Indicators of hydrophytic vegelstlon and _ Sarxly Mucky Mineral (Si) � Depleted Dark Surface (F7) wetland hydrology must be present, Sandy Gleyed Matrix (S4) Redox Depressions (F8) unless disturbed or problematic_ ..Restrietiva Layer(ff prrisenlj: _.._._...__.. _...... .�..,_...��.,�,„.„,�,�,�-..__.----_._ _ _.... Depth (Inches). Hydric 8011 Present? Yes Wo Remarks:. FA HYDROLOGY _... Welland Hydrology Indicators: Primary Indirarnm Iminirmim of nna rani�lrnrt qll that anorvl Surface Water (Al) _ Water-Stalned Leaves (69) (except _ Water-Slalned Leaves (B9) (MLIZA 1, 2, _ High Water Table (A2) MLRA 1, 2.4A, and 46) 4A, and 4B) Saturation (43) _ Salt Crust (B1 I) _ Drainage Patlerns (610) _ Water Marks (a1) _ Aquatic Inyerts0rates (813) _ Dry -Season Water Table (02) _.._ Sediment Deposits (132) _ Hydrogen Sulfide Odor (C1) _ Saturation Visible on Aerial Imagery (CO) _ Drift Deposits (83) _ Oxidized Rhlzospheros along Living Roots (C3) _ Geomorphlc Position (02) Algal Mat or Crust (134) _ Presence of Reduced Iran (C4) Shallow Aquilard (133) _ Iron Deposit; (136) Recent Iron Reduction in Tilled Soils (C5) _ FAC -Neutral Test (65) _ Surface Soil Cracks (B61 _ Stunted or Stressed Plants (D1) (LRRA) _ Raised Ant Mounds (D®) (LRR A) _ Inundation Visible on Aerial Imagery (B7) _ Other (Explain in Remarks) _ Frost -Heave Hummocks (137; Snarsely Veaetated Cencave Surface i8a) Surface Water Present? Yes No ;Vj� Depth (Inches): Water Table Present? Yes No Depth (inches): Saturation Present? Yes No Depth (inches): gauge, Wetland Hydrology Present? Yes No LS Army Corps of Engineers Wastem Mountains. Valleys, and Coast –Version 2.0 WETLAND DETERMINATION DATA FORM - Western Mountains, Valleys, and Coast Region Sarnnii— Date: ------------ CitylGounty. state: \0 Sam ling Point: j Section, Townaw'p. Landform (Irill1slope, ierr ce, etc.): convex. nona). 69 V1 ' J Slope Subregion (LRR):Let: Long: Datum: Sall map Unit Name" Are climatic I hydrologic cordlOons on .he site typical lor.this Urne of year? Yes t,0 (if no, explain In Remarks.) Na Are Vegetation —, Sall _, or Hydrology _ significantly disivrbed?AYes lo Are *Notmel Circumstances" present? ZA_ Are Vegetation Soil. or Hydrology —naturally problemaficlAji) (if needed, explain any answers In Remarks.) SUMMARv�elF�iNDIrN GS - Attacsitonap showl ng sampling point locations, transSCU, Important features, etc. Hysent? Yes No Hydric Soil Present? Yes o'c"No Is the Sampled Area Weiland Hydrology Present? Yes No within a Wetiand? Yes No VEGETATION - Use sclentifle names of plants. Number of Dominant Species (Plot size: _ -.I That Are 08L, FACVY' 'or FAC, (A) Total Number of Dominant -%LWM Species Across At I Strata: X3= Percent of Dominant Species C 2, -.21 . ....... Column Totals: (A) 4. 3(n, m Total Cover 2. ............ . 3. 4. S. k--) Total Cover (Plot size ftfkly" 2 2, 3. 10 � �fO �A �' 4. 4— ILCO 7. . . . ..... 10. Total Cover (plot size: . ........ . ...... 2, % Bare Ground In Herb Stratum Total Cove, . ..... — Number of Dominant Species MUNIDly bw That Are 08L, FACVY' 'or FAC, (A) Total Number of Dominant X2= Species Across At I Strata: X3= Percent of Dominant Species C That Are OBIL, FACK or FAQ 11� (AIB) 1Q1aL%-Q0yQLQL— MUNIDly bw OBL species x 1 0 FACW SpecleS X2= FAC species X3= FACU species X4= UPIL species X5= Column Totals: (A) Prevalence Index - BiA - 1 - Rapid Test for Hydrophytic Vegetation �K2 - Dominance Test Is >5,0% 3 - Revalonce Index Is OV' 4 - Morpbotagical Adaptations' (Provide suppodlng data In, Remarks or on a separate shoat) 8 - Welland Non -Vascular PIsnts' Problematic Hydrophytlu Vegetation' (Explain) 'Indicators of hydric Boll and watiand hydrology Must be present, unless disturbed or problernativ. Hydrophytic Vegetation Present? Yea —zlillo— US Army Corps of Engineers Western Mountains, Valleys, and Coast — Version 2.0 SOIL ,u d � f � ul' 0 � �, , I�o Q';.M ,�,.•Wnr'a � l4� l"" ! i V { ,�,'+ �V ,.4i "� � � � � ° I�.8 �'^�'��i "" Ntt I 1 Sampling Pointy „_ .. _ a� scrl tions Liaascrttao to the de th nyy��eaelerpJ t I rotate the a �..p�.�.. °docr'r�rrttthalrttlioattsr� dnllrnn e f Indicato.rs.,,) fi�_�.._ � �� w...� e abse�nc�o Depth flnobe6I—a.�. .p�l_ { ppyyo�y p r�'�.,irv'rfi II u ._....-- � ,' LQLQU � , surface water{A1) � VJ ater-Stained Leaves (89) (except _ Weter-Stained Leaves (139) (MLRA 1, 2, ® High Water Table (A2) MLRA 1, 2,4A. and 48) / 4A, and 413) .. _ Salt Crust (Bi 1) k Draklove Patterns (B10) (61) i , �Ap-�M �... j�u 0 • '�'"��� ..........e....—.,... 'urs — I F nn Hydric Soil indicators: (Appllcabie to all LR12s, unless peherwlse noted. _ Hislosol (Al) _ Sandy Redox (SS) Hislic Ppipedcn (A2) _ Stripped Matrix (SB) Black Hisllc (µ3) —Loamy Mucky Mineral (171) (except MLRA 1) _ Hydrogen Sulfide (A4) _ Loamy Glayad Matrix (172) _ Depleted Below Dark Surface (All) Depleted Matrix (F3) Thick Dark Surface (Al 2) Redox Dark Surface (176) _ Sandy Mucky Mineral (Si) Depleted Dark Surface (F7) Sandy Gleyed Matrix (84') � Redox Depressions {,F$) w� ... _ .. Restrictive Layer (tf prosent), Type: ...... �..� �... .. ��ww ��..._� Depth (Inches): for 2 cm Muck (A10) _ Red Parent Material (TF2) _ Very Shallow Dark Surface (TF12) _ Cdher (Plain In Remarks) 'Indicators of hydrophylic vegetation and wetland hydrology must be present, unless disturbed or problematic. Hydric sou Present? You _ Na A n m _➢ ea ,u d � f � ul' 0 � �, , I�o Q';.M ,�,.•Wnr'a � l4� l"" ! i V { ,�,'+ �V ,.4i "� � � � � ° I�.8 �'^�'��i "" Ntt I ✓" n b . HYDROLOGY 1th!"o d Hydrology Indleators: ._....-- � ,' LQLQU � , surface water{A1) � VJ ater-Stained Leaves (89) (except _ Weter-Stained Leaves (139) (MLRA 1, 2, ® High Water Table (A2) MLRA 1, 2,4A. and 48) / 4A, and 413) Saturation (A3) "gator Masks _ Salt Crust (Bi 1) k Draklove Patterns (B10) (61) _ Aquatic Invertebrates (1313) _ Dry -Season Water Table (C2) Sediment Deposits (132) Hydrogen Sulfide Odor (Ci)_ Saluratlon Visible on Aeflal Imagery (C9) Drift ® sits (83) _ Oxidized Rhlzospheres along LWnq Roots (C3) ✓Gaornorphlc Position (1)2) Algal Mat or Crust (134) _ Presence of Reduced Iron (C4) _ Shallow Aqultard (03) Iron Deposits g 5) _ Recent Iron Reduction in Tilled Salle (Ca) i FAC -Neutral Test (D5) Surface Soil Cracks (BB) _ Stunted or Stressed Plants (D1) (LRRA) _ Raised Ant Mounds (D8) (LRRA) )nundarllDn Mel s on Aerial Imagery (137) _ Other (Explain In Remarks) _ Frost -Heave Hummocks (07) ®°Spnrsepy Vawgetaat r�nroaBo St'aca (__) ..._,. Field Clbaenrattons: _�_ .............e.......,�.�.,.,.�._.._»..�,..., . .... _ Surface Water Present? Yea No 4 Depth (Inrshns), Water Yes Saturation Present? No` 'Depth (Inch l? Yes (Iraolw,tdes capillary frtra No Depth (Inoh)Y res)° Wetland Hydrology Present? Yes No Describe Racordoa l3 Ia {strt�arcan gauge, mcnitonng Wall, aortal photos, croutons Insrxaotlons9, If aavaCtbt la: I (�°�)✓��iiP' ui'i��F 41 ^,r, �� �`"I� � �i � n 0,° I' US Army Corps of Engineers 1Womern Mountains, Valleys, and Coast – Version 2.0 WETLAND DETERMINATION DATA FORM — Western Mountains, Valleys, and Coast Region CyfCounty.� Sampling Da.te Applicant/Owner, r r� State: Samp�Point: Sechon, Tow nshto, Range ' �...�..µ.... .. Inuestl oto s : Local relief (concave, convex, none). » ��, or'+� " - Shops om, Landform (hlllslape, ien-ace, etc.)'. W.„„„". ..__,.,�„„�.,„„� Subregion LRR �.q.. Lang' �,...NVVI classifi Datum: Soil Ma Unit Name 8g ( a �„�~�I �.,.. � cation: Are climatic! hydrologic conditions on the site typical for,this time of year? Yes „t. p _ Nc,„-„ ,.- (If no, expialn In Remarks,) Are Vegetation , Sail , or Hydrology significantly disturbed? Are °"Notmal ClrcumatanceV present? Yes No Are Vegetation . Soil or Hydrology naturally problematic? (If headed, explain any answers in Remarks,) SUMMARY OF FINDINGS — Attach site MAP showin .eampling point locatlons, transects, important features, etc. Hydr+ophytic Vegetation Present? Yes No m t Hydrtc Sop Present? Yes No "�,� ` Is the Sampled Area t Weiland Hydrology Present? Yes No within a wetland? Yes - No Rernarlls: VEGETATION — Use scientific names of plants. _ .m AAbsoiga...o Da, ,� �-� NurtiberofDoostwoSih rg trrtturn (Plot Saxe: � 1� ln1tRMtoK- f�umbern�o orni at SP960t3 e t� I1. That Are 13L, f A o or FAC: (A) 2 ”~� �0 (',i .M Total Number of Dornlnant r 3. _.. i Species Across All Strata: (3) 4. _.... _....�__�.�.-. I_ e Total Cover h t (Plo° size: 2. . ..... .-, 3.-_ 4. fi.-.e..... ..... ... 9" Total Cover 1 lttt (Plot size' ..... _ _...1 _ ...�—------.._ 2, ........ r, _.� ......r.."w�. _ .... ....... 8. ine Stratum Total Co VPlot slze l ver Worly 2. 0 Total Cover % Bare Ground In Herb Stratum Percent of Dominant Species 0 That Aro 08L, F'ACW, or FAIN. (A/B) 1 - Rapid Test for Hydrophytic Vegetation _ 2 - Dominance Test Is >50% — 3 - Prevalence Index Is 53.0' _ c - morphological Adaptations' (Provide supportin6 data in Renrarkf4 or on a soperats sheat) _ 8 - Wetland Non -Vascular Plants' _ Problematic; Hydrophylic Vegetation' (Explain) rlrxllcators of hydric sail and wetland hydrology must be present, unless disturbed or problematic. Hydrophytic Vegetation Present? Yes No US Amey Corps of Engineers Western Mountains" Valleys, and Coast - Version 2.0 h- 081. specles FACWspecies� x2� FAC species�.W, x. S _._. " ' _r FACU species r x 4 LIPL species x 3,. ( . Column Totals: (A) (B) 3 a Prevalence Index ' SIA e Ftirrlircrotnvtic Vaaetaiton Indlsaioy^a» 1 - Rapid Test for Hydrophytic Vegetation _ 2 - Dominance Test Is >50% — 3 - Prevalence Index Is 53.0' _ c - morphological Adaptations' (Provide supportin6 data in Renrarkf4 or on a soperats sheat) _ 8 - Wetland Non -Vascular Plants' _ Problematic; Hydrophylic Vegetation' (Explain) rlrxllcators of hydric sail and wetland hydrology must be present, unless disturbed or problematic. Hydrophytic Vegetation Present? Yes No US Amey Corps of Engineers Western Mountains" Valleys, and Coast - Version 2.0 SOIL to the depth neodoO to document the Indicator or con'flrm the, absence L�Sampling Pdinl-1�rd��^ Depth _taairrs ti - -moa K49Q" .. � I� � � n , r � r I l ' . I I i" IT.. d Hydric Soil Indicators: (Applicable to all MRs, unless otherwise noted.) _ Histosol (Al) _ Sandy Redox (S5) _ Histio Eplpedon (A2) _ Stripped Matrix (S6) Black Histic(A3) — Loamy Mucky Mineral (F1) (except MLRA 1) Hydrogen Sulfide 04) _ Loamy Gleyed Matrix (F2) Depleted Beloo Dark Sur'ace (All) _ Depleted Matrix (F3) Thick Dark Suiace (Al2) — Redox Dark Surface (F6) — Sandy Mucky Mineral (S1) Depleted Dark Surface (F7) — Sandy Gieyed Matrix (84) Redox Depressions (F'tt) Restrictive Layer (iipresent): Surface Soil G-acks (B6) Type:.�................��_W....�,,,, �....�......_�.. ...�. Depth (Inches):, HYDROLOGY Indicators for Problematic Hydric Sr _ 2 cm Muck (A10) Red Parent Material (TF2) _ Very Shallow Dark Surface (TF12) Other (Explain In Remarks) Indicators of hydraphytic vagelation and vtalland hydrology musl be present, unless disturbed or umbiemalic. Hydric Soil Prosent? Yes No ° Primary Indlrminrc of one rewired: check all rhai annlvl _ Surface Water (All _ Water -Stained Leaves (139) (except — High Water Table (A2) MLRA 1, 2,4A, and 4B) _ Saturation (A3) _ Sarlt Crust (8 11) _ Water Marks (B1) ` Aquatic Invertebrates (613) _ Sediment Deposits (82) _ Hydrogen Sulfide Odor (Cl) _ Drill Deposits (63) _ Oxidized Rhlzoapheres along Living Roots (C3) _ Algal Motor Crust (134) Presence of Reduced Iron (C4) _ Iron Deposits (135) _ Recent Iron Reduction In Tlllec Solis (CQ) Surface Soil G-acks (B6) _ Stunted or Stressed Plants (D') (LRR Al _ Inundation Visible on Aerial Imagery (W) _ Other (Explain In Remarks) Spartse4y Vanararrvl Concave Curfa— MRS Surface Water Present? Yes No –;zp Depth (Inches): Water Table Present? Yes No Gpth (Inches): Saturation Present? Yes No Depth (Inches): ueascrioa a,cocuv asc Mata (sttoam gauge, monitoring wall,, aerial photos, previr Ir Rfitmtlt3" ; r'tttef.("JA' "'l IdJS Army Co" of Engimot, tib, _ Water-Stalned Leaves (89) (MLRA 1, 2, 4A, and 48) Drainage Patterns (1310) _ Dry -Season Water Table (C2) Saturation Visible on Aerial Imagery (Cg) Geomorphic Position (02) _ Shallow Aqultard (D3) FAC-Nautral Test (D6) _ Raised Ant Mounds (136) (LRR A) Frost -Heave Hummocks (D7) Wetland Hydrology present? Yes No Western Mountains, Valleys, and Coast –Versior 2.4 WETLAND DETERMINATION DATA FORM — Western Mountains, Valleys, and Coast Region PraiecUSlte:0. r M" C ityPCou � " �, my �late, �, mpung pow:--- Applicantl9tar>er � t -�-- -. r�r t Investigator(s): (C�' Section Township, Ranga dam (hilFtpe, etc,}: Local etlef (concim, convex, none). DSlope Sube9 % R}. 7 Vit. Lon , (Y 1 NVVI classifioetlon: Soil Map UnUngName. Are dimatic I hydrologic condillons on the site typical for this time of year? Yes - No (If no, explain In Remarks.) Are Vegetation Soil or Hydrology significantly disturbed? Are %omisl Circumstances" present? Yes, :.°, two ..w....._..... Are Vegetation Soil or Hydrology naturally problematic? Of needed, explain any answers In Remarks.) SUMMARY OF FINDINGS — Attach site map sho irtg sampling point locations, transects, Important features, etc. Hydrophytic.Vegetabon Present? Yes No __;rL Hydric Soil Present? Yes No Is the Sampled Area Wetland Hydrology Presenl7 Yee No ...._may within a Wetland? Yes o VEGETATION — Use scientific names of plants. (Plot slze 2.� J 77 7 r 4. ".._ ���.... u D m Total Cover ���"... 2. (d I, �m � 12 +� Total Cowr itt�irints,Iaa_ G .. 1 11 I 2.. 4. 7._.�. _r....v.—----................_�- a i i. -"""-i Total Cover tl-. ,� er (Plot daze �� cr 2. Total Cover % Bare Ground In Herb Sbaturn Number of Dominant Species That Are OBL, FACW, or FAC: (A) Total Number of Dominent + " Spades Across All Strata: Percent of Dominant Species That Are OBL, FACW, or FAC. Total% Cover of — hw Oat. seci �) x2.= V-�W speolos FAC eche$ x 3 B FACMU species - x UFL species Column Totais: �(A) tt Prevalence Index = EVA • 9 Hydrophytic Vegetation Indicatom: _ 1 -Rapid Test for Hydrophytic Vegetation _ 2 - Dominance Teet Is ?50% _ 3 - Prevalence Index Is s3.4' _ d - Morphological Adaptations' (provide supporting data In Remorks or on p sopar°rata short) 5 - Welland Non -Vascular Plants' _ Problemallc Hydrophydc Vegetation' (Explain) 'Indicators of hydric sof and vualland Hydrology must be present, unless disturbed or problematic, Hydrophytit Vegieteden Present? Yes No US Army Corps of Engineers ftelem Mountains. Valleys, and Coast - Veralon 2.0 SOIL Sampling Point ) ....... i Profile sci$i � Deisaribe to The depth yr da t ... ,o ._. _ ... .........__ ....., P ( P o document the Indicator or conflrnn the absence of Indicators.) Depth tInches) 0; ler rpt Itl�al)i&07 �... u.r...... ... ...... CoCHydric Soil odicatoria (Applicable toalll.RRs unless lxlx, SVCoverod or .,oa ed Sand "-(ulna 2Locatlon: PL�Pt�rs Limtirn M -Matrix. _ DLwO q, RM. duces . ... �W _ , w.w.�. M�.. .._ ._ s otherwise noted,) Indicators far Problomatic Hydric Solis Hlstosol (Al" _ Sandy Redox (S5) _ 2 cm Muck (All 0) _ Histic Eplpedon (A2) Stripped Matrix (S6) _ Red Parent Material (TF2) _ Black Histic (A3) _ Loamy Mucky Mineral (Fl) (except IALRA 1) _ Very Shallow Dark Surface (TF1 2) _ Hydrogen Sulflde ;A4) _ Loamy Gleyed Matrix (F2) _ Other (Explain In Remarks) _ Depleted BeiuN Dark Surface (All) _ Depleted Matrix (F3) Thick Dark Surface (Al2) — Redox Dark Surface (176) 'Indicator, of hydrophytic vegetation and _ Sandy Mucky Mineral,SI) _Deplaced Dark Surface {F7) Wetland hydrology must be present, _ Sandy Gkryed Matrix ($4) _ Redox Depfossions (F8) unless disturbed or problenialtcd Restrictive Layer (11 present): Type: Depth (inches), _ Hy .. .......� dric Soil Present? Yea No HYDROLOGY PrImam Indlratnr of ane remtlrew rhprk all that annlu5 - _ Surface Water (At) _ Water -Stained Leaves (99) (except _ Water-Stalned Leaves (89) (MLRA 1, 2, Wgh Water Table 1,A2) MLRA 1, 2.4A. and 48) 4A, and 4131 _ Saturation (A3) _ Salt Cruet (B11) — Drainage Patterns (B1 D) Water Marks (Bl) — Aquatic Invertebrates (1313) _ Dry -So as on Water Tabla (C2) _ Sediment Deposits (132) _ Hydrogen Sulfide Odor (Cl) _ Saturation Vlslble on Aerial Imagery (CS) Drift Depoalts (B3) _ Oxidized Rhizosphares along _Mng Roots (03) _ Geomorphic Position (D2) _ Algal Mat or Crust (64) _ Presence of Reduced Iron (C4) _ Shallow Aquitard (03) _ Iron Deposits tES) _ Recent Iron Reduction In Tilled Salts (CB) _ FAC -Neutral Test (Db) _ Surface Soil Cracks (1391 „ Slurried or Stressed Plants (DI) (LRR A) _liaised Ant Mounds (06) (LRR A) _ Inundation Visible on Aerial Imagery (137) Other (Explain in Remarks) _ Frost -Heave Hummocks (07) v cooly Vogelalad- VVII�AVO Surfal.H Soo) Surface Water Present? Yes No – Ioplh (inches): Water Table Present? Yes Na ._ Depth (inches): Saturation Present? Yes No Depth (inches): includes err Ilia ilia a Describe Rec�onded Date (stroarn gauge, monitoring well, 40601 pholos Wetland Hydrology Present? Yes No US Army Corps of Engineers Western Mountains, Valleys, and Coast – Version 2.0 WETLAND DETERMINATION DATA FORM —Western Mountains, Valleys, and Coast Region ProiecvSheA�4 ° �lCity/County ioil g�>am P° IlngData mpliny PoinAppllcantJOwner t invesstar(s). Section, Township,Range: {R 14 °R r .—: IIS" Slope O. Landform (hillslope lerrac , etc.),—l') t LoCaf r®Ilei (can convex. none) _ Subregion (LRR)• Let: Long Datum:_,_,_, • gym....,......--. i�IX l..�.rw�w.iw.. Soil Map Unit Name: ra d ear? Y — �,�� e la'. r r � " r 1114'l ? r w� NWI Classification: Are climatic I hydrologic Corloldons on the site typical for this time of y es lilWrpn in f eritarPcs.} ,.. No,.—„„a. Ifti'io,ex Are Vegetation Soil , of Hydrology significantly disturbed? Aro 'Nornial CtrournlatsivoW present? Yes � Na Are Vegetation Sail . of Hydrology naturally problematic? (If needed, explain any answers in Remarks.) SUMMARY OF FINDINGS — Attach site fn p showing sampling point locations, transects, Important features, etc. Hydrophytic Vegetation Present? Yes No Hydric Soil Present? Yes No Is the Sar Area Wetland Hydrology Present? Yes No within a Weetlalls nd? Yes_zN0 Remarks: VEGETATION — Use scientific names of plants. (Plot size: 1. 2. m... 3. 4.. _ Sonlinall. h (Plot size, 3. 4. .-- -_ 5 Absokite Dotnlnant Indicator Dominance Test worksheet — Number of Dominant Species Thal Are CBL, FACW, or FAC: _._ (A) Total Number of Dominent Species Across All Strata: (B), Total Cover A c, Total �— Cover (Plot size° ) r 1. r A,t i, (t� 2t,71 u 4 IA.�ki"�alsv � 1 l" ( ire ICA 4. 5. _ mm . .. 6. 7. —� .�..na........ 8, 9. 1, Total Cover (Plot 2_ a Total Coiner % Bare Ground In Herb Stratum Peroent of Dominant Species () That Are OBL, FACW, or FAC: (AM) _ 1 - Rapid Test for Hydrophyllo Vegetation 2 - Dominance Test Is :50% _ 3 - Prevalence Index is 53,0' _ 4 -Morphological Adaptations' (Provide supporting data In Remarks or on a separate sheet) _ 5 - Wetland Non -Vascular Plante' Problematic Hydrophytic Vegetetlon' (Explaln) 'Indicators of hydric sell and wetland hydrology must be present, unless disturbed or problematic, a Hydrophytic Vegetation Present? Yes iil4 US Army Corps of Engineefs Western Mountains, Valleys, and Coast — Version 2.0 CBL species X1 FACW species x+ FAC species x 3 FACU species x 4 _. UPL species x to Column Totals: (A) --,.—„ (B) Prevalence Index = 61A _ 1 - Rapid Test for Hydrophyllo Vegetation 2 - Dominance Test Is :50% _ 3 - Prevalence Index is 53,0' _ 4 -Morphological Adaptations' (Provide supporting data In Remarks or on a separate sheet) _ 5 - Wetland Non -Vascular Plante' Problematic Hydrophytic Vegetetlon' (Explaln) 'Indicators of hydric sell and wetland hydrology must be present, unless disturbed or problematic, a Hydrophytic Vegetation Present? Yes iil4 US Army Corps of Engineefs Western Mountains, Valleys, and Coast — Version 2.0 Welland Hydrology Indicators, SOIL — Water -Stained Leaves (B9) (except o Water-StalnedIefiyes (99) (MLRA 1, 2, Sampling Point: Profile . ......... . . Description* (Describe to the depth needed to document the Indicator or confirm the absence of lndicators,) Depth --Rodox Features (inches) Color (malst) ........... 5.ji! .......... Drainage Patterns (B10) .190 I, Dry -Season Water Table (C2) Sediment Deposits (W) . . . . ................ . ..... t, RM-Reduqd Matt ix MAIAjgfjx, Soil indicators: (Applicabla to all LRRs, unless otherwise noted.) Indicators for Problematic Hyddc`-SoIP-1-­­­- Histosol (Al) Sandy Redox (SS) — 2 cm Muck (A10) — Histic Eolpedon (A2) Stripped Matrix (SO) — Red Parent Material (TF2) — Black Histle (A3) Loamy Mucky Mineral (Fl) (except MLRA 1) _ Very Shallow Dark Surface (TF12) Hydrogen Sulfide (A4) [)epleied Below Dark Surface (All) Loomy Gloyed Matrix (F2) 011ier (Explain In Remarks) Depleted Matrix (0) Thick Dark Surface (Al 2) Redox Dark Surface (F6) 'Indicators of hydrophylic vegetation and Sandy Mucky Mineral (Sl) Depleted Dark Surface (F7) wetland hydrology must be present. Sandy Gleyed Matrix (64) ............ Redox Depressions (FO) unless disturbed or promommic, i6l' . ..... .... Type: . . ... . ............ ­­_­­­­­­­ Depth Conches): I/ Hydric Soil Iresent? yes No Welland Hydrology Indicators, Surface Water Pros erO Yes --No V -Depth (Inches): Water Table Present? Yes No -��Depth (Inches);_ Saturation PreGent?'r A, J, �, k 0, (includes capillary Noce), Yes No Depth (Inches): �' Vktland Hydrology Present? Yes No Describe Recorded Gla-filrearn —gauge, monliorinjI —setiatphotos, previous ingpettlDrIS), jjsVjafaoje� US Army Corps of Engineers Western Mountains, Valleys, and Coast -Version 2.0 - Sufface Wolter (Al) — Water -Stained Leaves (B9) (except o Water-StalnedIefiyes (99) (MLRA 1, 2, — High Water Table (A2) MLRA 1, 2,4A. and 48) 404, and 4B) Saturation (AS) — Sell Crust (13111) Drainage Patterns (B10) Water Marks (BI) — Aquatic Invertebrates (813) Dry -Season Water Table (C2) Sediment Deposits (W) — Hydrogen Sulfide Odor (Cl) Saturation VislblI on Aerial Imagery (CO) Drift Deposits (133) — Oxidized Rhizosphefes. along Living Roots (C3) — Geomorphic Position (D2) Algal Mat or Crust (B4) — Presence of Reduced Iron (C4) — Shallow Aquillard (D3) Iron Deposits (B5) — Recent Iron Reduction In Tilled Solls, (CIO) FAC -Neutral Test (D5) Surface Soil Cracks (86) — Stunted or Stressed Plants (DI) (ILRR A) Raised Ant Mounds (06) (LRR A) Inundation %Islole an Aerial Imagery (67) _ Other (Explain In Remarks) Froal-Heave Hummocks (D7) VeVggl -A Surface Water Pros erO Yes --No V -Depth (Inches): Water Table Present? Yes No -��Depth (Inches);_ Saturation PreGent?'r A, J, �, k 0, (includes capillary Noce), Yes No Depth (Inches): �' Vktland Hydrology Present? Yes No Describe Recorded Gla-filrearn —gauge, monliorinjI —setiatphotos, previous ingpettlDrIS), jjsVjafaoje� US Army Corps of Engineers Western Mountains, Valleys, and Coast -Version 2.0 WETLAND DETERMINATION DATA FORM — Western Mountains, Valleys, and Coast Region Project/Site: ",/ 1w 1 emQA f r City/County(" `s i Sampling Date: � Sampt ng Point: Applicant/Owner: ( C' 0IN� w Section, Township, Range: ata. (D Investigator(s):p Landform (hillslope, terrace, etc.): I Local relief (concave, convex, none): i,� Slope (°�): Z Subregion (LRR): Let: Long: ��pp t mt^ Soil Map Unit Name' i' t : ✓) 510M-kssification: e�F Are climatic/ hydrologic cond��.� � Are Vegetation ,Soil or Hydrology significant? disturbed? Are "Normal no, explain in Remarks -)_— ons on the site typical for Ibis -time of ear? Yes No g y gy y al Circumstances" present? Yes No. Are Vegetation Soil or Hydrology naturally problematic? (If needed, explain any answers in Remarks.) SUMMARY OF FINDINGS — Attach site map showing sampling point locations, transects, Important features, etc. Hydrophytic Vegetation Present? Yeso' Hydric Soil Present? Yes � No Is the Sampled Area Welland Hydrology Present? Yes 1 No within a Wetland? Yes No Remarks: 1 h 1 1Ja a A J A VEGETATION — Use scientific names of plants. Absolute Dominant indicator oommance 1e81woFKsneet: %Cover Specie Number of Dominant Species 2 1 ree Stratum (Plot size:� That Are OBL, FACW or FAC: J (A) 2. 3. 4. Total Cover Saounaishiub Siralum (P ¢ttsize: 2.%a OMG i z � ito N 4. v' rpt 5. = Total Cover (Plot size: 1. AN fA(, 2� .._ 1FAW 3.' lie a �+,n V `h 4. 5. _ 6. 7 8. 9. 10. 11, C l i r =Total Cover (Plot size: J 1. Z2 FACO 2. % Bare Ground in Herb Stratum Total Cover Remarks: Total Number of Dominant Species Across All Strata: (B) Percent of Dominant Species That Are OBL, FACW, or FAC: " (A/B) Total % 2f' Muflioly bv: OBL species x 1 FACW species x2= FAC species x3= FACU species x 4 a UPL species x 5 = Column Totals: (A) (B) Prevalence Index = B/A - _ 1 - Rapid Test for Hydrophytic Vegetation 12S\2 - Dominance Test is >50% _ 3 - Prevalence Index is 53.0' _ 4 - Morphological Adaptations' (Provide supporting data In Remarks or on a separate sheet) _ 5 - Wetland Non -Vascular Plants' Problematic Hydrophytic Vegetation' (Explain) 'Indicators of hydric soil and wetland hydrology must be present, unless disturbed or problematic. Hydrophytic Vegetation Present? Yes YNo US Army Corps of Engineers Western Mountains, Valleys, and Coast– Version 2.0 SOIL Sampling Paint, Profile Description; il5aaciibe-t-ot"b—o"-d'o-"p th—needed —to documoni ih" "a' Indicator or 'coatflsln tiro aftssnca oifIn di,cal'o". . . . ... ... ............. Depth (M I'nr.heG) ori 1119itib . ...... __2L_ Redox Foalures ___.QgjgLWMWj1_ ....TML ........ . . .......... — Water -Stained Leaves (B9) (11111111. 2. Hlgh Water Table (A2) MLRA 1, Z 4A, and 48) 4A, and 46) . ............ . . . . ........ . . .... .......... ......... .... ..... GVIConcent fats n QtD on.,11M=11'educed Matrix. GS=Covared at Cooled Send Grains, �Locndon, PL=PDI"e LlNq:g,M=NIa1dx Hydric Soil Indicators; (Applkable to al LRRs, unless otherwise notqd.1 I ndicators for Problematic Hydric So I Is3: Histesial (All Sandy Redox (S5) — 2 em Muck (Ala) Histic EpIpedon (A2) Stripped Matrix (30) — Red Parent Material (TF2) Black Histic (A3) Loamy Mucky Mineral (Fl) (except FALRA 1) — Very Shaltow Dark Surface (TF12) Hydrogen Sv fide (A.4 Dopleied Uow DorK Surface (All) Loamy Gleyed Matrix (F2) - 7 Deplated Malwix (0) — Other (Explain In Remarks) Thick CMM &i On ce (A 12) — Redox Dirk Surface (1713) 31ndioators of hydrophylic vegetation and Sandy Mucky III (Sl) — Depleted Dark Surface (F7) wetland hydrology must be present, Sandy Glayed Matrix (34) — Redox Depressions (FO) unless disturbed or problematic, Riiir_1cfi_v_eUjer Ill present): Type: Depth (inches)., Hydric Soil Present? Yes No Remarks: HYDROLQGY cher, n1i th.1" Indcalors Q or mom"Sluimm Surface Water (Al) — Water -Stained Leaves (tag) (except — Water -Stained Leaves (B9) (11111111. 2. Hlgh Water Table (A2) MLRA 1, Z 4A, and 48) 4A, and 46) Saturation (A3) — Sell Cruel (8 11) — Drainage Patterns (B10) Water Marks (1311) _ Aquatic Invertebrates (1313) — Dry -Season Water Table (C2) Sediment Deposits (112) — Hydrogen Sulfide Odor (Cl) — Saturation Visible on Aerial Imagery (09) Drlft Deposits (B3) — Oxidized RhIzospheres along Living Roots (0) — Geomorphic Position (02) Algal Mat or Crust (13f) — Presence of Reduced Iron (C4) — Shallow Aqul(ard (133) Iron Deposits (1351 — Recent Iron Reduction In Thled Sails (CO) — FAC -Neutral Test (IDS) Surface Soil Cracks (BG) — Stunted or Stressed Plants (01) (LRR A) Raised Ant Mounds (D13) (LRR A) Inundation Visible on Aerial Imagery (137) — Other (Explain in Remarks) Frost -Heave Hummocks (07) Spersely Vegetated Surface Btk r 0a S [, Surface Water Present? Yes- No Depth Cinches): Water Table Present? Yes 17— Na Depth Cnches):i="= Saturation Pre . sent? Yes No Wplh (inches)! Wetland Hydrology Present? Yes No , It ave US Army Corps of Engineers Westem Mountains, Valleys, and Coast — Version 2.11 SHANNON WLSON, IIo APPENDIX C WETLAND RATING FORMS — WESTERN WASHINGTON 21-1-22082-002 Wetland name or number A Name of wetland (or ID #): Wetland A Date of site visit: 7/6 and 7/7/15 Rated by S. orbija pWSI Trained by Ecology? -2L Yes No Date of training 10/09 and 5/14 HGM Class used for rating Slope Wetland has multiple HGM classes?_Y X N NOTE: Form is not complete without the figures requested (figures can be combined). Source of base aerial photo/map Goo le Earth OVERALL WETLAND CATEGORY IV (based on functions X or special characteristics_) 1. Category of wetland based on FUNCTIONS Category I —Total score = 23 - 27 Category II — Total score = 20 - 22 Category III —Total score = 16 - 19 X Category IV — Total score = 9 - 15 FUNCTION Site Potential Landscape Potential Value Score Based on Improving Hydrologic Habitat Water Quality _] Circle the appropriate ratings H M L HM L_ H M H L H_M OL H_ M H M L H L H L TOTAL 5 4 4 13 2. Category based on SPECIAL CHARACTERISTICS of wetland CHARACTERISTIC Estuarine Wetland of High Conservation Value CATEGORY I II I Bog I Mature Forest I Old Growth Forest I Coastal Lagoon I II Interdunal I II III IV None of the above Score for each function based on three ratings (order of ratings is not important) 9 = H,H,H 8 = H,H,M 7 = H,H,L 7 = H,M,M 6 = H,M,L 6 = M,M,M 5 = H,L,L 5 = M,M,L 4 = M,L,L 3=L,L,L Wetland Rating System for Western WA: 2014 Update 1 Rating Form - Effective January 1, 2015 Wetland name or number A Maps and figures required to answer questions correctly for 'western Washington Slone WPtlanric Wetland Rating System for Western WA: 2014 Update 2 Rating Form - Effective January 1, 2015 Wetland name or number A MGM Classification of Wetlands in Western Washington. For questions 1-7, the criteria described must apply to the entire unit being rated. If the hydrologic criteria listed in each question do not apply to the entire unit being rated, you probably have a unit with multiple HGM classes. In this case, identify which hydrologic criteria in questions 1-7 apply, and go to Question 8. 1. Are the water levels in the entire unit usually controlled by tides except during floods? 0 go to 2 YES -the wetland class is Tidal Fringe - go to 1.1 1.1 Is the salinity of the water during periods of annual low flow below 0.5 ppt (parts per thousand)? - Saltwater Tidal Fringe (Estuar ine_�) YES - Freshwater Tidal Fringe c" Ify. our we 5 -"r shwater Tidal Fringe use the forms for Riverine wetlands. If it is Saltwater Tidal Fringe it is an Estuarine wetland and is not scored. This method cannot be used to score functions for estuarine wetlands. 2. The entire wetland unit is flat and precipitation is the only source (>90%) of water to it. Groundwater and surface water runoff are NOT sources of water to the unit. NO - go to 3 YES - The wetland class is Flats ,r pan be classified as a Flats wetland, use the form for Depressional wetlands. 3. Does the entire wetland unit meet all of the following criteria? _The vegetated part of the wetland is on the shores of a body of permanent open water (without any plants on the surface at any time of the year) at least 20 ac (8 ha) in size; _At least 30% of the open water area is deeper than 6.6 ft (2 m). o k ---go to 4C:> YES - The wetland class is Lake Fringe (Lacustrine Fringe) 4. Does the entire wetland unit meet all of the following criteria? X The wetland is on a slope (slope can be very gradual), X The water flows through the wetland in one direction (unidirectional) and usually comes from seeps. It may flow subsurface, as sheetflow, or in a swale without distinct banks, X The water leaves the wetland without being impound` NO - go to 5 YES - The wetland class is Slope' NOTE: Surface water does not pond in these type of wetlan a slt all and shallow depressions or behind hummocks (depressions are usually <3 ft diameter and less than 1 ft deep). 5. Does the entire wetland unit meet all of the following criteria? The unit is in a valley, or stream channel, where it gets inundated by overbank flooding from that stream or river, The overbank flooding occurs at least once every 2 years. Wetland Raring System for Western WA: 2014 Update 3 Rating Form - Effective January 1, 2015 Wetland name or number A NO - go to 6 YES - The wetland class is Riverine NOTE: The Riverine unit can contain depressions that are filled with water when the river is not flooding 6. Is the entire wetland unit in a topographic depression in which water ponds, or is saturated to the surface, at sometime during the year? This means that any outlet, if present, is higher than the interior of the wetland. NO-goto7 YES - The wetland class is Depressional 7. Is the entire wetland unit located in a very flat area with no obvious depression and no overbank flooding? The unit does not pond surface water more than a few inches. The unit seems to be maintained by high groundwater in the area. The wetland may be ditched, but has no obvious natural outlet. NO-goto8 YES - The wetland class is Depressional 8. Your wetland unit seems to be difficult to classify and probably contains several different HGM classes. For example, seeps at the base of a slope may grade into a riverine floodplain, or a small stream within a Depressional wetland has a zone of flooding along its sides. GO BACK AND IDENTIFY WHICH OF THE HYDROLOGIC REGIMES DESCRIBED IN QUESTIONS 1-7 APPLY TO DIFFERENT AREAS IN THE UNIT (make a rough sketch to help you decide). Use the following table to identify the appropriate class to use for the rating system if you have several HGM classes present within the wetland unit being scored. NOTE: Use this table only if the class that is recommended in the second column represents 10% or more of the total area of the wetland unit being rated. If the area of the HGM class listed in column 2 is less than 10% of the unit; classify the wetland using the class that represents more than 90% of the total area. HGM classes within the wetland unit being rated Slope + Riverine HGM class to use in rating Riverine Slope + Depressional Depressional Slope + Lake Fringe Lake Fringe Depressional + Riverine along stream Depressional within boundary of depression Depressional + Lake Fringe _ Depressional Riverine +Lake Fringe Riverin e Salt Water Tidal Fringe and any other Treat as class of freshwater wetland ESTUARINE Ifyou are still unable to determine which of the above criteria apply to your wetland, or ifyou have more than 2 HGM classes within a wetland boundary, classify the wetland as Depressional for the rating. Wetland Rating System for Western WA: 2014 Update 4 Rating Form - Effective January 1, 2015 Wetland name or number. A_ .. / / r r 1 f// ��/ / i .✓ ,,/ / if,i „/ iii i S 1.0. Does the site have the potential to improve water quality? S 1.1. Characteristics of the average slope of the wetland: (a 1% slope has a 1 ft vertical drop in elevation for every 100 ft of horizontal distance) Slope is 1% or less points = 3 0 Slope is > 1%-2% points = 2 Slope is > 2%-5% points = 1 Slope is greater than 5%oints = 0 S 1.2. The soil 2 in below the surface for duff la er is true clay or true organic (use NRCS deny"tions): Yes = 3 No = 0 0 S 1.3. Characteristics of the plants in the wetland that trap sediments and pollutants: Choose the points appropriate for the description that best fits the plants in the wetland. Dense means you have trouble seeing the soil surface (>75% cover), and uncut means not grazed or mowed and plants are higher than 6 in. Dense, uncut, herbaceous plants > 90% of the wetland area points = 6 Dense, uncut, herbaceous plants > %: of area 2 Dense, woody, plants > %: of area oi�=2 Dense, uncut, herbaceous plants > % of area points = 1 Does not meet any of the criteria above for plants points = 0 Total for S 1 Add the points in the boxes above 2 Rating of Site Potential If score is:-12 = H _6-11= M X___0-S = L Record the rating on the first page Rating of Landscape Potential If score is: X 1-2 = M _0 = L Record the rating on the first page Rating of Value If score is: 2-4 = H X 1= M _0 = L Record the rating on the first page Wetland Rating System for Western WA: 2014 Update 11 Rating Form - Effective January 1, 2015 Wetland name or number _A S 4.0. Does the site have the potential to reduce flooding and stream erosion? S 4.1. Characteristics of plants that reduce the velocity of surface flows during storms: Choose the points appropriate for the description that best fits conditions in the wetland. Stems of plants should be thick enough (usually> 118 in), or dense enough, to remain erect during surface flows. 0 Dense, uncut, rigid plants cover > 90% of the area of the wetland points =1 All other conditions Rating of Site Potential If score is:—IL = M g0 = L Record the rating on the first page S 5.0. Does the landscape have the potential to support the hydrologic functions of the site? S 5.1. Is more than 25% of the area within 150 ft upslope of wetland in land uses or cover that generate excess surface runoff? Yes = 1a = 0 0 Rating of Landscape Potential If score is:_1= M g0 = L Record the rating on the first page S 6.0. Are the hydrologic functions provided by the site valuable to society? S 6.1. Distance to the nearest areas downstream that have flooding problems: The sub -basin immediately down -gradient of site has flooding problems that result in damage to human or natural resources (e.g., houses or salmon redds) points = 2 1 Surface flooding problems are in a sub -basin farther down-gradientodnts=D No flooding problems anywhere downstream points —=, 0 S 6.2. Has the site been identified as important for flood storage or flood conveyance in a regional flood control ]an? Yes = 2 _ 0 Total for S 6 Add the points in the boxes above 1 Rating of Value If score is: _2-4=H _X1= M _0 = L Record the rating on the first page NOTES and FIELD OBSERVATIONS: Wetland Rating System for Western WA.: 2014 Update 12 Rating Form - Effective January 1, 2015 Wetland name or number A These questions apply to wetlands of all HGM classes. HABITAT FUNCTIONS - Indicators that site functions to provide important habitat H 1.0. Does the site have the potential to provide habitat? H 1.1. Structure of plant community: Indicators are Cowardin classes and strata within the Forested class. Check the Cowardin plant classes in the wetland. Up to 10 patches may be combined for each class to meet the threshold of '4 ac or more than 10% of the unit if it is smaller than 2.5 ac. Add the number of structures checked. Aquatic bed 4 structures or more: points = 4 Emergent 3 structures: points = 2 X Scrub -shrub (areas where shrubs have > 30% cover) 2 structures: points = 1 Forested (areas where trees have > 30% cover) 1 structure: points = 0 If the unit has a Forested class, check if.• The Forested class has 3 out of 5 strata (canopy, sub -canopy, shrubs, herbaceous, moss/ground-cover) that each cover 20% within the Forested polygon H 1.2. Hydroperiods Check the types of water regimes (hydroperiods) present within the wetland. The water regime has to cover more than 10% of the wetland or % ac to count (see text for descriptions of hydroperiods). Permanently flooded or inundated 4 or more types present: points = 3 Seasonally flooded or inundated 3 types present: points = 2 Occasionally flooded or inundated 2 types present: points = 1 0 _Saturated only 1 type present: points = 0 Permanently flowing stream or river in, or adjacent to, the wetland Seasonally flowing stream in, or adjacent to, the wetland Lake Fringe wetland 2 points Freshwater tidal wetland 2 points H 1.3. Richness of plant species Count the number of plant species in the wetland that cover at least 10 ftZ. Different patches of the same species can be combined to meet the size threshold and you do not have to name the species. Do not include Eurasian milfoil, reed canarygrass, purple loosestrife, Canadian thistle If you counted: > 19 species points = 2 1 5 - 19 species points = 1 < 5 species points = 0 H 1.4. Interspersion of habitats Decide from the diagrams below whether interspersion among Cowardin plants classes (described in H 1.1), or the classes and unvegetated areas (can include open water or mudflats) is high, moderate, low, or none. If you have four or more plant classes or three classes and open water, the rating is always high. CD1 0 None = 0 points Low = 1 point Moderate = 2 points ' All three diagrams n this row are HIGH = 3points Wetland Rating System for Western WA: 2014 Update 13 Rating Form — Effective January 1, 2015 Wetland name or number A H 1.5. Special habitat features: Check the habitat features that are present in the wetland. The number of checks is the number of points. Large, downed, woody debris within the wetland (> 4 in diameter and 6 ft long). Standing snags (dbh > 4 in) within the wetland Undercut banks are present for at least 6.6 ft (2 m) and/or overhanging plants extends at least 3.3 ft (1 m) over a stream (or ditch) in, or contiguous with the wetland, for at least 33 ft (10 m) Stable steep banks of fine material that might be used by beaver or muskrat for denning (> 30 degree slope) OR signs of recent beaver activity are present (cut shrubs or trees that have not yet weathered where wood is exposed) At least % ac of thin -stemmed persistent plants or woody branches are present in areas that are permanently or seasonally inundated (structures for egg -laying by amphibians) XInvasive plants cover less than 25% of the wetland area in every stratum of plants (see H 1.1 for list of Total for H 1 Add the points in the boxes above 2 �] Rating of Site Potential If score is: 15-18 = H _7-14 = M g0-6 = L Record the rating on the first page H 2.0. Does the landscape have the potential to support the habitat functions of the site? H 2.1. Accessible habitat (include only habitat that directly abuts wetland unit). Calculate: % undisturbed habitat_A+ [(/ moderate and low intensity land uses)/2] 0 =_0 If total accessible habitat is: > 1/3 (33.3%) of 1 km Polygon points = 3 0 20-33% of 1 km Polygon points = 2 10-19% of 1 km Polygon points = 1 < 10% of 1 km Polygon points = 0 H 2.2. Undisturbed habitat in 1 km Polygon around the wetland. Calculate: % undisturbed habitat+ [(/ moderate and low intensity land uses)/210 = 0 Undisturbed habitat > 50% of Polygon points = 3 Undisturbed habitat 10-50% and in 1-3 patches points = 2 0 Undisturbed habitat 10-50% and > 3 patches points = 1 Undisturbed habitat < 10% of 1 km Polygon points = 0 H 2.3. Land use intensity in 1 km Polygon: If > 50% of 1 km Polygon is high intensity land use points = (- 2) -2 <- 50% of 1 km Polygon is high Intensity points = 0 Total for H 2 Add the points in the boxes above -2 Rating of Landscape Potential If score is: 4-6 = H _1-3 = M _X_< 1= L Record the rating on the first page H 3.0. Is the habitat provided by the site valuable to society? H 3.1. Does the site provide habitat for species valued in laws, regulations, or policies? Choose only the highest score that applies to the wetland being rated. Site meets ANY of the following criteria: points = 2 — It has 3 or more priority habitats within 100 m (see next page) — It provides habitat for Threatened or Endangered species (any plant or animal on the state or federal lists) — It is mapped as a location for an individual WDFW priority species — It is a Wetland of High Conservation Value as determined by the Department of Natural Resources — It has been categorized as an important habitat site in a local or regional comprehensive plan, in a Shoreline Master Plan, or in a watershed plan Site has 1 or 2 priority habitats (listed on next page) within 100 m points = 1 Site does not meet any of the criteria above _ Dints -0 Rating of Value If score is: _2=H _X_1= M _0 = L Record the rating on the first page Wetland Rating System for Western WA: 2014 Update 14 Rating Form - Effective January 1, 2015 Wetland name or number A WDFW Priority Habitats Priol-Ity habitats listed by W , W (see complete descriptions of WDFW priority habitats, and the counties in which they can be found, in: Washington Department of Fish and Wildlife. 2008. Priority Habitat and Species List. Olympia, Washington. 177 pp. . Jm fw A ° / tib • 00 Wdfwv0„Q165,p- or access the list from here: h"akwd AMA con e Count how many of the following priority habitats are within 330 ft (100 m) of the wetland unit: NOTE. This question is independent of the land use between the wetland unit and the priority habitat. Aspen Stands: Pure or mixed stands of aspen greater than 1 ac (0.4 ha). Biodiversity Areas and Corridors: Areas of habitat that are relatively important to various species of native fish and wildlife (full descriptions in WDFW PHS report). — Herbaceous Balds: Variable size patches of grass and forbs on shallow soils over bedrock. — Old-growth/Mature forests: tl - w , ade c .. ` - Stands of at least 2 tree species, forming a multi- layered canopy with occasional small openings; with at least 8 trees/ac (20 trees/ha ) > 32 in (81 cm) dbh or > 200 years of age. t a Lesti, - Stands with average diameters exceeding 21 in (53 cm) dbh; crown cover may be less than 100%; decay, decadence, numbers of snags, and quantity of large downed material is generally less than that found in old-growth; 80-200 years old west of the Cascade crest. Oregon White Oak: Woodland stands of pure oak or oak/conifer associations where canopy coverage of the oak componentis important (full descriptions in WDFW PHS report p. 158 - see web link above). Riparian: The area adjacent to aquatic systems with flowing water that contains elements of both aquatic and terrestrial ecosystems which mutually influence each other. — Westside Prairies: Herbaceous, non -forested plant communities that can either take the form of a dry prairie or a wet prairie (full descriptions in WDFW PHS report p. 161 - see web link above). — Instream: The combination of physical, biological, and chemical processes and conditions that interact to provide functional life history requirements for instream fish and wildlife resources. — Nearshore: Relatively undisturbed nearshore habitats. These include Coastal Nearshore, Open Coast Nearshore, and Puget Sound Nearshore. (full descriptions of habitats and the definition of relatively undisturbed are in WDFW report - see web link on previous page). — Caves: A naturally occurring cavity, recess, void, or system of interconnected passages under the earth in soils, rock, ice, or other geological formations and is large enough to contain a human. — Cliffs: Greater than 25 ft (7.6 m) high and occurring below 5000 ft elevation. — Talus: Homogenous areas of rock rubble ranging in average size 0.5 - 6.5 ft (0.15 - 2.0 m), composed of basalt, andesite, and/or sedimentary rock, including riprap slides and mine tailings. May be associated with cliffs. X Snags and Logs: Trees are considered snags if they are dead or dying and exhibit sufficient decay characteristics to enable cavity excavation/use by wildlife. Priority snags have a diameter at breast height of > 20 in (51 cm) in western Washington and are > 6.5 ft (2 m) in height. Priority logs are > 12 in (30 cm) in diameter at the largest end, and > 20 ft (6 m) long. Note: All vegetated wetlands are by definition a priority habitat but are not included in this list because they are addressed elsewhere. Wetland Rating System for Western WA: 2014 Update 15 Rating Form - Effective January 1, 2015 Wetland name or number A CATEGORIZATION BASED ON SPECIAL CHARACTERISTICS , / t ir/ /i SC 1.0. Estuarine wetlands Does the wetland meet the following criteria for Estuarine wetlands? — The dominant water regime is tidal, — Vegetated, and With a salinity greater than 0.5 ppt Yes -Go to SC 1.1 No-=- Not an estuarine wetland SC 1.1. Is the wetland within a National Wildlife Refuge, National Park, National Estuary �.vseAW1uraJ Preserve, State Park or Educational, Environmental, or Scientific Reserve designated under WAC 332-30-1.51.? Yes = Category I No - Go to SC 1..2 Cat. l SC 1.2. Is the wetland unit at least 1 ac in size and meets at least two of the following three conditions? —The wetland is relatively undisturbed (has no diking, ditching, filling, cultivation, grazing, and has less than 10% cover of non-native plant species. (If non-native species are Spartina, see page 25) Cat. —At least % of the landward edge of the wetland has a 100 ft buffer of shrub, forest, or un -grazed or un - mowed grassland. —The wetland has at least two of the following features: tidal channels, depressions with open water, or Cat. II contiguous freshwater wetlands. Yes = Category I No = Category II SC 2.0. Wetlands of High Conservation Value (WHCV) SC 2.1. Has the WA Department of Natural Resources updated their website to include the list of Wetlands of High Conservation Value? Yes - Go to SC 2.2 No - Go to SC 2.3 Cat. SC 2.2. Is the wetland listed on the WDNR database as a Wetland of High Conservation Value?_ Yes= CategoryI (No = Not a WHCV SC 2.3. Is the wetland in a Section/Township/Range that contains a Natural Heritage wetland?� .. lett wwwl.dnr.wa. ov nh refdek datasearcl� nh r,�et9and,odi' Yes - Contact WNHP/WDNR and go to SC 2.4 No =Not a WHCV SC 2.4. Has WDNR identified the wetland within the S/T/R as a Wetland of High Conservation Value and listed it on their website? Yes= Category I No = Not a WHCV SC 3.0. Bogs Does the wetland (or any part of the unit) meet both the criteria for soils and vegetation in bogs? Use the key below. If you answer YES you will still need to rate the wetland based on its functions. SC 3.1. Does an area within the wetland unit have organic soil horizons, either peats or mucks, thaCto- pc more of the first 32 in of the soil profile? Yes - Go to SC 3.3 to SC 3.2 SC 3.2. Does an area within the wetland unit have organic soils, either peats or mucks, that are lesxl over bedrock, or an impermeable hardpan such as clay or volcanic ash, or that are floating on t P.014 or pond? Yes - Go to SC 3.3 o = Is not a bog SC 3.3. Does an area with peats or mucks have more than 70% cover of mosses at ground level, AN caw t a 39 cover of plant species listed in Table 4? Yes = Is a Category I bog No - Go to SC 3.4 NOTE: If you are uncertain about the extent of mosses in the understory, you may substitute that criterion by measuring the pH of the water that seeps into a hole dug at least 16 in deep. If the pH is less than 5.0 and the plant species in Table 4 are present, the wetland is a bog. Cat. SC 3.4. Is an area with peats or mucks forested (> 30% cover) with Sitka spruce, subalpine fir, western red cedar, western hemlock, lodgepole pine, quaking aspen, Engelmann spruce, or western white pine, AND any of the species (or combination of species) listed in Table 4 provide more than 30% of the cover under the canopy? Yes = Is a Category I bog No = Is not a bog Wetland Rating System for Western WA: 2014 Update 16 Rating Form - Effective January 1, 2015 Wetland name or number A SC 4.0. Forested Wetlands Does the wetland have at least 1 confi nous acre of forest that meets one of these criteria for the WA Department of Fish and Wildlife's forests as priority habitats? If you answer YES you will still need to rate the wetland based on its functions. — Old-growth forests (west of Cascade crest): Stands of at least two tree species, forming a multi -layered canopy with occasional small openings; with at least 8 trees/ac (20 trees/ha) that are at least 200 years of age OR have a diameter at breast height (dbh) of 32 in (81 cm) or more. — Mature forests (west of the Cascade Crest): Stands where the largest trees are 80- 200 years old OR the species that make up the canopy have an average diameter (dbh Yes= Category I o = Not a forested wetland for this section Cat. I SC 5.0. Wetlands in Coastal Lagoons Does the wetland meet all of the following criteria of a wetland in a coastal lagoon? — The wetland lies in a depression adjacent to marine waters that is wholly or partially separated from marine waters by sandbanks, gravel banks, shingle, or, less frequently, rocks —The lagoon in which the wetland is located contains ponded water that is saline or brackish (> 0.5 ppt) during most of the year in at least a portion of the lagoon (needsrNo 7Nota near the o Cat. Yes - Go to SC 5.1 etland in a coastal lagoon SC 5.1. Does the wetland meet all of the following three conditions? —The wetland is relatively undisturbed (has no diking, ditching, filling, cultivation, grazing), and has less than 20% cover of aggressive, opportunistic plant species (see list of species on p. 100). Cat. II —At least % of the landward edge of the wetland has a 100 ft buffer of shrub, forest, or un -grazed or un - mowed grassland. —The wetland is larger than 1/10 ac (4350 ft') Yes= Category I No = Category II SC 6.0. Interdunal Wetlands Is the wetland west of the 1889 line (also called the Western Boundary of Upland Ownership or WBUO)? If you answer yes you will still need to rate the wetland based on its habitat functions. In practical terms that means the following geographic areas: — Long Beach Peninsula: Lands west of SR 103 — Grayland-Westport: Lands west of SR 105 Cat I — Ocean Shores-Copalis: Lands west of SR 115 and SR 109 Yes - Go to SC 6.1No = not an interdunal wetland for rating SC 6.1. Is the wetland 1 ac or larger and scores an 8 or 9 for the habitat functions on the form (rates H,H,H or H,H,M Cat. II for the three aspects of function)? Yes= CategoryI No - Go to SC 6.2 SC 6.2. Is the wetland 1 ac or larger, or is it in a mosaic of wetlands that is 1 ac or larger? Yes = Category II No - Go to SC 6.3 Cat. III SC 6.3. Is the unit between 0.1 and 1 ac, or is it in a mosaic of wetlands that is between 0.1 and 1 ac? Yes = Category III No = Category IV Cat. IV Category of wetland based on Special Characteristics If you answered No for all types, enter "Not Applicable" on Summary Form N/A Wetland Rating System for Western WA: 2014 Update 17 Rating Form - Effective January 1, 2015 C) 2015 Google v ° r' k' Ur Nrj( 'C[7 � �t fir � z r 151f 5� -32nd S.t �� w Ca c; •t� �' ry r �,' ';�� 'cn=y, itoil � c �I i it , AW r ii U) �; ' 23 Olh,S1� s ' ''4,rth� F?I S��r t� v,., v 1 242n c "i. CO Z * 100% of 1 km ilf �EwYN ,buffer= intensiI • � w I pJi T= „ r � mm�y c (TI 0 s m. N,; ff, , 2 v Y° e ie b � w.„ Zvi env 419E ,OgKo oye In `v G M,aAV 43ti8 a f�l `waxy, 0,JOJIII W +LI ... ILI CIO Lo N � Sq. AV 41$6 C2. �� "' � � �k41 r 'w 060 �,w tyy�"anq�y#�F � aMim m w q>Jvy X14 MN RAV %%ll 9 f r r uMal V-11 Y° e ie b � w.„ Zvi env 419E ,OgKo oye In `v G M,aAV 43ti8 a f�l `waxy, 0,JOJIII W +LI ... ILI CIO Lo N � Sq. AV 41$6 C2. �� "' � � �k41 r 'w 060 �,w tyy�"anq�y#�F � aMim m w q>Jvy X14 MN RAV %%ll WATER QUALITY IMPROVEMENT PROTECTS (TMDLS) overview of the process Project Catalog by WRIA by _County Funding opportunities Project Development Priority Lists Related information TMDL Contacts RELATED ECOLOGY PROGRAMS Water Quality !&Oar nEwI. , )NLAINE "Ir 1�' ` 1-1, 1,11 '''UHH11 MIII 1, h WRIA 8- Cedar-Sammamiso; The following table lists overview information for water quality improvement JY1 projects (including total maximum daily loads, or TMDLs) for this water resource inventory area Please use links (where available) for more information on a project. Counties - I I I III I I I I J I I 1 1 1 1 1 1 1 1 1 11 1 1 1 1W TVIUK' IM1110,11ON1 "- j"I ;:;Iwig oft -M&M n Wetland name or number _ RATING SUMMARY — Western Washington Name of wetland (or ID #): Wetland B Date of site visit: 7/6 and 7/7/15 Rated by --§ Corbin, (PWS) Trained by Ecology?_X Yes No Date of training 10/09 and 5/ 1 HGM Class used for rating Depressional Wetland has multiple HGM classes?_Y X N NOTE: Form is not complete without the figures requested (figures can be combined), Source of base aerial photo/map c;,,,,Oe Earth OVERALL WETLAND CATEGORY III (based on functions X or special characteristics_) 1. Category of wetland based on FUNCTIONS Category I — Total score = 23 - 27 Category II — Total score = 20 - 22 X Category III —Total score = 16 - 19 Category IV — Total score = 9 - 15 FUNCTIONto Water Hydrologic Habitat Circle the appropriate ratings ite Potential H L H L H M L -. ........ _. .M......... ,andscape Potential M L H M L H M O Value H �M L H M L H L TOTAL 'core Based on latings 7 7 4 18 2. Category based on SPECIAL CHARACTERISTICS of wetland CHARACTERISTIC CATEGORY Estuarine I II Wetland of High Conservation Value I Bog I Mature Forest I Old Growth Forest I Coastal Lagoon I II Interdunal III III IV None of the above Score for each function based on three ratings (order of ratings is not important) 9 = H,H,H 8 = H, H, M 7 = H,H,L 7 = H,M,M 6 = H,M,L 6 = M, M, M 5 = H,L,L 5 = M,M,L 4 = M,L,L 3 = LLL Wetland Rating System for Western WA: 2014 Update 1 Rating Form - Effective January 1, 2015 Wetland name or number B Maps and figures required to answer questions correctly for Western Washington Riverine Wetlands Nuke Fringe Wetlands Slope Wetlands Wetland Rating,System for Western WA: 2014 Update Rating Form - Effective January 1, 2015 Wetland name or number B HGIVIClassification of Wetlands in Western Washington For questions 1-7, the criteria described must apply to the entire unit being rated. If the hydrologic criteria listed in each question do not apply to the entire unit being rated, you probably have a unit with multiple HGM classes. In this case, identify which hydrologic criteria in questions 1-7 apply, and go to Question 8. 1. Are the water levels in the entire unit usually controlled by tides except during floods? --go to YES - the wetland class is Tidal Fringe - go to 1.1 1.1 Is the salinity of the water during periods of annual low flow below 0.5 ppt (parts per thousand)? NO - Saltwater Tidal Fringe (Estuarine) YES - Freshwater Tidal Fringe Ifyour wetland can be classified as a Freshwater Tidal Fringe use the forms for Riverine wetlands. If it is Saltwater Tidal Fringe it is an Estuarine wetland and is not scored. This method cannot be used to score functions for estuarine wetlands. 2. The entire wetland unit is flat and precipitation is the only source (>90%) of water to it. Groundwater and surface water runoff are NOT sources of water to the unit. NO - go to 3 YES - The wetland class is Flats can be classified as a Flats wetland, use the form for Depressional wetlands. 3. Does the entire wetland unit meet all of the following criteria? _The vegetated part of the wetland is on the shores of a body of permanent open water (without any plants on the surface at any time of the year) at least 20 ac (8 ha) in size; .At least 30% of the open water area is deeper than 6.6 ft (2 m). NO - go to 4 YES - The wetland class is Lake Fringe (Lacustrine Fringe) N 4. Does the entire wetland unit meet all of the following criteria? _The wetland is on a slope (slope can be very gradual), The water flows through the wetland in one direction (unidirectional) and usually comes from seeps. It may flow subsurface, as sheetflow, or in a swale without distinct banks, The water leaves the wetland without being impounded. NO - go to YES - The wetland class is Slope NOTE: Surface water does not pond in these type of wetlands except occasionally in very small and shallow depressions or behind hummocks (depressions are usually <3 ft diameter and less than 1 ft deep). 5. Does the entire wetland unit meet all of the following criteria? The unit is in a valley, or stream channel, where it gets inundated by overbank flooding from that stream or river, _The overbank flooding occurs at least once every 2 years. Wetland Rating System for Western WA: 2014 Update 3 Rating Form - Effective January 1, 2015 Wetland name or number B 0 - go to 6 YES - The wetland class is Riverine erine unit can contain depressions that are filled with water when the river is not flooding 6. Is the entire wetland unit in a topographic depression in which water ponds, or is saturated to the surface, at sometime during the year? This means that any outlet, if present, is higher than the interior of the wetland�w NO - go to 7YES - The wetland class is Depressional 7. Is the entire wetland unit located in a very flat areGa with-iiw'tya -d �- ono overbank flooding? The unit does not pond surface water more than a few inches. The unit seems to be maintained by high groundwater in the area. The wetland may be ditched, but has no obvious natural outlet. NO-goto8 YES - The wetland class is Depressional 8. Your wetland unit seems to be difficult to classify and probably contains several different HGM classes. For example, seeps at the base of a slope may grade into a riverine floodplain, or a small stream within a Depressional wetland has a zone of flooding along its sides. GO BACK AND IDENTIFY WHICH OF THE HYDROLOGIC REGIMES DESCRIBED IN QUESTIONS 1-7 APPLY TO DIFFERENT AREAS IN THE UNIT (make a rough sketch to help you decide). Use the following table to identify the appropriate class to use for the rating system if you have several HGM classes present within the wetland unit being scored. NOTE: Use this table only if the class that is recommended in the second column represents 10% or more of the total area of the wetland unit being rated. If the area of the HGM class listed in column 2 is less than 10% of the unit; classify the wetland using the class that represents more than 90% of the total area. HGM classes within the wetland unit HGM class to being rated use in rating Slope + Riverine Riverine Slope + Depressional Depressional Slope + Lake Fringe Lake Fringe Depressional + Riverine along stream Depressional within boundary of depression Depressional + Lake Fringe Depressional Riverine + Lake Fringe Riverine Salt Water Tidal Fringe and any other Treat as class of freshwater wetland ESTUARINE Ifyou are still unable to determine which of the above criteria apply to your wetland, or ifyou have more than 2 HGM classes within a wetland boundary, classify the wetland as Depressional for the rating. Wetland Rating System for Western WA: 2014 Update 4 Rating Form - Effective January 1, 2015 Wetland name or number B DEPRESSIQNAL AND FLATS WETLANDS Water'Quality Functions - Indicators that the site functions to improve water ill D 1.0. Does the site have the potential to improve water quality? D 1.1. Characteristics of surface water outflows from the wetland: Wetland is a depression or flat depression (QUESTION 7 on key) with no surface water leaving it (no outlet), points �3 Wetland has an intermittently flowing stream or ditch, OR highly constricted permanently flowing outlet. 3 points = 2 Wetland has an unconstricted, or slightly constricted, surface outlet that is permanently flowing points = 1 Wetland is a flat depression (QUESTION 7 on key), whose outlet is a permanently flowing ditch. points = 1 D 1..2. The soil 2 in below the surface or duff layeris true cfay or true orgacic fuse tyR definitiorrs),Yes = 40-- I 0 0 D 1.3. Characteristics and distribution of persistent plants (Emergent, Scrub -shrub, and/or Forested Cowardin classes): Wetland has persistent, ungrazed, plants > 95% of area points = 5 Wetland has persistent, ungrazed, plants > %: of area points = 3 1 Wetland has persistent, ungrazed plants > 1/10 of area points fZj> Wetland has persistent, ungrazed plants <1/io of area points = 0 D 1.4. Characteristics of seasonal ppnding or inundation: This is the area that is ponded for at least 2 months. See description in manual. Area seasonally ponded is > % total area of wetland ints = 4 4 Area seasonally ponded is > % total area of wetland points = 2 Area seasonally ponded is < % total area of wetland points = 0 Total for D 1 Add the points in the boxes above g Rating of Site Potential If score is: 12-16 = H X 6-11= M _0-5 = L Record the rating on the first page D 2.0. Does the landscape have the potential to support the water quality function of the site? D 2.1. Does the wetland unit receive stormwater discharges? es = No = 0 1 D 2.2. Is > 10% of the area within 150 ft of the wetland in land uses that generate pollutants? es = No = 0 1 D 2.3. Are there septic systems within 250 ft of the wetland? Yes= 1 OED) 0 D 2.4. Are there other sources of pollutants coming into the wetland that are not listed in questions2.3? 4D Source residential, do poopfrom do walkers es = No = 0 1 Total for D 2 Add the points in the boxes above 3 Rating of Landscape Potential If score is: X 3 or 4 = H �1 or 2 = M 0 = L Record the rating on the first page D 3.0. Is the water quality improvement provided by the site valuable to society? D 3.1. Does the wetland discharge directly (i.e., within 1 mi) to a stream, river, lake, or marine water that is on 303(d) list? Yes = 1 0 0 ........ D 3.2. Is the wetland in a basin or sub -basin where an aquatic resource is on the 303(d) list?"Ces _ No = 0 ._.. . _.. ., 1 D 3.3 been identified in a water ed or local Ian s important for mai p maintaining water quality(2ns YDS there is a TMDL or the basin in which - f h ) o f —__ ___._ _.�___.a the units ound 0 Total for D 3 Add the points in the boxes above 1 Rating of Value If score is: _-2-4=H X 1=M _0 = L Record the rating on the first page Wetland Rating System for Western WA: 2014 Update Rating Form — Effective January 1, 2015 Wetland name or number B e_ "s -MNAl: wNNI6 1A` S WETLANDS, Hydrologic Functions,- Indicatbrs,that:the site functions to reduce flboding and stream degradation D 4.0. Does the site have the potential to reduce flooding and erosion? D 4.1. Characteristics of surface water outflows from the wetland: Wetland is a depression or flat depression with no surface water leaving it (no outlet) points = 4 Wetland has an intermittently flowing stream or ditch, OR highly constricted permanently flowing outletpoints = 2 Wetland is a flat depression (QUESTION 7 on key), whose outlet is a permanently flowing ditch points = 1 Wetland has an unconstricted, or slightly constricted, surface outlet that is permanently flowing points = 0 D 4.2. De th of store a durin wetperiods; Estimate the height of ponding above the bottom of the outlet. For wetlands with no outlet measure from the surface of permanent water or if dry, the deepest part. Marks of ponding are 3 ft or more above the surface or bottom of outlet points = 7 Marks of ponding between 2 ft to < 3 ft from surface or bottom of outlet points = 5 3 Marks are at least 0.5 ft to < 2 ft from surface or bottom of outleto nts�= The wetland is a "headwater" wetland points = 3 Wetland is flat but has small depressions on the surface that trap water points = 1 Marks of ponding less than 0.5 ft (6 in) points = 0 D 4.3. Contribution of the wetland to storaize in the watershed: Estimate the ratio of the area of upstream basin contributing surface water to the wetland to the area of the wetland unit itself. The area of the basin is less than 10 times the area of the unit points = 5 3 The area of the basin is 10 to 100 times the area of the unit Q ,oint _ The area of the basin is more than 100 times the area of the unit points = 0 Entire wetland is in the Flats class points = 5 Total for D 4 Add the points in the boxes above 10 Rating of Site Potential If score is: 12-16 = H X6-11 = M 0-5 = L Record the rating on the first page Rating of Landscape Potential If score is:_X3 = H _1 or 2 = M _0 = L Recora the raring on me jirsr page D 6.0. Are the hydrologic functions Provided by the site valuable to soci D 6.1. The unit Is in a landsca a that has floodin roblems. Choose the description that best matches conditions around the wetland unit being rated. Do not add points. Choose the hi hest score if more than one condition is met. The wetland captures surface water that would otherwise flow down -gradient into areas where flooding has damaged human or natural resources (e.g., houses or salmon redds): • Flooding occurs in a sub -basin that is immediately down -gradient of unit. points = 2 • Surface flooding problems are in a sub -basin farther down -gradient. oints - Flooding from groundwater is an issue in the sub -basin. points = 1 The existing or potential outflow from the wetland is so constrained by human or natural conditions that the water stored by the wetland cannot reach areas that flood. Explain why points = 0 There are no problems with flooding downstream of the wetland. points = 0 D 6.2. Has the site been identified as important for flood storage or flood conveyance in a regional flood control Ian? Y e s = 2 X10=0 Total for D 6 Rating of Value If score is: _-2-4=H X I=M _0 = L Wetland Rating System for Western WA: 2014 Update Rating Form - Effective January 1, 2015 1 Add the points in the boxes above N 1 Record the rating on the first page 0 Wetland name or number R These questions apply to wetlands of all HGM classes. HABITAT FUNCTIONS - Indicators that site functions to provide important habitat H 1.0. Does the site have the potential to provide habitat? H 1.1. Structure of plant community: Indicators are Cowardin classes and strata within the Forested class. Check the Cowardin plant classes in the wetland. Up to 10 patches may be combined for each class to meet the threshold of % ac or more than 10% of the unit if it is smaller than 2.5 ac. Add the number of structures checked. Aquatic bed 4 structures or more: points = 4 Emergent 3 structures: points = 2 Scrub -shrub (areas where shrubs have > 30% cover) 2 structures: points = 1 0 _Forested (areas where trees have > 30% cover) 1 structure: points = 0 If the unit has a Forested class, check if.• The Forested class has 3 out of 5 strata (canopy, sub -canopy, shrubs, herbaceous, moss/ground-cover) that each cover 20% within the Forested polygon H 1.2. Hydroperiods Check the types of water regimes (hydroperiods) present within the wetland. The water regime has to cover more than 10% of the wetland or % ac to count (see text for descriptions of hydroperiods). Permanently flooded or inundated 4 or more types present: points = 3 _XSeasonally flooded or inundated 3 types present: points = 2 Occasionally flooded or inundated 2 types present: points = 1 Saturated only 1 type present: points = 0 1 Permanently flowing stream or river in, or adjacent to, the wetland Seasonally flowing stream in, or adjacent to, the wetland Lake Fringe wetland 2 points Freshwater tidal wetland 2 points H 1.3. Richness of plant species Count the number of plant species in the wetland that cover at least 10 ft'. Different patches of the same species can be combined to meet the size threshold and you do not have to name the species. Do not include Eurasian milfoil, reed canarygrass, purple loosestrife, Canadian thistle 1 If you counted: > 19 species points = 2 5 - 19 species points = 1 < 5 species points = 0 H 1.4. Interspersion of habitats Decide from the diagrams below whether interspersion among Cowardin plants classes (described in H 1.1), or the classes and unvegetated areas (can include open water or mudflats) is high, moderate, low, or none. If you have four or more plant classes or three classes and open water, the rating is always high. None = 0 points Low = 1 point Moderate = 2 points 0 i All three diagrams in this row ///i % 0 �%///%/ a!i 6� J'/ • /iii / �/� /� / �i / ��/ �O /�i////� ��a���/lDl are HIGH= 3pOlnts a/j,/ //,,,, , J, ,�,,,r � �i�% o %0/�ii//iii/D/;J/ J Wetland Rating System for Western WA: 2014 Update 13 Rating Form — Effective January 1, 2015 Wetland name or number B H 1.5. Special habitat features: Check the habitat features that are present in the wetland. The number of checks is the number of points. X Large, downed, woody debris within the wetland (> 4 in diameter and 6 ft long). Standing snags (dbh > 4 in) within the wetland Undercut banks are present for at least 6.6 ft (2 m) and/or overhanging plants extends at least 3.3 ft (1 m) over a stream (or ditch) in, or contiguous with the wetland, for at least 33 ft (10 m) Stable steep banks of fine material that might be used by beaver or muskrat for denning (> 30 degree slope) OR signs of recent beaver activity are present (cut shrubs or trees that have not yet weathered 3 where wood is exposed) At least X ac of thin -stemmed persistent plants or woody branches are present in areas that are permanently or seasonally inundated (structures for egg -laying by amphibians) X Invasive plants cover less than 25% of the wetland area in every stratum of plants (see H 1.1 for list of strata) Total for H 1 Add the points in the boxes above 1 5 Rating of Site Potential If score is: 15-18 = H _7-14 = M __X_0-6 = L Record the rating on the first page H 2.0. Does the landscape have the potential to support the habitat functions of the site? H 2.1. Accessible habitat (include only habitat that directly abuts wetland unit). Calculate: % undisturbed habitat 0 + [(% moderate and low intensity land uses)/2]D = 0 % If total accessible habitat is: > 1/3 (33.3%) of 1 km Polygon points = 3 20-33% of 1 km Polygon points = 2 0 10-19% of 1 km Polygon points = 1 < 10% of 1 km Polygonpoints = 0 ........ ....... H 2.2. Undisturbed habitat in 1 km Polygon around the wetland. Calculate: % undisturbed habitat 0 + [(% moderate and low intensity land uses)/2] 0 = 0 Undisturbed habitat > 50% of Polygon points = 3 Undisturbed habitat 10-50% and in 1-3 patches points = 2 0 Undisturbed habitat 10-50% and > 3 patches points = 1 Undisturbed habitat < 10% of 1 km Polygon points = 0 H 2.3. Land use intensity in 1 km Polygon: If �- > 50% of 1 km Polygon is high intensity land use 2T! = (-]2) -2 5 50% of 1 km Polygon is high intensity points = 0 Total for H 2 Add the points in the boxes above -2 Rating of Landscape Potential If score is: _4-6=H —1-3=M X <1=L Record the rating on the first page H 3.0. Is the habitat provided by the site valuable to society? H 3.1. Does the site provide habitat for species valued in laws, regulations, or policies? Choose only the highest score that applies to the wetland being rated. Site meets ANY of the following criteria: points = 2 — It has 3 or more priority habitats within 100 m (see next page) — It provides habitat for Threatened or Endangered species (any plant or animal on the state or federal lists) — It is mapped as a location for an individual WDFW priority species — It is a Wetland of High Conservation Value as determined by the Department of Natural Resources — It has been categorized as an important habitat site in a local or regional comprehensive plan, in a Shoreline Master Plan, or in a watershed plan Site has 1 or 2 priority habitats (listed on next page) within 100 m (Zoints = 1 Site does not meet anv of the criteria above points = 0 Rating of Value If score is:_2 = H -X__1= M _0 = L Record the rating on the first page Wetland Rating System for Western WA: 2014 Update 14 Rating Form - Effective January 1, 2015 Wetland name or number B WDF'W Prionty Habitats Prigrity habitats listed by WDEW (see complete descriptions of WDFW priority habitats, and the counties in which they can be found, in: Washington Department of Fish and Wildlife. 2008. Priority Habitat and Species List. Olympia, Washington. 177 pp. moi: /wdf&w,wa,ggyl li a t o- s Rdf- or access the list from here: http-:// dfw.wa,aov Qut L . (jp..k : Count how many of the following priority habitats are within 330 ft (100 m) of the wetland unit: NOTE. This question is independent of the land use between the wetland unit and the priority habitat. — Aspen Stands: Pure or mixed stands of aspen greater than 1 ac (0.4 ha). Biodiversity Areas and Corridors: Areas of habitat that are relatively important to various species of native fish and wildlife (full descriptions in WDFW PHS report). — Herbaceous Balds: Variable size patches of grass and fortis on shallow soils over bedrock. — Old-growth/Mature forests: - Stands of at least 2 tree species, forming a multi- layered canopy with occasional small openings; with at least 8 trees/ac (20 trees/ha ) > 32 in (81 cm) dbh or > 200 years of age. MatUre forests - Stands with average diameters exceeding 21 in (53 cm) dbh; crown cover may be less than 100%; decay, decadence, numbers of snags, and quantity of large downed material is generally less than that found in old-growth; 80-200 years old west of the Cascade crest. Oregon White Oak: Woodland stands of pure oak or oak/conifer associations where canopy coverage of the oak component is important (full descriptions in WDFW PHS report p. 158 - see web link above). — Riparian: The area adjacent to aquatic systems with flowing water that contains elements of both aquatic and terrestrial ecosystems which mutually influence each other. — Westside Prairies: Herbaceous, non -forested plant communities that can either take the form of a dry prairie or a wet prairie (full descriptions in WDFW PHS report p. 161 - see web link above). — Instream: The combination of physical, biological, and chemical processes and conditions that interact to provide functional life history requirements for instream fish and wildlife resources. Nearshore: Relatively undisturbed nearshore habitats. These include Coastal Nearshore, Open Coast Nearshore, and Puget Sound Nearshore. (full descriptions of habitats and the definition of relatively undisturbed are in WDFW report - see web link on previous page). — Caves: A naturally occurring cavity, recess, void, or system of interconnected passages under the earth in soils, rock, ice, or other geological formations and is large enough to contain a human. — Cliffs: Greater than 25 ft (7.6 m) high and occurring below 5000 ft elevation. — Talus: Homogenous areas of rock rubble ranging in average size 0.5 - 6.5 ft (0.15 - 2.0 m), composed of basalt, andesite, and/or sedimentary rock, including riprap slides and mine tailings. May be associated with cliffs. X Snags and Logs: Trees are considered snags if they are dead or dying and exhibit sufficient decay characteristics to enable cavity excavation/use by wildlife. Priority snags have a diameter at breast height of > 20 in (51 cm) in western Washington and are > 6.5 ft (2 m) in height. Priority logs are > 12 in (30 cm) in diameter at the largest end, and > 20 ft (6 m) long. Note: All vegetated wetlands are by definition a priority habitat but are not included in this list because they are addressed elsewhere. Wetland Rating System for Western WA: 2014 Update 15 Rating Form - Effective January 1, 2015 Wetland name or number B CATEGORIZATION BASED ON SPECIAL CHARACTERISTICS SC 1.0. Estuarine wetlands Does the wetland meet the following criteria for Estuarine wetlands? —The dominant water regime is tidal, —Vegetated, and — With a salinity greater than 0.5 ppt Yes –Go to SC 1.1 QI blot an estuarine wellJw SC 1.1. Is the wetland within a National Wildlife Refuge, National Park, National Estuary Reserve, Natural Area Preserve, State Park or Educational, Environmental, or Scientific Reserve designated under WAC 332-30-151? Yes = Category I No - Go to SC 1.2 Cat. I SC 1.2. Is the wetland unit at least 1 ac in size and meets at least two of the following three conditions? —The wetland is relatively undisturbed (has no diking, ditching, filling, cultivation, grazing, and has less than 10% cover of non-native plant species. (If non-native species are Spartina, see page 25) Cat. I —At least % of the landward edge of the wetland has a 100 ft buffer of shrub, forest, or un -grazed or un - mowed grassland. Cat. II —The wetland has at least two of the following features: tidal channels, depressions with open water, or contiguous freshwater wetlands. Yes = Category I No = Category 11 SC 2.0. Wetlands of High Conservation Value (WHCV) SC 2.1. Has the WA Department of Natural Resources updated their website to include the list of Wetlands of High Conservation Value? Yes – Go to SC 2.2 No – Go to SC 2.3 Cat. I SC 2.2. Is the wetland listed on the WDNR database as a Wetland of High Conservation Value? Yes= Category INo = Not a WHCV SC 2.3. Is the wetland in a Section/Township/Range that contains a Natural Heritage wetland? I�tt : wwwl.d�nr.w°a. acv nh refdesk datasearch wunh wetNands. df Yes – Contact WNHP/WDNR and go to SC 2.4 No =Not a WHCV SC 2.4. Has WDNR identified the wetland within the S/T/R as a Wetland of High Conservation Value and listed it on their website? Yes= Category I No = Not a WHCV SC 3.0. Bogs Does the wetland (or any part of the unit) meet both the criteria for soils and vegetation in bogs? Use the key below. If you answer YES you will still need to rate the wetland based on its functions. SC 3.1. Does an area within the wetland unit have organic soil horizons, either peats or mucks, that compose 16 in or more of the first 32 in of the soil profile? Yes - Go to SC 3.3 No - Go to SC 3.2 SC 3.2. Does an area within the wetland unit have organic soils, either peats or mucks, that are less than 16 in deep over bedrock, or an impermeable hardpan such as clay or volcanic ash, or that are floating or pond? Yes - Go to SC 3.3 No = Is not a bo SC 3.3. Does an area with peats or mucks have more than 70% cover of mosses at ground level, AND at a cover of plant species listed in Table 4? Yes = Is a Category I bog No – Go to SC 3.4 NOTE: If you are uncertain about the extent of mosses in the understory, you may substitute that criterion by measuring the pH of the water that seeps into a hole dug at least 16 in deep. If the pH is less than 5.0 and the plant species in Table 4 are present, the wetland is a bog. Cat. 1 SC 3.4. Is an area with peats or mucks forested (> 30% cover) with Sitka spruce, subalpine fir, western red cedar, western hemlock, lodgepole pine, quaking aspen, Engelmann spruce, or western white pine, AND any of the species (or combination of species) listed in Table 4 provide more than 30% of the cover under the canopy? Yes = Is a Category I bog No = Is not a bog Wetland Rating System for Western WA: 2014 Update 16 Rating Form – Effective January 1, 2015 Wetland name or number B SC 4.0. Forested Wetlands Does the wetland have at least ccnt�,uoars acre of forest that meets one of these criteria for the WA Department of Fish and Wildlife's forests as priority habitats? If you answer YES you will still need to rate the wetland based on its functions. — Old-growth forests (west of Cascade crest): Stands of at least two tree species, forming a multi -layered canopy with occasional small openings; with at least 8 trees/ac (20 trees/ha) that are at least 200 years of age OR have a diameter at breast height (dbh) of 32 in (81 cm) or more. — Mature forests (west of the Cascade Crest): Stands where the largest trees are 80- 200 years old OR the species that make up the canopy have an average diameter (dbh) exceed _2 in 15ASm Yes= Category 1 - Nat a forested wetland for this sectio Cat. SC 5.0. Wetlands in Coastal Lagoons Does the wetland meet all of the following criteria of a wetland in a coastal lagoon? —The wetland lies in a depression adjacent to marine waters that is wholly or partially separated from marine waters by sandbanks, gravel banks, shingle, or, less frequently, rocks The lagoon in which the wetland is located contains ponded water that is saline or brackish (> 0.5 ppt) during most of the year in at least a portion of the lagoon (needs t "fired near the bottom Yes - Go to SC S. o = Not a wetland in a coastal lagoon Cat. SC 5.1. Does the wetland meet all of the following three conditions? —The wetland is relatively undisturbed (has no diking, ditching, filling, cultivation; grazing , end lies less than 20% cover of aggressive, opportunistic plant species (see list of species on p. 100). Cat. II —At least % of the landward edge of the wetland has a 100 ft buffer of shrub, forest, or un -grazed or un - mowed grassland. —The wetland is larger than 1/10 ac (4350 ftZ) Yes = Category I No = Category II SC 6.0. Interdunal Wetlands Is the wetland west of the 1889 line (also called the Western Boundary of Upland Ownership or WBUO)? If you answer yes you will still need to rate the wetland based on its habitat functions. In practical terms that means the following geographic areas: — Long Beach Peninsula: Lands west of SR 103 — Grayland-Westport: Lands west of SR 105 Cat I — Ocean Shores-Copalis: Lands west of SR 115 and SR 109 Yes - Go to SC 6.1 No = not an interdunal wetland for rating "Cat. SC 6.1. Is the wetland 1 ac or larger and scores an 8 or 9 for the habitat functions on tKe—T& es ;W, or H,H,M 11 for the three aspects of function)? Yes= CategoryI No - Go to SC 6.2 SC 6.2. Is the wetland 1 ac or larger, or is it in a mosaic of wetlands that is 1 ac or larger? Yes = Category II No - Go to SC 6.3 Cat. III SC 6.3. Is the unit between 0.1 and 1 ac, or is it in a mosaic of wetlands that is between 0.1 and 1 ac? Yes = Category III No = Category IV Cat. IV Category of wetland based on Special Characteristics If you answered No for all types, enter "Not Applicable" on Summary Form N/A Wetland Rating System for Western WA: 2014 Update 17 Rating Form - Effective January 1, 2015 "Al t �'at!rl�J4 OP ff g fy f fi :l or !ld it/i f%ro ��gy"', �y r�e�,vw�j�u,�o,,n"ioDUl Nwi «� I�r�tt➢11N�lilrrw8(�i�i".' i �;� u gyl/////!(Giiiiiaii, (forI wmg N ple fg)'s Ave AVE OX Z 41 AA DA, ra w E r " ee� xS R #i- MR)"O Jq M:QAV 44'08 N"a"N' p"A0111Y, W9 C4 11V mm z a AV 4096 4 A tV, M DAV pito L A Im,OAM 1412L 21" MN, OAV qjCL '*Ad VV 66 ov 1,14 0 1 MI J014W J, L QhIflez N OA V too, 0 '���/��� /,/!!/c%rim , ...... ....... M WATER QUALITY IMPROVEMENT PROJECTS (TMDLS) overview of the process Project Catalog by WRIA by county Funding Opportunities Project Development Priority Lists Related information TMDL Contacts RELATED ECOLOGY PROGRAMS Water Quality Im-Ap�. WRIA 8: Cedar- Samnia mish The following table lists overview information for water quality improvement projects (including total maximum daily loads, or TMDLs) for this water resource NO inventory area (ARIA). Please use links (where available) for more information on a project. Counties 07i • King • Snohomish Waterbody Name Pollutants Status" I TMOL Lead -- ---------- --- ------ ­­ . ..... . -111-1- - - - — - - ---------------- - Eallon r q jLkk gj . ..... Total Phosphorus Approved by EPA Tricia Shoblom 425-649-7288 rear- —Lam 1 �rr A&A ILI P Fecal Coliform Approved by EPA Joan Nolan Dissolved Oxygen .. . .. . ........... Approved by EPA 425-649-4425 Temperature . ..................... Cotta _qe.Lake Total Phosphorus Approved by EPA Tricia Shoblom Has an implementation 425-649-7286 plan - Fecal Coliform - -- --------- ---------- Approved by EPA )oan No 1425-649-4425 �p44r fir, ---- Fecal coliform ---- .... . ..................... . . Approved by EPA .... __ ........ .... . . ......... Ralph svricek 425-649-7036 Tributaries: Trout Stream Great Dane Creek Cutthroat Creek -1111-- ----------------------- North Creek . . .............. . . . . Fecal Coliform . . ...... . ........... Approved by EPA ..................... Bpi ���k Has an implementation 425-649-7036 plan Pipers Creak Fecal Coliform Approved by EPA loan Nolan 425-649-"25 ammami5h Rver Dissolvad C;;;gr Fe Ra 1ph Sv r c e 425-649-7036 Temperature summer 2015 .... . . . . ........................ . aAqMp Creek Fecal Coliform Approved by EPA Ralh Svrice 425-649-7036 Has an implementation Wetland name or number C TING SUMMARY - Western Washington Name of wetland (or ID #): wetland C Date of site visit: 7/6 and 7/7/15 Rated by S. Corbin PW Trained by Ecology?_ Yes No Date of trainingl0/09 and 5/14 HGM Class used for rating Slope Wetland has multiple HGM classes?_Y X N NOTE: Form is not complete without the figures requested (figures can be combined). Source of base aerial photo/map Google Earth OVERALL WETLAND CATEGORY IV (based on functions or special characteristics_) 1. Category of wetland based on FUNCTIONS Category I — Total score = 23 - 27 Category II — Total score = 20 - 22 Category III — Total score = 16 - 19 X Category IV — Total score = 9 - 15 FUNCTION Improving Hydrologic Habitat Water Quality Circle the appropriate ratings ite Potential H M L H M L H M L ._ m . ....... _W .andscape Potential H M L H M L H M L Value H L H L H M i L TOTAL .-......... _....... . core Based on 5 4 4 13 tatings 2. Category based on SPECIAL CHARACTERISTICS of wetland CHARACTERISTIC CATEGORY Estuarine I II Wetland of High Conservation Value I Bog L Mature Forest I Old Growth Forest I Coastal Lagoon I II Interdunal I II III IV None of the above Wetland Rating System for Western WA: 2014 Update Rating Form - Effective January 1, 2015 Score for each function based on three ratings (order of ratings is not important) 9 = H,H,H 8 = H,H,M 7 = H,H,L 7 = H,M,M 6 = H,M,L 6 = M,M,M 5 = H,L,L 5 = M, M, L 4 = M,L,L 3 = L,L,L 1 Wetland name or number C Maps and figures required to answer questions correctly for Western Washington Depression l Wetlands Map of: To answer questions: Figure # Cowardin plant classes D 1.3, H 1.1, H 1.4 ............... Hydroperiods D 1.4, H 1.2 Location of outlet (can be added to map of hydroperiods) D 1.1, D 4.1 Boundary of area within 150 ft of the wetland (can be added to another figure) D 2.2,D 5.2 Map of the contributing basin D 4.3, D 5.3 1 km Polygon: Area that extends 1 km from entire wetland edge - including H 2.1, H 2.2, H 2.3 polygons for accessible habitat and undisturbed habitat Screen capture of map of 303(d) listed waters in basin (from Ecology website) D 3.1, D 3.2 Screen capture of list of TMDLs for WRIA in which unit is found (from web) D 3.3 Riverine Wetlands Map of: To answer questions: Figure # Cowardin plant classes H 1.1, H 1.4 Hydroperiods H 1.2 Ponded depressions R 1.1 Boundary of area within 150 ft of the wetland (can be added to another figure) R 2.4 Plant cover of trees, shrubs, and herbaceous plants R 1.2, R 4.2 Width of unit vs. width of stream (can be added to another figure) R 4.1 Map of the contributing basin R 2.2, R 2.3, R 5.2 1 km Polygon: Area that extends 1 km from entire wetland edge - including H 2. 1, H 2.2, H 2.3 Polygons for accessible habitat and undisturbed habitat Screen capture of map of 303(d) listed waters in basin (from Ecology website) R 3.1 Screen capture of list of TMDLs for WRIA in which unit is found (from web) R 3.2, R 3.3 Lake Fringe Wetlands Map of: To answer questions: Figure # Cowardin plant classes L 1.1, L 4.1, H 1.1, H 1.4 Plant cover of trees, shrubs, and herbaceous plants L 1.2 Boundary of area within 150 ft of the wetland (can be added to another figure) L 2.2 .......... --. 1 km Polygon: Area that extends 1 km from entire wetland edge - including H 2.1, H 2.2, H 2.3 polygons for accessible habitat and undisturbed habitat Screen capture of map of 303(d) listed waters in basin (from Ecology website) L 3.1, L 3.2 Screen capture of list of TMDLs for WRIA in which unit is found (from web) L 3.3 Slope Wetlands Map of: To answer questions: Figure # Cowardin plant classes H 1.1, H 1.4 1 Hydroperiods H 1.2 1 Plant....... cover of dense trees, shrubs, and herbaceous plants S 1.3 1 _ Plant cover of dense, rigid trees, shrubs, and herbaceous plants S4.1 1 (can be added to figure above) Boundary of 150 ft buffer (can be added to another figure) S 2.1, S 5.1 1 1 km Polygon: Area that extends 1 km from entire wetland edge - including H 2.1, H 2.2, H 2.3 2 polygons for accessible habitat and undisturbed habitat Screen capture of map of 303(d) listed waters in basin (from Ecology website) S 3.1, S 3.2 3 Screen capture of list of TMDLs for WRIA in which unit is found (from web) S3.3 4 Wetland Rating System for Western WA: 2014 Update 2 Rating Form - Effective January 1, 2015 Wetland name or number C HGM Classification of Wetlands in 'western Washington For questions 1-7, the criteria described must apply to the entire unit being rated. If the hydrologic criteria listed in each question do not apply to the entire unit being rated, you probably have a unit with multiple HGM classes. In this case, identify which hydrologic criteria in questions 1-7 apply, and go to Question B. 1. Are hp ter levels in the entire unit usually controlled by tides except during floods? �NO - go to 2 YES - the wetland class is Tidal Fringe - go to 1.1 1.1 Is the salinity of the water during periods of annual low flow below 0.5 ppt (parts per thousand)? NO - Saltwater Tidal Fringe (Estuarine) YES - Freshwater Tidal Fringe Ifyour wetland can be classified as a Freshwater Tidal Fringe use the forms for Riverine wetlands. If it is Saltwater Tidal Fringe it is an Estuarine wetland and is not scored. This method cannot be used to score functions for estuarine wetlands. 2. The entire wetland unit is flat and precipitation is the only source (>90%) of water to it. Groundwater and surface water runoff are NOT sources of water to the unit. g - go to 3 YES - The wetland class is Flats Z=h can be classified as a Flats wetland, use the form for Depressional wetlands. 3. Does the entire wetland unit meet all of the following criteria? _The vegetated part of the wetland is on the shores of a body of permanent open water (without any plants on the surface at anytime of the year) at least 20 ac (8 ha) in size; _At least 30% of the open water area is deeper than 6.6 ft (2 m).. CNO - go to 4 YES - The wetland class is Lake Fringe (Lacustrine Fringe) 4. Doi 'i the e�Aire wetland unit meet all of the following criteria? The wetland is on a slope (slope can be very gradual), _ The water flows through the wetland in one direction (unidirectional) and usually comes from seeps. It may flow subsurface, as sheetflow, or in a swale without distinct banks, The water leaves the wetland without being impounded. NO - go to 5 Y - The wetland class is Slope NOTE: Surface water does not pond in these type of wetlands except occasi n l in very small and shallow depressions or behind hummocks (depressions are usually <3 ft diameter and less than 1 ft deep). 5. Does the entire wetland unit meet all of the following criteria? The unit is in a valley, or stream channel, where it gets inundated by overbank flooding from that stream or river, The overbank flooding occurs at least once every 2 years. Wetland Rating System for Western WA: 2014 Update Rating Form - Effective January 1, 2015 Wetland name or number C NO - go to 6 YES - The wetland class is Riverine NOTE: The Riverine unit can contain depressions that are filled with water when the river is not flooding 6. Is the entire wetland unit in a topographic depression in which water ponds, or is saturated to the surface, at sometime during the year? This means that any outlet, if present, is higher than the interior of the wetland. NO-goto7 YES - The wetland class is Depressional 7. Is the entire wetland unit located in a very flat area with no obvious depression and no overbank flooding? The unit does not pond surface water more than a few inches. The unit seems to be maintained by high groundwater in the area. The wetland may be ditched, but has no obvious natural outlet. NO-goto8 YES - The wetland class is Depressional 8. Your wetland unit seems to be difficult to classify and probably contains several different HGM classes. For example, seeps at the base of a slope may grade into a riverine floodplain, or a small stream within a Depressional wetland has a zone of flooding along its sides. GO BACK AND IDENTIFY WHICH OF THE HYDROLOGIC REGIMES DESCRIBED IN QUESTIONS 1-7 APPLY TO DIFFERENT AREAS IN THE UNIT (make a rough sketch to help you decide). Use the following table to identify the appropriate class to use for the rating system if you have several HGM classes present within the wetland unit being scored. NOTE: Use this table only if the class that is recommended in the second column represents 10% or more of the total area of the wetland unit being rated. If the area of the HGM class listed in column 2 is less than 10% of the unit; classify the wetland using the class that represents more than 90% of the total area. HGM classes within the wetland unit HGM class to being rated use in rating Slope + Riverine Riverine Slope + Depressional Depressional Slope + Lake Fringe Lake Fringe Depressional + Riverine along stream Depressional within boundary of depression Depressional + Lake Fringe Depressional Riverine + Lake Fringe Riverine Salt Water Tidal Fringe and any other Treat as class of freshwater wetland ESTUARINE Ifyou are still unable to determine which of the above criteria apply to your wetland, or ifyou have more than 2 HGM classes within a wetland boundary, classify the wetland as Depressional for the rating. Wetland Rating System for Western WA: 2014 Update 4 Rating Form - Effective January 1, 2015 Wetland name or number C /.,/%//! ,,,,i,,, . /�,,,, ;nil i„/i�����i��// �,,,i ,;,,, �;���//��� ii, . ,.,� ✓iii /,�,, �/, ! . , y/ i� ,,. //I�(/�.,,, ,,�.1 �� i ,/�/"/�. ///%%/i // S 1.0. Does the site have the potential to improve water quality? S 1.1. Characteristics of the average slope of the wetland: (a 1% slope has a 1 ft vertical drop in elevation for every 100 ft of horizontal distance) Slope is 1% or less points — 3 0 Slope is > 1%-2% points — 2 Slope is > 2%-5% Doints — 1 Slope is greater than 5% points = 0 S 1.2. The soil 2 in below the surface 12r duff Ia er is true clay or true organic (case NRCS definitions): Yes = 3 No = 0 0 S 1.3. Characteristics of the plants in the wetland that trap sediments and pollutants: Choose the points appropriate for the description that best fits the plants in the wetland. Dense means you have trouble seeing the soil surface (>75% cover), and uncut means not grazed or mowed and plants are higher than 6 in. Dense, uncut, herbaceous plants > 90% of the wetland area points = 6 0 Dense, uncut, herbaceous plants > % of area points = 3 Dense, woody, plants > % of area points = 2 Dense, uncut, herbaceous plants > % of area points = 1 Does not meet any of the criteria above for plants points = 0 Total for S 1 Add the points in the boxes above L 0 Rating of Site Potential If score is:_12 = H _6-11= M XO -5 = L Record the rating on the first page S 2.0. Does the landscape have the potential to support the water quality function of the site? S 2.1. Is > 10% of the area within 150 ft on the uphill side of the wetland in land uses that generate pollutants? Yes=1 No= 0 0 S 2.2. Are there other sources of pollutants coming into the wetland that are not listed in question S 2.1? Other sources dog poop Yes = 1 No = 0 1 Total for S 2 Add the points in the boxes above 1 Rating of Landscape Potential If score is: X1-2 = M 0 = L Record the rating on the first page S 3.0. Is the water quality improvement provided by the site valuable to society? S 3.1. Does the wetland discharge directly (i.e., within 1 mi) to a stream, river, lake, or marine water that is on the 303(d) list? Yes = 1 No = 0 0 S3.2. Is the wetland in a basin or sub -basin where water quality is an issue? At least one aquatic resource in the basin is on the 303(d) list. Yes = 1 No = 0 1 S Has the si e been :.dentiJ•iled :1 . a -watershed _- 1___1 plan __ '„- ._."._._ c_._ .. n YES) .+.�..i. 1 �aJ ulC DrtG UCCII IU CIIUIICU 111 d -watershed VI IUl.dl �Jldll d� I11I�u1 ldfll. IUI Ifldirl �a�n�fl�' water quaiity� Hnswer rt.i 0 if there is a TMDL for the basin in which unit is found. Yes = 2 No= 0 — Total for S 3 Add the points in the boxes above 1 Rating of Value If score is: L2 -4=H _X1= M _0 = L Record the rating on the first page Wetland Rating System for Western WA: 2014 Update 11 Rating Form — Effective January 1, 2015 Wetland name or number C S 4.0. Does the site have the potential to reduce flooding and stream erosion? S 4.1. Characteristics of plants that reduce the velocity of surface flows during storms: Choose the points appropriate for the description that best fits conditions in the wetland. Stems of plants should be thick enough (usually> 1/s in), or dense enough, to remain erect during surface flows. 0 Dense, uncut, rigid plants cover > 90% of the area of the wetland points =1 All other conditions points = 0 Rating of Site Potential If score is:_1= M _X_0 = L Record the rating on the first page S 5.0. Does the landscape have the potential to support the hydrologic functions of the site? S 5.1. Is more than 25% of the area within 150 ft upslope of wetland in land uses or cover that generate excess 0 surface runoff? Yes = 1 No = 0 Rating of Landscape Potential If score is:_1= M _X0 = L Record the rating on the first page S 6.0. Are the hydrologic functions provided by the site valuable to society? S 6.1. Distance to the nearest areas downstream that have flooding problems: The sub -basin immediately down -gradient of site has flooding problems that result in damage to human or natural resources (e.g., houses or salmon redds) points = 2 1 Surface flooding problems are in a sub -basin farther down -gradient points = 1 No flooding problems anywhere downstream points = 0 S 6.2. Has the site been identified as important for flood storage or flood conveyance in a regional flood control plan? 0 Yes=2 No=0 Total for S 6 Add the points in the boxes above 1 Rating of Value If score is: _-2-4=H X 1=M _0 = L Record the rating on the first page NOTES and FIELD OBSERVATIONS: Wetland Rating System for Western WA: 2014 Update 12 Rating Form - Effective January 1, 2015 Wetland name or number C These questions apply to wetlands of all HGM classes. HABITAT FUNCTIONS - Indicators that site functions to provide important habitat H 1.0. Does the site have the potential to provide habitat? H 1.1. Structure of plant community: Indicators are Cowardin classes and strata within the Forested class. Check the Cowardin plant classes in the wetland. Up to 10 patches may be combined for each class to meet the threshold of % ac or more than 10% of the unit if it is smaller than 2.5 ac. Add the number of structures checked. Aquatic bed 4 structures or more: points = 4 X Emergent 3 structures: points = 2 Scrub -shrub (areas where shrubs have > 30% cover) 2 structures: points = 1 Forested (areas where trees have > 30% cover) 1 structure: points = 0 0 If the unit has a Forested class, check if.• The Forested class has 3 out of 5 strata (canopy, sub -canopy, shrubs, herbaceous, moss/ground-cover) that each cover 20% within the Forested polygon H 1.2. Hydroperiods Check the types of water regimes (hydroperiods) present within the wetland. The water regime has to cover more than 10% of the wetland or % ac to count (see text for descriptions of hydroperiods). Permanently flooded or inundated 4 or more types present: points = 3 Seasonally flooded or inundated 3 types present: points = 2 Occasionally flooded or inundated 2 types present: points = 1 p XSaturated only 1 type present: points = 0 Permanently flowing stream or river in, or adjacent to, the wetland Seasonally flowing stream in, or adjacent to, the wetland Lake Fringe wetland 2 points Freshwater tidal wetland 2 points H 1.3. Richness of plant species Count the number of plant species in the wetland that cover at least 10 ft2. Different patches of the same species can be combined to meet the size threshold and you do not have to name the species. Do not include Eurasian milfoil, reed canarygrass, purple loosestrife, Canadian thistle If you counted: > 19 species points = 2 1 5 - 19 species points = 1 < 5 species points = 0 H 1.4. Interspersion of habitats Decide from the diagrams below whether interspersion among Cowardin plants classes (described in H 1.1), or the classes and unvegetated areas (can include open water or mudflats) is high, moderate, low, or none. If you have four or more plant classes or three classes and open water, the rating is always high. i \� n v None = 0 points Low = 1 point Moderate = 2 points r All three diagrams 0 in this row are HIGH = 3points ;;,, Wetland Rating System for Western WA: 2014 Update 13 Rating Form — Effective January 1, 2015 Wetland name or number C H 1.5. Special habitat features: Check the habitat features that are present in the wetland. The number of checks is the number of points. Large, downed, woody debris within the wetland (> 4 in diameter and 6 ft long). Standing snags (dbh > 4 in) within the wetland Undercut banks are present for at least 6.6 ft (2 m) and/or overhanging plants extends at least 3.3 ft (1 m) over a stream (or ditch) in, or contiguous with the wetland, for at least 33 ft (10 m) Stable steep banks of fine material that might be used by beaver or muskrat for denning (> 30 degree slope) OR signs of recent beaver activity are present (cut shrubs or trees that have not yet weathered where wood is exposed) At least X ac of thin -stemmed persistent plants or woody branches are present in areas that are permanently or seasonally inundated (structures for egg -laying by amphibians) X Invasive plants cover less than 25% of the wetland area in every stratum of plants (see H 1.1 for list of Total for H 1 Add the points in the boxes above 2 Rating of Site Potential If score is: 15-18 = H _7-14 = M g0-6 = L Record the rating on the first page H 2.0. Does the landscape have the potential to support the habitat functions of the site? H 2.1. Accessible habitat (include only habitat that directly abuts wetland unit). Calculate: % undisturbed habitatQ+ [(% moderate and low intensity land uses)/2]Q = 0 % If total accessible habitat is: > 1/3 (33.3%) of 1 km Polygon points = 3 20-33% of 1 km Polygon points = 2 0 10-19% of 1 km Polygon points = 1 < 10% of 1 km Polygon points = 0 H 2.2. Undisturbed habitat in 1 km Polygon around the wetland. Calculate: % undisturbed habitat+ [(% moderate and low intensity land uses)/2]Q = 0 Undisturbed habitat > 50% of Polygon points = 3 Undisturbed habitat 10-50% and in 1-3 patches points = 2 0 Undisturbed habitat 10-50% and > 3 patches points = 1 Undisturbed habitat < 10% of 1 km 'Polygon points = 0 H 2.3. Land use intensity in 1 km Polygon: If > 50% of 1 km Polygon is high intensity land use points = (- 2) -2 <- 50% of 1 km Polygon is high intensity points = 0 Total for H 2 Add the points in the boxes above -2 Rating of Landscape Potential If score is: 4-6 = H _1-3 = M __X_< 1= L Record the rating on the first page H 3.0. Is the habitat provided by the site valuable to society? H 3.1. Does the site provide habitat for species valued in laws, regulations, or policies? Choose only the highest score that applies to the wetland being rated. Site meets ANY of the following criteria: points = 2 — It has 3 or more priority habitats within 100 m (see next page) — It provides habitat for Threatened or Endangered species (any plant or animal on the state or federal lists) — It is mapped as a location for an individual WDFW priority species — It is a Wetland of High Conservation Value as determined by the Department of Natural Resources — It has been categorized as an important habitat site in a local or regional comprehensive plan, in a Shoreline Master Plan, or in a watershed plan Site has 1 or 2 priority habitats (listed on next page) within 100 m points = 1 Site does not meet any of the criteria above points = 0 Rating of Value If score is:__2 = H X 1= M _0 = L Record the rating on the first page Wetland Rating System for Western WA: 2014 Update 14 Rating Form - Effective January 1, 2015 Wetland name or number C WDFW Priority Habitats J joritv habitataby DFW (see complete descriptions of WDFW priority habitats, and the counties in which they can be found, in: Washington Department of Fish and Wildlife. 2008. Priority Habitat and Species List. Olympia, Washington. 177 pp.1 io aiblic• t" 0 65 d , or access the list from here: tt wdfw a. oy o s "o5t ) Count how many of the following priority habitats are within 330 ft (100 m) of the wetland unit: NOTE. This question is independent of the land use between the wetland unit and the priority habitat. — Aspen Stands: Pure or mixed stands of aspen greater than 1 ac (0.4 ha).. — Biodiversity Areas and Corridors: Areas of habitat that are relatively important to various species of native fish and wildlife (full descriptions in WDFW PHS report). Herbaceous Balds: Variable size patches of grass and forbs on shallow soils over bedrock. Old-growth/Mature forests:s ii e � - Stands of at least 2 tree species, forming a multi- wthws�tofCa canopy with occasional small openings; with at least 8 trees/ac (20 trees/ha ) > 32 in (81 cm) dbh or > 200 years of age. Mature forests - Stands with average diameters exceeding 21 in (53 cm) dbh; crown cover may be less than 100%; decay, decadence, numbers of snags, and quantity of large downed material is generally less than that found in old-growth; 80-200 years old west of the Cascade crest. Oregon White Oak: Woodland stands of pure oak or oak/conifer associations where canopy coverage of the oak component is important (full descriptions in WDFW PHS report p. 158 - see web link above). Riparian: The area adjacent to aquatic systems with flowing water that contains elements of both aquatic and terrestrial ecosystems which mutually influence each other. Westside Prairies: Herbaceous, non -forested plant communities that can either take the form of a dry prairie or a wet prairie (full descriptions in WDFW PHS report p. 161 - see web link above). Instream: The combination of physical, biological, and chemical processes and conditions that interact to provide functional life history requirements for instream fish and wildlife resources. Nearshore: Relatively undisturbed nearshore habitats. These include Coastal Nearshore, Open Coast Nearshore, and Puget Sound Nearshore. (full descriptions of habitats and the definition of relatively undisturbed are in WDFW report - see web link on previous page). Caves: A naturally occurring cavity, recess, void, or system of interconnected passages under the earth in soils, rock, ice, or other geological formations and is large enough to contain a human. — Cliffs: Greater than 25 ft (7.6 m) high and occurring below 5000 ft elevation. — Talus: Homogenous areas of rock rubble ranging in average size 0.5 - 6.5 ft (Q.15 - 2.0 m), composed of basalt, andesite, and/or sedimentary rock, including riprap slides and mine tailings. May be associated with cliffs. Snags and Logs: Trees are considered snags if they are dead or dying and exhibit sufficient decay characteristics to enable cavity excavation/use by wildlife. Priority snags have a diameter at breast height of > 20 in (51 cm) in western Washington and are > 6.5 ft (2 m) in height. Priority logs are > 12 in (30 cm) in diameter at the largest end, and > 20 ft (6 m) long. Note: All vegetated wetlands are by definition a priority habitat but are not included in this list because they are addressed elsewhere. Wetland Rating System for Western WA: 2014 Update 15 Rating Form - Effective January 1, 2015 Wetland name or number C_ CATEGORIZATION BASED ON SPECIAL CHARACTERISTICS ,;,................. � ,r � , / / ,rre / , � ; / i � l ✓i � /////iii/,//% �i i � '� /«,ii/j SC 1.0. Estuarine wetlands Does the wetland meet the following criteria for Estuarine wetlands? — The dominant water regime is tidal, —Vegetated, and — With a salinity greater than 0.5 ppt Yes -Go to SC 1.1 No= Not an estuarine wetland SC 1.1. Is the wetland within a National Wildlife Refuge, National Park, National Estuary Reserve, Natural Area Preserve, State Park or Educational, Environmental, or Scientific Reserve designated under WAC 332-30-151? Yes= Category I No - Go to SC 1.2 Cat. SC 1.2. Is the wetland unit at least 1 ac in size and meets at least two of the following three conditions? —The wetland is relatively undisturbed (has no diking, ditching, filling, cultivation, grazing, and has less than 10% cover of non-native plant species. (If non-native species are Spartina, see page 25) Cat. I —At least % of the landward edge of the wetland has a 100 ft buffer of shrub, forest, or un -grazed or un - mowed grassland. —The wetland has at least two of the following features: tidal channels, depressions with open water, or Cat. II contiguous freshwater wetlands. Yes= Category I No = Category II SC 2.0. Wetlands of High Conservation Value (WHCV) SC 2.1. Has the WA Department of Natural Resources updated their website to include the list of Wetlands of High Conservation Value? Yes - Go to SC 2.2 No - Go to SC 2.3 Cat. SC 2.2. Is the wetland listed on the WDNR database as a Wetland of High Conservation Value? Yes= Category I No = Not a WHCV SC 2.3. Is the wetland in a Section/Township/Range that contains a Natural Heritage wetland? ham: wwwl.dnr,wa, ov nh refdeskdatasearch vwnh wetlands, df Yes - Contact WNHP/WDNR and go to SC 2.4 No =Not a WHCV SC 2.4. Has WDNR identified the wetland within the S/T/R as a Wetland of High Conservation Value and listed it on their website? Yes = Category I No = Not a WHCV SC 3.0. Bogs Does the wetland (or any part of the unit) meet both the criteria for soils and vegetation in bogs? Use the key below. if you answer YES you will still need to rate the wetland based on its functions. SC 3.1. Does an area within the wetland unit have organic soil horizons, either peats or mucks, that compose 16 in or more of the first 32 in of the soil profile? Yes - Go to SC 3.3 No - Go to SC 3.2 SC 3.2. Does an area within the wetland unit have organic soils, either peats or mucks, that are less than 16 in deep over bedrock, or an impermeable hardpan such as clay or volcanic ash, or that are floating on top of a lake or pond? Yes - Go to SC 3.3 No = Is not a bog SC 3.3. Does an area with peats or mucks have more than 70% cover of mosses at ground level, AND at least a 30% cover of plant species listed in Table 4? Yes = Is a Category I bog No - Go to SC 3.4 NOTE: If you are uncertain about the extent of mosses in the understory, you may substitute that criterion by measuring the pH of the water that seeps into a hole dug at least 16 in deep. If the pH is less than 5.0 and the plant species in Table 4 are present, the wetland is a bog. Cat. I SC 3.4. Is an area with peats or mucks forested (> 30% cover) with Sitka spruce, subalpine fir, western red cedar, western hemlock, lodgepole pine, quaking aspen, Engelmann spruce, or western white pine, AND any of the species (or combination of species) listed in Table 4 provide more than 30% of the cover under the canopy? Yes = Is a Category I bog No = Is nota bog Wetland Rating System for Western WA: 2014 Update 16 Rating Form - Effective January 1, 2015 Wetland name or number SC 4.0. Forested Wetlands Does the wetland have at least 1 contigy us acre of forest that meets one of these criteria for the WA Department of Fish and Wildlife's forests as priority habitats? If you answer YES you will still need to rate the wetland based on its functions. — Old-growth forests (west of Cascade crest): Stands of at least two tree species, forming a multi -layered canopy with occasional small openings; with at least 8 trees/ac (20 trees/ha) that are at least 200 years of age OR have a diameter at breast height (dbh) of 32 in (81 cm) or more. — Mature forests (west of the Cascade Crest): Stands where the largest trees are 80- 200 years old OR the species that make up the canopy have an average diameter (dbh) exceeding 21 in (53 cm). Yes= Category I No = Not a forested wetland for this section Cat. I SC 5.0. Wetlands in Coastal Lagoons Does the wetland meet all of the following criteria of a wetland in a coastal lagoon? — The wetland lies in a depression adjacent to marine waters that is wholly or partially separated from marine waters by sandbanks, gravel banks, shingle, or, less frequently, rocks —The lagoon in which the wetland is located contains ponded water that is saline or brackish (> 0.5 ppt) during most of the year in at least a portion of the lagoon (needs to be measured near the bottom) Cat. I Yes - Go to SC 5.1 No = Not a wetland in a coastal lagoon SC 5.1. Does the wetland meet all of the following three conditions? —The wetland is relatively undisturbed (has no diking, ditching, filling, cultivation, grazing), and has less than 20% cover of aggressive, opportunistic plant species (see list of species on p. 100). Cat. II —At least % of the landward edge of the wetland has a 100 ft buffer of shrub, forest, or un -grazed or un - mowed grassland. —The wetland is larger than 1/10 ac (4350 ftZ) Yes= CategoryI No =Category II SC 6.0. Interdunal Wetlands Is the wetland west of the 1889 line (also called the Western Boundary of Upland Ownership or WBUO)? If you answer yes you will still need to rate the wetland based on its habitat functions. In practical terms that means the following geographic areas: — Long Beach Peninsula: Lands west of SR 103 — Grayland-Westport: Lands west of SR 105 Cat i — Ocean Shores-Copalis: Lands west of SR 115 and SR 109 Yes - Go to SC 6.1 No = not an Interdunal wetland for rating SC 6.1. Is the wetland 1 ac or larger and scores an 8 or 9 for the habitat functions on the form (rates H,H,H or H,H,M Cat. II for the three aspects of function)? Yes= CategoryI No - Go to SC 6.2 SC 6.2. Is the wetland 1 ac or larger, or is it in a mosaic of wetlands that is 1 ac or larger? Yes = Category II No - Go to SC 6.3 Cat. III SC 6.3. Is the unit between 0.1 and 1 ac, or is it in a mosaic of wetlands that is between 0.1 and 1 ac? Yes = Category III No = Category IV Cat. IV Category of wetland based on Special Characteristics If you answered No for all types, enter "Not Applicable" on Summary Form Wetland Rating System for Western WA: 2014 Update 17 Rating Form - Effective January 1, 2015 x ollut P llPoutant r generating t surface ro rr tt m r L+�'�� µ r�{ r 1M,�.ua LE7 i ' ,Rm 5 44 �Sf � -I W 24 i,tiCyt w � , Cz7r% 7. �'32rr��i c r �t �i '` CD z n y aV 9Y7�14 } (p uu f'�' fit^"' �7 ri" „ ian lTi row x' x a tiJ V (1) /14 ollq 17� Sl 23 7l 11Ut !✓��wU �,l Mw w ws M- A b' Lam'}� � 5 . .. - m r a w RPM, M)PIN" " * r c3 �� "� 100% i1 kmi ,� e "" ❑ �7 �� 'M `buffer= � r� a ,„ 'w land use � ,�✓ (�y �"+Mx, /4 Ow") � Ilvhv g8A'V b t�h NSI 'rq Z QI fA "f v c Alf "196 [V en r � Ilvhv g8A'V b 'rq Z f 'IIl -AAN OW WGA' ��;�MN�an11��N9F P If m ®. 4 Ito L Im o+�b 4121 r" act V k WO Vt MN v Woe, MPO wro �, . WATER QUALITY IMPROVEMENT PROJECTS (TMDLs) Overview of the process Project Catalog by WWRIA by County Funding opportunities Project Development Priority Lists Related information TMDL Contacts RELATED ECOLOGY PROGRAMS Water Quality dk WRIA 8- Cedar-Sammalit The following table lists overview information for water quality improvement PollutantsStatus"`TMlDL Lead -------- - - poi projects (including total maximum daily loads, or TMDLs) for this water resource - - -------- - ----- ---- Approved by EPA Incia-1hoblom inventory area (ASIA). Please use links (where available) for more information jX Fecal Coliform . ........ Dissolved Oxygen Approved by EPA .............. Approved by EPA - ------ ------ Joan Nolan gm ............. 425-649-4425 Temperature . ......... . . . . .............................. . ......... . ..... . ...... . .. . ............ . ............ V on a project. Total Phosphorus Approved by EPA Tricia Shoblo 425T649-7288 Has an implementation plan ..... . . . ..... ...................... 11"Aah r—r=k-fig= K' I N G A loan Nolan 425-649-4425 Counties .. ...................... . - Fecal Coliform . . . . . ... ... ... .. .................................... ... Approved by EPA — - Ralph Svrice 425-649-7036 • King Trout Stream m U Great Dane •anohom-ish Creek Cutthroat Creek North Creek — ------------------- Fecal Coliform Waterbody Name PollutantsStatus"`TMlDL Lead -------- - - poi -- ---- Total Phosphorus - - -------- - ----- ---- Approved by EPA Incia-1hoblom 425-649-7288 Sear Evans Creek Basin Fecal Coliform . ........ Dissolved Oxygen Approved by EPA .............. Approved by EPA - ------ ------ Joan Nolan gm ............. 425-649-4425 Temperature . ......... . . . . .............................. . ......... . ..... . ...... . .. . ............ . ............ ................ Cottage Lake Total Phosphorus Approved by EPA Tricia Shoblo 425T649-7288 Has an implementation plan ..... . . . ..... ...................... 11"Aah r—r=k-fig= Fecal Coliform ......... Approved by EPA loan Nolan 425-649-4425 ........... . . . ....... .. ...................... . - Fecal Coliform . . . . . ... ... ... .. .................................... ... Approved by EPA — - Ralph Svrice 425-649-7036 Tributaries: Trout Stream m Great Dane Creek Cutthroat Creek North Creek — ------------------- Fecal Coliform ----------------------------------- - ---------- ---- - Approved by EPA Svrcek Has an implementation 425-649-7036 plan PMiers Crr&k Fecal Coliform Approved by EPA JoanNolan 425-649-4425 . ............... . .................. . . . . . . . . . . . --- Sammamish River ...... . ...... Dissolved Oxygen Field work starts ................ .. ... Bgisl h Syr cek ---j— ........ ...... Temperature --- --- — — summer 2015 - ------ 425-649-7036 aAgl �Cr Creek Fecal Coliform Approved by EPA Svricek Has an implementation 425-649-7036 qetland C Rating Figure 3. WRIA 8 TMDL Screen Shot SHANNON WLSON. Wa APPENDIX D IMPORTANT INFORMATION ABOUT YOUR WETJ. ANI) DELINEATION/MITI A, BION ANIWOR STREAMLA SI�� �OATION REPORT 21-1-22082-002 SHANNON $ WILSON, INC. Attachment to and part of Report 21-1-22082-002 Geotechnical and Environmental Consultants Date: August 4, 2016 To: Ms. Taine Wilton _ Edmonds School District #15 IMPORTANT INFORMATION ABOUT YOUR WETLAND DELINEATIONNITIGATION AND/OR STREAM CLASSIFICATION DEPORT A WETLAND/STREAM REPORT IS BASED ON PROJECT -SPECIFIC FACTORS. Wetland delineation/mitigation and stream classification reports are based on a unique set of project -specific factors. These typically include the general nature of the project and property involved, its size, and its configuration; historical use and practice; the location of the project on the site and its orientation; and the level of additional risk the client assumed by virtue of limitations imposed upon the exploratory program. The jurisdiction of any particular wetland/stream is determined by the regulatory authority(s) issuing the permit(s). As a result, one or more agencies will have jurisdiction over a particular wetland or stream with sometimes confusing regulations. It is necessary to involve a consultant who understands which agency(s) has jurisdiction over a particular wetland/stream and what the agency(s) permitting requirements are for that wetland/stream. To help reduce or avoid potential costly problems, have the consultant determine how any factors or regulations (which can change subsequent to the report) may affect the recommendations. Unless your consultant indicates otherwise, your report should not be used: ► If the size or configuration of the proposed project is altered. ► If the location or orientation of the proposed project is modified. ► If there is a change of ownership. ► For application to an adjacent site. ► For construction at an adjacent site or on site. ► Following floods, earthquakes, or other acts of nature. Wetland/stream consultants cannot accept responsibility for problems that may develop if they are not consulted after factors considered in their reports have changed. Therefore, it is incumbent upon you to notify your consultant of any factors that may have changed prior to submission of our final report. Wetland boundaries identified and stream classifications made by Shannon & Wilson are considered preliminary until validated by the U.S. Army Corps of Engineers (Corps) and/or the local jurisdictional agency. Validation by the regulating agency(s) provides a certification, usually written, that the wetland boundaries verified are the boundaries that will be regulated by the agency(s) until a specified date, or until the regulations are modified, and that the stream has been properly classified. Only the regulating agency(s) can provide this certification. MOST WETLAND/STREAM "FINDINGS" ARE PROFESSIONAL ESTIMATES. Site exploration identifies wetland/stream conditions at only those points where samples are taken and when they are taken, but the physical means of obtaining data preclude the determination of precise conditions. Consequently, the information obtained is intended to be sufficiently accurate for design, but is subject to interpretation. Additionally, data derived through sampling and subsequent laboratory testing are extrapolated by the consultant who then renders an opinion about overall conditions, the likely reaction to proposed construction activity, and/or appropriate design. Even under optimal circumstances, actual conditions may differ from those thought to exist because no consultant, no matter how qualified, and no exploration program, no matter how comprehensive, can reveal what is hidden by earth, rock, and time. Nothing can be done to prevent the unanticipated, but steps can be taken to help reduce their impacts. For this reason, most experienced owners retain their consultants through the construction or wetland mitigation/stream classification stage to identify variances, to conduct additional evaluations that may be needed, and to recommend solutions to problems encountered on site. Page 1 oft 1/2016 WETLAND/STREAM CONDITIONS CAN CHANGE. Since natural systems are dynamic systems affected by both natural processes and human activities, changes in wetland boundaries and stream conditions may be expected. Therefore, delineated wetland boundaries and stream classifications cannot remain valid for an indefmite period of time. The Corps typically recognizes the validity of wetland delineations for a period of five years after completion. Some city and county agencies recognize the validity of wetland delineations for a period of two years. If a period of years have passed since the wetland/stream report was completed, the owner is advised to have the consultant reexamine the wetland/stream to determine if the classification is still accurate. Construction operations at or adjacent to the site and natural events such as floods, earthquakes, or water fluctuations may also affect conditions and, thus, the continuing adequacy of the wetland/stream report. The consultant should be kept apprised of any such events and should be consulted to determine if additional evaluation is necessary. THE WETLAND/STREAM REPORT IS SUBJECT TO MISINTERPRETATION. Costly problems can occur when plans are developed based on misinterpretation of a wetland/stream report. To help avoid these problems, the consultant should be retained to work with other appropriate professionals to explain relevant wetland, stream, geological, and other findings, and to review the adequacy of plans and specifications relative to these issues. DATA FORMS SHOULD NOT BE SEPARATED FROM THE REPORT. Final data forms are developed by the consultant based on interpretation of field sheets (assembled by site personnel) and laboratory evaluation of field samples. Only final data forms customarily are included in a report. These data forms should not, under any circumstances, be drawn for inclusion in other drawings because drafters may commit errors or omissions in the transfer process. Although photographic reproduction eliminates this problem, it does nothing to reduce the possibility of misinterpreting the forms. When this occurs, delays, disputes, and unanticipated costs are frequently the result. To reduce the likelihood of data form misinterpretation, contractors, engineers, and planners should be given ready access to the complete report. Those who do not provide such access may proceed under the mistaken impression that simply disclaiming responsibility for the accuracy of information always insulates them from attendant liability. Providing the best available information to contractors, engineers, and planners helps prevent costly problems and the adversarial attitudes that aggravate them to a disproportionate scale. READ RESPONSIBILITY CLAUSES CLOSELY„ Because a wetland delineation/stream classification is based extensively on judgment and opinion, it is far less exact than other design disciplines. This situation has resulted in wholly unwarranted claims being lodged against consultants. To help prevent this problem, consultants have developed a number of clauses for use in written transmittals. These are not exculpatory clauses designed to foist the consultant's liabilities onto someone else; rather, they are definitive clauses that identify where the consultant's responsibilities begin and end. Their use helps all parties involved recognize their individual responsibilities and take appropriate action. Some of these definitive clauses are likely to appear in your report, and you are encouraged to read them closely. Your consultant will be pleased to give full and frank answers to your questions. THERE MAY BE OTHER STEPS YOU CAN TAKE TO REDUCE RISK. Your consultant will be pleased to discuss other techniques or designs that can be employed to mitigate the risk of delays and to provide a variety of alternatives that may be beneficial to your project. Contact your consultant for further information. Page 2 of 2 1/2016