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Critical Area Notice of Decision.pdfCity of Edmonds Critical Area Notice of Decision Applicant: Property Owner: #: I Permit Number: Ir I. Site Location: Parcel Number: Project Description: 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. T Critical Area Report Required. The proposedproject is within a critical area and/or a critical area / buffer and a critical area report is required. A critical area report has been submitted and evaluated for compliance with the following criteria pursuant to . C1 C'23.40�.1,60: 1. V/ The proposal initfli tines the impact on criticM 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 j 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. _ZThe 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 as described above and as shown on the attached site plan meets or is exempt from the criteria in ECDC 23.40.160, 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 l above. See referenced permit number for specific condition(s). 9 Notice on Title. Critical area notice on title recorded under AFN *20I105�tyOCL525. Appeals: Any decision to approve, condition, or deny a development proposal or other activity based on the requirements of critical area regulations maybe appealed according to, and as part of, the appeal procedure, if any, for the permit or approval involved. Revised 11/29/2016 April 10, 2017 Project No. 150499EO01 Mr. Mark Bailey 101512 th Avenue North Edmonds, Washington 98020 a s s o c i e t e d earth sciences i r -, c o r p o r x t e d Subject: Geotechnical Consultation Slope Tree Removal Assessment Bailey Residence 101512 th Avenue North Edmonds, Washington Dear Mr. Bailey: .C-D� qu, qifffollr M APR 13 2017 11VELIPMENT COUNTER As requested, this letter provides our opinion regarding proposed tree removal at your property located at 1015 12th Avenue North in Edmonds, Washington. We have previously prepared a "Subsurface Exploration, Geologic Hazard, and Geotechnical Engineering Report — Bailey Residence", dated May 6, 2016, for the proposed slope and settlement mitigation project at the subject site. Based on our correspondence with Mr. Chad Wichers of Studio 342, we understand that you wish to remove three maple trees, a cedar tree, a cherry tree, and a Japanese camellia from the slope to the west of the residence, and that the City of Edmonds has requested a geotechnical opinion addressing slope stability and erosion control when these specific trees are removed. Site Observations The subject site is a single-family residential parcel located at 1015 12th Avenue North in Edmonds, Washington. The ground surface at the subject site is generally moderately sloping, with steeply -sloping ground leading downward to the west beyond the property line. The existing residence is a one-story structure with a daylight basement that opens to the west. A series of low retaining walls, including both rock and timber walls, facilitates a portion of the grade change between the subject site and the property to the west. The slope along the western portion of this property is in excess of 40 percent with greater than 10 feet of vertical relief. As such, it is considered a Landslide Hazard Area by the City of Edmonds. The site has been subject to past grading, including the placement of fill out over the rear yard area likely during the original construction of the residence. One objective of the currently proposed project is to improve rear yard stability along the top of the western slope through the placement of a retaining wall designed to current standards. Review of the regional geologic map titled Geologic Map of the Edmonds East and part of the Edmonds West Quadrangles, by J.P. Minard (1983) indicates that the area of the subject site is underlain by Vashon advance outwash deposits (Qva), with Vashon lodgement till (Qvt) mapped Kirkland Office 1911 Fifth Avenue I Kirkland, WA 98033 P 1425.827.7701 FI 425.827.5424 Everett Office 12911 Y. Hewitt Avenue, Suite 2 1 Everett, WA 98201 P 1425.259.0522 F 1 425.827.5424 Tacoma Office 11552 Commerce Street, Suite 102 1 Tacoma, WA 98402 P 1253.722.2992 F 1253.722.2993 www.aesgeo.com nearby. Our interpretation of the sediments encountered during the explorations completed as part of our 2016 study was in general agreement with the Vashon lodgement till (Qvt) mapped in the area. Conclusions Based on our site observations and upon review of the above-mentioned information, it is our opinion that the proposed tree removal can be completed without a long-term decrease in the stability of the subject slope. We recommend that the trunk and limbs be removed from the slope in a manner to minimize ground disturbance (e.g., using a crane). Tree stumps should be left in place to provide support to surface soils. In our 2016 report, we stated "To the extent possible, we recommend that native vegetation be left on the slope to provide erosion control." Therefore, the slope should be replanted as soon as possible with landscaping trees and shrubs, as desired, and the disturbed ground surface mulched to mitigate erosion. Irrigation of the vegetation should be limited to prevent excessive saturation of the slope and potential soil movement. Limitations This letter has been prepared for, and limited to, the evaluation of the proposed tree removal. Our conclusions and recommendations have been prepared in accordance with generally accepted professional engineering and geologic principles and practices. We make no other warranty, either express or implied. Our conclusions are based on the results of our interpretation of surface conditions. If subsurface conditions are encountered that appear to be different than those described in this report, we should be notified so that we may review and verify or modify our recommendations. Closure We hope this information meets your present needs. If there are any further questions, feel free to contact the undersigned at (425) 827-7701. Sincerely, ASSOCIATED EARTH SCIENCES, INC. Kirkland, Washington µ Jeffrey P. La , L.G., L.E.G. Senior Project Engineering Geologist J PL/pc-15499E001-3 — Projects\20150499\KE\W P 2 Bruce L. Blyton, P.E. Senior Principal Engineer o c i a t e Ow"03 r t h s c i i n c c r p o r a t e d Subsurface Exploration, Geologic Hazard, and Geotechnical Engineering Report BAILEY RESIDENCE Edmonds, Washington Prepared For: MR. MARK BAILEY Project No. KE150499A May 6, 2016 M; a a s o o G a t e d Ir t s c e n May 6, 2016 Project No. KE150499A Mr. Mark Bailey 101512 th Avenue North Edmonds, Washington 98020 Subject: Subsurface Exploration, Geologic Hazard, and Geotechnical Engineering Report Bailey Residence 1015 12th Avenue North Edmonds, Washington Dear Mr. Bailey: We are pleased to present the enclosed copies of the above -referenced report. This report summarizes the results of our subsurface exploration, geologic hazard, and geotechnical engineering studies, and offers recommendations for the design and development of the proposed project. We have enjoyed working with you on this study and are confident that the recommendations presented in this report will aid in the successful completion of your project. If you should have any questions, or if we can be of additional help to you, please do not hesitate to call. Sincerely, ASSOCIATED EARTH SCIENCES, INC. Kirkland, Washington Bruce 1. Blyton, P.E. Senior Principal Engineer BLB/Id KE150499A2 Projects\20150499\KE\WP Kirkland Office 1911 Fifth Avenue I Kirkland, WA 98033 P 1425.827.7701 FI 425.827.5424 Everett Office 1 2911 %: Hewitt Avenue, Suite 2 1 Everett, WA 98201 P 1425.259.0522 F 1425.827.5424 Tacoma Office 1 1552 Commerce Street, Suite 102 1 Tacoma, WA 98402 P 1253.722.2992 F 1253.722.2993 www.aesgeo.com SUBSURFACE EXPLORATION, GEOLOGIC HAZARD, AND GEOTECHNICAL ENGINEERING REPORT Edmonds, Washington Prepared for: Mr. Mark Bailey 1015 12th Avenue North Edmonds, Washington 98020 Prepared by: Associated Earth Sciences, Inc. 9115th Avenue Kirkland, Washington 98033 425-827-7701 Fax: 425-827-5424 May 6, 2016 Project No. KE150499A Subsurface Exploration, Geologic Hazard, Bailey Residence and Geotechnical Engineering Report Edmonds, Washington Proiect and Site Conditions 1. PROJECT AND SITE CONDITIONS 1.0 INTRODUCTION This report presents the results of our subsurface exploration, geologic hazard, and geotechnical engineering study for the proposed slope and settlement mitigation project. The location of the site is shown on the "Vicinity Map," Figure 1, and the locations of the explorations accomplished for this study are presented on the "Site and Exploration Plan," Figure 2. In the event that any changes in the nature, design, or location of the structures are planned, the conclusions and recommendations contained in this report should be reviewed and modified, or verified, as necessary. The purpose of this study was to provide subsurface data to be utilized in the design and development of the subject project. Our study included a review of available geologic and past project literature, drilling three exploration borings, and performing geologic studies to assess the type, thickness, distribution, and physical properties of the subsurface sediments and shallow ground water conditions. Geologic hazard evaluations and geotechnical engineering studies were also conducted to select the type of retaining system, lateral earth pressures, and drainage considerations. This report summarizes our current fieldwork and development recommendations based on our present understanding of the project. 1.2 Authorization Written authorization to proceed with this study was granted by Mr. Mark Bailey. Our study was accomplished in general accordance with our scope of work letter dated August 26, 2015. This report has been prepared for the exclusive use of Mr. Mark Bailey and his agents for specific application to this project. Within the limitations of scope, schedule, and budget, our services have been performed in accordance with generally accepted geotechnical engineering and engineering geology practices in effect in this area at the time our report was prepared. No other warranty, express or implied, is made. Our observations, findings, and opinions are a means to identify and reduce the inherent risks to the owner. The subject site is a single-family residential parcel located at 1015 12th Avenue North in Edmonds, Washington. The ground surface at the subject site is generally moderately sloping, with steeply -sloping ground leading downward to the west beyond the property line. The existing residence is a one-story structure with a daylight basement that opens to the west. A May 6, 2016 ASSOCIATED EARTH SCIENCES, INC. JPL11d—KE150499A2—Projectsk20150499�KEJWP Page 1 Subsurface Exploration, Geologic Hazard, Bailey Residence and Geotechnical Engineering Report Edmonds, Washington Project and Site Conditions series of low retaining walls, including both rock and timber walls, facilitates a portion of the grade change between the subject site and the property to the west. Portions of the west side of the main residential structure, along with paved surfacing to the west of the residence, display signs of settlement. Also, a portion of the western foundation stemwall is bulging outward. Surficial soil erosion is apparent along the slope west of the residence. We understand that you wish to address the problem to mitigate future significant impacts to the structures, and that the currently -proposed mitigations may include the underpinning of portions of the existing residence or the construction of a retaining wall at the top of the slope to the west of the residence. 3.0 SITE EXPLORATION The site exploration was conducted on November 11, 2015, and consisted of three exploration borings and a geologic and geologic hazard reconnaissance to gain information about the site. The various types of materials and sediments encountered in the explorations, as well as the depths where characteristics of these materials changed, are indicated on the exploration boring logs presented in the Appendix. The depths indicated on the logs where conditions changed may represent gradational variations between sediment types in the field. If changes occurred between sample intervals in our borings, they were interpreted. The locations of the exploration borings are shown on the "Site and Exploration Plan," Figure 2. The conclusions and recommendations presented in this report are based on the exploration borings completed for this study. The number, locations, and depths of the explorations were completed within site and budgetary constraints. Because of the nature of exploratory work below ground, interpolation of subsurface conditions between field explorations is necessary. It should be noted that differing subsurface conditions may sometimes be present due to the random nature of deposition and the alteration of topography by past grading and/or filling. The nature and extent of any variations between the field explorations may not become fully evident until construction. If variations are observed at that time, it may be necessary to re-evaluate specific recommendations in this report and make appropriate changes. ,ir r �N ^� The borings were completed on the property using a hand -portable drill rig advancing a 3.75 -inch, inside -diameter, hollow -stem auger. During the drilling process, samples were obtained at generally 2.5- or 5 -foot intervals. The borings were continuously observed and logged by an engineer from our firm. The exploration logs presented in the Appendix are based on the field logs, drilling action, and inspection of the samples secured. May 6, 2016 ASSOCIATED EARTH SCIENCES, INC. JPL11d — KE150499A2 —Projects �20150499�KEJ WP Page 2 Subsurface Exploration, Geologic Hazard, Bailey Residence and Geotechnical Engineering Report Edmonds, Washington Project and Site Conditions Disturbed but representative samples were obtained by using the Standard Penetration Test (SPT) procedure in accordance with American Society for Testing and Materials (ASTM) D-1586. This test and sampling method consists of driving a standard, 2 -inch, outside -diameter, split -barrel sampler a distance of 18 inches into the soil with a 140 -pound hammer free -falling a distance of 30 inches. The number of blows for each 6 -inch interval is recorded, and the number of blows required to drive the sampler the final 12 inches is known as the Standard Penetration Resistance ("N") or blow count. If a total of 50 blows are recorded at or before the end of one 6 -inch interval, the blow count is recorded as the number of blows for the corresponding number of inches of penetration. The resistance, or N -value, provides a measure of the relative density of granular soils or the relative consistency of cohesive soils. These values are plotted on the attached boring logs. The samples obtained from the split -barrel sampler were classified in the field and representative portions placed in watertight containers. The samples were then transported to our laboratory for further visual classification and geotechnical laboratory testing, as necessary. The various types of soil and ground water elevations, as well as the depths where soil and ground water characteristics changed, are indicated on the exploration boring logs presented in the Appendix of this report. Our explorations and reconnaissance were approximately located by measuring from known site features. 4.0 SUBSURFACE CONDITIONS Subsurface conditions at the project site were inferred from the field explorations accomplished for this study, visual reconnaissance of the site, and review of applicable geologic literature. As shown on the exploration logs, the exploration borings generally encountered consolidated, granular, glacial sediments overlain by fill. The following section presents more detailed subsurface information organized from the youngest to the oldest sediment types. 4.1 Stratigraphy Fill Fill (soils not naturally placed) soils were encountered at the locations of our exploration borings to depths ranging from approximately 5 to 7% feet below the ground surface. The fill generally consisted of loose, fine to medium sand with varying amounts of silt and gravel. Portions of the fill contained organic material and woody debris. Fill is also expected in unexplored areas of the site, such as the area surrounding and under existing structure foundations, in utility trenches, and in the existing paved and landscaped areas. Due to their variable density and organic content, the existing fill soils are not suitable for foundation support. May 6, 2016 ASSOCIATED EARTH SCIENCES, INC. JPL/Id—KE150499A2—ProjectsJ20150499JKE�WP Page 3 Subsurface Exploration, Geologic Hazard, Bailey Residence and Geotechnical Engineering Report Edmonds, Washington Project and Site Conditions Vashon Lodgement Till Sediments encountered below the fill at the locations of exploration borings E13-1 through E13-3 generally consisted of medium dense silty sand with gravel. These sediments were observed to generally become dense to very dense below depths of approximately 2 to 4 feet below the bottom of the overlying fill. We interpret these sediments to be representative of Vashon lodgement till. The Vashon lodgement till was deposited directly from basal, debris -laden glacial ice during the Vashon Stade of the Fraser Glaciation approximately 12,500 to 15,000 years ago. The reduced density observed within 2 to 4 feet of the overlying fill is interpreted to be due to weathering. The high relative density of the unweathered till is due to its consolidation by the massive weight of the glacial ice from which it was deposited. At the locations of exploration borings E13-1 through E13-3, the till extended beyond the maximum depths explored. Review of the regional geologic map titled Geologic Map of the Edmonds East and part of the Edmonds West Quadrangles, by J.P. Minard (1983) indicates that the area of the subject site is underlain by Vashon advance outwash deposits (Qva), with Vashon lodgement till (Qvt) mapped nearby. Our interpretation of the sediments encountered at the subject site is in general agreement with the Vashon lodgement till (Qvt) mapped in the area. Ground water was not encountered in the exploration borings. We also did not observe ground water emanating from the slope. We expect ground water seepage across much of the site to be limited to interflow. Interflow occurs when surface water percolates down through the surficial weathered or higher -permeability sediments and becomes perched atop underlying, lower -permeability sediments. It should be noted that the occurrence and level of ground water seepage at the site may vary in response to such factors as changes in season, precipitation, and site use. May 6, 2016 ASSOCIATED EARTH SCIENCES, INC. JPL/Id—KE150499A2—ProjectsJ20150499JKE�WP Page 4 Subsurface Exploration, Geologic Hazard, Bailey Residence and Geotechnical Engineering Report Edmonds, Washington Geologic Hazards and Mitigations II. GEOLOGIC HAZARDS AND MITIGATIONS The following discussion of potential geologic hazards is based on the geologic conditions, as observed and discussed herein. The slope along the western portion of this property is in excess of 40 percent with greater than 10 feet of vertical relief. As such, it is considered a Landslide Hazard Area by the City of Edmonds. The site has been subject to past grading, including the placement of fill out over the rear yard area likely during the original construction of the residence. One objective of the currently proposed project is to improve rear yard stability along the top of the western slope through the placement of a retaining wall designed to current standards. The following paragraphs discuss the stability of the slopes and recommendations to mitigate risks to the public health, safety, or welfare. It must be understood that no recommendations or engineering design can yield a guarantee of stable slopes. Our observations, findings, and opinions are a means to identify and reduce the inherent risks to the owner. 5.1 Slope Stability Assessment Associated Earth Sciences, Inc. (AESI) used GeoStudio 2007, Version 7.17, by Geo -Slope International, Ltd. to perform the analysis of slope stability with the proposed retaining wall. The Morgenstern -Price method was used for both static and seismic models. The 2012 International Building Code (IBC) seismic design parameter for peak ground acceleration (PGA) was determined by the latitude and longitude of the project site using the U.S. Geological Survey (USGS) National Seismic Hazard Mapping Project websites. The USGS website interpolated PGA at the project site to be 0.538, with a 2 percent chance of exceedance in 50 years. Seismic stability modeling included a horizontal seismic coefficient of 0.265g. We used the topography presented on a "Boundary and Topographic Survey," prepared by Greene Land Surveying and dated April 3, 2016, to create a profile through the subject parcel. A graphical representation of the cross-section we used for input is presented on Figure 3. Surcharges used for our analysis included 500 pounds per square foot (psf) to represent the existing residence. Data from the subsurface explorations performed for this study were used to model the steep slope and underlying soil contacts. The soil densities and other soil properties in the model were estimated based on SPT blow counts from our explorations, our experience with similar soils, and correlation with published information. Soil strength parameters used for our analysis included a 36 -degree friction angle for the native Vashon ' http://earthquake.usgs.gov/hazmaps/ May 6, 2016 ASSOCIATED EARTH SCIENCES, INC. IPL/1d—KE150499A2—Projects �20150499JKEJWP Page 5 Subsurface Exploration, Geologic Hazard, Bailey Residence and Geotechnical Engineering Report Edmonds, Washington Geologic Hazards and Mitigations lodgement till, 32 degrees for weathered Vashon lodgement till, and 30 degrees for the fill encountered in our explorations. Our slope stability analysis evaluated the risk of deep-seated landslides extending through the underlying Vashon lodgement till deposits and below the approximate location of the proposed retaining wall. Slope stability is expressed as a factor of safety, which is a ratio between resisting and driving forces for a given slope failure scenario. A factor of safety of 1.0 indicates that resisting and driving forces are equal, and a failure is predicted. Factors of safety greater than 1 indicate that resisting forces exceed driving forces, and a failure is not predicted. City of Edmonds standards call for minimum slope stability factors of safety of 1.5 under static conditions and 1.2 under simulated seismic conditions. Using the above soil parameters and the geometry shown on Figure 3, the resulting factors of safety meet or exceed the recommended minimum values of 1.2 under seismic conditions and 1.5 under static conditions. Based on our analyses, the proposed construction of a retaining wall at the approximate location shown on Figure 2 appears feasible from a geotechnical standpoint provided the wall is designed as a retaining wall with sufficient embedment to provide the factors of safety predicted by our model. The near -surface soil underlying the area along the western slope consists primarily of a zone of loose fill overlying dense to very dense glacial deposits. Due to the loose nature of the fill soils encountered in our explorations, it is our opinion that the improvements on the site should include the use of a retaining wall with a deep foundation system, such as embedded soldier piles. To the extent possible, we recommend that native vegetation be left on the slope to provide erosion control. As with all steep slopes, surface drainage should be properly controlled and directed away from sloping areas. At no time should loose fill be pushed over the top of the slope or soil excavated from the toe area without support by an engineered retaining structure. Uncontrolled fill on slopes or toe excavation may promote landslides or debris flow activity. AESI should review grading plans if grading is desired at the top of, on, or near the toe of the steep slope. 6.0 SEISMIC HAZARDS AND MITIGATION Earthquakes occur in the Puget Lowland with great regularity. The vast majority of these events are small and are usually not felt by people. However, large earthquakes do occur, as evidenced by the 1949, 7.2 -magnitude event; the 1965, 6.5 -magnitude event; and the 2001, 6.8 -magnitude event. The 1949 earthquake appears to have been the largest in this area during May 6, 2016 ASSOCIATED EARTH SCIENCES, INC. JPL11d — KE150499A2 — ProjectsJ20150499�KEJWP Page 6 Subsurface Exploration, Geologic Hazard, Bailey Residence and Geotechnical Engineering Report Edmonds, Washington Geologic Hazards and Mitigations recorded history. Evaluation of return rates indicates that an earthquake of a magnitude between 6.0 and 7.0 is likely within a given 25- to 40 -year period. Generally, there are four types of potential geologic hazards associated with large seismic events: 1) surficial ground rupture, 2) seismically induced landslides, 3) liquefaction, and 4) ground motion. The potential for each of these hazards to adversely impact the proposed project is discussed below. 6*1 Surficial Ground Rupture The nearest known fault trace to the project site is the South Whidbey Island Fault Zone (SWIFZ). A recent study by USGS (Sherrod et al., 2005, Holocene Fault Scarps and Shallow Magnetic Anomalies Along the Southern Whidbey Island Fault Zone Near Woodinville, Washington, Open -File Report 2005-1136, March 2005) indicates that "strong" evidence of prehistoric earthquake activity has been observed along associated fault strands thought to be part of the SWIFZ. The study suggests as many as nine earthquake events along the SWIFZ may have occurred within the last 16,400 years. The recognition of this fault splay is relatively new, and data pertaining to it are limited, with the studies still ongoing. The recurrence interval of movement along this fault system is still unknown, although it is hypothesized to be in excess of 1,000 years. Due to the suspected long recurrence interval, it is our opinion that the potential for damage to the proposed wall and existing residence by surficial ground rupture is considered to be low. No mitigations other than complying with 2012 IBC seismic design recommendations are recommended. .«lmllffllm Our slope stability modeling has included "pseudostatic" analyses that incorporate loads associated with an earthquake. Slope stability analyses and results are described in further detail in the "Landslide Hazards and Mitigation" section of this report. 6.3 Liquefaction The encountered stratigraphy has a low potential for liquefaction due to its dense state and lack of adverse ground water conditions. No mitigation of liquefaction hazards is warranted. 6.4 Ground Motion Design of the structures should follow 2012 IBC standards using Site Class "C" as defined in Table 20.3-1 of American Society of Civil Engineers (ASCE) 7 — Minimum Design Loads for Buildings and Other Structures. May 6, 2016 ASSOCIATED EARTH SCIENCES, INC. JPL/Id—KE150499A2—Pro%ectsJ20150499JKEJWP Page 7 Subsurface Exploration, Geologic Hazard, Bailey Residence and Geotechnical Engineering Report Edmonds, Washington Geologic Hazards and Mitigations 7.0 EROSION HAZARDS AND MITIGATION A properly developed, constructed, and maintained erosion control plan consistent with City of Edmonds standards and best management erosion control practices will be required for this project. AESI is available to assist the project civil engineer in developing site-specific erosion control plans. Based on past experience, it will be necessary to make adjustments and provide additional measures to the Temporary Erosion and Sedimentation Control (TESC) plan in order to optimize its effectiveness. Ultimately, the success of the TESC plan depends on a proactive approach to project planning and contractor implementation and maintenance. Due to the steep slope present within the site, we expect that grading will be restricted to the dry season without a waiver granted by the City of Edmonds. The recommendations presented in this section are intended to address grading activities during both the dry and wet seasons. To mitigate the erosion hazards and potential for off-site sediment transport, we would recommend the following: 1. The erosion hazard of the site soils is relatively low in the flat -lying areas and moderate to high on the steep slopes. Maintaining cover measures atop disturbed ground provides a significant reduction to the potential generation of turbid runoff and sediment transport. During the local wet season (October 1st through March 31St), exposed soil should not remain uncovered for more than 2 days unless it is actively being worked. Ground -cover measures can include erosion control matting, plastic sheeting, straw or wood mulch, crushed rock or recycled concrete, or mature hydroseed. The contractor must implement and maintain the required measures. 2. All TESC measures for a given area to be graded or otherwise worked should be installed prior to any construction activity. 3. Construction access points should be surfaced to mitigate sediment track -out onto adjacent streets. Any sediment that is tracked onto adjacent streets should be promptly swept up. 4. Silt fencing should be utilized as buffer protection and not as a flow -control measure. Silt fencing should be placed parallel with topographic contours to prevent sediment -laden runoff from leaving a work area or entering a sensitive area. Silt fences that cross contour lines should have separate flow control in front of the silt fence. A swale/berm combination should be used to provide flow control. May 6, 2016 ASSOCIATED EARTH SCIENCES, INC. JPL/Id—KE150499A2—Projects 1201504991KEIWP Page 8 Subsurface Exploration, Geologic Hazard, Bailey Residence and Geotechnical Engineering Report Edmonds, Washington Geologic Hazards and Mitigations 5. During the wetter months of the year, or when large storm events are predicted during the summer months, each work area should be stabilized so that if showers occur, the work area can receive the rainfall without excessive erosion or sediment transport. The required measures will depend on the time of year and the duration the area will be left unworked. During the winter months, areas that are to be left unworked for more than 2 days should be mulched or covered with plastic. During the summer months, stabilization will usually consist of seal -rolling the subgrade. 6. All disturbed areas should be revegetated as soon as possible. If it is outside of the growing season, the disturbed areas should be covered with mulch. Straw mulch provides an effective cover measure and can be made wind -resistant with the application of a tackifier after it is placed. 7. Surface runoff and discharge should be controlled during and following development. Uncontrolled discharge may promote erosion and sediment transport. Under no circumstances should concentrated discharges be allowed to flow over the top of steep slopes. 8. Soils that are to be reused around the site should be stored in such a manner as to reduce erosion from the stockpile. Protective measures may include, but are not limited to, covering with plastic sheeting, the use of low stockpiles in flat areas, or the use of straw bales/silt fences around pile perimeters. During the period between October 311t and March 3111, these measures are required. It is our opinion that with the proper implementation of the TESC plans and by field -adjusting appropriate mitigation elements (best management practices) during construction, the potential adverse impacts from erosion hazards on the project may be mitigated. May 6, 2016 ASSOCIATED EARTH SCIENCES, INC. JPL11d—KE150499A2—ProjectsJ20150499JKEJWP Page 9 Subsurface Exploration, Geologic Hazard, Bailey Residence and Geotechnical Engineering Report Edmonds, Washinqton Desian Recommendations III. DESIGN RECOMMENDATIONS 8.0 INTRODUCTION Our exploration indicates that, from a geotechnical standpoint, the parcel is suitable for the proposed project provided the risks discussed are accepted and the recommendations contained herein are properly followed. It is our opinion that the proposed soldier pile retaining wall system should provide mitigation for the risk of local shallow landsliding along the upper portion of the western slope face, relative to the existing condition. To mitigate the risk of future settlement for the western portion of the residence, we recommend that the affected footings of the house be underpinned. We recommend that a floor survey be completed to evaluate the extent and degree of settlement within the existing structure. This information will aid the structural engineer in designing the pile layout for underpinning of existing structures. The extent of the underpinning should include the exterior continuous foundation and the isolated interior column pads, if present. Footings that are not underpinned (such as the isolated piers) should be considered to be at risk of future settlement and damage due to differential settlement. The underpinning would connect to the existing footings and penetrate through the loose fill and into the competent, Vashon lodgement till bearing soils at depth. 9.0 SITE PREPARATION Site preparation of the planned wall alignment should include removal of all trees, brush, debris, and any other deleterious materials in the immediate construction zone. Tree/vegetation removal should be kept to the minimum required for site access and construction with small equipment. These unsuitable materials should be properly disposed of. Additionally, any areas of organic topsoil should be removed and the remaining roots grubbed. Areas where loose surficial soils exist due to grubbing operations should be considered as fill to the depth of disturbance and treated as subsequently recommended for structural fill placement. Any buried utilities should be removed or relocated if they are under building areas. The resulting depressions should be backfilled with structural fill, as discussed under the "Structural Fill" section of this report. In our opinion, stable construction slopes should be the responsibility of the contractor and should be determined during construction based on the local conditions encountered at that time. For planning purposes, we anticipate that temporary, unsupported cut slopes in the loose to medium dense fill or weathered till sediments can be made at a maximum slope of 1.5H:1V May 6, 2016 ASSOCIATED EARTH SCIENCES, INC. JPL11d—KE150499A2—ProjectsJ20150499IKE�WP Page 10 Subsurface Exploration, Geologic Hazard, Bailey Residence and Geotechnical Engineering Report Edmonds, Washington Design Recommendations (Horizontal:Vertical). For temporary cut slopes within the dense to very dense, unweathered till, up to a 1H:1V inclination may be planned. We recommend that temporary cuts be limited to 4 feet or less in vertical height to reduce the risk posed by sloughing of surficial fill soils. We anticipate that a minor of amount of cutting and filling will be needed to create an access road for equipment used for retaining wall installation. We recommend that this grading be kept to the least practical degree to allow access for small -tracked machines. Also, we recommend that fills for the access road be comprised of "hog fuel' wood chips, which can be incorporated as a mulch into the existing site soils subsequent to construction of the retaining walls. This practice will promote revegetation of areas disturbed by grading activities during access road construction. Alternatively, washed crushed rock may be used for access surfacing. As is typical with earthwork operations, some sloughing and raveling may occur, and cut slopes may have to be adjusted in the field. Flatter, temporary cut slopes should be anticipated in areas of ground water seepage. In addition, WISHA/OSHA regulations should be followed at all times. 10.0 STRUCTURAL FILL Structural fill may be necessary to establish desired grades for hard surfaces or to backfill around foundations and utilities, or behind the proposed wall. All references to structural fill in this report refer to subgrade preparation, fill type, placement, and compaction of materials, as discussed in this section. If a percentage of compaction is specified under another section of this report, the value given in that section should be used. After overexcavation/stripping has been performed to the satisfaction of the geotechnical engineer/engineering geologist, the upper 12 inches of exposed ground should be recompacted to a firm and unyielding condition. If the subgrade contains too much moisture, adequate recompaction may be difficult or impossible to obtain and should probably not be attempted. In lieu of recompaction, the area to receive fill should be blanketed with washed rock or quarry spalls to act as a capillary break between the new fill and the wet subgrade. Where the exposed ground remains soft and further overexcavation is impractical, placement of an engineering stabilization fabric may be necessary to prevent contamination of the free -draining layer by silt migration from below. After stripping and subgrade preparation of the exposed ground is approved, or a free -draining rock course is laid, structural fill may be placed to attain desired grades. Structural fill is defined as non-organic soil, acceptable to the geotechnical engineer, placed in maximum 8 -inch loose lifts, with each lift being typically compacted to 95 percent of the modified Proctor maximum density using ASTM D-1557 as the standard. For structural fill placed as backfill behind the proposed wall alignments, a standard of 90 percent of the modified Proctor maximum density using ASTM D-1557 may be used. May 6, 2016 ASSOCIATED EARTH SCIENCES, INC. IPL/Id—KE150499A2—Projects120150499WIWP Page 11 Subsurface Exploration, Geologic Hazard, Bailey Residence and Geotechnical Engineering Report Edmonds, Washington Design Recommendations The contractor should note that any proposed fill soils must be evaluated by AESI prior to their use in fills. This would require that we have a sample of the material 72 hours in advance to perform a Proctor test and determine its field compaction standard. Soils in which the amount of fine-grained material (smaller than the No. 200 sieve) is greater than approximately 5 percent (measured on the minus No. 4 sieve size) should be considered moisture -sensitive. Use of moisture -sensitive soil in structural fills should be limited to favorable dry weather and dry subgrade conditions. In addition, construction equipment traversing the site when the soils are wet can cause considerable disturbance. The on-site soils contained variable amounts of silt and are considered moisture -sensitive, and we expect that this material may be difficult to compact to structural fill specifications, particularly during and following wet weather. Alternatively, we recommend that a select, import material consisting of a clean, free -draining gravel and/or sand be used. Free -draining fill consists of non-organic soil with the amount of fine-grained material limited to 5 percent by weight when measured on the minus No. 4 sieve fraction. A representative from our firm should inspect the stripped subgrade and be present during placement of structural fill to observe the work and perform a representative number of in-place density tests. In this way, the adequacy of the earthwork may be evaluated as filling progresses and any problem areas may be corrected at that time. It is important to understand that taking random compaction tests on a part-time basis will not assure uniformity or acceptable performance of a fill. As such, we are available to aid the owner in developing a suitable monitoring and testing frequency. 11.0 FOUNDATIONS Based on the soil conditions encountered in our explorations, we recommend that the footings along the west side of the residence which display signs of settlement, along with other settlement -sensitive ancillary structures in the backyard area, be supported by a deep foundation, such as small -diameter, driven pipe piles. The piles should consist of 2 -inch -diameter, Schedule 80 pipe driven to refusal in the medium dense to dense site soils. For pipe piling driven to refusal, we recommend using an allowable bearing capacity of 4,000 pounds per pile. Refusal is defined as less than 1 inch of vertical movement after 60 seconds of sustained driving with a 90 -pound jack hammer. Resistance to lateral loads for a pipe pile -supported foundation would be provided by a passive soil resistance against the foundation pad (equivalent fluid equal to 200 pounds per cubic foot [pcf]) and, if necessary, using batter piles. The upper 2 feet on the passive (downslope) side of the foundation pads should be neglected and truncated from a triangular distribution. The lateral resistance of batter piles would be equal to the horizontal component of the axial pile load. The maximum batter recommended is 1H:4V. A structural engineer should determine the extent, number and spacing of piles required and if batter piles are to be used. We recommend that a May 6, 2016 ASSOCIATED EARTH SCIENCES, INC. 1PL11d—KE150499A2—ProiectsJ20150499JKE�WP Page 12 Subsurface Exploration, Geologic Hazard, Bailey Residence and Geotechnical Engineering Report Edmonds, Washington Design Recommendations representative from our firm observe installation of the piles to verify suitable embedment and driving resistance in the bearing soils. The City of Edmonds may require such observations. 12.0 SOLDIER PILE WALL We anticipate that a soldier pile wall consisting of closely spaced, wide -flange beam piles suitably embedded in the underlying, very dense lodgement till deposits will provide suitable lateral support when designed by a qualified structural engineer. Treated timber lagging, as specified by the structural engineer, should be used to support the soil between the piles. The construction sequence for pile retaining systems typically involves installing each pile to the minimum specified embedment depth below the ground surface under the observation of the geotechnical engineer or designated field representative. Drilled and grouted piles should be allowed to set for at least 72 hours prior to beginning excavation or filling activities. Once the piles have been installed to the satisfaction of the geotechnical engineer, fill placement behind the piles may proceed. Treated -timber lagging should be installed and backfilled with permeable soils to prevent the buildup of water behind the lagging boards. We recommend that the cantilever soldier pile retaining wall system be designed to resist an "active" lateral earth pressure modeled as an equivalent fluid with a density of 40 pcf for a level backslope. The active earth pressure is assumed to act over the pile spacing extending downward to an elevation of 2 feet below the existing ground surface. An allowable "passive" soil resistance of 250 pcf can be assumed to act over twice the pile width for the portions of the piles beginning 10 feet below the existing ground surface. Additionally, we recommend a minimum depth of embedment of 10 feet below the base of the existing fill for all piles. These recommendations for lateral earth pressures are illustrated on Figure 4. 24:? In accordance with the i,,",2012 retaining wall design should include seismic design parameters. Based on the'—site" 01"1 and assumed wall backfill materials, we recommend a seismic surcharge pressure in addition to the equivalent fluid pressures presented above. A rectangular pressure distribution of 5H and 10H psf (where H is the height of the wall in feet) should be included in design for "active" and "at -rest" loading conditions, respectively. The resultant of the rectangular seismic surcharge should be applied at the midpoint of the walls. If adjacent structures, heavy construction traffic, materials stockpiling, or other substantial surcharges are to be applied during construction, these surcharges should also be included in the design. The drilling contractor should be prepared to use casing, drilling slurry, or other methods of stabilizing the hole in the case of caving, ground water, or heaving soil conditions. If more than 6 inches of standing water or slough is present at the bottom of the boring prior to grout May 6, 2016 ASSOCIATED EARTH SCIENCES, INC. JPL/Id—KE150499A2—ProjectsJ20150499JKEJWP Page 13 Subsurface Exploration, Geologic Hazard, Bailey Residence and Geotechnical Engineering Report Edmonds, Washington Design Recommendations placement, the contractor should be prepared to use a tremie pipe to place grout continuously from the bottom up. Timber lagging can be designed to resist reduced lateral earth pressures as a result of soil arching between piles. For the site soils, the lagging can be designed to resist 50 percent of the calculated lateral load at any given point. The lagging should extend at least 2 feet below the existing ground surface to provide lateral resistance for the upper portion of the existing, loose fill zone. Any void spaces behind lagging should be filled with pea gravel, controlled density fill (CDF), or other suitable material to prevent caving and loss of support for adjacent ground. 12.1 Tiebacks Tiebacks may be needed to provide additional lateral resistance for the retaining system, or to mitigate the risk of future bulging of the western foundation stemwall. Grouted tieback anchors are frequently included in the design. For tiebacks used in the retaining system, the anchors must be located far enough behind the soldier pile wall to develop anchorage within a stable, natural soil mass to prevent a global failure or excessive deformation. We recommend that this anchorage be obtained behind an assumed failure plane defined by a horizontal line extending a distance equal to H/4 behind the retained soil at the base of the projected fill zone, which then rotates 60 degrees from the horizontal and extends upward to the ground surface. The area between this assumed failure plane and the wall is referred to as the "no-load zone." Depending on the wall location, anchor inclination, and local fill depth, anchor lengths may have to be increased to reach suitable, dense, native soil below the loose fill and behind the no-load zone. These recommendations are presented on Figure 4. The grouted anchor loads are transmitted to the surrounding soil by side friction or adhesion with the soil. Tieback anchors installed by hollow -stem auger techniques may be designed for a presumptive allowable shaft friction of 2,000 psf in the dense to very dense sediments if located greater than 20 feet below the existing ground surface. However, it may be necessary to "score" the perimeter of the anchor drillhole and/or use post grouting techniques to achieve this load. Presumptive anchor design loads should be confirmed by proof -testing, as outlined subsequently for both anchors using installation techniques and materials that match the production anchors. All grouted anchors should extend a minimum of 10 feet behind the no-load zone. Care must be exercised when installing tiebacks to avoid existing utilities and foundations. We recommend for this site that each anchor be sized for a design or allowable load of not more than 50 percent of the ultimate load available through the anchor (as indicated by 200 percent verification tests). Anchors should be tested and evaluated according to Post -Tensioning Institute (PTI) guidelines. The test anchors should be capable of holding the ultimate load without excessive yield or creep so that a factor of safety of at least 2.0 is available for May 6, 2016 ASSOCIATED EARTH SCIENCES, INC. JPL11d — KE150499A2 —Projects 120150499�KE�WP Page 14 Subsurface Exploration, Geologic Hazard, Bailey Residence and Geotechnical Engineering Report Edmonds, Washington Design Recommendations production anchors should further stressing occur. The rods or cables should transmit the anchor load to the soldier pile in such a manner to avoid eccentric loading. 12.2 Anchor Tests A series of anchor tests should be performed to verify the design and ultimate skin friction or adhesion of the tieback anchors. Because of the variation in the soil types and their densities, we recommend that AESI monitor the anchor test program. A common anchor testing program would consist of at least two 200 -percent verification tests of the design or allowable load in the soil plus proof -loading every production anchor to 130 percent of the design load. Verification test anchors are usually loaded in 25 -percent increments that are held for 5 minutes up to the final load of 200 -percent design load. The 200 -percent load is commonly held for an hour and creep measured. The other component of the anchor test program for the project would be proof -loading each of the production anchors to 130 percent of the design load. Each anchor should withstand this load for at least 5 minutes. The anchor should then be locked off at the design load. Subsequent to locking off the tiebacks at the design load, all of the tieback holes should be backfilled to prevent possible collapse of the holes and any related consequences. Typically, sand is used as backfill material; however, most non -cohesive mixtures are suitable (subject to approval by the geotechnical engineer) provided there is no bonding to the tierods. 13.0 PROJECT DESIGN AND CONSTRUCTION MONITORING At the time of this report, site grading, structural plans, and construction methods have not been finalized. We are available to provide additional geotechnical consultation as the project design develops and possibly changes from that upon which this report is based. We recommend that AESI perform a geotechnical review of the plans prior to final design completion. In this way, our earthwork and foundation recommendations may be properly interpreted and implemented in the design. We are also available to provide geotechnical engineering and monitoring services during construction. The integrity of the planned improvements depends on proper site preparation and construction procedures. These inspections may be required by the City of Edmonds as a part of the building permit conditions. In addition, engineering decisions may have to be made in the field in the event that variations in subsurface conditions become apparent. Construction monitoring services are not part of this current scope of work. If these services are desired, please let us know, and we will prepare a cost proposal. May 6, 2016 ASSOCIATED EARTH SCIENCES, INC. JPL11d — KE150499A2— ProjectsJ20150499JKE�WP Page 15 Subsurface Exploration, Geologic Hazard, Bailey Residence and Geotechnical Engineering Report Edmonds, Washington Design Recommendations We have enjoyed working with you on this study and are confident that these recommendations will aid in the successful completion of your project. If you should have any questions or require further assistance, please do not hesitate to call. Sincerely, ASSOCIATED EARTH SCIENCES, INC. Kirkland, Washington Jeffrey P. Laub, L.G., L.E.G. Senior Project Engineering Geologist Bruce L. Blyton, P.E. Senior Principal Engineer Attachments: Figure 1: Vicinity Map Figure 2: Site and Exploration Plan Figure 3: Slope Stability Analysis Cross -Section A -A' Figure 4: Soldier Pile Retaining Wall Design Criteria Appendix: Exploration Logs May 6, 2016 ASSOCIATED EARTH SCIENCES, INC. JPL/Id—KE150499A2—Projects 120150499�KEJWP Page 16 t A c E Li 0 � Y A r°� � w� V OEr6� 1 lie u1 L >/ r o �� s "',;r a ,d KJ M �.d, ' 'Ak uui� ttv an r� rrmN', 'rovr ��� i �lmwnrrluw�v nnn:arama� DATA SOURCES/REFERENCES: USGS: 24K SERIES TOPOGRPAHIC MAPS SNOHOMISH CO: STREETS, PARCELS LOCATIONS AND DISTANCES SHOWN ARE APPROXIMATE W ((4 w t J ed ryN �WY MIO � "m�ry ry�y �'� fa " IN w � M M II � , S 1 T E ���1'W"'�r �l4wi 'ICK✓ r �r ��� ID�r..mw,�,r„r;Tu � � romuw'r �u f if ZIP 1Tw �" " i f u!w r � r l I� a y% MAlli .ur'w .v ld r r i li rftrb, WiIrma � wrKik�k L"1 r ° r w ,al "��r"rroomm' wue t ty f K a"amW mnwiikm a ..01 it 4" � / r Kkm a "'T �Fu�,wP,IQQ ra 1 1 ) 7 IK T yy^rf; „ rr , �fi rc r y V 41rI' a l e Ty" f 1 �I f 9 a r� I' 1.'k11,h 1',Krn r�rrrr Li Ko'K�,. 'i A� go r u` A y t a s s o c i a t e d N earth sciences i n c o r p o r a t e d 0 1000 2000 VICINITY MAP FEET BAILEY RESIDENCE NOTE: BLACK EDMONDS, WASHINGTON UCTIOAND OFTHIS REPRODUCTION OF THIS COLOR ORIGINAL MAY REDUCE ITS EFFECTIVENESS AND LEAD TO PROJ NO DATE: FIGURE: INCORRECT INTERPRETATION KE150499A 4/16 1 1 NOlONIHSVM'SONOWO3 33NMISM A31IV8 NV -1d NOI1VHO-IdX3 ONNVV 33311116 S 2OU3105 yIJ2e W p e 7 e I a O s s 911 1101 J33H5 I/Z qw ON SOfI Mw)ffM HW HINON MN3AVMH kglol30A3AHI15 DIMVLRJOWI. AWON 'ONIA3AHnSUW3N33H0:30 HIJ HdVA3W9 I �oF RWXOWad HVNMOHSMW1MGUWN V001:31ON ,Z=NAa31NI YnoiNoo y,WAPM,p W 11W a'uMOW SNI OGNOUV80-d 3 930 X31 r � � wa1 YsuZ 4 � '. gnu "art .SZ I i V . •, , YYcO . <45Z ......... . Wt AM t5ot a N a n, f eoq a0w qq y Y { u � M N 4D dA" w PadfiWY II .SZ 0 LEGEND, A6"dpA A, 1,= FILL MURCHARGR FROM. WEATHERED VASHON LODGEMENT na VASHONLODGEMENTTK-L NOTE lJ 41 1. Distance (R) SEISMIC CASE A_ eu xeP SURCHARGE FROM EXISTING RESIDENCE In Al PS—MOR—Me—IM a e :rl ho sccii entese sd p ,,/j , �� ,�, , ,� ; � SLOPE STABILITY ANALYSIS CROSS-SECTION A -A Distance (a) BAILEY RESIDENCE EDMONDS, WASHINGTON '—; KE150499AI51161"..­ 3 NO-LOAD ZONE LIMIT V w � J 60�` a w J O �w x 1 4 5H PSF SEISMIC ..,., . gra r�4 } • . SURCHARGE "Al- ..� . V X ADDITIONAL 2 FOOT LAGGING BELOW EXISTING GROUND SURFACE ------------- F R B FV LOA K UDISE H/4 X = 40 (H+2) PSF ACTIVE PRESSURE ACTS OVER PILE SPACING NOTES: 1. SOLDIER PILE EMBEDMENT DEPTH "D" SHOULD CONSIDER NECESSARY VERTICAL CAPACITY, KICKOUT, AND OVERTURNING RESISTANCE. 2. ALL TIEBACK ANCHORS SHALL BE PRESTRESSED TO 130 PERCENT OF DESIGN LOAD AND LOCKED OFF AT 100 PERCENT OF DESIGN LOAD. AT LEAST TWO ANCHORS SHALL BE PRESTRESSED TO 200 PERCENT AND MONITORED FOR CREEP. TIE -BACK ANCHOR ZONE IS TO BE LOCATED BEHIND THE NO-LOAD ZONE. 250 (D) PSF PASSIVE PRESSURE ACTS OVER TWICE PILE DIAMETER I 3, PRESUMPTIVE ALLOWABLE TIEBACK -SOIL ADHESION= 2 KIPS PER SQUARE FOOT (KSF) IN DENSE NATURAL SOIL BENEATH FILL ZONE. SEE REPORT TEXT FOR PRESUMPTIVE DRIVEN ANCHOR RESISTANCE VALUES. 4. PASSIVE PRESSURES INCLUDE A FACTOR OF SAFETY OF 1,5, 5. ALLOWABLE SKIN FRICTION OF SOLDIER PILE - 1500 PSF OVER DEPTH "D". ALLOWABLE END BEARING = 30 KSF. 6. DIAGRAM DOES NOT INCLUDE HYDROSTATIC PRESSURES AND ASSUMES WALLS ARE SUITABLY DRAINED TO PREVENT BUILDUP OF HYDROSTATIC PRESSURE. 7. DIAGRAM IS ILLUSTRATIVE AND NOT REFERENCED TO A PARTICULAR LOCATION. 8, DIAGRAM DOES NOT INCLUDE PRESSURES DUE TO SURFACE SURCHARGES FROM ANY ADJACENT STRUCTURES. THESE PRESSURES MUST BE PROVIDED BY THE STRUCTURAL ENGINEER. 9. BASE OF FILL ZONE SHALL BE DEFINED AS 10 FEET BELOW THE EXISTING GROUND SURFACE. 10. ANCHOR MUST BE DEVELOPED ENTIRELY BEHIND THE NO-LOAD ZONE AND IN DENSE NATIVE SOIL BENEATH LOOSE FILL. p 0 0 1' Exploration Logs Classifications of soils in this report are based on visual field and/or laboratory observations, which include density/consistency, moisture oonaition, grain size, and plasticity estimates and should not be construed to imply field or laboratory testing unless presented herein. Visual -manual and/or laboratory classification methods of ASTM D-2487 and D-2488 were used as an identification guide for the Unified Soil Classification System. a s s o c 1 a t e d e a r t h s c e n c s EXPLORATION LOG KEY FIGURE Al I n c o r p o r a t 9 d 0Terms Well graded gravel and Describing Relative Density and Consistency Q 2 I>. � 0 0 LL 0; 0 GW gravel with sand, little to 2) ensity SPT( blows/foot (D no fines ry Loose 6 to 424) D 1ZCoarse- M > g 0 q? 0�-.O U Poorly graded gravel ose 4 to 10 Grained Soils Medium Dense 10 to 30 Test Symbols U) in mto.0�0 rp�o'u G P and gravel with sand, Dense 30 to 50 0 0 o'Q'o Cj 0.0�0 little to no fines Very Dense >50 G =Grain Size 04 6 Z 0 (1 0 0 c — .1 P M = Moisture Content Consistency SPV*blows/foot A = Afterberg Limits Z U) 0 � .0 C -0 Silty gravel and silty Very Soft 0 to 2 C= Chemical 0 _0 M a] hc; GM gravel with sand Fine- Soft 2 to 4 DD = Dry Density W - . IM Grained Soils Medium Stiff 4 to 8 K =Permeability CD 0 Stiff 8 to 15 Clayey gravel and Very Stiff 15 to 30 GC clayey gravel with sand Hard >30 > Component Definitions ro �Wel_l graded d and Descriptive Term Size Ranae and Sieve Number -S .2 SW sand with gravel, little Boulders Larger than 12" 0 to no fines Cobbles 3" to 12" LL (D . ...... Gravel 3" to No. 4 (4.75 mm) E2 co Poorly graded sand Coarse Gravel 3" to 3/4" 0 Cn 0 0 Mf SP and sand with gravel, Fine Gravel 3/4" to No. 4 (4.75 mm) o little to no fines Sand No. 4 (4.75 mm) to No. 200 (0.075 mm) 12 0 Z Coarse Sand No. 4 (4.75 mm) to No. 10 (2.00 mm) q at 2, (D —Silty sand and Medium Sand No. 10 (2.00 mm) to No. 40 (0.425 mm) 12 2 � sm silty sand with Fine Sand No. 40 (0,425 mm) to No. 200 (0.075 mm) M 0 L) a- CO gravel Silt and Clay Smaller than No. 200 (0,075 mm) Lo_..m-......-.. X'�' . . . ........ . ..... Clayey sand and (3) Estimated Percentage Moisture Content 1, A I sc clayey sand with gravel Component Percentacie bv Weiqht Dry - Absence of moisture, U) dusty, dry to the touch Trace <5 Slightly Moist - Perceptible Silt, sandy silt, gravelly silt, moisture LO0 ML silt with sand or gravel Some 5 to <12 Moist -Damp but no visible > 4) 05 CD F_ LO Ca i� ;5 , — Modifier 12 to <30 water - Very Moist Water visible but Clay of low to medium (silty, sandy, gravelly) plasticity; silty, sandy, or not free draining 6 Z CIL gravelly clay, lean clay Very modifier 30 to <50 Wet -Visible free water, usually W CD E (silty, sandy, gravelly) from below water table vj -V Organic clay or silt of low Symbols a_ 2? OL plasticity Blows/6" or 0 2 Sampler portion of 6" Cement grout 8Type �clayey surface seal j M.._ riai�tic silt, silt, silt 2.0" OD Bentonite H With micaceous or Split-Spoon sea) to diatomaceous fine sand or Sampler 3.0" ODS plit-Spoon Sampler Filter pack with N Giltblank . ........ . 3.25'OD Split-Spoon Ring Sampler imp casing (SPT).._.to Clay of high plasticity, section Bulk sample aai 'a = sandy or gravelly clay, fat 3.011 OD Thin -Wall Tube Sampler Screened casing m E 40 clay with sand or gravel (including Shelby tube) "1 or I lydratlip V11 th pillar Pack .5 Grab Sample End En cap Organic clay or silt of 0 Portion not recovered OH medium to high ..... . .... . . . ........ . . . ......................µ Percentage by dry weight (4) Depth of ground water plasticity (2) (SPT) Standard Penetration Test Y ATD = At time of drilling Peat, muck and other (ASTM D-1 586) V Static water level (date) (3) In General Accordance with 2)9 xa' PT highly organic soils Standard Practice for Description (5) Combined USCS symbols used for 0 � N and Identification of Soils (ASTM D-2488) fines between 5% and 12% Classifications of soils in this report are based on visual field and/or laboratory observations, which include density/consistency, moisture oonaition, grain size, and plasticity estimates and should not be construed to imply field or laboratory testing unless presented herein. Visual -manual and/or laboratory classification methods of ASTM D-2487 and D-2488 were used as an identification guide for the Unified Soil Classification System. a s s o c 1 a t e d e a r t h s c e n c s EXPLORATION LOG KEY FIGURE Al I n c o r p o r a t 9 d d EXELi�i,6 OQ F, --------------Proje ct mbe .. .. Ua n CSiaE n -Number Sheet -,.,. ' ,P KE 50 99 4 1 of 1 Project Name _-----_...��_.�._.�� �� _._��._ _ Bailey II:I fElevation_.,. _ ........� Surface (ft) Location Edmond,*,, AA......................._ - - --- ------ --.-. ------ Datumd KI/A,_ _____ __ Driller/Equipment N,�IiOt lAht DateStart/Finish „ 11/11/15,11/11/15 Hammer Weight/Drop O / " .. ......... Hole Diameter (in) F,,!nnhac.. vN U d CL a .O N� a� N J Blows/Foot y to a)N a S a)rn T E 2T C7 E m ° Co t �' DESCRIPTION " 3 10 20 30 40 ° ............_...�.. ........ ........ Fill ......... ...... _ _.. S-1 1 •5 Moist, brownish gray, fine to medium SAND, some silt, some organics 4 (SP -SM). S-2 Moist to wet, brownish gray, silty fine to medium SAND, trace gravel (SM).1 1 1 5 S-3 Moist, slightly rust -stained brownish gray, Cine to medium SAND, some silt,2 ♦5 trace gravel, trace burned wood fragments (SP -SM). g q Driller added water at 8 Feet —-..-.... ---. ........._... ...... .... .... ........ ....... S 4 1Nashon Lodgement Till 4 j Moist, slightly rust -stained brownish gray, silty fine to medium SAND, some 16 14 gravel (SM). - 10 S-5 Moist, brownish gray, silty fine to medium SAND, some gravel (SM). 8 A4 27 - 15 .•.As IL I S-6 above. 5 31 )15. 5" 16601 !,5" Bottom of wploration boring at 16 feet No ground water encountered. - 20 - 25 z Sampler Type (ST): ❑ 2" OD Split Spoon Sampler (SPT) ❑ No Recovery M - Moisture Logged by: JPL Y OD Split Spoon Sampler (D & M) Ring Sample Water Level() Approved by: JNS ® Grab Sample ❑ Shelby Tube Sample 1 Water Level at time of drilling (ATD) Exploration Loa i" Project N ..... --.�. :Uth ie11l d :� _ Proj umber E�loration Number Sheet fli 6 0, 0 lo I � E150499A EB -2 1 of 1 Project Name ..... _------------ -....... -- Ground Surface Elevation (ft) _ Location ..Eft s W ................................. Datum N/A.......... Driller/Equipment) ill If1C A( _ Date Start/Finish 11 /11 /15-;11 /11 /15 Hammer Weight/Drop.: .... Q Hole Diameter (in) 6..1nche%- C d) L -6O > f, N =Z Blows/Foot t- o T rn cD Cn E m° t M DESCRIPTION 10 20 30 40 ° Fill' S-1 Moist, brown, silty SAND, some organics, trace gravel (SM). 2 ♦g 4 S-2 As above, with woody debris. /1 4 1 1 5 _ Weathered a il o ._ ....., Till 1 S-3 Moist, reddish brown to brownish gray,Lodgement silty fine to medium SAND, some gravel 2 11 SM. 9 Vashon Lodgement Till S-4 Moist, brownish gray, silty fine to medium SAND, some gravel (SM). 23 35 A k74 39 Driller added water at 9 feet. 10 S Moist, brownish gray, fine to medium SAND, some silt, some gravel (SP -SM). 33 „ 5ia11 Bottom of exploration boring at 11 feet No ground water encountered. - 15 - 20 - 25 0 +Y. m. E m 'o - Z I IL c7_ Sampler Type ... (ST): ...................................... ❑ 2" OD Split Spoon Sampler (SPT) ❑ No Recovery M - Moisture Logged by: JPL o 3" OD Split Spoon Sampler (D & M) Ring Sample Q Water Level O Approved by: JNS W ® Grab Sample ❑ Shelby Tube Sample 1 Water Level at time of drilling (ATD) a n 9 a, c � a a 0 d Exploration Log """�� a o :a r C qu s c u e uu ic es Project Number Exploration Number Sheet f�� , a7 r ' � ° e d KE150499A EB -3 1 of 1 Project Name ...................._..._... ......... _Ballt?v Residence _.....__ Ground Surface Elevation (ft) Location B.NTl..n,., .. Datum .N/A_.. Driller/Equipment �l I%hI44..�<l -.- Date Start/Finish 1.,.1 /11 /15.11 /1111.5 ........ Weight/Drop A Hole e .,40 l 30. �.. � Diameter in (�) c..lnrhPs . � L N U � s mE C O>� N _J N Blows/Foot N 0 T O rn EE � —m0 L DESCRIPTION 10 20 30 40 Fill S-1 Moist, slightly rust -stained brownish gray, silty fine to medium SAND, some 12 Aly gravel (SM). 13 S-2 As above. 4 8 1 11 5 As above. 11 105 ♦1 u Cement odor at 5 1/2 to 6 feet (cement treatment?)., Drilledd water ......... m feet. � at 7 1 /2 feet r .. S 4 Weathered Weathered Vashon Lodgement Till 3 k10 sh brown to brownish gray, silty fine to medium SAND, some gravel Moistreddish 5 (SM). 5 - 10 S-5 Moist rust -stained brownish gray, silty fine to medium SAND, some gravel 3 4 A16 14 Vashon Lodgement Till S-6 Must, brownish a sill fine to medium SAND sorne #vel SM . Ml ------- gray, a. :., .: Bottom of exploration boring at 13 feet No ground water encountered. - 15 - 20 - 25 gra Sampler Type (ST): ❑ 2" OD Split Spoon Sampler (SPT) ❑ No Recovery M - Moisture Logged by: JPL 3" OD Split Spoon Sampler (D & M) !.N Ring Sample Water Level() Approved by: JNS ® Grab Sample ❑ Shelby Tube Sample 1 Water Level at time of drilling (ATD) r o o u a t o ear-th scgences May 25, 2017 Project No. 150499E001 R:F' 1 rztt Mr. Mark Bailey MAY 2 6 101512 th Avenue North Edmonds, Washington 98020 g Subject: Response to City Comments Bailey Residence 101512 th Avenue North CIPIT Edmonds, Washington opy Dear Mr. Bailey: As requested, Associated Earth Sciences, Inc. (AESI) has reviewed the comments provided in a "Plan Review Comments for Plan Check #BLD20170496" letter, prepared by the City of Edmonds and dated May 18, 2017. We have previously prepared a "Subsurface Exploration, Geologic Hazard, and Geotechnical Engineering Report — Bailey Residence", dated May 6, 2016, for the proposed slope and settlement mitigation project at the subject site, along with a "Geotechnical Consultation — Slope Tree Removal Assessment" letter, dated April 10, 2017. Review Comment Number 4, as outlined in the City of Edmonds letter, with AESI's response, is as follows. Comment 4 The geotechnical letter dated April 10, 2017 by Associated Earth Sciences Inc. states the following: "...the slope should be replanted as soon as possible with landscaping trees and shrubs, as desired..." The geotechnical engineer, however, must review the proposed tree cutting and planting plans and provide written documentation of how the entire project proposal is in compliance with the applicable standards of ECDC Chapters 23.40 and 23.80, including the specific design standards in 23.80.060 and 23.80.070. Chapter 23.40 of the Edmonds Community Development Code (ECDC) includes general provisions for all types of environmentally critical areas (including wetlands, fish, and wildlife habitat conservation areas, etc.), while Chapter 23.80 of the ECDC speaks directly to "Geologically Hazardous Areas", which fall under the purview of geotechnical study. Our responses to specific design standards outlined in ECDC 23.80.060 and 23.80.070 are presented in the following paragraphs. ECDC 23.80.060 limits alterations of geologically hazardous areas to activities that mitigate the hazard and will not adversely impact adjacent properties or other critical areas. For our review in preparing this letter, we were provided with the following plans: Kirkland Office 1911 Fifth Avenue I Kirkland, WA 98033 P 1425.827.7701 F 1425.827.5424 Everett Office 12911 Y,. Hewitt Avenue, Suite 2 1 Everett, WA 98201 P 1425.259.0522 F 1425.827.5424 Tacoma Office 1 1552 Commerce Street, Suite 102 1 Tacoma, WA 98402 P 1253.722.2992 F 1253.722.2993 www.aesgeo.com Studio 342 Landscape Architecture, "Bailey Silhacek Residence," Sheets L-1 through L-4, dated May 23, 2017 SSF Structural Engineering, "Bailey Residence Shoring," Sheets S1.1, SH2.1 and SH3.1, dated May 22, 2017 Based on our review of the provided plans, it is our opinion that: a) the proposed project will not increase the threat of the geological hazard to adjacent properties beyond predevelopment conditions; b) will not adversely impact other critical area; and c) is designed so that the hazard to the project is mitigated to a level equal to less than predevelopment conditions. It is also our opinion that the temporary irrigation plan for the proposed plantings, as described in Sheets L-3 and L-4, should not adversely impact slope stability. We recommend that the temporary irrigation system be periodically checked for leaks. ECDC 2.3,80.070 includes design standards for projects in landslide hazard areas, including minimum factors of safety for landslide occurrences. Our May 6, 2016 report included slope stability modeling which resulted in factors of safety meeting or exceeding the recommended minimum values of 1.2 under seismic conditions and 1.5 under static conditions. Our report then stated that the proposed retaining wall "appears feasible from a geotechnical standpoint provided the wall is designed as a retaining wall with sufficient embedment to provide the factors of safety predicted by our model." Based on our review of the above-mentioned project plans, it is our opinion that the proposed soldier pile retaining wall is designed with sufficient embedment to provide the predicted factors of safety. If you should have any questions concerning this letter, please do not hesitate to call our office. Sincerely, ASSOCIATED EARTH SCIENCES, INC. Kirkland, Washington c A-1 Jeffrey P. Laub, L. L.E.G. Bruce L. Blyton, P.E. Senior Project Er ' ineering Geologist Senior Principal Engineer J PL/pc—150499E001-5 — Projects\20150499\KE\W P 2