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RECEIVED
MAY 3 0 2001
CITY COPY
BUILDING DEPT.
FOOTING DRAINS SHAU NOT BE CONNECTED TO DETENTION SYSTEM
NOTES:
1. Call Engineering Division (771-0220) for a tightline and detention system inspectio
before backfilling and for final inspections. APPROVED BY
2, Responsibility for operation and maintenance of drainage systems on private properly is
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responsibility of the property owner. M
out and removed from tile catch basins to allow proper operation. The mulet control orifice DATE
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CONFORMED COPY
200107190730
07/19/2001 03:15 PM Snohomish
P-0002 RECORDED County
NO EXCISE TAX
RF.01J1PFr)
JUL 19 2001
BOB DANT101, S0011W501 UU11VI IfeBSUrOf
�By 1ROB _DANTINI
EASEMENT FOR STORM DRAINAGE LINE AND RETENTION SYSTEM
TIUS AGREEMENT, made this; Iq A day of —J 2001
by Billy and Ilona Anderson , hereinafter called the Grantor owners c,
Lots 35 and 36, Block 80, City of Edmonds, acc. to the plat recorded in Volume 2 of Plats,
pa e 39, records of Snohomish County, Wa. Together with vacated North 10 feet of
g Lots 35 and
Edmonds Street between 8th Avenue North and 9th Avenue North, adjacent to
36. Hereinafter referred to as Parcel A.
Tax Parcel #4342 -080-035
WITNESSETH: That for and in consideration of the sum of one dollar($ 1.00) and other valuable
consideration, it is hereby agreed that the Grantor grants to the owner of ;
Lots 33 and 34, Block 90, City of Edmonds, acc. to the plat recorded in Volume 2 of Plats,
page 39, records of Snohomish County, Wa. Together with vacated North 10 feet of
Edmonds Street between Sth Avenue North and 9th Avenue North, adjacent to Lots 33 and
34 . Hereinafter referred to as Parcel B.
Tax Parcel #4342-080-033
herein called the Grantee, its successors and assigns, an easement for utilities described as follows;
A utility easement over the South 20 feet of Parcel A for the purpose of.constructing,
maintaining and repairing a storm retention system including drain line into said retention
system from Parcel B. Said storm retention system is to be used by the Grantor also and
therefore any maintenance and/or repair work required to the retention system shall be shared
equally between Grantee and Grantor.
This agreement shall be a covenant running with the land and shall be binding upon all parties
and their successors and assigns forever
In any action between the parties hereto to enforce any of the terms of this Easement , the
prevailing party shall be entitled to recover all its expenses incurred in connection therewith,
including actual attorney's fees, including in connection with appeals.
RECEIVED
JUL 2 0 2001
OEVELOPMENT SERVICES CTR.
CITY OF EDMONDS
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IN WITNESS WHEREOF this mstru7,nt has been executed
By:3 !&-( W(,� ' 7 76'�
Billy Anderson
-11-.na �A.d,,..n
year first above written.
t4o
STATE OF WASHINGTON SS.
COUNTY OF Snohomish
On this Lft— day of 2001, before me personally appeared
Ilona And-ijerson, to me known to be the individual descnbw in and who executed the within and
foregoing instrument, and acknowledged that she signed the same as her free and voluntary act
and deed, for the uses and purposes therein mentioned.
IN WITNESS WHEROF, I have herunto set my hand and ixed my official seo the day and year
af
above written.
f
tary Public in and o e te f
,40, 0
ashington, residing at —
y commission expires
STATE OFWASHINGTON SS.
COUNTY SNOHOMISP,
Onthisia!dayof .
2001, 1 certify that I know or have satisfactory
evidence that n0L �-s- v-� signed this instrument & on oath stated that
torn
a authorized to execute the instrument and acknowledged it as the At Me �nFact of
'purposes
Biltv Anderson to be the free and voluntary
act of such party for the uses an&
meni-to-ne-dl-n -the instrument.
IN WITNESS WHEROF, I have herunto set
my hand my official seal the day and year
above written.
*andixed
I
otary Public in and f he S. of
residing at 500H )r)/,>/-(
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TERRA ASSOCIATES, Inc.
Consultants in Geotechnical Engineering, Geolc)gy
and
Environmental Earth Sciences
RECF--IVF.D
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W1 May 21, 2001
.'RM T Coli,1101 Project No. T-4482
PERMI
Billy and Ilona Anderson
321 NW 201st Place
Shoreline, Washington 98177
Subject: Geotechnical Consultation
Anderson Addition
811 Edmonds Street
Edmonds, Washington
Reference: preliminary Geotechnical Report, Anderson Additions, by Terra Associates, Inc.,
Project No. T-4482, dated October 15, 1999
Dear Mr. and Mrs. Anderson:
Based on our conversation with your architect, Mr. Ron Johnson, we understand that the proposed
north foundation wall of the building at 811 Edmonds Street will be approximately six feet north of the
north side of the existing residence. In our referenced report, we recommended that additions to the
existing residences extend no further north than the current northern edge of the existing structures.
We reviewed the proposed building location and foundation on plan sheets prepared by Ronald D.
Johnson Architect, dated May 1, 2001. Based on our review of these plans and our preliminary
geotechnical report, it is our opinion that the north building wall can be located as planned, provided
the foundation is supported by competent native soil with the outer edge of the footing at least ten feet
from the face of the slope, and. building and lot &ainage is not directed toward the slope in an
uncontrollelf manner. Based on conditions observed in Boring B-2, it may be necessary to lower
footing elevations on the north side ofthe building by several feet to reach the native bearing soil.
REcEIVED
MAY 3 0 2001
CITY COPY
12525 Willows Road, �.uite Jul, —.1 ..... 11— ---- -
Phone (425) 821-7777 - Fax (425) 821-4334 - terra@terra-associates.com
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Billy and Ilona Anderson
May 21, 2001
We trust this infonnation is sufficient for your current needs. If you have any questions or require
additional inforniation, please call.
Sincerely yours,
TERRA ASSOCIATES, INC.
a
Project No. T-4482
Page No. 2
a ga'wa w. -mw
PRELI INARY GEOTECHNICAL REPORT
Fg
�A
Anderson Addition S
811 and 821 Edmonds Street
Edmonds, Washington
Project No. T-4482
Terra Associates5 Inc.
A A A
WN
!'q%q
Prepared for:
A,
Billy and Ilona Anderson
Edmonds, Washington
October 15, 1999
RECEIVED
MAY 3 0 2001
BUILDING DEPT.
CITY COPY
K
�� � 77 NIm I
TERRA ASSOCIATESf Inc.
Consultants in Geotechnical Engineering, Geology
and
Environmental Earth Sciences
I
October 15, 1999
Project No. T-4482
Billy and Dona Anderson
321 NW 201stPlace
Shoreline, Washington 98177
Subject: preliminary Geotechnical Report
Anderson Additions
811 and 821 Edmonds Street
Edmonds, Washington
Dear Mr. and Ms. Anderson:
As requested,, we have conducted a preliminary geotechnical engineering study for the subject project. The
attached report presents our findings and recommenclations for the geotechnical aspects of project design and
construction.
Our field exploration indicates the site is generally underlain by medium dense to very dense sand with varying
amounts of gravel, followed by hard silt and clay. We did not encounter groundwater in either of the borings
drilled at the site. We did not observe indications of recent significant instability, groundwater seepage, or
erosion on the steep slope in the central and northern portions of the site.
In our opinion, the site conditions are suitable for the planned renovation/expansion. The undisturbed native
soils are suitable for sup orting the expected building loads. However, based on the results of our stability
P , e northern edges of the existing residences.
analyses, we do not recommend expansion beyond th
Provided the recommendations presented in this report are incorporated into project design and construction, we
do not expect that the planned renovation/expansion will have an adverse impact on the stability of the steep
slope at the site, or on adjacent properties. g the design phase of this project and look forward to
We appreciate the opportunity to be of service to you durin
working with you during the final design and construction phases.
: . - anl,i
12525 Wi I lows Koao, zounu 1 u 1, — ... , - --
Phone (425) 821-7777 - Fax (425) 821-4334 - terra@terra-associates.com
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Bill, and Ilona Anderson
October 15, 1999
We trust the information presented in this report is sufficient for your current needs. If you have any questions or
require additional information, please call.
Sincerely yours,
TERRA ASSOCIATES, INC.
i2C. Sadler, R P.G.
ing Ge ob 4
Project Engineer
742
T eodore J. er, P.
Principal E.Sc r
gi
JCS/TJS:dvp
ES 611WO1
cc: Mr. Percy Tse, Roth M11 Engineering Partners
Project No. T-4482
Page No. ii
TABLE OF CONTENTS
Page
1.0 project Description ................. .............................................................
1
2.0 Scope of Work .......... ......................................................................
...............................
3.0 Site Conditions ...........................................................................
3.1 Surface .............................................................................
......
.................................
3.2 Soils ......................................................................................
2
............................... 3
3.3 Groundwater .......................................................................
3
4.0 Geologic Hazards ................................ I ..............................................
.............................
.......
It
4.1 Erosion ..................................................................................
4.2 Steep Slope ........................................................................................................
3
4.3 Landslide .............................................................................
4.4 Seisrnic .................................................. 4 ..............................................
4 ............. 5
5.0 Discussion and Preliminary Recorturiendations .................................................... I ......... 5
5.1 General .............................................................................................................. . 5
5
0
5.2 Building Setbacks from Steep Slopes ....... t ..........................................
Grading
4 ..............
5
5.3 site Preparation and .............................................................................
5.4 Foundations ................................................................
................................. 6
5.5 Drainage .................................................
6.0 Additional Services ................... . ... ! ............................................................... 4 ................ 7
7.0 Limitations ................................. I ................. ............................................ ............... 8
Fiffu
Vicinity Map ........................................................
....... Figure I
Figure 2
Exploration Location Plan ......................................
.
........................
Figure 3
General ized Geologic Section A -A ...........................................
Generalized Geologic Section B-B . ............................ ..............................
..............
........................ Figure 4
APPendi
A
Field Exploration and Laboratory Testing .....................................................................
Appendix
CRI.
X1
Preliminary Geotechnical Report
Anderson Additions
811 and 821 Edmonds Street
Edmonds, Washington
1.0 PROJECT DESCRIPTION
The proposed project consists of the renovationtexpansion of the two existing residences on the site. No building
or development plans were available at the time of our study.
The recommendations contained in this report are based on limited site development information. Therefore, our
recommendations should be considered preliminary. We should review final design drawings and specifications
to verify that our recommendations have been properly interpreted and incorporated into project design.
2.0 SCOPE OF WORK
surface
On September 8, 1999, we drilled 2 test borings to a maximum depth of 31.5 feet below the existing
grades. Using the information obtained from the subsurface exploration, we developed preliminary geotechnical
recommendations for project design and construction. Specifically, this report addresses the following:
Soil and groundwater conditions
Geologic hazards
Site preparation and excavation
Building setbacks from steep slopes
Foundation design
Surface and subsurface drainage
3.0 SITE CONDITIONS
3.1 Surface
The project site is comprised of two residential lots located at 811 and 821 Edmonds Street in Edmonds,
Washington. The approximate location of the site is shown on Figure 1. The site is bordered by Edmonds Street
to the south, single-family residences to the east and west, and a steep ravine to the north. Shell Creek is located
at the bottom of the ravine.
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October 15, 1999
Project No. T-4482
Both lots are occupied by single-family residences. The residence at 811 Edmonds Street is a single -story wood -
frame building with a daylight basement and a carport. A topographic survey by Roth Hill Engineering Partners,
Inc., dated July 29, 1999, indicates that the main and basement floor elevations of the residence are Elev. 209.3
and Elev. 201.8, respectively. A large wooden deck extends from the northern side of the residence at the main
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floor elevation.
The residence at 821 Edmonds Street is single -story concrete block building. A floor elevation of 210.0 is shown
on the topographic plan. An eight -foot wide concrete patio extends from the northern side of the residence. A
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wood -frame shed is adjacent to the northeastern comer of the residence. We did not observe any signs of
significant distress to the buildings due to settlement or apparent slope movement.
Site grades are relatively flat on the southern side of the residences. The gradient slopes moderately to steeply
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down to the north-northeast on the northern side of the residences. The topographic survey indicates the slope on
60 to 70 feet high, with elevations ranging from abo ut Elev.
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the northern side of the residences is approximately
Shell Creek. Grades on
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210 near the southeastern comer of the site to about Elev. 140 along the southern edge of
Grades the lower 40 feet of the slope
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the upper 20 to 25 feet of the slope range between 20 and 50 percent. on
range between about 75 and 90 percent.
C 2
We did not observe indications of recent significant movement or instability on the slope. We did not observe
indications of groundwater seepage, saturated surface conditions, or recent significant erosion on the slope.
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However, in addition to relatively straight coniferous trees, we did observe several mature conifers with bowed
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trunks on the steeper portions of the slope, indicating long-term relatively shallow soil creep.
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Site vegetation in the vicinity of the residences generally consists of mature coniferous trees and landscaping
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shrubs and bushes. The slope is generally vegetated with mature coniferous and deciduous trees with a brush
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undergrowth.
3.2 Soil
The soil encountered in the borings generally consists of 26.5 to 3 1.0 feet of medium dense to dense sand with
varying amounts of gravel overlying hard clay. We encountered dry, very loose to loose sand in the upper six to
seven feet of each boring. The very loose sand appeared to be fill that was placed when the houses were
constructed. The fill appears to be localized to the northern side of the houses and does not appe at to extend
0
downslope.
m
Detailed descriptions of the subsurface conditions encountered in the borings are presented in Appendix A. The
approximate boring locations are shown on Figure 2.
The Geologic Map of the Ednionds East and Part of the Edmonds West Quadrangles, Washington, by James P.
Minard, dated 1983, classifies the soils in the vicinity of the site as advance outwash sands. Transitional bed
sediments, described as massive to bedded clay, silt, and fine to very fine sand, are shown underlying the advance
in the borings are consistent with this classification. The map
outwash sands. The silt and clay soils encountered
shows the contact between the advance outwash and the transitional beds at approximately Elev. 120. We
encountered the silt and clay at elevations of approximately Elev, 170 to Elev. 180.
Page No. 2
I
V,
October 15, 1999
Project No. T-4482
3.3 Groundwater
We did not encounter groundwater in the borings. However, the sands immediately above the silt and clay in
Boring B-2 were wet. We expect that a perched water table will develop on top of the hard silt and clay during
the wet winter and spring months.
In gen
p rme
,:rat, water infiltrates through the sands and becomes perched on the bard silt and clay. The relatively low
e bility of the silt and clay impedes the downward migration of water and causes it to flow laterally along
the surface of the silt and clay, where it can emerge as seeps and springs at lower elevations.
4.0 GEOLOGIC HAZARDS
4.1 Erosion
The Soil Conservation Service (SCS) has mapped the site soils as Alderwood-Urban land complex, 8 to 15
percent slopes in the relatively flat southern portion of the site, and Alderwood-Everett gravelly sandy loams, 25
to 70 percent slopes in the sloping northern portion of the site. The hard silt and clay observed at depth in the
borings, and expected to occur at lower elevations on the slope, would best correlate with Kitsap silt loam, 25 to
50 percent slopes.
The erosion hazards for soils classified as Alderwood-Urban land complex, 8 to 15 percent slopes and
Alderwood-Everett gravelly sandy loams, 25 to 70 percent slopes are classified as slight and moderate,
respectively. The erosion hazard for soils classified as Kitsap silt loam, 25 to 50 percent slopes is considered
high. While we did not observe indications of significant active erosion on the slope at the site, the soils on the
slope will be susceptible to erosion if exposed. Erosion protection measures, as required by the City of Edmonds,
will need to be in place prior to and during grading activities at the site.
4.2 Steep Slone
The City of Edmonds defines steep slope hazard areas as any ground that rises at an inclination of 40 percent or
more within a vertical elevation change of at least 20 feet. Based on this definition and the topographic
information provided to us, the slope located north of the eastern residence (821 Edmonds Street) is considered a
steep slope hazard area.
The slope located immediately north of the western residence (811 Edmonds Street) is not considered a steep
slope hazard area. The topographic information provided to us indicates that slope grades in that area range
between about 23 and 39 percent. The slope located off the northern edge of the subject property would be
considered a steep slope hazard area.
Page No. 3
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October 15, 1999
Project No. T-4482
4.3 Landslide
The City of Edmonds defines landslide hazard areas as follows:
1. Any area with slopes of 15 percent or greater and impermeable soils (typically silt and clay) frequently
interbedded with granular soils (predoirdnantly sand and gravel) and springs or groundwater.
2. Any area that includes areas with significant visible evidence of groundwater seepage, which also
includes existing landslide deposits, regardless of slopes.
3. Any area that has shown movement during the Holocene epoch (from 10,000 years ago to present) or is
underlain by mass wastage debris of that epoch as determined by a qualified geologist or geotechnical
engineer.
4. Any area potentially unstable as a result of rapid stream incision or stream bank erosion.
5. Any area located on an alluvial fan, presently subject to or potentially subject to, inundation by debris
flow or deposition of stream -transported sediments.
During our site visit, we did not observe on -site indications of recent significant instability, groundwater seepage,
or significant erosion on the slope face. The slope generally supported growth of mature trees, including some
relatively straight coniferous trees. However, because of the soil conditions observed at the test boring, the site
slopes would be defined as a landslide hazard area.
Stability analysis indicates that the steep slope north of the residences is currently stable and would be marginally
stable during a severe seismic event. The minimum factors of safety determined by our analysis for static
conditions and under severe seismic loading conditions north of each resi dence are as follows:
811 Edmonds Street
Static: Minimum factor of safety = 1.53
Seismic: Minimum factor of safety = 1.03
821 Edmonds Street
Static: Minimum factor of safety = 1.45
Seismic: Minimum factor of safety= 1 .001
our pseudostatic (seismic) analysis is based on a horizontal acceleration value of 0.2g.
Our test borings and available geologic information indicate that the soils on the slope consist primarily of
medium dense to dense sand and gravel overlying hard transitional bed silt and clays. In our opinion, provided
the recommendations in this report are followed, the proposed project will not increase the potential for slope
instability on -site or on adjacent properties, and the risk for such an occurrence is minimal.
Page No. 4
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Project No. T-4482
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The Puget Sound area falls within Seismic Zone 3. as classified by the 1997 Uniform Building Code (UBC).
Based on the soil conditions encountered and the local geology, a soil profile type of Sc, from Table 16-J of the
1997 UBC, should be used in design. ase in
Liquefaction is a phenomenon where there is a reduction or complete loss of soil strength due to an incre ained
water pressure induced by vibrations. Liquefaction mainly affects geologically recent deposits of fine-gr
sands that are below the groundwater table. Based on the soil and groundwater conditions we encountered, it is
our opinion that the risk for liquefaction to occur in potential building areas at this site is negligible.
5.0 DISCUSSION AND PRELIMINARY RECOMMENDATIONS
5.1 Genera
Based on our study, the site is suitable for the planned expansiontremodel from a geotechnical standpoint. The
Ils are suitable for supporting residential building loads.
native soils encountered below the surricial fii
The following recommendations should be incorporated into the project design drawings and construction
specifications. These recommendations are preliminary and may be altered or augmented upon review of the
final plans.
5.2 Buildin Setbacks from Steen Slopes
Because of the proximity of the steep slope to the existing residences, we used the results of our stability analyses
to determine limits of encroachment to the steep slope areas. As discussed, our analysis indicates the stability of
the slope will be marginal during a severe seismic event. The failure surface representing the lowest determined
factors of safety would affect the slope within about 24 feet of the northern edge of the western residence, and
immediately north of the northern edge of the eastern residence. ,
Based on our study, it is our opinion that additions to the existing residences should extend no further north than
the current northern edge of the existing structures. The approximate locations of the failure surfaces
representing the lowest seismic safety factors determined by our analysis are shown on Figures 3 and 4.
5.3 Site Preparation and Grading
Areas to be prepared for new construction should be stripped of all vegetation, organic surface soils, and other
deleterious materials. Soils containing organic material will not be suitable for use as structural fill but may be
used in nonstructural areas or for landscaping purposes.
Page No. 5
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October 15, 1999
Project No. T-4482
The on -site soils generally appear suitable for use as structural fill. However, the sands are fine grained and may
be difficult to compact as structural fill when too wet. The ability to use the on -site soils as structural fill will
depend on their moisture content and the prevailing weather conditions at the time of construction. In addition,
the upper three to four feet of soil is generally dry and will likely need moisture conditioning.
If the moisture content of the on -site soils cannot be maintained near their optimum percentage or if grading
activities will take place during the wet winter or spring months, the owner should be prepared to import wet
weather structural fill. For this purpose, we recommend importing a granular soil that meets the following
grading requirements:
U.S. Sieve Size
Percent Passing
3 inches
100
No. 4
75 maximum
No. 200
5 maximum*
*based on the 3/4-inch fraction
Prior to use, Terra Associates, Inc. should examine and test all materials imported to the site for use as structural
fill.
Structural fill should be placed on a firm subgrade of undisturbed native soil in uniform loose layers not
exceeding 12 inches. It should then be compacted to a minimum of 95 percent of the soil's maximum dry
density, as determined by ASTM Test Designation D-698 (Standard Proctor). The moisture content of the soil at
the time of compaction should be within two percent of its optimum, as deterrnined by this same ASTM standard.
In nonstructural areas or for backfill in utility trenches below a depth of 4 feet, the degree of compaction could be
reduced to 90 percent.
Fill should not be placed at the top or on the face of the steep slope. Final grade:s at the top of the slope must
promote surface drainage away from the slope crest.
5.4 Foundations
Spread Footings
New construction may be supported on conventional spread footing foundations bearing on competent native
soils or on structural fills placed above competent native soils, as recommended in the Section 5.3 of this report.
Perimeter foundations should be placed at least 1.5 feet below final exterior grades for frost protection. New
foundations on the northern sides of the building areas should be placed to a depth that results in at least ten feet
of lateral separation between the outer edge of the footing and the face of the slope. Interior foundations can be
constructed at any convenient depth.
Page No. 6
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We recommend designing foundations for a net allowable bearing capacity of 2,500 pounds per square foot (Psf).
For short-term loads, such as wind and seismic, a one-third increase in this allowable capacity can be used. For
the anticipated building loads and this bearing pressure applied, building settlements should be negligible.
For designing foundations to resist lateral loads, a friction coefficient of 0.4 can be used. Passive earth pressures
acting on the side of the footing and buried portion of the foundation stem wall can also be considered. We
recommend calculating this lateral resistance using an equivalent fluid weight of 350 pounds per cubic foot (pcf).
We recommend not including the upper 12 inches of soil in this computation because it can be affected by
weather or disturbed by future grading activity. This value assumes the foundation will be constructed neat
against competent native soil or backfilled with structural fill as described in Section 5.3 of this report. The
values recommended include a safety factor of 1.5.
5.5 Drainae
Surface
Water must not be allowed to flow uncontrolled over the crest of the steep slope or onto the slope face. Surface
water should be directed away from the slope crest to a point of collection and controlled discharge. If proposed
site grades do not allow for directing surface water away from the slope, then water should be collected and
tightlined to the bottom of the slope in a controlled manner.
Final exterior grades should promote free and positive drainage away from the building area. We recommend
p 'd'
rovi ing a gradient ofat least three percent for a rninimum distance often feet from the building perimeter.
Subsurface
We recommend installing a continuous drain along the outside lower edge of the perimeter building founclations.
The foundation drains and roof downspouts should be tightlined to an approved discharge facility. Subsurface
drains must be laid with a gradient sufficient to promote positive flow to a controlled point of approved
discharge. All drains should be provided with cleanouts at easily accessible locations. These cleanouts; should
be serviced at least once every year.
6.0 ADDITIONAL SERVICES
Terra Associates, Inc. should review the final design and specifications to verify that earthwork and foundation
recommendations have been properly interpreted and implemented in project design, We should also provide
geotechnical services during construction to observe compliance with the design concepts, specifications, and
recommendations. This will also allow for design changes if subsurface conditions differ from those anticipated
prior to the start of construction.
Page No. 7
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7.0 LIMITATIONS
We prepared this report in accordance with general ly accepted geotechnical engineering practices'. No other
warranty, expressed or implied, is made. This report is the property of Terra Associates, Inc. and is intended for
specific application to the Anderson Additions project in Edmonds, Washington. This report is for the exclusive
use of Billy and Ilona Anderson and their authorized representatives.
The analyses and preliminary recommendations presented in this report are based upon data obtained from the
on -site borings. Variations in soil conditions can occur, the nature and extent of which may not become evident
until construction. if variations appear evident, Terra Associates, Inc. should be requested to re-evaluate the
recommendations in this report prior to proceeding with construction.
Page No. 8
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REFERENCE: THE THOMAS GUIDE, METROPOLITAN PUGET SOUND, PAGE 454, 2000 EDITION.
VICINITY MAP
TERRA ANDERSON ADDITIONS
EDMONDS, WASHINGTON
OCIATES
ASS
Geotechnical Consultants Proj.No. 448 Date OCT. 1999 Figure
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APPROXIMATE SCALE
30 0 30 60 feet
LEGEND:
* APPROXIMATE BORING LOCATION
REFERENCE:
SITE PLAN PREPARED BY ROTH HILL ENGINEERING
PARTNERS, INC., JOB No. 99-459-11, SHEET 1 OF 1,
DATED 07/29/99.
SCALE: I" = 20' (H & V)
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SCALE: I' = 20' (H & V)
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APPENDIX A
FIELD EXPLORATION AND LABORATORY TESTING
Anderson Additions
Edmonds, Washington
On September 8, 1999, we explored subsurface conditions at the site by drilling 2 test borings to a maximum
depth of 31.5 feet below the existing ground surface. Soil samples were collected during drilling using the
Standard Penetration Test (SPT) in general accordance with ASTM Test Designation D-1586. The test boring
locations are shown on Figure. 2. The Boring Logs are presented on Figures A-2 and A-3.
An engineering geologist from our office conducted the field exploration, classified the soil conditions
encountered, maintained a log of each test boring, obtained representative soil samples, and observed pertinent
site features. All soil samples were visually classified in accordance with the Unified Soil Classification System
(USCS) described on Figure A-1.
Representative soil samples obtained from the borings were placed in sealed containers and taken to our
laboratory for further examination and testing. Laboratory testing included measuring the moisture content of all
soil samples. In addition, we performed grain size analyses on five of the soil samples, and determined the
limit analyses are
Atterberg limits of two soil samples. The results of the moisture content and Atterberg
rain size analyses are presented in Figures A-4 through A-6.
presented in Appendix A. The results of the g
Project No. T-4482
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LETTER
MAJOR DIVISIONS SYMBOL
B L
M oRd
TYPICAL DESCRIPTION
TY
Clean
G W
GW
__; __
well -graded gravels, gravel -sand mixtures, little or no
GRAVELS Gravels
fines.
0) (lass than
1-10
Poorly -graded gravels, gravel -sand mbdures, little or
..ry.gr.ded gra
_j
-8 QN) More than 5% fines)
%01F
no fines.
50% of coarse
GM
Silly gravels, gravel -sand -slit mixtures, non -plastic
a) fraction is Gravels
fines.
Lil
z
3) larger than No. With fines
4 sieve
GC
Clayey gravels, gravel -sand -clay mixtures, plastic fines.
cc
e 8 Clean
CIJ
SIN
Well -graded sands, gravelly sands, little or no lines.
0
Ln SANDS Sands
6
LU
r_ z (less than
SP
Poorly -graded sands or gravelly sands, little or no
More than 5% fines)
—
lines.
0
6.r-50% of coarse
fraction is
SIM
Silty sands, sand -silt mixtures, non-postic fines.
smaller than Sands
a M
No. 4 sieve with fines
SC
Clayey sands, sand -clay mixtures, plastic fines.
ML
Inorganic silts, took flour, clayey silts with slight
0
i
U)
SILTS AND CLAYS
plasticity.
�
M!p
2 C'J
CL
Inorganic clays of low to medium plasticity, (loan clay).
'0_4
W
0
E 6 a) Liquid limit Is less than 50%
'. Z L4
OL
Organic silts and organic clays of low Plasticity.
W
0
a
U) Co Q)
>
MH
Inorganic silts, elastic.
0
Er
to
=_ 0 SILTS AND CLAYS
(a
CH
Inorganic clays of high plasticity. fat clays.
W
Z
2!
0 E Liquid limit is greater than 50%
Organic of high
'Fno
CL
OH
clays plasticity.
HIGHLY ORGANIC SOILS
PT
Peat.
8.
0.
DEFINITION
OF TERMS AND SYMBOLS
Lu
Standard Penetration
2' OUTSIDE DIAMETER SPLIT
Density Resistance in BlowgE221:
SPOON SAMPLER
cc:
(D
Very loose 0-4
2.4" INSIDE DIAMETER RING SAMPLER
(a
Loose 4-10
0 R SHELBY TUBE SAMPLER
Z.
Medium dense 10-30
Dense 30-50
Y WATER LEVEL (DATE)
9'
z
<
CD
Very dense >50
Tr TORVANE READINGS, tsf
0
M
Sta Penetration
Pp PENETROMETER READING, tst
in Bit)
Consistenc Resis= ws/Foot
DD DRY DENSITY, pounds per cubic toot
C
Very soft 0-2
LL LIQUID LIMIT, percent
Soft 2-4
Medium stiff 48
pl PLASTIC INDEX
t
stiff 8-16
N STANDARD PENETRATION, blows per foot
Very stiff 16-32
Hard >32
UNIFIED SOIL CLASSIFICATION SYSTEM
TERRA
ASSOCIATES
ANDERSON ADDITIONS
EDMONDS, WASHINGTON
Geotechnical Consultants
Figure A-1
Boring No. B-1
Logged by: JCS
Approximate Elev. 206
Date: 9/8/99
Consistency/
CL
(N)
Moisture
Soil Description
Relative
Depth
(ft.)
E
0
Blows/
Content
Notes
Density
U)
ft.
N
Light brown SAND, fine grained, dry (SP)
Very Loose
3
6
With a few fine gravel.
Dry to moist.
Loose
7
2
----------------------------------------------
------- L�qq�t ------
5
6
2
Gray -brown SAND with gravel, fine to
Medium Dense
24
2
medium sand, fine gravel, moist (SP).
Medium Dense
10
28
3
Becomes fine grained, with occasional
Dense
15
32
2
fine gravel.
Dense
20
41
2
Very Dense
25
50
6
LL=22
Gray SILT, moist (ML).
Blue -gray SILT and CLAY, molst (CL-ML).
Hard
30
Bs-
13
L"
Gravel In Up of sampler.
Boring term1nated at 31.5 feet.
No groundwater.
Blow counts may not be accurate due to gravel In tip of sampler.
BORING LOG
TERRA
ANDERSON ADDITIONS
EDMONDS, WASHINGTON
ASSOCIATES
Proj. No. T-44 2 1
Date OCT 1999TFgre A-2
Geotechnlcal Consultants
M
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Boring No. B-2
Logged by: JCS
Approximate Elev. 200
Date: 9/8/99 ?
Consistency/ (N) Moisture
Soil Description Relative Depth E Blows/ Content Notes
Density (ft.) UW) ft.
Bro n SAND, fine to medium grained, Very Loose 2 5
w
dry (SP) (Appears to be fill based on i
topography). 2 7
Very Loose I
------------------------ ----------------------------_ -_------------------ 5 9 2
Gray -brown SAND with gravel. fine sand,
Loose
fine gravel, moist (SP). --------- ---------------------
-----------------------
Gray-brown SAND, fine grained, moist Medium Dense 18 2 1
(SP). With occasional fine gravel. :0 1
Medium Dense 10 14 3
Medium Dense 15 21 4
------------------------------ ----------------------- --------------------- z
Gray -brown SAND with gravel, fine sand,
fine 1. coarse gravel, moist (SP). Dense 20 31 4
M
Medium Dense 25 27 4
Becomes wet. Dense 3.5 tonstfe
P
Brown to �_a [3 7:1 l: Hard 30 37 LE �22
(CL-ML). ilhoca!:1rq11111:1'
Boring terminated at 31.5 feet.
Wet soils encountered at approximately 30 feet.
M,
BORING LOG
ANDERSON ADDITIONS
TERRA EDMONDS, WASHINGTON
ASSOCIATES
Geotechnicol Consultants
Proj. No. T-448,2 D t:-ES:EP�T �1999 1719�-r-A-3
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STATE SUACHARGiao,
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ENG. INSPECTION FEE
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THE OWNER. I AGREE TOO MPLY
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IN VIOLATION OF THE LABOR CODE OF THE STATE OF WASHINGTON RELATING TO
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IT IS UNLAWFULTO USE OR OCCUPY A BUILDING OR STRUCTURE UNTIL
A FINAL INSPECTION HAS BEEN MADE AND APPROVAL OR ACERTIFI- 371-0221
ORIGINAL - FILE YELLOW - INSPECTOR
CATE OF OCCUPANCY HAS BEEN GRANTED. UBC SECTION 109
FAX PINK - OWNER GOLD - ASSESSOR
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