HomeMy WebLinkAboutSlope Analysis for BLD2004-00770 - BLD Engineering / Geo-tech Reports - 5/20/2001 August 23,2004
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GEOTECHNICAL
TESTING LABORATORY
SEAN DOYLE
PO Box 2598
BELFAIR, WA98528 RECEIVED
CMG 2
BELFAlk OFFICE
Re: pole barn
421 Cutlass Way
Belfair, WA
Gentlemen:
This letter is written to confirm that we did a slope analysis on the property at 411 Cutlass Way and found the
slope conditions on the two properties to be very similar. It is our opinion that no further geotechnical study
will be needed for construction of the above referenced pole barn.
Thank you for this opportunity to be of service to you. If you have any questions, or if we can be of any further
assistance please call on us at (360) 754-4612.
Respectfully Submitted,
GEOTECHNICAL TESTING LABORATORY
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Harold Parks
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HAROLD PARKS
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10011 Blomberg Street SW,Olympia,WA 98512
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RECEIVED
N, 2 8 2004
426 W! CEDAR ST.
Slope Stability Investigation
au�k
311 NE Cutlass `
Apes Belfair, WA
Prepared for
Stephen Johnson,Inc.
by
Geotechnical Testing Lab
Olympia, WA
May 20, 2001
GEOTECI-INICAL
TESTING LABORATORY
STEPHEN JOHNSON,INC.
P.O. BOX 488
BELFAIR,WA 98528
Re: Slope stability &setback analysis
311 NE Cutlass Court
Belfair,WA
Gentlemen:
As per your request, we have conducted a slope stability investigation for a home located on the above referenced
property. The result of this investigation, together with our recommendations, are to be found in the following report.
The site is located in Mason County, Washington.
SUBSURFACE EXPLORATION PROGRAM
The subsurface exploration program consisted of a site reconnaissance and a review of information from our files of
similar,work performed in this area. The slope was observed by our geologist, who studied the soils exposed at the
site. The soil criteria shown on the slope profile were confirmed on the geological maps.
SITE CONDITIONS
The proposed home is to be located at the highest point of the lot on a leveled area to the west of the main access
street. No excessive erosion or deep seated instability was observed. Under the surface,the soil was found to be a
dense sandy gravel. The vegetation consists of grasses and trees indigenous to the northwest. The slope is bare of
vegetation except for a few Fir trees.
GEOLOGIC CONDITIONS
The geology of the area as mapped by the Coastal Zone Atlas of Mason County Vol. 9 is Vashon Till (Qvt)
characterized by Pleistocene silt deposits of sands, silty sands, and pebbly sands commonly bedded. It may contain
large erratics with gravel lenses. The lower slopes are composed of a Vashon recessional outwash(Qvr). These are
the youngest member of the Vashon Drift, consisting mainly of sandy and gravely meltwater or ablation deposits
which have not been compacted by.the continental ice sheet.
The native soils can be considered to be at or near their natural angle of repose, and the factor of safety for most of
the slope is near unity in the unsaturated condition.
HYDROLOGIC CONDITIONS
The lot slopes to the west and all surface runoff discharges to well established drainage ways that ultimately run
south and to the Hood Canal. Runoff from the roof and/or parking areas will not pose significant problems due to
the high porosity of the native soils.
SLOPE STABILILTY MODELING& ANALYSIS
The site was modeled using a slope program and we have included a profile of the model later in this report. The
native soils were modeled using 124 lbs/ft3 unit weight with an assumed phi angle of 33' in their cemented state.
10011 Blomberg Street SW,Olympia, WA 98512
Phone#:(206)7544612 Fax#: (206)7544848
GEOTECHNICAL
TESTING LABORATORY
We have calculated the slope and have found no indication of deep seated instability there.
Slope 1 is a profile of the natural slope to the west. Sectional failure may occur under saturated conditions. The
slope stability is mapped by the Coastal Zone Atlas of Mason County Vol. 9 as "stable". Sloughing in this area
will not impact the home because of the distance from the home to the western slope.
Our study also indicates that the slope is stable.
IMPACT ANALYSIS
We do not anticipate that the proposed project will have any off-site impact.
HISTORY OF LANDSLIDE ACTIVITY
Landslide activity has not occurred historically on the subject property. However occasional sloughing does occur
during periods of heavy precipitation along the North Shore Road over a mile from this site and under different
hydrologic and geologic conditions.
OPINION OF POTENTIAL STABILITY
Potential for instability is minimal. Potential for minor erosion is probable since all vegetation has been removed
from the site. To correct this annoyance,the bare ground should be seeded with grass or straw.
HILLSIDE FOUNDATIONS (DAYLIGHT DIMENSION)
Structures built on sloping sites offer a number of potential problems. Fig. I illustrates a basic consideration for
what is called the"daylight" dimension, which is the horizontal distance from the bottom of the footing to the
adjacent ground surface. Many building codes require a minimum distance for this dimension in order to assure
some safety against the pushing out of the footing in the downslope direction. Logically, the limit for this distance
depends on the type of soil and the angle of the slope of the ground surface.
For low slope angles, a reasonable daylight dimension is assured simply because of the usual requirements for the
minimum depth of the bottom of the footing below the surface in a vertical direction. As the slope increases, the
daylight dimension is less assured and should be limited to some minimum distance. A setback of 8 feet from the
horizontal intersect of the slope will provide the critical exposure necessary. (see Fig. 1)
A common problem with hillside construction is that shown in Fig. 2, where recontouring of the construction site
results in a portion of the building being placed on some significant depth of fill. If possible, all of the footings
should be carried down to a depth below the fill. If structural fill is used and placed with reasonable compaction, it
may be possible to rest the footings in the fill, provided that this is done only with inspection and supervision by a
qualified soils consultant.
RECOMMENDATIONS
All material excavated from the site cannot be dumped on site without adequate subgrade preparation at the spoils
location and proper fencing and runoff controls. All spoils soil must be compacted to 90% MDD (maximum dry
density)as per ASTM D-1557 and protected from erosion.
10011 Blomberg Street SW,Olympia, WA 98512
Phone#:(206)7544612 Fax#: (206)7544848
GEOTECIINICAL
TESTING LABORATORY
The conclusions and recommendations in this report are based on our interpretation of the site conditions as they
presently exist, anticipated future construction activities, and the expectation that our exploratory efforts adequately
define the subsurface conditions throughout the site. In the event that the scope or location of the project should
change, or subsurface conditions different from those encountered during our study be observed or suspected, we
should be advised. At that time, a review of the changed conditions will be made and alternative or remedial
recommendations given as requested.
Thank your for this opportunity to be of service to you. If you have any questions concerning this report, please
contact us at (360)754-4612.
Respecfully submitted,
GEOTEC�IFIND ICAL TESTING LAB
Harold Parks,
Engineering Geologist
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10011 Blomberg Street SW,Olympia, WA 98512
Phone#: (206)754-4612 Fax#: (206)754A848
G EOTECHNICAL
TESTING LABORATORY
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SLOPE STABILITY
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Steve Johnson
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¢angle: 33.0°
Unit Weight: 124
Critical Slope Angle,Saturated: 17.9°
Horizontal Sectional Sectional Angle of Total Saturated Saturated Unsaturatec Unsaturated
X Y Z Elevation Distance % Slope Factor Total Total Total Total Internal Factor Section Total Section Total Sectional
Grid Station Elevation Change From Last Slope Angle of Safety Horisontal Change Slope Angle Friction of Safety P> P> (S> (1> Factor
Line Point Feet Feet Ste.pt.(ft) P F Feet Feet % p ¢' F Critical Critical ¢ ¢ of Safety From To
1 0 175.00 0.00 0.00 0 0.0° n/e 0 0 0 0.01 16.5 e/a F Ste. Sta.
1 1 175.00 0.00 10.00 0.0% 0.0° n/e 10.00 0 0.0% 0.01 16.5 n/a Safe Safe Safe Safe n/o 0 1
1 2 175.00 0.00 10.00 0.0% 0.01 de 20.00 0 0.0% 0.0° 16.5 n/a Safe Safe Safe Safe n/a 0 2
1 3 175.00 0.00 10,00 0.0% 0.01 a/a 30.00 0 0.0% 0.0° 16.5 n/a Safe Safe Safe Safe n/a 0 3
1 4 174,00 1.00 10.00 10.0% 5.7° 2.% 40.00 1 2.5% 1.4° 16.5 11.85 Safe Safe Safe Safe 2.96 0 4
1 5 174.00 0.00 10.00 0.0% 0.0° Ida 50.00 1 2.0% 1.1° 16.5 14.81 Safe Safe Safe Safe 5.92 4 5
1 6 171.00 3.00 40.00 7.5% 4.3° 3.95 90.00 4 4.4% 2.5° 16.5 6.66 Safe Safe Safe Safe 3.95 0 6
1 7 171.00 0.00 15.00 0.0% 0.0° Ala 105.00 4 3.8% 2.2° 16.5 7.78 Safe Safe Safe Safe 5.43 6 7
1 8 166,00 5.00 50.00 10.0% 5.7° 2.% 155.00 9 5.8% 3.3° 16.5 5.10 Safe Safe Safe Safe 2.96 0 8
1 9 165.00 1.00 40.00 2.5% 1.4° 11.89 195.00 10 5.1% 2.9° 16.5 5.78 Safe Safe Safe Safe 4.44 8 9
1 10 160.00 5.00 18.00 27.8% 15.5° 1.07 213.00 15 7.0% 4.0° 16.5 4.21 Safe Safe Safe Safe 1.07 0 10
1 11 155.00 5.00 18.00 27.8°A 15.5° 1.07 231.00 20 8.7% 4.9° 16.5 3.42 Safe Safe Safe Safe 1.07 0 11
1 12 150.00 5.00 15.00 33.3% 18.4° 0.89 246.00 25 10.2% 5.8° 16.5 2.91 Yes Safe Safe Safe 0.89 0 12
1 13 145.00 5,00 18.00 27.8% 15.51 1.07 264.00 30 11.4% 6.5° 16.5 2.61 Safe Safe Safe Safe 0.98 12 13
1 14 140.00 5,00 21.00 23.8% 13.4° 1.24 285.00 35 12.3% 7.0° 16.5 2.41 Safe Safe Safe Safe 1.07 10 14
1 15 135.00 5.00 22.00 22.7% 12.8° 1.30 307.00 40 13.0% 7.4° 16.5 2.77 Safe Safe Safe we 1.11 10 15
1 16 130.00 5.00 22.00 22.7% 12.8° 1.30 329.00 45 13.7% 7.8° 16.5 2.17 Safe Safe Safe Safe 1.13 10 16
1 17 125.00 5.00 23.00 21.7% 12.3° 1.36 352.00 50 14.2% 8.1° 16.5 2.09 Safe Safe Safe Safe 1.16 10 17
1 18 125.00 0.00 54.00 0.0% 0.01 a/e 406.00 50 12.3% 7.0° 16.3 2.41 Safe .Safe Safe Safe 1.56 10 18
1 19 120.00 5.00 30.00 16.7% 9.5° 1.79 436.00 55 12.6% 7.2° 16.5 2.35 Safe Safe Safe Safe 1.59 10 19
1 20 120.00 0.00 30.00 0.0% 0.01 a/e 466.00 55 11.8% 6.7° 16.5 2.51 Safe Safe Safe Safe 1.78 10 20
Slope Profile
180,00 -- --- _...
r ad
170.00 h m e s i t e ;.
180.00 --- ----. ----- r ---•----------
150.00 .....-------------- - ... - •-- •---' i
Etevatlon
(feet) 140.00 --------.....------- ----
130.00 --.. ------------ .__d..r-e.i .,f.i_e_l.d_..a.r9
110.00 -----------------`------•----------,-
MAO
0 100 200 300 400 500
Horizontal Distance(Feet)
GEOTECHNICAL
TESTING LABORATORY
SITE PLAN
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10011 Blomberg Street SW, Olympia, WA 98512
G EOTECHNICAL
TESTING LABORATORY
daylight
FIGURE, 1 Critic:ul exposure colidilion for a IiWslde'fvotlng.
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FIGURE 2 1'roblenis of foundations on graded liWslde sites.
10011 Blomberg.StrW SW,Olympia, WA 98512