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8110 LARIMER RD 2016-01-01 MF Import
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8110 LARIMER RD 2016-01-01 MF Import
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Last modified
5/18/2017 5:16:57 PM
Creation date
2/19/2017 1:24:00 PM
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Address Document
Street Name
LARIMER RD
Street Number
8110
Imported From Microfiche
Yes
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GeoTest Services, Inc. March 22, 2007 <br />8110 Lanmer Road, Everett, WA Job No. 07-0153 <br />below the surface, where the unweathered glacial till was encountered. TP-2 was <br />terminated at a depth of 10 feet. <br />Surface soil conditions at the site and in the vicini;y consisted of a thin topsoil cover <br />overlying what has been mapped as Aldenvood-Everett Gravelly Sand;� Loams - 25 to <br />70 Percent Slopes on the Soil Survey of Snohomish County Area, Washington (1978). <br />Visual observation of the soils in the test pits tend to confirm the mapped soil type was <br />present beneath the subject site. <br />Groundwater was not encountered in the test pits at the time of our investigation. <br />Discussion <br />The subject property is listed in the Snohomish County Code as a geologically <br />hazardous area, due to the presence of slopes with inclinations greater than 33% (-18°). <br />In general, it is our opinion that the subject lot slope is stable in its present condition and <br />r.onfnuration. Due to the hard glacial till interpreted to underlie the site, a deep seated <br />rotational type failure is unlikely to occur. <br />Evidence of a large deep-seated rotational type failure was not observed on the property <br />or in the immediate vicinity. Rotational failures can extend down into the subsurface <br />substantial depths. These failures leave typical geomorphic evidence of their existence <br />on the slope. Typical indicators are head scarps, tension cracks, sag ponds, seepage <br />zones, hummocky ground surface and slump blocks. As we did not perform a detailed <br />s�bsurface exploration for this assessment, we focused on traversing the accessible site <br />slope for visual evidence of past failures. No obvious visual indications of large-sr.ale <br />slope instability, such as those referenced above or signs of shallow sliding or excessive <br />erosion were observed on the lot or in the immediately surrounding vicinity. <br />Based upon the above information, it is our opinion that the proposea 60 foo; �•,etback <br />from the top of the steep slope will provide protection equal to or greater than that <br />provided by Snohomish County Code Section 30.62.210, which would be approximately <br />8 feet. <br />No evidence of groundwater was encountered in the test pits. Because of the lack of <br />groundwater, and the medium dense granular soils and hard, impermeable, fine grained <br />soils encountered at the proposed residence location, the potential for liquefaction at lhis <br />site is very unlikely. <br />Allowable Bearing Capacity <br />mtinuous or isolated spread footings founded directly on suitably prepared native, <br />�n dium dense, weathered till, may be proportioned using a maximum net allowable soii <br />i= :3ring pressure of 1,500 pounds per square ft(ps�. F^� t.`�� •`•�rd, �nweathered till, a <br />n,�.eimum net allowable soii bearing pressure of 2,500 p�r may be used. The term "net <br />allowable bearing pressure" refers to the pressure that can be imposed on the soil at <br />foundation level resulting from the total of all dead plus live loads, exclusive of the weight <br />of the focting or any backfill placed above the footing. The net allowable bearing <br />pressure may be increased by one-third for transient wind or seismic loads. <br />Page 2 0� 5 <br />
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