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• <br /> Pearson Property Slope Stabilization NGA File No 945216 <br /> 1907 West Mukilteo Boulevard February 19,2016 <br /> Everett,Washington Page 5 <br /> The medium dense or better native glacial soils interpreted to form the core of the site slope are <br /> considered stable with respect to deep-seated slope failures. However, the loose surficial materials and <br /> undocumented fill on the slope have the potential for shallow sloughing failures during seismic events. <br /> Such events should not directly affect the proposed wall provided our recommendations as described in <br /> this report are followed. <br /> Landslide Hazard/Slope Stability <br /> The criteria used for evaluation of landslide hazards include soil type, slope gradient, and groundwater <br /> conditions. A steep west-facing slope with gradients up to 38 degrees (78 percent) is located below the <br /> existing residence. We did not observe significant evidence of past deep-seated slopes instability, or <br /> major erosion or sloughing events, on the slope directly below the residence during our site visit. <br /> However, indications of settlement and erosion were observed within the upper surficial soils along the <br /> top of the steep slope. We also observed evidence of surficial instability on the neighboring property to <br /> the west. Some groundwater seepage was observed emitting from near the toe of the steep slope. <br /> Our explorations and observations indicate that the core of the steep slope consists primarily of medium <br /> dense or better glacial soils. Inclinations up to 38 degrees on the slope indicate high strength and internal <br /> friction angle within the underlying soils. Relatively shallow failures as well as surficial erosion are <br /> natural processes and should be expected on these slopes especially within the loose surficial soils and the <br /> undocumented fill soils on the slopes. There is evidence that such events have taken place on the steep <br /> slopes in the vicinity of this site. It is our opinion that while there is potential for on-going sloughing, soil <br /> creep, and shallow failures within the loose surficial and undocumented fill soils on the steep slope, there <br /> is not a significant potential for deep-seated rotational slope failures under current site conditions. Proper <br /> site grading and drainage as well as retaining wall construction as recommended in this report should help <br /> maintain current stability conditions. <br /> CONCLUSIONS AND RECOMMENDATIONS <br /> General <br /> Based on our explorations and observations of the current conditions in the vicinity of the top of slope <br /> area, it is our opinion that the proposed installation of a soldier pile cantilever retaining wall along the top <br /> of the steep slope is feasible from a geotechnical standpoint. Due to the presence of loose, undocumented <br /> fill soils within the yard and steep slope within the vicinity of the top of the steep slope, it is also our <br /> opinion that these soils may experience continued settlement and failures potentially impacting the back <br /> yard area and residence, especially during a seismic event if a retaining wall is not constructed. In our <br /> NELSON GEOTECHNICAL ASSOCIATES, INC. <br />