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Geotechnical Engineering Evaluen • NGA File No. 1238721 <br /> Spencer Garage Addition February 11,2021 <br /> Everett,Washington Page 2 <br /> 8. Providing recommendations for subsurface utilities and pavement subgrade <br /> preparation. <br /> 9. Providing our opinion on stormwater infiltration feasibility. <br /> 10. Providing recommendations for infiltration/bioretention system installation, if feasible. <br /> 11. Providing general recommendations for site drainage and erosion control. <br /> 12. Documenting the results of our findings,conclusions, and recommendations in a written <br /> geotechnical report. <br /> SITE CONDITIONS <br /> Surface Conditions <br /> The site consists of a rectangular-shaped parcel covering approximately 0.45 acres. The site is occupied <br /> by a single-family residence with a detached garage and sport court to the south west. Topography <br /> within the site is generally level to gently sloping to the north. A graded, east- and north-facing slope <br /> with approximate vertical relief of 13 feet occupies the extreme southwest,corner of the.property, as <br /> shown on Cross Section A-A' in Figure 3.The slope includes a rockery supporting the base,which ranges <br /> up to 3.5 feet in exposed height. Vegetation within the site consists of grass=covered yard areas <br /> bordered by shrubs and one tree on the north side of the driveway. The site is bordered to the south <br /> and west by existing residential properties,to the north by West Mukilteo Boulevard,and to the east by <br /> Water Way. We did not observe surface water within the site during our site reconnaissance on <br /> February 4, 2021. <br /> Subsurface Conditions <br /> Geology: The geologic units for this site are shown on Geologic Map of the Everett 7.5 Minute <br /> Quadrangle, Snohomish County, Washington, by Minard, J.P. (USGS, 1985). The site is mapped as <br /> transitional beds (Qtb). Transitional beds are described as beds of gray clay, silt, and very fine to fine <br /> sand with some layers of peaty sand and gravel and may include some members of Pilchuck clay, <br /> Admiralty Clay, and Whidbey Formation. Our explorations typically encountered undocumented fill <br /> underlain by fine to,coarse silty sand with varying amounts of trace gravel which we interpreted as <br /> native transitional bed deposits. <br /> Explorations: The subsurface conditions within the site were explored on February 4, 2021 by <br /> excavating one test pit to an approximate depth of 6.5 feet below the existing ground surface using a <br /> mini-trackhoe. We also performed three hand augers to depths of approximately 5.5, 5.0, and 4.5 feet <br /> below the existing ground surface.The approximate locations of our explorations are shown on the Site <br /> Plan in Figure 2. <br /> NELSON GEOTECHNICAL ASSOCIATES, INC. <br />