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GeoTest Services, Inc. <br />Mukilteo SD —Wall Design, Everett, Washington <br />Site Conditions <br />February 26, 2018 <br />Job No. 18-0068 <br />The subject area (proposed wall location vicinity) is located on the south side of an <br />existing asphalt parking lot and along the northern portion of a wetland buffer. The <br />southern edge of the parking lot contained level surfaces and a curb that separated the <br />hardscape from south -facing, 2- to 4-foot tall slopes. A portion of the edge of the parking <br />area, within the subject area, is currently supported by a 2- to 3-foot tall rockery wall. A <br />catch basin and drain pipe existed within the southern portion of the subject area and <br />just south of the proposed retaining wall location (Figure 2). <br />The proposed retaining wall location existed within a vegetated area consisting of <br />juvenile and mature deciduous trees and blackberry briars. A wetland area existed to the <br />south and east of the subject area and retaining wall location. <br />Subsurface Conditions <br />Subsurface conditions were explored by excavating three test pits (TP-1 through TP-3) <br />with a subcontracted tracked excavator/operator subcontracted through GTS and <br />supervised by a staff Engineering Geologist. The test pits were advanced into soils at <br />the location at the base of the proposed retaining wall location (Figure 2). <br />The upper 12 inches of TP-1 consisted of soft, brown, moist, sandy silt with and roots <br />and organics (topsoil). Below the topsoil was approximately 4 feet of medium dense tan <br />to orange -brown, moist, silty sand with gravel (Weathered Glacial Till). Within this layer, <br />a lens of wood debris was present at 2 to 3 feet below ground surface (BGS). Below the <br />weathered layer was hard, gray and slightly sandy with gravels. This is interpreted to be <br />native (Glacial Till). Slight groundwater seepage was encountered at 5 feet BGS in the <br />test pit. <br />The upper 12 inches of TP-2 consisted of soft, brown, moist, sandy silt with and roots <br />and organics (topsoil). Below the topsoil was approximately 4 feet of medium dense tan <br />to orange -brown, moist silty sand with gravel (Weathered Glacial Till). At 2.8 feet BGS, <br />rapid (perched) groundwater seepage was observed in the north side of the excavation. <br />Below the weathered layer was hard, gray, and slightly sandy with gravels (Glacial Till). <br />The upper 6 inches of TP-3 consisted of soft, brown, moist sandy silt with and roots and <br />organics (topsoil). Below the topsoil was approximately 18 inches of medium dense tan <br />to orange -brown, moist, silty sand with gravel (Weathered Glacial Till). Below the layer of <br />Weathered Glacial Till was approximately 20 inches of native soft to medium stiff, gray <br />silt/clay fill (Glacial Till) fill. At approximately 4.5 feet BGS we encountered slightly <br />Weathered Glacial Till followed by native Glacial Till at approximately 7 feet to full depth <br />of our exploration. <br />Please refer to the attached test pit logs for more detail (Figures 9 and 10). <br />Groundwater <br />Slight groundwater seepage was encountered within TP-1 at 5 feet BGS and rapid <br />seepage in TP-2 at 2.8 feet BGS. We anticipate that the groundwater found in these two <br />test pits is in a perched condition at the transition between weathered and un-weathered <br />soil No groundwater was encountered within TP-3 to the full depth of the exploration. <br />Page 2 of 8 <br />