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CASCADE GEOTECHNICAL <br />A WASION OF CASCADE TESTING LABORATORY, INC. <br />12919 N.E.126TM PLACE KIRKLAND, WASHINGTON 98034 <br />KIRKLAND: (206) 821•SM SF.ATTLE: (206) 52"700 <br />March 21, 1985 <br />Cart. No. 853-13G <br />Mr. Jim Hesseltine <br />P.O. Box 615 <br />Snohomish, WA 98290 <br />Reference: Hesseltine Property <br />5829 Fleming Street <br />Everett, Washington <br />Dear Mr. Hesseltine: <br />On March 20, 1985 a geologist from Cascade Geotechnical visited <br />the above referenced site in order to conduct a study to determine <br />the type, depth and condition of the existing sub surface soils. <br />Three tests pits were dug using a self propelled backhoe. These <br />test pits .were located near the southeast corner, northeast corner <br />and midpoint of the west wall of the proposed building. P. maximum <br />excavation depth of thirteen and one-half (13 1/2) feet belo%. exist- <br />ing grade was achieved in the southeast corner pit. <br />In all three of the test pits a light gray gravelly silty sand with <br />construction rubble was found from the surface to a depth ranging <br />from two (2) feet (TP-3) to eleven (11) feet (TP-1)below existing <br />grades. This light gray soil layer is old dill. This fill unit is <br />underlain by a layer of highly organic silty sand, that ranges in <br />thickness from one-half (1/2) to three-quarters (3/4) of a foot <br />thick. Underlaying the organic layer was a reddish brown silty <br />sand. This material is the native soil and is of undetermined <br />thickness. No ground water seepage was encountered in any of: the <br />test pit excavations. <br />From our findings we have determined that the fill found across the <br />site may be suitable for carrying structural loads. However, since <br />we have no way of knowing how well the fill was compacted during <br />placement we can not accurately determine the potential for differ- <br />