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March 31, 2008 <br /> Mr. Paul Tessier <br /> L&A Job No. 8A027 <br /> Page 3 <br /> the Puget Sound Lowland is referred to as the Vashon Stade of the Fraser Glaciation, which has <br /> occurrcd during the later stagcs of the Pleistocene Epoch and retreated from the region some <br /> 14,500 yc:us ago. <br /> The Vashon till soil unit is depositcd direcUy by glucial ice during thc most recent glacial period <br /> as it advanced over an eroded, irregular surfacc of older formations and sedimcnts. It is a vcry <br /> dcnse mixture of unsorted clay, silt, sand, gravel, and scattcred cobbies and boulders, often <br /> rcicrred to as "hard pan". The V;�shon till over the top two to four feet is normally weathered to a <br /> medium-dense state, and is moderately permcable and compressible. The underlying fresh till is <br /> very dense and is practically impervious to stormwatcr infiltration. The Gesh till has the strength <br /> of low-grade concrete and can stand in a steep natural or cut slope for a long period. If rcmains <br /> undisturbed and well-dr�ined, the fresh till can provide excellent foundation suppoR with IitUe <br /> scltlement cxpected. <br /> Thc advancc outwash soil unit undcrlying thc Vashon !ill is compused of stratificd sand and <br /> gravcl with minor amounts of silt and clay, dcposited by thc mcltwatcr of advuncing glacial icc. <br /> Duc to thcir gencrally granular com�msition, the advance outwash deposits are of moderately <br /> high pemieability and generally drains fairly well. The advance outwash deposits are glacially <br /> overriddcn :uid are generally dcnse to very dense in its natural, undisturbed state,except the top 2 <br /> to 4 fect where cxposed on slopes which may be wcathered to a loose to medium-dense slate. <br /> "1'hc advancc outwash dcposits can stand in stcep cuts or natural slopes for extended period when <br /> undisturbcd. Whcre exposed on slopcs with Ewor vegetation cover and subject to storm runotTor <br /> groundwater seepagc, thc advance outwash deposits can be gradually eroded and may slough and <br /> redeposit to a flatter inclination. �l'hc underlying fresh advance outwash deposits in their native, <br /> LIU & ASSOCIATES, INC. <br /> _ , . <br />