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J A tJ - 2 2- 9 3 FRI 1 4 -,1 9 R.04 <br />DAVID L. NELSON AND ASSOCIATES, INC. <br />Consulting Enginctring Geology <br />October 10, 1990 <br />Project No. 9490 <br />Page 2 <br />findings of the subsurface conditions, including soils and hydrologic <br />csnditiom, and our conclusions and rooasealdations for development and <br />construction within the site area. In general, we concluded that the <br />evaluated site area should be carpatable with the proposed residential <br />devalckimb. He then presented our recasmardations for development and <br />construction of the proposed residences within the lot areas. <br />7be information presented in this letter should be considered as additional <br />and supplement,l information to our original geotechnical evaluation report on <br />the site area. <br />SENSITIVE 11NFA EVAUWION <br />The subject site area was evaluated for sensitive area evaluation, as <br />recaknauded in the now ordinance. Of the potential reasons for classification <br />as ouvircemastally sensitive (ennvironmmntally sensitive characteristics), the <br />following could occur on site; unstable soils hazard areas, landslide hazard <br />areas, seismic hazard areas, springs, ground water seepage, and steep slopes <br />associated or in conjunction with are or more of the environmentally sensitive <br />area elemanta. He will discuss these potential oleeants below. <br />Seismic Hazard <br />The Puget Sound region in classified as a zone 3 by the uniform Building Cade. <br />Seismic considerations for this type of site include liquefaction potential <br />and attenuation of ground motions by soft soil deposits. Typically, seismic <br />hazards are highest for thick alluvial (organic and/or normally Consolidated) <br />soils. The liquefaction potential is highest for loose sand and silty sand <br />deposits with a high ground water table. The thickness of the sand deposit <br />should be considered, as liquefaction is dependent on the ability of excess <br />pore pressured to dissipate. That is, if the deposit is relatively thin with <br />a short drainage path, the pore pressures can dissipate fairly rapidly. <br />He did not encounter any alluvial type soils on site which are typically <br />liquefaction sensitive. we did not find a significant thickness of fill or <br />