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DAVID L. NELSON AND ASSOCIATES, INC. <br /> Consulting Engineering Gcology <br /> November 27, 1991 <br /> Project No. 10591 <br /> Page 5 <br /> mitigated by design or a setback used to locate structures a�,uay <br /> from areas expected to slough with time. <br /> ^_'he steeper gradients to the nor'_�� and somewhat to the west on <br /> site could be susceptible to sha�'.cw sloughing failures <br /> downslope, if ground water seepag+: (springs) were to occur in <br /> this vicinity. This could occu7: if the Whidbey Formation is at <br /> shallow deptti near the base of the ravine . 47e did not encounter <br /> any obvious signs of outcropping ground water within the steep <br /> slopes. Provisions for maintaining �.xisting slope stability, <br /> including drainage control, earthwork (filling and grading) <br /> control and struct�ire placement, are presented herein to reduce <br /> potential risk of �;l�pe failures . <br /> Springs/Ground Wate: Seepage Areas <br /> These two elements mentioned in the ordinance are similar <br /> conditions, which are discussed together in this letter. During <br /> our evaluation of the site, we observeQ the surface areas for <br /> springs and seeps, and observtd our backhoe exploration (test) <br /> pits for ground �aater seepage conditions. <br /> We did not encounter any evidence of springs or seeps within the <br /> site along the northerly or westerly slope. We did observe <br /> evidence of water within the swale area to the northeast, off- <br /> site. This water appears to be drainage within the swale from <br /> upslope. We also noted that a utility line had been constructed <br /> within this swale which may contribute to the observed wet <br /> conditions . Indications of seasonal wet and seepage conditions <br /> observed within the test pits just above and within the basal <br /> Whidbey Formation silts gives potential for perched ground water <br /> within the area. However, this would be considered as interflow <br /> and per�;hed water within the surficial sandy soils and above the <br /> relatively impermeable intei•glacial silts (Whidbey) . These <br /> conditions are expected to be seasonal in nature, and to lessen <br /> during the normally drier periods of the year. Our discussions <br /> in the RECOhS7ENDATIONS section present methods of mitigation of <br /> any perched or seepage waters encountered during construction. <br /> Dewatering and control of the drainage within this site will <br /> greatly increase the stability within the more sensitive soils <br /> and slope areas . ' <br /> Steep Slopes Associated with The Above Elements <br /> The ordinance states that steep slopes are those at 25 percent or <br /> - greater. Within this site, the steep slopes as defined appear to <br /> occur within the northerly and westerly portion of the site. We <br /> specifically observed this area, and performed test pits <br /> dcwnslope of the proposed residence area, to ascertain our <br /> � <br /> _ _ '. _" ._,w,,,....—_. __ :...._.:i'�fcF',.3�rirn.. <br />