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northeastcm comer of lhe silc, immcdialcly nortlt ol I 10'�' Strcet SG. 'I7iesc broad survcys, howc��er <br /> are Uased on secondary sources such as aerial photographs, and are not necess�nily based on a site I <br /> visit. <br /> The Silver Lake wetland invcntory conductcd in 1990 identifies one Category II riparian �veQand � <br /> (Invcntory Wetiand N38) co��crine 43,G38 sc�uare fcet in lhe vicinity of lhe property's casterr. <br /> boundary (DEA, 1990). Thc �vciland was Jescribed as having an emcrgent componcnt dominated <br /> by reed canarygrass within its northem pertion and a forested component dominated by�vestern red <br /> cedar (77u jn p/icata), immature red alder, and salmonberry (Rt�Gus spectnbilis) (DEA, 1992). A <br /> drninage is a�so iclentificd that conveys Ilows from a �vetland Iocated north of I10°i (Im�entory <br /> Wetland 1t39) through a channel to Wetland 1138. The �vater was described as continuing south <br /> from WcUand I{38 and entcring a culvert that crosses SR 52? and dischargcs into Silvcr Lakr,. <br /> The Snohomish County soil si�rvey iJcntifies Alden��ood-Urban Land Complex soils throughout '� <br /> the site (SCS, 1983j. Aldenvood-Urban Land Complcx soils arc described as moderately well I <br /> drainrd with pernieability modcratcly rapid abovc a h:vdpan layer and vcry slow duough the <br /> hardpan. Aldcnvood-UrUan L:md Complex soils suppori a scasonal pc�ched �varer table at a depth � <br /> of 18 to 36 inches from January to March (SCS, 19831. Aldenvood-Urban Land Complex soils are <br /> not on thc Washington Statc Ilydric Soil List, but it can support Uydric soil inclusions(SCS, 1°90). <br /> 3.3 rIrLD INVGST[GATION <br /> 3.3.1 �Vctlands <br /> The results of the field investigation conducted by DEA on Decembcr 1 l, 2003, identificd hydric <br /> soils, hydropl�ytic planls, and evidence of wedand hydrology in one area on the property. This area <br /> was dctennincd to mcct thc criteria for jurisdictional wetlands, therefore, it was delir.caled and <br /> identified as Wclland A. �Vcd�u�d A spans thc dramage Ihat llows along the eastern property <br /> boundary:u�d occurs primarily off-site(Appendix B). Wetland A covers a total of 4.2f,R sauare feet <br /> (0.10 acrcj, of which 2,191 square fcet (0.05 acre) occurs on-sit t 4 documents the <br /> rcpresenh:tive conditions in WeUand A, while data plots 1, 2, 3, and 5 document adjacent upland <br /> areas on-sitc(Appcndix A). <br /> 'fhe wcqand has cxpericnced considerable degradation from past grading and on-going trash <br /> dumping ancl pcdestri:m traf(ia As a result, the vegetation in and around the wetland are dominated <br /> by weed specics, arcas wilh compacted soils devoid of vegetation are present, and an abundance of <br /> trash occurs throughout Wetland A and its buffer. <br /> Soils. Soils consistcd of a vcry dark gray (lUYR3/f) silty day loam �vithin 1G inches of the soil <br /> surface at data plot d. Soils contained sand dcposits in the upper d to 6 incL•es in somc parls of the <br /> wetlaud clusest to the drainagc. Thesc soils wcre detennined to be hydric based on the presence of <br /> a lo�v(1) matrix chroma color immediately bclow 10 inches depth. <br /> P.b10015D0117-01I.M`.�0.MFeviscd WCIIanJRepal JuN 70Dl.doc <br /> SenSili��c:1reas li��:dua�ion i July 200d � <br /> Sih•cr Lakc Cenhr Property �- <br />