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5900 36TH AVE W SEPA 015 - 034 - SOUNDVIEW BUSINESS CAMPUS - VERITAS Land Use Decision Documents 2025-04-22
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5900 36TH AVE W SEPA 015 - 034 - SOUNDVIEW BUSINESS CAMPUS - VERITAS Land Use Decision Documents 2025-04-22
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4/22/2025 9:53:29 AM
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36TH AVE W
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5900
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SEPA 015 - 034 - SOUNDVIEW BUSINESS CAMPUS - VERITAS
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Land Use Decision Documents
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listed as hydric, the predicted inclusions of Terric Medisaprists, McKenna, and Norma soils are <br />listed as hydric on the Washington State Hydric Soils List. <br />Alderwood-Everett gravelly sand, loam oam is on till plains, terraces, and outwash plains. This unit is <br />about 60 percent Alderwood gravelly sandy loam and about 25 percent Everett gravelly sandy <br />loam. Included in this unit are small areas of Ragnar, Indianola, McKenna, and Norma soils and <br />Terric Medisaprists in depressional areas and drainageways on plains. Also included are colluvial <br />soils, slump areas, and escarpments. Included areas make up about 15 percent of the total <br />acreage. The Alderwood soil is moderately deep over a hardpan and is moderately well drained. <br />It formed in glacial till. Typically, the surface layer is very dark grayish brown gravelly sandy <br />loam about 7 inches thick. The upper part of the subsoil is dark yellowish brown and dark brown <br />very gravelly sandy loam about 23 inches thick. A weakly cemented hardpan is at a depth of <br />about 35 inches. Depth to the hardpan ranges from 20 to 40 inches. Permeability of the <br />Alderwood soil is moderately rapid above the hardpan and very slow through it. A seasonal <br />perched water table is at a depth of 18 to 36 inches from January to March. Springs or seep areas <br />are common. Although Alderwood-Everett gravelly sandy loam is not listed as hydric, the <br />predicted inclusions of Terric Medisaprists, McKenna, and Norma soils are listed as hydric on <br />the Washington State Hydric Soils List. <br />3.1.3 Hydrology Criteria <br />As stated in the 2010 Regional Supplement, the "term wetland hydrology encompasses all <br />hydrologic characteristics of areas that are periodically inundated or have soils saturated to the <br />surface for a sufficient duration during the growing season." It also explains "areas with evident <br />characteristics of wetland hydrology are those where the presence of water has an overriding <br />influence on characteristics of vegetation and soils due to anaerobic and chemically reducing <br />conditions, respectively." <br />Additionally, the US Army Corps of Engineers 1987 Wetland Delineation Manual states that <br />"areas which are seasonally inundated and/or saturated to the surface for a consecutive number <br />of days >_ 12.5 percent of the growing season are wetlands, provided the soil and vegetation <br />parameters are met. Areas inundated or saturated between 5 and 12.5 percent of the growing <br />season in most years may or may not be wetlands. Areas saturated to the surface for less than 5 <br />percent of the growing season are non -wetlands." Field indicators were used to determine <br />whether wetland hydrology parameters were met on this site. <br />Critical Area Study 5 WRI# 15202 <br />Soundview Business Campus Rev. #2: October 2, 2015 <br />
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