700 52ND ST SE 2016-01-01 MF Import

and areas of McKenna soils, Norma soils and Terric Medisaprists in drainageways on plains. Also included are small areas of Everett, Indianola and Ragnar soils on terraces and outwash plains. � Permeabifity of this Alderwood soil is moderately rapid above the hardpan and very slow through it. Available water capacity is low. Effective rooting depth is 20 to 40 inches. Runoff is slow, and the hazard af water erosion is slight. A seasonal perched water table is at a depth of 18 to 36 inches from January to March. Everett aravellv sandv loam Everett gra��elly sandy loam is a very deep and somewhat excessively drained soil on terraces and outwash plains. It formed in glacial outwash. Typically the surface layer, where mixed to a depth of about 6 inches, is daric brown (7.5YR 3/2) gravelly sandy loam. The subsoils are dark brown (7.5YR 3/2 to 4/2) very gravelly sandy loam about 12 inches thidc. The upper part of the substratum is brown (7.5YR 5/2) very gravelly loamy sand about 5 inches [hick. Permeability of this Everett soil is rapid. Available water capacity is low. Effective rooting depth is at 60 inches or more. Runoff is slow, and the hazard of water erosion is slight. Included in this unit are small areas of Alderwood soils on till plai�ys, Indianola soils on terraces and outwash plains, and Ragnar soils on outwash plains. Mukilteo muck MukiReo muck is very deep very poorly drained soil in depressional areas. It formed in organic material derived dominantly from sedges. Typically, the upper layer is dark reddish brown (5YR 2/2) muck about 4 inches thick. The next layer is dark reddish brown and black (5YR 2/2 to 3/2 and 10YR 2'0) organic material 4 to 35 inches thick. Pertneability of this Mukilteo soil is moderate. Available water capacity is high. Effective rooting depth is Iimited by a high water table that is at or near the surface from October to May. Runoff is ponded. In most areas of this unit, the water table is art�cially drained to a depth of about 3 to 4 feet during the growing season. Some areas are ponded during the rainy season. Included in this unit are areas of Terric Medisaprists, Orcas peat, and Mukilteo soils that have noi been artficially drained. During the site invesiigation in July 2006, numerous test pits were dug to detertnine the presence or lack of hydric soils and wetfands. The majority of the test pits match the description of Alderwood gravelly loam, with the exception of those areas identified as wetland. 9 (Z