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2908 49TH ST SW 2016-01-01 MF Import
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2908 49TH ST SW 2016-01-01 MF Import
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Last modified
4/25/2017 5:28:24 PM
Creation date
3/31/2017 2:59:56 PM
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Address Document
Street Name
49TH ST SW
Street Number
2908
Imported From Microfiche
Yes
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f <br />( September 7, 2010 <br />Mr. John Mustach <br />IL&A Job No. 10-03G <br />I'agc 2 <br />SI7'F. CONDITIONS <br />Surfacc Conditions <br />The general lication of the subjcct plat site is shown on Plate 1— Vicinity Map. The site is <br />situated on a moderate to sieep, predominately northedy-declining hillside. As shown on Plate 2 <br />— Partial Sitc Plan, Lots 5, 6 and 7 of the plat are bounded by Sca Breeze Way to the east and <br />lying to thc cast of this strcet is a steep ravine with a creek at its bottom. Th� terrain within these <br />lots generally slopes gendy to moderately northeasterly initially at about 7 to 27 percent grade, <br />then descends modcrately to steeply eastward at 30 percent or more down to Sea Breeze Way. <br />7'he lots are currenUy vacant and are covered with grass and weeds. <br />Gcologic Setting <br />"I'he Prcliminarv Surlicial Geolor:ic Map of thc Mukilteo and Fvcrctt Ouadran�les Snohomish <br />Countv. Washineton, by Mackey Smith, published by U. S. Geological Survey in 1976, was <br />referenced f'or the geologic and soil conditions at the site. According to this publication, the <br />suriicial soil unit at and in the vicinity of the subject lots is mapped as Esperance Sand (Q�). <br />'I'he gcology of thc 1'uget Sound Lowland has becn modificd by the advance and retreat of <br />scveral glacicrs in the past and subsequent deposits and erosion. Thc latest glacier advanced to <br />the Puget Sound Lowland is rclerred to as the Vashon Stade of the Fraser Glaciation, which has <br />occurred during the later stages of the Pleistocene Gpoch and retrcated from the region some <br />14,500 ycars ago. <br />Thc 8sperancc Sand soil unil is composcd of proglacial tlu��ial ouhvash deposits laid down tsy <br />slow-moving meltwuter streams finm thc advancing but distant Vashon glaciec It generally <br />consists of light-brown to light-gray, well-sortcd, fine-to-medium-graincd sand, with occasional <br />thin Ienses of silt or coarse sand and small gravel. In confined situation, the Esperance Sand <br />dcposits arc gencrally in dcnsc to very dense state and are quitc stable. Where exposed on slopes <br />devoid of vegetation, the Gsperance Sand deposits can be subjected to rainwash erosion and <br />LIU & ASSOCIATES, INC. <br />
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