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3611 FEDERAL AVE 2018-01-02 MF Import
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3611 FEDERAL AVE 2018-01-02 MF Import
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Last modified
2/4/2022 2:23:54 PM
Creation date
2/10/2017 4:07:52 PM
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Address Document
Street Name
FEDERAL AVE
Street Number
3611
Imported From Microfiche
Yes
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Geologic Investigation and Geotechnical Enitineerin¢ Report <br />Jones Residence <br />3611 Federal are. <br />Everett, Washington <br />98-08-10 <br />Site grades in the proposed construction area range from moderately sloping to moderately flat or slightly <br />sloping in an easterly direction. Elevations, based on the supplied Sit Plan, range front a high of el. 382 at <br />the southwestern property corner to a low of el. 347 at the northeastern property corner. Silty dirt is <br />exposed in most areas on the property. A siltation fence has been placed along the lower eastern property <br />line. <br />A Site Map showing the existing topography and the location of our test pits is included in Appendix B of <br />this report. <br />3.2 Geoloeic Setting <br />The site lies in a geologic region known as the Puget Sound Lowland Physiographic Province. The Puget <br />Sound Lowland Physiographic Province consists of a linear depression that trends in a north -south <br />direction between the Olympic Mountains to the west and the Cascade Mountains to the east. The Lo%%land <br />contains the majority of the Puget Sound Basin area. During the recent geologic past, within the last I <br />million years or so, the topography of the Lowland was altered by a series of glacial events originating out <br />of the Canadian Rockies (cordilleran ice flows) and the northern Cascade Mountains (alpine ice flows) <br />Deposits of at least four -(a) Pleistocene aged glaciations have been identified in the Puget Sound Lowland <br />Physiographic Province. The last of these glaciations has been named the Fraser. The Fraser Glaciation <br />includes two-(1) recognized advances (slades) separated by an interstade — or retreat period. The younger <br />stade of the Fraser Glaciation is locally known as the Sumas, while the older is called the Vashon Stade <br />Deposits from the Vashon Stade and a later interstade (post-Vashon) are found within the project area. <br />Surficial geologic deposits in the project area have been mapped by the USGS and published in the <br />Geologic Map of the Everett 7.5 Minute Quadrangle, .Snohomish County, Wa. by J.P. Minard dated 1985. <br />For reference purposes, a copy of a portion of this map containing the project site has been included as a <br />Geologic Map in Appendix C of this report. <br />4 GES, Inc. <br />
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