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1920 GRAND AVE Geotech Report 2022-10-25
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1920 GRAND AVE Geotech Report 2022-10-25
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Last modified
10/25/2022 11:20:29 AM
Creation date
6/3/2019 3:31:33 PM
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Address Document
Street Name
GRAND AVE
Street Number
1920
Address Document Type
Geotech Report
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Mr. Bill Messner ES-6132 <br /> October 5, 2018 Page 3 <br /> The referenced geologic map resource identifies Vashon advance outwash (Qva)and transitional <br /> beds (Qtb) across the site and slope. Vashon advance outwash is typically a well-sorted sand <br /> and gravel deposit, which was formed by streams issuing from the advancing ice sheet. The <br /> Vashon advance outwash commonly grades upward into glacial till (mapped east of Grand <br /> Avenue). Transitional beds are largely clay, silt, and very fine to fine sand, deposited in still or <br /> slowly moving water. In general, the referenced WSS resource identifies Alderwood series soils, <br /> either disturbed or undisturbed, across the site and surrounding areas. The Alderwood series <br /> was formed in glacial till plains. Based on the conditions reported at the boring locations, native <br /> soils on site appear consistent with the geologic setting outlined in this section. <br /> Groundwater was not reported at the boring locations during the November 2000 ECI fieldwork. <br /> It should be noted seepage rates and elevations fluctuate depending on many factors, including <br /> precipitation duration and intensity, the time of year, and soil conditions. In general, groundwater <br /> flow rates are higher during the winter, spring, and early summer months. <br /> Geologically Hazardous Areas <br /> We reviewed both the referenced City maps and EMC Title 19 to determine the presence of <br /> geologically hazardous areas (GHAs) on site. Based on our review, the following GHAs are <br /> present on site, all associated with the slope: high to very high and/or severe erosion hazard, <br /> medium to very high landslide hazard, and seismic hazard. <br /> Based on the observed sloughing and/or eroding, slope instability is shallow and can be <br /> remediated by the proposed system. Both the soldier pile and tieback installations will require <br /> isolated intrusions into the slope, which will be grouted, thereby increasing local slope stability. <br /> The combination of soldier piles and tiebacks will both protect the slope area from future <br /> weathering and erosion and stabilize the upper loose to medium dense soils. Considering these <br /> benefits, it is our opinion the proposed construction is appropriate from a geotechnical standpoint <br /> and will reduce the overall hazard associated with the mapped GHAs. <br /> Cantilever and Single-Tieback Soldier Pile Walls <br /> The shoring system should be designed to resist lateral soil pressure based on an active earth <br /> pressure condition given the proposed excavation depth. The following parameters may be used <br /> for shoring design: <br /> • Active earth pressure (level backfill) 35 pcf <br /> • Traffic and existing wall surcharge Negligible* <br /> • Passive earth pressure** 175 pcf(neglect upper three feet) <br /> * Existing pile-supported wall and related backfill is assumed negligible with respect to surcharge <br /> ** Passive earth pressure value may be applied over two-and-one-half pile diameters <br /> Earth Solutions NW,LLC <br />
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