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8920 EVERGREEN WAY THE RESERVE 2025-07-25
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8920 EVERGREEN WAY THE RESERVE 2025-07-25
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Last modified
7/25/2025 4:05:36 PM
Creation date
7/25/2025 3:34:51 PM
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Address Document
Street Name
EVERGREEN WAY
Street Number
8920
Tenant Name
THE RESERVE
Notes
STORMWATER SITE PLAN REPORT
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Zipper Geo Associates, LLC <br /> Reserve at Everett <br /> Project No.1117.01 <br /> May 1,2013 <br /> Soil Conditions <br /> The subsurface evaluation for this project included 10 test pits (TP-1 to TP-10). The test pits were <br /> advanced to depths ranging from about 4 to 16.5 feet below existing site grades using a track-mounted <br /> excavator. The approximate exploration locations are shown on the Site and Exploration Plan, Figure 2. <br /> Soils were visually classified in general accordance with the Unified Soil Classification System. <br /> Descriptive logs of the subsurface explorations and the procedures utilized in the subsurface exploration <br /> program are presented in Appendix A. A generalized description of soil conditions encountered in the <br /> test pits is presented below. Detailed descriptions of soils encountered are provided on the descriptive <br /> logs in Appendix A. <br /> Soils encountered in the test pits completed generally consisted of a surficial layer of forest duff and topsoil <br /> ranging from 6 inches to two feet thick. However,3 inches of concrete underlain by about 5 inches of pea <br /> gravel was encountered directly below the surface in test pit TP-9. Below the surficial layers, soils <br /> encountered in the tests pits generally consisted loose to medium dense,wet to saturated, silty sand with <br /> some gravel (weathered Glacial Till)extending to about 2 to 5 feet below existing site grades. However, in <br /> local areas (TP-2, TP-4) a thin layer of variable fill was encountered directly below the forest duff and <br /> topsoil. Below the fill in these test pits,weathered Glacial Till was encountered. Soils encountered below <br /> the weathered Glacial Till in all the test pits generally consisted of dense to very dense, moist to wet, <br /> gravelly, silty sand (Glacial Till). However, in test pit TP-5 at about 12 feet below existing site grade <br /> (approximately elevation 546 feet), a two foot layer of fine sand with some silt underlain by sandy gravel <br /> with trace silt was encountered below the Glacial Till. The sandy gravel was encountered to the completion <br /> depth of about 16.5 feet below existing site grade. Heavy groundwater seepage and caving of the test pit <br /> sidewalls was observed below 12 feet in test pit TP-5. Similar conditions were observed in test pit TP-6 from <br /> about 7 to 10 feet below existing site grade. <br /> Groundwater Conditions <br /> Groundwater was observed in test pits TP-4 through TP-6, TP-7, TP-9 and TP-10. In test pits TP-4 <br /> through TP-6, moderate to heavy groundwater seepage was observed at about 7 to 16.5 feet below <br /> existing site grades(approximately elevations 540 to 546 feet). Groundwater observed in these test pits <br /> is interpreted to be a shallow, local confined aquifer of unknown thickness. Test pits TP-4 through TP-6 <br /> were completed to a minimum elevation of about 537 feet. A lower groundwater confining layer was <br /> not encountered down to elevation 537 feet. In test pits TP-7, TP-9 and TP-10, groundwater was <br /> encountered at about 2 to 3 feet below existing site grades. Groundwater encountered in these test pits <br /> is interpreted to be a thin layer of saturated soils at the bottom of the weathered glacial till unit. <br /> Fluctuations in groundwater levels will likely occur due to seasonal variations in the amount of rainfall, <br /> runoff and other factors not evident at the time the explorations were performed. Therefore, <br /> groundwater levels during construction or at other times in the life of the structure may be higher than <br /> Page 3 <br />
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