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740 Big Island - 22-117-23-14-0001
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77-309, SUBD
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Project Packet
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2/10/2026 1:00:25 PM
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Page -2- <br />Medium <br />Blue <br />0 <br />Medium <br />Grecn <br />11 <br />hamel loam Vessel loam <br />rlavden loam Shorewood i 1 t y clay loam <br />Lake Beaches, sandy <br />A brief description of each soil is provided. Map symbols and colors are <br />provided to facilitate locating the soil V,7pes on the detailed soil map <br />provided with this report. <br />Hamel ] team <br />The map symbol for this soil is Ila and the map color is medium blue. <br />This is a deep, poorly drained soil that formed in loamy collurvium over <br />lo..:y till. The soil occurs in short, narrow drainage%ays on foot slopes <br />and in long winding drainageways between knolls and hills. The native <br />vegetation was mainly sedges, grasses and scattered poplar trees. During <br />wet periods of the year there is a perch,d watertablc within 1 foot of <br />the surface and ponding may o...r-isr. The high organic matter content in <br />the upper soil horizons means soil has low bearing values. There is <br />ii <br />high potential for frost as i <br />I{avden loam: <br />This is a deep, well -drained .nil that formed in loamy glacial till and <br />occurs on gently sloping to very steep slopes on lrnolls and hillsides. <br />The soil was strongly influenced by a forest environment in its develop- <br />ment. The natural vegetation was mixed hardwood forest. Shale and llro- <br />stone fragments as well as granitic cobbles and boulders are common through- <br />out. Several slope phases are mapped in Hennepin County. Each slope <br />phase mapped in the area of proposed development is distissed separately. <br />Hayden loam-- 2 to 6 percent slope: <br />the map symIxil for this soil is HbB and the map color is mediir7 green. <br />This is a gently undulating soil occupying areas on knolls and hillsides. <br />This soil is well -drained and therefore never saturated although sidc- <br />hi ll seepage is not uncommon around basement %.':115 dUrin;; ra inv se• ,:�!n.< <br />or spring thaws. The rolling slopes offer attractive building sites. <br />Soil strength is adequate. Shrink -swell (volume change) is low to rwxi- <br />crate Hith ckuinges in moisture content. The soil is r:ixlc:ratel•. rvIr-- <br />cable. Erosion is a hazard if the soil is left cxreced for extended <br />periods. <br />
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