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11-07-1977 Planning Packet
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11-07-1977 Planning Packet
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1/25/2024 11:17:10 AM
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Page -6- <br />iun green, <br />hillsides <br />aturated <br />Lis during <br />ractive <br />9linie change) <br />LI is mod- <br />scposed for <br />green <br />11 sides <br />saturated, <br />rainy <br />t ei^sed. <br />tural <br />is adequate, <br />in moisture <br />a. Ihis is <br />:ones sat- <br />Fie steepness <br />if the <br />>sion hazard <br />rink-swell <br />mtent. The <br />le difference <br />1 has been <br />s of this <br />n the area <br />Medium <br />Green <br />Page -7- <br />t <br />ifegfen cUy loam - 6 to 12 percent slop.. <br />TtS s ’S "“P Is green, <br />hillsides. Because this erioSS^th^^ stoped areas on lowlls and <br />The rolling mraSivr^i5$f “ '=^ ^ <br />however, ***P*«* “ "»* uncoamon <br />strength is adequate for iSi^tial*dSrf?Ii^?^c?'-®!!*‘^ <br />change) is moderate with changes^in^iwistmT^tent^'iS^®^!"K srsi M <br />Minnetonka <br />clayey sediments. fhi?is ^'*®s ofbroad flat tracts and drainaeewavs Th^r^A « ^ soil occurring in mainlv iimt- _^ere are a few ston-e <br />root depth during wet periods of the cD?i '*®^®rtable at a 1 to '3 <br />residential development. The soil strength is adequate for <br />permeable, ohrink-swell Tvolume rhanoAi i * soil is moderately to slowl <br />M moisture content. ^ moderate to high with changes <br />Nessel loam: <br />till. « calcare <br />y^etation was ad^ed^torS^'roe’sSfll^ "““vein Hennepin County. mapped in only one slope phas< <br />Nessel loam - 1 to 4 percent sinp#>» <br />soil is nwly Iwel^ NeB and the color is light green. Th <br />a f^ hilltops that are above^Hayden*^oS^m^the relief and <br />sou IS nearly level little graJng is r^ir^f®*' <br />This <br />on <br />Dark <br />Blue <br />■'i. I. -J •< <br />The m <br />is an <br />more <br />iment <br />near ‘ <br />value: <br />Shorewc <br />This is <br />clayey <br />vegetal <br />mapped <br />develop <br />Shorewt <br />The m <br />is a <br />smootL <br />requii <br />at a <br />with c <br />gth is <br />The ro <br />is a I <br />Since <br />soil ; <br />depth, <br />moisti <br />for r<
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