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.•> •, .:■• , ^ <br />mj <br />.‘•Jediun ,«-.«***Clencog siltv rlav. <br />JJ^is Wue. <br />loamy colluvitoi over calcareous Tmnr^°i^^ii *oil was formed in <br />®J^ypyins depressions and drainacekavs^^^Ti- is nearly lex'el <br />*»inantly sednes and vetsite^^e^' n!?^ vegetation ws <br />)-ear the watertable is with” llSr tf'-e <br />occur. 7h- high organic matter the surface and ponding mav <br />wans the soil has lo2 heSJLTvIS^ffor frost action. values. There is a high potential <br />Hamel loam: <br />loam- till. The^i/oeSrs in Lf ^ colluviun over <br />and in long winding drSSgLiJs »^°P®s <br />wet periods of the x-i*ar tSre if^ SrSli ^"®s- Purine <br />the surface and ponding mav occur watertabie within 1 foot of^ <br />the Wr soil horizon! me^ Srsoil^h^J^ in <br />a high potential for frost^tiSf. ^ “ntere is <br />Le Sueur loam: <br />Sr^’ «a'^’T;:?'Lu'i?cu« itr *" -i-^ye the closely intenningled cJrdiil^Lfif ” ^ ^ f®«t <br />boulders near the surface.® The rative atones and <br />a grass understory. The soil is manned »*« mixed hardKx>ods andCo'^ty. ™PPed in only one slope phase in Hennepin <br />Le Sueur loam ■ 1 to 4 percent- <br />The nap s>Tibol for this soil i« ir# n».i »■. <br />soil is nearly level to RenLy «^««n- This <br />is a perched uatertable within 3 feet^of^M?*^^^**^®®* ®" i®** Jmolls. There <br />the ve,r. Creinasc »ccds tote pSjLSd ilLSl*" »• P"lo<l» o" soil IS ncarlv level there is usLiwfirff”^ tasement walls. Since the cth IS adcoiL^f/. fn.. d 1__r little grading reouirtwi <br />-- *y..r. L-rainage needs to be provid^ k, Periods of <br />soil IS ncarlv level there is usLiwfirff”^ tasement walls. Since the <br />Rth IS ade^^t-e for residential deviiommi* required. Soil stren <br />IS low to moderate with changes in m^iS!‘coJ?S?!'* <br />V . •• -V.’ ’«{' »’ <br />mmm:;f. M r ♦♦ <br />Vr ,:y <br />'■ ' ■ •' ■'■■■.■ •'.j? ■ -I : .'-I..;*. <br />■'. i:-. •; .:.• .3®SM1 <br />• :: ■ . *.*. ' <br />.. .. Vv':^ <br />V. ^;■ <br />iMmM, -