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URRcca /~(~tyLL cnnp~Y ZS - GS'% <br />'FF - r _. <br />These steep to w sry steep soils aro un stoep fens, and valloy an•1 m untain <br />sines}.,p^s ut ela•mti~~na of (i50n to R00~ feet. Th9 a••era~e annual prncinitation <br />is s},rn~•. 7.n inohes, tho m,an annual air tr,mpcraturn is about 44°F., end the average <br />fr•?st-r roe r.oriod is a',out t15 gays. The 7,illman soil occupies the broad, slightly <br />corcavn, ;mrts of the landscape. It makes up about ~,5 percent of t}:e unit. The <br />unnamed coh},ly loam soil occupies tho sonowhat aonvoz positions. It makes up <br />'about .45:peroont of the unit. Zillman riiffers in having a finer textured subsoil. <br />The Zillman soil is moder•atoly deep and well drained. It formed in glacial, <br />'-outwasli from mixed minerology parent matorials. <br />.. T;.pically the surfeco layer is dark h~~own stony loam about 3 inches thick. <br />Tlio suhsuil is dark brrnm stony sandy clay loam about 12 inches thick. The <br />'k~.'~'sui,strut,rso is very stony loamy sand. <br />~. Ponn,eability is rapid. affective rooting dopth ie 15 to 25 ~_nchos and the <br />availahin rater cap^.city is ~`.14 to O.1P in.~i~S. Surface runoff is slow and <br />the erosion hazard is alight. - <br />_The unnamad'cobbly loam soil is modoratel.y deep end well drained. It <br />- I~~formed in P:lacisl outwash from mixed winerolory parent materials. <br />. Tyricnlly the eurfac~ layer is dark hrown cohbl;• loam about 8 inches thick. <br />The enbsurface is brown very cobbly san-i;• loam about 32 inohes thick. This <br />grades into sand, cobble, and gravel nt depths between 40 and t;0 inches. <br />Pnrrwabillty is rapid. F.ffnetive rooting :lepth is 15 to ZO inohes end the <br />availa},ln o:ater cap city ie 0.06 to 0.11 in.~in. Surface runoff is slow and the <br />orosior~ hazard is alight. <br />. ~ ~: ~~_ <br />~-~ , <br />