Laserfiche WebLink
1 <br /> <br />t <br /> <br />EXHIH~IT I <br />SOILS I NFOF2MAT I ON <br />:~i •;e lei .t ±: ;pes ~;cc~.-: r- r.: r, site -- agi.u:-~ l i s anc. aquents, <br />ary`f@: ,y ':LItJ'StY'a't.'_Im, Faoll ..::.•n1, ;..i -o i. perct_:r.'t. s:Lopes, Ccid'/ <br />lo~;m. 1 to percen.. aLopes., L:..im Laa.n, i. i:... _ or-rcer,r: .lopes., :~i~d <br />h:. i m loam, :5 i~~,-: ':% perr.[er~t ~ai r_pc: s, as mapped L; :: the USDA Sal i <br />Con=er•;~rta on 5er~.ice. Weld C~r_rnty Sur••:ey. <br />Aquolls and aquents - _ occurring on bottom <br />iloodplains of streams, are deep, poor.Ly drained =_ <br />formed in recent alluvium. Commonly, these lolls h-,avc- <br />' mlLdly alkaline to moderately a14:alinz loam~:• ar clays <br />layer and underlying material and are ;-rnderletln by son <br />and gravel within ~{13 inches. L-'. places, they I-:a•:e a a:! <br />' in the underlying material. The waterJCable is ~~t or <br />=_ur-fac~=~ earl.•~ In spring and recede.=- to de~ap as -i;=i in <br />i.r-. Ta.l i. Same VedYS. <br />1 <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br />1 <br /> <br /> <br />ands -and <br />:ill that <br />~nott:!ed, <br />surface <br />or sand <br />yed 1 aye-r <br />near the <br />hes L at.e <br />the ',qu~_~~.L s ~:r;d agr_trants mapping unit gtnFraL Ly h6r+'e =i~ ~~ r:chz=. <br />-. i::iant. growtl-: rnedlu:n, however'., locai.ized scouring rro fiar_di.i-ta <br />.r.a..~ hnve e::;-•oseci the gra~•: el l y subsoil . <br />H1= the Southeast end of the site lies a srnail p rtion of <br />4'aol.i loam - ~4. This i_ a deep well urai:-red soii on terraces, <br />formed :in all:_r•~ia.l deposits. <br />T'yp; ca~i.iy, tf;F sue+ace la~•.-•~r _ arayl sh brawn ~i as and tine <br />o~llli ': Loaln 3bi]ll t. ,:, lilC~lee l.hi c4;. Th,~ V.NJrarl yi n~.l math? ial to a <br />Je;,i:h of -•.-, ir-:chc--~::; is fine sandy J.oam. rerm~abiity .i ^c.ier-:~+_;-. <br />:-titn a high-: avaiaa6l~ water cap city. ~urfar_e r-i•.nar is ~=ry <br />slow and the erosion hazard i=_ low. <br />Colby loam, 15, is a deep ~.•~ell draineii soil. iJ_. far~ned in <br />calcarer~_r=_ eolian deposit=_. Typir_a.ily the sue+ace la; r is pale <br />brown abot.iJ-. 1:? inches thicFr.. The underlying materia. is very <br />gale--_ brawn silt loam ±o a depth of cU inche=_. <br />f'zrmc-abilit; is :moderate. Available water capnciL-~= is high. <br />Er+,-ci:ive rooting depth is oC! inches or mare. tier+ace rune+f is <br />:r:c:Jlum, and tl-te er~o=ion hazard .is moderate. <br />k:am loam„ '1, is a deep, well drainea ._11 ~.-n sma <br />rand aliuvlai fans.. It formed :in ml;;ed eoli.ar; deposit: <br />sedi~ner~t from a wide variety e+ bed:•-ocr::. Tyi:ncail+: t.. <br />ta•;ar is hr-owr-~ aru.-i pal= brown about: 1 inches thi.c4, <br />?0 inches of ti-~e undar.lyina material i=_ pale bro:•:n loam <br />:ti`r pi.ains <br />and parent <br />sur+a.ce <br />The iappe+^ <br />[-1 <br />