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~_ ~ ; ~ =CEIVED <br />.__ r.sull~rr i I;~.;f ? 4 2fl(~n <br />. _ ~ ~ _.f..l~ <br />i r., ~~~I:~ I:~ I.h-'~'t:Ill:'~- ~ '.h~ hrupl+Yl'd Itllllc III(' ,:. .' ~Iti IUlll,\\'~ IdeSl'Cll)llllnS aS pL't rile <br />S,vl ~unc\ o: L:u'tuic: l'outn\. h\ thr tiod ('nnsl,\au,m ticniccl <br />Balicr-hock oulcn,p complex. 15 to ~j't„ slup~~s - 'this complex ;onsisu of strc,n;~ly <br />>luputc to steep soils un ndecs and hogback>. It is :thnut ~(r•., Bailer stone sanliu Inam <br />and about ±D"~, ruck outcn,p. Bailer fumy sandy loam is mainlc an the cast-;acing slopes <br />of the edges :nxl consish of shallo\c. grautsh bnncn slum' s:uuly loam shout i+ inches <br />thick l'hr subsurface Ltucr is dark grayish hro\\'n ucr} stun\ sandy loam about S inches <br />thick prrnuahilny i~ nu,(Icratcly rapui and thc:luailahlc aster capacity is lo\u. 'I'hcsc <br />:oils o\crlir the sandstone to he mined (i,r the proposed (ilalle Quam. <br />Flaplustulls. hilly - Tltesc strongly sloping to steep sliils arc un fans and lo\cer sole slope, <br />of ridges m the tbothills. Thc surface and subsurface layers arc nlainl~ Inam or lau\ <br />lo:ml. fiat texture is cxtrenlcly xariahlc. uttcn within short distances. Some areas of these <br />soils hauc cohhly and stony surface and subsurface layers. Sall depth ran_es item <br />shallo\u u, deep. Thcsc .oils roponlxll~ occur at the stte a(liacent to the cast sole o1'thc <br />sanduonc riditc to fire nnn('Yl. <br />I i;u'lan tine s;utdy loam. I to ?"'~• slopes - Tltis nearl} level soil is on the tetraus. fans sell <br />_ _ • '.:,lieu sides, It consists o(dcep. \ucll drained soils that li,nne(i in alluvium \ueathrrc(I <br />tr,nn.nddish sandaonc and sh:de. In a rcpresrntatiue pn+tile the surface layer is dark <br />- i,Jdish Lrau' fine saadu loam shout 'inches thick. Thl: suhsod is reddish brown !ighi <br />~" ~Lrv loath shout ?II inches thick. Thc underl\•ing matcnal is fight reddish hrmcn Inam. <br />I'cm)eahility is moderate and the arailable walcr capacity is hi•~h. This sail repnn~xily <br />._ ~+.xurs ul the northern half of the potenn:d \uctland :tees along the wort side of the <br />~- proposed none site. It also reportedly occurs in the northeast portion of the proposed <br />._ pernlit area and extends ncarh' to i'S High\+'ay _'2+%. <br />Harbor fine :and}' loam. ? to <)°ro slopes This gently sloping to strongly slopittg soil is <br />on tertaces, fans sell Salle\' stdcs. Tins soil has a profile :>_s dcscrihcYl in the prcl:aimg <br />partgraph. hu: the combined thickness of the surface l;tucr and suhsotl is shout aft in _'a <br />iuches, 1'cnneahiiitu' is moderate and the acaiiai,lc wa;cr c:tpacih is hick- 'flux soil <br />reparte<lh occurs in the southern half of the potential wetland area located :dung the \\'(,•st <br />sill: of Ihr proposed pl.~rtllit area. <br />(-Ultnertnn-Barti(lnt U,inplex. Z h, On u Slopes -Tills complex consists of gcnth~ sloping u) <br />strongh sloping soils on the terraces and fans. It is shout 6(1°„ Connenon tine s:mdy <br />loam :old about '>"~ Barnum Inam. Thc Connenon fine san(h !solo is higher arts more <br />slupinc the Bantam loam is on the lower pans of fans an(I ul areas near streams, swalcs. <br />and drau;aeroaus. <br />' - Thc Connenon series consists of decrp, well drained soils that ti,nncd ut mixed <br />• .tlluuial material weathered from roll s andstone and shale . In a typical profile the <br />~~ <br />