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C <br />The :ina1 soil ty- cansi is of c.,~ Cr.;,:.. s::.-.<iy '., ... .... . <br />Cli7 ie5 a Vary SC:a^.:~ x_23 _.. t.:< SJL'~CJ_:: ?Jt~1.)^. J: .... ..... .. <br />covering only 3% o_= _.... s`__<. _..~..~ so:.~ .._ ~_ ~~). .. _ .. ~ .. <br />erne were fo-':.ed .n ~vei :v a__uv_u:::. ...< ~:.r:.._. _. , . ... .... <br />grayish brotan sandyJioar. coat 4 is:chJS _..ic:. :'::-::....... <br />~T.iOdct"a Le tdiC~: a lOw a!~;ter-.:JS.~...^.,.'~ C.:7::.: _~}•, F:IL' ;~ ...'.J~ ~ ~ ~ .. .. . <br />The hazard of soil blowing is severer ar,d the i:azara J: t:..,::- <br />erJS1Jn is moderate. <br />In sur.~~ary, the soils occt:rri.~ _., tl:e r-o~osad lea7a ~_,.. _...._ <br />will be impacted by surface disturbance generally haves ,. ,_.~o.. <br />reclamation pocentiai. ., <br />_ , : ., ~ . ~ :.~ r <br />The Cryorthents soils cont:.ia cite majo~ _c. _,.~,.~ ... _ .., <br />reclamation. These soils era iow in fertility, :..< _..i:. ....... <br />a loos water-holding capacity aaZ are ,,u;,~ect co soy; _, t ....., .. <br />due to slope and tai;,d; by applying establis::ed t."..,,..., . <br />contouring, fertilizatior. for proc:nt estabiisi:::.::t of .......- <br />tion and snow feacir:g to' reduce the i:anact o_~ wi::.. o:~ tt.: ,, ... <br />surface and cc trap sno.a to provide more soil r.o~stu:"~ _...~, <br />factors can he sufficiently reduced sJ't;^.e site t:JUld hay, ... <br />potential for satisfactory reeler„ation. <br />~~ <br />F. '.Dater I.esources - <br />1.. Ground (i~ater -USGS is in the process of establisiri.-,^ ^r.,.:::.'. <br />water.mor.itoring in conjunction with the :IcCa11uT~ S}t;L\ ~ .:~• <br />but to date has gathered insufficient data tti accurately - <br />dict the ground water siiuatior. on tl:e site. USGS was i)~. ...) <br />~. SUDDly general information based on corn drill i::~ do::; _o~ _.... <br />:McCallum Open Filer'Report and preii:ainary core cc.ca fro::; ~.... <br />EdRIA Study drilling. \o major aquifers Caere ~ncour.t:tc~ ....: _ ., <br />tilt'. drilling. Aiinor amoun~s of water Caere intorc~nt<d ... ...,..;~_ <br />the 50 foot level. Tha material above the coal t:~s f_. .,_ ..... <br />and tightly bound. These conditions are not lavorabl:: fJr _ .•- <br />ductive aquifers, The geologic structure above ti;e coal _:, <br />heavily fractured and dipping at steep gradients. T;::: coaditio:::: <br />~~ will lead to small localized pockets of water. LocatiJ:l~Jf~ <br />these pockets were difficult to predict. <br />The existing '.Cerr operation has not encountered ..ay acc~i,'.~t~; <br />and has had no problems with ground taater cffecti::~ _...:ir <br />mining operation. USGS indicated that similar cor.dicL%;a .::.:; <br />be e:coec[ed on the proposed least tract and t.`.cy critic _p::.:~ <br />no adverse impacts to the ground taater and that ~-ou::~ o;~~,: <br />will noC limit Cher ?ro?osed operation of the mina. <br />2. Surface '.Dater -Detailed infprmation on the surface tla,cr ... <br />also lac'.cing.. The proposzd acreage is located _ . ~h;: Ca:t::,`.:.... <br />Fiver watershed. Tl:er„ err? no live strenm~ witl:i., t.., _... . . <br />A stock teetering improvement is located is Section 2~ .... .. <br />spring development is located in Section 2?. Tt:o '..nr ... <br /> <br />1~ <br />