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<br /> <br />,,~T~_ <br />h:.' <br /> <br />.. ... '. ,., -' .. ~~~~: <br />a~l~'b .t.3 <br />.'. "U. t <br /> <br />Fort1f1cation C~'eek J(ep~ t. <br />:Revise!! 30 Sap 48t,~~:: <br />.....~, <br /> <br />" <br /> <br />-:-' <br />.;/-:. ".',. .~ <br />.<~:~.> <br /> <br /> <br />.. <br /> <br />Fortifice,tlori Creek and trlbutar:f.es in the mounta1.r~o;.lS upstream parts of <br />the basin are perennial except during dry yoarfl. and tributaries in other <br /> <br />'".'\'. <br />.;....{ <br />. .,;~>.:_' <br />:::;,-:') <br /> <br />p~ts of the basin ate intermittent. <br /> <br />., .~. <br /> <br />" <br /> <br />10. TopogrBpby.--Rolling hill., whioh con.titute mo.t of the ba.in! <br /> <br /> <br />are flanked by the Elkhead Mountains in the north pavt of the oaBin. Narrow <br /> <br />':./~..-.. <br /> <br />..';. <br /> <br /> <br /> <br />..:' <br /> <br />.yalleys are along the straamso Elevs.t1oZl.8 in tha basin r8ll€e frofll about: <br /> <br />10.500 feot in the Elkh.ed Mountain. to about 6,200 f..t n.ar Craig. <br />11. GeoloKY and Boils.__I.n, ~e..'1orel. the mo,mtaiua and gently sJ,o:p1ng- <br />hi1~e,. which. compose B. large pll.rt of the Fortification Creek B9:siJ1, are ot <br /> <br />',' <br /> <br />Sedilnantary fo:nnat1oi.1.so SOIlle of thes8 are htghly rr:etamorphosed... An ign8Q11B <br /> <br />intrusive formation aovers a re]A.tiv.I3J.:r sms...:.l a:rE::il. of the basin in Elkhead <br /> <br />Mountains$. The valleys flloDg F,):..~tif::'r:ation Croel:: and aJ.~')Dg YS.I:lpa :aiver <br /> <br />near Craig, COloo, are all'lVinl fille o~ varying depth~ The soil in tha <br /> <br />.. ,. <br />.'. <br /> <br />valleys 1s fertile alid cr'Jp yif:o~.de are high') The soils that reeul t from <br /> <br />the sedimentary for~ations in the Fortlfic2tion Croek Dasin betw~en Craig <br /> <br />and the junction of tittle :Bear and Fortific:l.tion Creek are. i:n general, of <br /> <br />;' <br /> <br />" - ..:;.... .~,'..:~. ;::~., ')-:.~~.:~.-~\;~ <br />.: :.'~',' , " <br /> <br />., :: ,'~<:~:f~:;,:': <br />:,,"",'~~n;";r;.;~: . <br />:.,; <br />: .,: ~. ~:. .. . <br /> <br />,~.. . <br /> <br />.adeq'Wite depth and ferUl.i. ty for d1'7....faI.mec. 16~'aiD.fJ'" <br /> <br /> <br />12~ Stream characte~~ice~__~he elevation of Fortification Creek Is <br /> <br />approxtDa~ely 10,000 f.et a~ it. .ouroe and 6,170 feet a~ it. '~nfl~nc. with <br /> <br />Yampa River. In the uPPf:lr part of H,~ c1rnl:r.e.ge bau:in, the oraek 1s in. <br /> <br />steep-we.l~ed canyons~ About 25 miles nor.~h of Craig the c:reek enters a <br /> <br />. ;.. ~ <br /> <br />na~row valley bordered by rolling hills, tb~ough which it meanders to the <br /> <br />'~l <br /> <br />:..'. <br /> <br />,....> ..>';-.;-<~.. .'. <br /> <br />confluenoe with Yampa River. The low-flow o.L2nnel re,Dgea from 10 to 30 <br /> <br />,~. . <br /> <br />"~:....../.:., <.. ~.;~"... <br /> <br />, . ',:,::'{:;~:':;f,iii,j,: <br /> <br />.. :- <br /> <br />f..t in width end from 5 to 15 fe.t in d.pth. ~he slop. of the channel <br /> <br />--;,;{.. . <br /> <br />,. <br /> <br />.'.. <br /> <br />" <br /> <br />ranges from about 500 f~et per mile in the moun't.ains to al:out g feet per. <br />m~l. near Craig. <br />13. 'V.lletat1on"",",A hea-q gro\<th of /l:l'a.... oovere th.nonoul,ttvato<i <br />)?art of 1Ib,e alluvial eoile ill, the et;ream vall eye. Grasses and sagebrush <br />are on the hUrls in the lower pa.rt at the besin.. Forests o~ aspen, pine,. <br />fir, and spruce grow above elevat~o~ 9,OOO~ B~ush and grasses ~re ~o~on <br />1~ the upper ba.in. <br /> <br />.., ',.:~:\ <br /> <br />\,',;.. <br /> <br />..., ,.'~ <br /> <br />','.' <br /> <br />. ..~ <br /> <br />\. <br /></: <br /> <br />'" <br /> <br />...".;i.\}\: <br />," <br />." ~ . <br />, . ~,,>: 1 <br />.<,.... <br /> <br />.., <br /> <br />" <br /> <br />," .i.. <br /> <br />',' <br /> <br /> <br />11 <br /> <br />..; <br /> <br />:,.. <br /> <br />,-. <br /> <br />,,', '"i,.'"",~,... "'," '-.' , ,... <.' "':;:"".:.;'",_ '" ,,"~';':)"'~ ,';:....~~,:;.~' <br />,',,, ":f.;"';~}1?-."-~! 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