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1. Increased bank erosion <br />2. Increase sedimentation <br />3, band loss <br />4. isl: habitat loss <br />5. Loss of riparian and floodpiain function (due to aC.andormen¢ of the floodplair~} <br />6. Bead-cuts which have altered the rive: profile outsice of ;oes nit areas <br />7. Lowering of the water table and dayiag-uu s'ueaY: ad;acent la>~tus <br />8. Increased wid4h/deptitrario which: <br />a. Decreases flood capacity <br />b. Increases stress in a;e near-bank-region, adding to Decelerated bank erosion <br />c. 'Decreases over-winter and Eate su:rirr~erlfail ris1.1-.: h::Qt zr>~s*-s~~^rtr cover <br />d. Increases temperatuae extremes (winter ecsd Scnu;ter) <br />e. increases chartnei slope <br />f. decreases sinuosity, ~:d tr,eander widfia rariJ {bz12 widY°tt/bzfticftsl! widPh) <br />g. Increases mesrder length and radius cf curvature whic;~ does ~eot allow the <br />seam to d;ssip~te its own e, ergy <br />The overall result of these chanrei ad}ustments ts~saugnout the aantin affected reach is or" <br />cha.~:net iastabitety grad severely degraded raver i:za±ta and functia:. :"l:a dimensions and patte:;s <br />of zhe stable C4 s~eg>n Type {see artac};ed paper on sze:-v:: clsssfcaL~on fo: refarence), should <br />Fsave the fol9owin5 vxiues as determined ;;°rom the t7SG1S gage data turd from aerial photo <br />interpretation of less-imgaced (non-graveled).~aches: <br />bankfull discharge (13 year return periodj: 3,4i3~ abcvo ien'tsosa Creea:, ~,Jv'J yfs betaw <br />bankfuEl width: T20 feet - (Current condiiicn: 250-350 Feei) <br />mean ben:<ful? deyth: 4 feet - {Current ccnditioa 0.9-1.5) <br />widtn/depth ratio: 30 - {%une~nP condition i67- 389, w;~'ch var,'es greatly) <br />meander 3ength :140G feet - {Garret t cordirlor Z$JQ•35fii~ feet) <br />zad:us of carvaruze: 324 et - (3 SQO-2COG ;eel} <br />it~eande: vrtdd; ratio: 7-8 - {C;urre::f cer;3ition i-l.~} <br />