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<br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br /><jA&EI?S tJtf51f <br />rtMrt/C05 ffi>I/J16.A/T <br />51!;.) [0G- C( r.")./S I(.;L/E.. <br />Acres <br /> <br />C 5 tJ'7t.I.2. <br /> <br />SURF ACE GEOLOOY <br />(e) <br /> <br />(10) <br />.0 Marille shales and re- .. <br />lated mudetoD" and <br />sil tatODe. <br /> <br />IV-14 <br /> <br />Watershed // T State <br /> <br />SiJbwatershed l?iZ ;/AJI-T/, T6 <br />~/11> h4V P <br /> <br />FIJI <br /> <br />I/AI./ (. ;;;; <br />Condition <br /> <br />Nallle H4If#1 - ,1!J./.,#J <br /> <br />Date ~'dl- 10 <br /> <br />PSIAC - 1968 <br /> <br />SEDIMENT YIELD FACTOR RATING <br /> <br />SOILS <br />(b) <br /> <br />CLIMATE <br />(c) <br /> <br />RUNOFF <br />(d) <br /> <br />TOPOORAPHY <br />(e) <br /> <br />(10) <br /> <br />HiCh peak nows per .. <br />unit area <br />Lars. volume of flow b. <br />per unit area <br /> <br />(20) <br /> <br />Steep upland slopes <br />(in excess of 30"7.) <br />Rich relie!; little or <br />no floodplain devel- <br />opment <br /> <br />(10) <br /> <br />Fine textured; ...i- .0 Storms of several e. <br />ly diaperaed; ..line- day.' duraUoa. with <br />atka11ae; bicb shrink. sbort periods of ill. b. <br />awell characteristics teue raiAfa11 <br />b. Sial!. If.in sUts anc:l[b. Frequent intense COD <br />fine sanda . veet1ve storms <br />c. Freez..thaw oceur- <br />reDce <br /> <br />N <br />N <br />00 <br />r.. <br /> <br />(10) <br /> <br /> (S) (5) (5) (5) (10) <br />e. Rocka of medium. .0 Medium textured soU .. Storms of moderate 0. Moderate peek nows a. Mo<1erate upland <br /> hartin.sa b. Occaaiona1 !'bet frac- duratioo. and intensity per umt area Slopes (less than 20~0) <br />b. Moderately weathered ments b. Infrequent convective b. Moderate volume of b. Moderate fan or flood. <br />c. Moderately fractured c. Calicbe layers storm. now per unit area plaia. development <br /> <br />(0) <br /> <br />Low peak floWS per a. <br />umtarea <br />Low volume of runoff b. <br />per unit area <br />Rare runoff events <br /> <br />(0) <br />Gentle upland slopes <br />(less tban 5,"0) <br />Extensive alluvial <br />plains <br /> <br /> (0) (0) (0) <br />.. Massive, hard forma- a. Hllh percentage of a. Humi4 cUmate with a. <br /> tions rock fraementa rainfaU of low inten- <br /> b. Accregated <:lays sity b. <br /> c. Hit;hin ol'lanlc matter b. Pre~itation in form <br /> of snow c. <br /> c. Arid climate, low in- <br /> tensity storms <br /> d. Arid cUmate; rare <br /> convective storms <br /> <br />F-.ctor <br />value <br /> <br />() <br /> <br />GROUND COVER <br /> <br />(0 <br /> <br />Ground cover does not <br />ceed 2()l'!0 <br />.. Vegetation sparse; little <br />or no Utter <br />b. No rock in surface soU <br />(\ C t; <br />t':' :J 1(.' :(':'(l <br /> <br />Cover Dot exceedi.nc 40'1. <br />s. Noticeable Utter <br />b. If trees present under- <br />story not well developed <br /> <br />1(#.:.. All'd4'1fP <br /> <br />:!J', I... DuLL. . <br />c --, (-10) <br />a. Area completely protect- <br />ed by vecetatioD., rock <br />fra~ents. litter <br />b. Little opportunity for <br />rainfall to reach erocUble <br />material <br />1(, '!/;~~tUi'" 5it '('5 <br />;"/;0;/ ,-~'. ,..t. t' 1 t ,(i5 <br /> <br />Factor , ,'/ <br />value 0 <br /> <br />I Subtotal (a) - (0) <br />(lrlst~C~IO"$ on '~tle'se) <br /> <br />r: <br />v <br /> <br />,r <br /> <br />LAND USE <br /> <br />(0) <br /> <br />(10) I <br />ex- a. <br />b. <br /> <br />(10) <br /> <br />More tban 50% cultivlted <br />Almost a.11 of area inten- <br />sively grazed <br />c. All of area recently <br />bwned <br /> <br />(0) <br /> <br />(0) <br /> <br />.. Less than 25,. cultivated <br />b. 50'1. or less recently <br />1...eeI <br />c. Less than 50'!. WeAsiva- <br />I,. iP'szed <br />d. OIdinary rold and other <br />consuuct!on <br /> <br />(-10) <br /> <br />.. No cultivation <br />b. No recent log&inl <br />c. Low intensity crazinc <br /> <br />/!' t.{"1.A <br /> <br />o <br />..21 <br /> <br />);. ;-)';- 00 <br /> <br />r"l <br />c.< <br /> <br />UPLAND EROSION <br /> <br />(b) <br /> <br />(25) <br /> <br />.. More than SO'T. of the <br />area characterized by rill <br />aDd gully or landslide <br />erosion <br /> <br />r ,? f.'" <br />C'. d!,. ;'f..,c 'j,,- <br /> <br />(10) <br /> <br />L About 2S-ro of tbe area <br />characterized by rill and. <br />Cully or landslide erosion <br />b. Wind erosion with depo- <br />sition in stream. channels <br /> <br />(0) <br />.. No apparent: sips of <br />erosion <br /> <br />9' <br />" <br /> <br />'/ <br /> <br />CHANNEL EROSION AND <br />SEDIMENT TRANSPORT <br />(i) <br /> <br />(25) <br /> <br />a. Eroding banks continu. <br />ously or at frequent in. <br />terv Rls witb large depths <br />and long Clow duration <br />b. Active he adcuts and de- <br />gradation in tributary <br />channels <br /> <br />(10) <br /> <br />a. Moderate now depth$. <br />medium now duration <br />withocc:asionally eroding <br />banks or bed. <br /> <br />f~jI~ ,;. !'r~/~' <br /> <br /> <br />(0) <br /> <br />.. Wide shaUow channels <br />with nat gradients and <br />short: now duration <br />b. Chaone Is in mas sive <br />rock. large boulders, or <br />well vegetated <br />c. Artificially controlled <br />channels <br /> <br />1-./ <br /> <br />I TOTAL ':{O = ,31-j <br />RAT1N~/- - - -. - ac.ft.!sq. mL/yr. <br /> <br />Subtotal (h) - (i) ) ). <br /> <br />,j ~ 5'....Y NJ J/w <br />SHEET l.!:i- OF R <br />