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<br />VELOCITIES OF FLOW <br /> <br />llurin!l:Rlfl(}-yearl1ood,aVNal'(e"elocityof <br />flow in main channels and o'-erbank areas <br /> <br />FLOODED AREAS <br /> <br />would he as shown in Table;-,. <br /> <br />Thl'approxirnal<' Ii mil<< ,,(illuod>ltiotl thRt <br />would '",ult from a !;DO-year flood on the <br />~tr',am' und"," ~tud}- ar,- "hown On Plat." 1. <br />which ;'alw an index to more detailed map' <br />,hm\'lnf(th.. "rea' that would be inu,,,bh:dLy <br />th,- ll~l, antl500'l'~ar l1,-"-"ls (1'1""" 2-\;;). A, <br />may Ii<' ",'en from those plates, th,- area <br />inonda<<-dbythelllH-yearfloodalon!l:the <br />Animas Hiverwould eseentially extend anOS'i <br />tJw vall,'y fl(~))' throuJ<hout the ;tudy reach. <br />FhJtl oHrflow along lIermu:sa Cn."k would <br />dosely parallel the ,tream in the upper <br />portivnof the,;tudy reach. b"t woulddiverl'(e <br />int<' a wi<leni"l':fi>n sharl€ ea't<,r1y of the West <br />An;mas Road cro;,ing-, The .~OO-year flood <br />w,mld jl;pn"rally follow the ,;ame patkrn. a, <br />the lOG-year flood, but. in -<orne location~. <br />inundation would pxwnd farther [rom th~ <br />main str~am channels and bp ,uhstantiall)' <br />d,-,'pt'r.i:ionwar,'a.<wouldb"wbjedto.h,...t <br />now, which, '" noterl"&rlier.;~hr()ad."hallow <br />(",,,rland n",'ding g,'nerally Ips" than 2 fpp!. <br /><kcp,Sh,-ct flow fh><lin.: is charaderiz,-d by <br /> <br />TABLE 5 <br /> <br />AVERAGE VELOCITIES OF FLOW <br />lOO-YEAR FLOOO <br /> <br />SlreamJApproximateReach <br />A!\Il-lASRIVlm: <br />Baken; Br;dl'(t'torh'cr mile,,{ <br />River mile :,l:l to momh of llerm'lSa Cr,,('k <br />Mouth of Hermo~& Creek to <br />lowe,' hmitof ,t\l<J.Y <1"':\ <br /> <br />IJEHMOS.'\ CJU:~;K: <br />Upper limitof,wdy ar~a to <br />s(ation:L-lllO <br />Station 3.-100 W mouth o[ cr~d;' <br /> <br />\'doc;'}' ,00",-",<<'<1 t>v ,\oim", f(jvorO'lorban" o"~., <br /> <br />Vel,,,-'.ity of flow durin..: " 1;111)-,-"", fl,~,d <br />would l~' ,li!l:hth' hi!l:h,'r than durinI' " ]00. <br />-""",.n",Kl.I",h"e\fJu"--c'a,,-a,,vP](>citi,., <br />\\'"uldr"n~0from \.:jfc..tl'cr"'cond,ln",,,,,,, <br />h':1.1i7..,d "Ir""m ",';whe~_ for ,'xumpl" "",l<",d <br />I)(>nd, or d"wn,l,wlol fr"m natllralor man" <br />mad" "h~".",'t;o"", .....I",'jly nf no", wntlld <br />"ill'jifi,.,mtly ~".",.rl !.hl' av<'r"~,,, ohuwn in <br />T"ble r" <br /> <br />11.",,,1,,,;,,.,,,.,.,,.,:;.,,,, ''''""'",...Ih;,,,tt,,,,, I,'. ,".' <br /> <br />Velocity <br />(feet)Jf'r,,-'comi) <br />M.ln Channal O~arb.a"k Areas <br /> <br />" <br />, <br /> <br />., <br />2 <br /> <br />5 <br /> <br />, <br /> <br />\(l <br /> <br />" <br /> <br />, <br /> <br />, <br /> <br />FLOOD DAMAGES <br /> <br />Wau-r flowinl-! ut " r"tcof 7 fed pc,'sl'cond <br />or ~H""tprwillcuu""evl'r,'"r,-",io""f,tream- <br />banb am\ i, ""pahle of transportinJl,"larll'e <br />pwb. ~tr"amlmnb and th,'fill"",a,,,l bridl-:" <br />"I".t"",,,t, m"y h~ .-rod,'.d, ami tar>!~ :lTnO\lnl, <br />ofKmveL,,,ncl.aml,iltm,,yhetmnsportedh; <br />W".t~r fln,,'i"!,: at ~ '"'.- "f ",7/c'f't r<'r ",<'on<l <br />Wall'" nnwin" "t "bout 2 r(~'t I~"'",'e"n,lnr k,,, <br />wil\c1"j"'"i\,,,,,,!,silt.~mlfloodbC)rnfdchr:,, <br /> <br />,\ l'~I. nr :"~l-Y"'tl. n,"~'i ;n th~ ,tudy an,a <br />",,,,,1,1 ","''''. .ul"(:<nliaT ;Wr;"lllt"..al and <br />!.unlic i,wili(y dama,,~. RHi,j,'ntml. tnmnwr. <br /><'ial. and ,,,.I11,tri;d damaj('- w"uld b,. Jp" <br />Sili";fi('.,,nt duo' t" minim,,1 dev']"!"''''''l in <br />fh"l prO!l~ aft'''" A,,;riculturallos",', w"uld <br />""npl'i"" d~'tr"ction of crop" and liv(-sltK'k; <br />dam"K" to [arm and ran~h impf<"','nwnts <br />s!l"h '" i,'rijl;atior. ,)',wm" fem','" bui]di!ll:~. <br />pri\'i\l" I(.v,".' and farm ,'""ds; :<nc1t,n(' eo,t,,~ <br />r'-'"'Inrirw (,l'lp and p",,\ur,' land erod,'d nr <br />"(OVf'redw;th,illandd"Lri"It.,;i,l<'ntialh.;,,'~ <br />woul" intlud,' dar!laj(~ Il' f~llnd"tions, e,t~- <br />rior a'H] in!.'ri",' '~'"Il,. fle)o,.,', furnl.<hinli,,,nd <br /> <br />j:{ <br /> <br />unpredi('!.abl(' flow path~, It~ water _"urface <br />~I~vation would 0.' e!',..ntiall)' imlplw'ml<>nt of <br />thr water ,urfaee ei~vati"n nr flow alonyth~ <br />wljaeent .tr('amw",- aod i, aff,>eU'd princi- <br />pally u." m_tllral and manmade harrien to <br />[low inthl'ana" flooded_ The depth of flow in <br />th,' ch"nnd. of the Anim~' Ri\','r a"d H..r- <br />mo""-Cr"ckandadjaeentn,,,,(h>dar~:u;canlw <br />deU'nnin,'d from the water garfacf profil", <br />sho,,--non I'lat,'1< H;-32, <br />In total. the WO-}'earfl()(wlwo"ld;nundate <br />approximately 4,(~)() a('ft". of which :l,(i{)1) <br />a('reS are a,,;ricultur...l, 3.~O acfC' arc stn'am <br />ehmlnel. and ~O aere" are ro"d &nd railroad <br />r;;rhL,."f-way.lt,houldhenokdth"tallofthe <br />fl""dedan'a"hownon Plate"~,15m,,-vnothc <br />i"undakd at the same !.;me Le"a",e fhxl <br />producin.:comlition8inthedraio"K,'baoinsof <br />thp Anima, R;ver and Horm""a Creek would <br />not ""l'c"-'ar;ly '>ceur concun'ently. AI,o. <br />"hallow flc",din>"(.:,,nerall.v l",,,than ~ ;o<'h,," <br />,h,,'plmal'oCCllrheynndthpfloodpda,.ell,o <br />shown. <br /> <br />applia"""',and()\lt>ldeimpNHtnenL,_"",,ha>> <br />bwns '\1HJ ,..-a...1<-"" Publ;,. fa".il;t;' I""", <br />"--o,,ld """'pri,e d,nr.a>"" 111 rnadf",d and <br />,U','alll er"",ill>!', >L,lli Ii,..-, ,0',(,; of flc~)d <br />[ij(htinj(, cleanup. "nd re~toration, Hailt'oad <br />tra('k and emhankmentw"ul,l he,uLj,'ctt<, <br />.-lama>,," frnm immd"tiQIl, and .tft'ambanh <br />w",ulrlllf,"bj,'ctUlerosi"". A"",.",w.."riou, <br />area>, could u,. cut off for l~-t'i(>d. n\l\!l:iol: <br />frmn" few hotlr" W p"u!",hly ",ot rnnn' thao a <br />f,,\\' d~y, <1"e to hwh W"roT rnnmwr"l:1.ll"",,, <br />would indud,' structural and equipment <br />d"maj~"_ tl'm!".>rary 10"' of f,tl;;,,,,ss, and 10"' <br />,:if in\"\'"l<lry ,ulrcd em lower fl",rx, <br /> <br />u <br />