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<br />0011.70 <br /> <br />with about ~r,..toO acre" und"'T irrigllliun in 19-H. <br />Tl:',lching II peak of about 96,000 acre... hy 1964. then <br />decreasing 10 abfllll ,'..S.:300 aeft';; in 197s, Total head <br />I)f livestock han. \-arifc-d from \ ear to \f'lIT hut in j;!:t'n- <br />(-fa] han- steadil.... df'creibE-d a -10181 or" about 1 million <br />hpad ()\(>r thf' 19H 10 197.>\ period. <br /> <br />Streamflow al'l"rdilln,. dut' In f"fl:'st mana!':f'ment <br />practic{'s in thE' subbasin were estimalt'd at 19....(10 <br />acn..ff:'t'l in 19H inc-reo,.ing 10 H.6r)l1 acrf.--f",et an- <br />nually In 1971".. <br /> <br />During the 19..t-i to 1918 perilld. thl' plJpulatLOn <br />..hifted from a primarily rural population of alltlUl <br />1~1).401l. or 6:2(', nf tht' 11l1al populotion. to a primanlv <br />urhan population with 1:10.7/10 rural and Ifll,.Jo:,! ur. <br />ban. ThiS change in population fel1t>('l,.; the growth due <br />to f'IlN10" dl'\'f:'lnpnlt'1l1 in the >;llhha~in. <br /> <br />Figure 27 <br />Yellowstone Subbasin <br />1978 level Depleted Streamflow <br />Yellowstone River near Sidney, Montana <br />1944. 1960 and 1978 <br /> <br />. <br />;: <br />~ <br />o <br />, <br />9 <br />E <br />. <br />. <br /> <br />SubbaSIn HISlorlC DeplelK)/1 <br />-Hi5tonc Streamflow <br />SubbasIn 1978 level <br />DepleliOfl <br />-1978 level <br />0. S <br /> <br />. <br />> <br />. <br />u <br />< <br />8 <br />~ <br /> <br />10.000 <br /> <br /> Vi "","" l,eamllOw _ <br /> ;: <br /> z <br /> I- <br /> ~ <br /> ~ <br /> Average HistOriC Stream'lo.. 1944"{97 <br /> 9360,000 A.F <br /> Average 1978 lever Depleted Stream/lOw 1944- <br /> _ 9.270,000 A F <br />- <br /> ~ <br /> <br />15.000 <br /> <br />14,000 <br /> <br />"000 <br /> <br />12000 <br /> <br />11,000 <br /> <br />9.000 <br /> <br />1978 <br /> <br />6.000 <br /> <br />7.000 <br /> <br />6000 <br /> <br />5.000 <br /> <br />, 000 <br /> <br />19~.l <br /> <br />19130 <br />Yea' <br /> <br />1918 <br /> <br />FrlJm HlH to W:.'i. total d{'pletion>; jncrl'a~t.d only <br />by ahout 2.'iO,1I1I0 anl'.feec howl'wr, during I9HO. total <br />dt'p]t'tion~ wert' llhout ...flll,non (1nl'.ff't"t aho\'l' the 197~ <br />]E-HI. The dt'ITell.;(> in total annual de-pletion~ Iwtwf't'n <br />19fi1l and 197..., i~ attrihule-d to a change in irrigation <br />praClH'e and a df'crt'ilse- in ITrigatt'-d acrb throughout <br />the perino 01 timt'. <br /> <br />:\ graph 01 .;e]h.!t.d .\'ear.; oltht. 19:;0;, lewl dl'p]He-d <br />"trt'aml1ow i,.. shown on Fi"'lJrt' 27 On thl' a\'erage, <br />haH.d on (tw Hl,1--I to 197," adju"'led ~lreaml1ow and <br />~uhjecl tn ,,\:Ite- waler right~, inter,..ul1f' compact" and <br />in~trl'amf1m\ n'4uirement~. ~1.:!70,(HIIl <tert'-ft'e-t an. <br />nllall~ an' availahle- for all non-consumpll\'l' and ne'" <br />l'on,..umpti\(' u,..f'~ aho\'l' Ihis ~trt'llm gilg:e. <br /> <br />Wl'slern Dakotas Subbasin <br /> <br />The \restern Uakota~ Stlhba~in co\'t'rs 77,119 <br />squart' miles in lht' north central part of the :\lissouri <br />Rin'r ha"in, FiJ:Urt' :!A (page 3:ll. <br /> <br />l'rinnpal trihut:-trit',.. tll tht' \!l..;,..(Juri Hin-r Includf' <br />the Little \tl~sotlri, Knife, Ht'llrt, Cannunhall. (;rand. <br />\loreau, Che-.\'t'nnt'. Had and \\'hite Hi\e-rs_ TIlt" to- <br />pography i,; rolling with e-It'\'ations i1vera~ing :!,OOO <br />("'l'!. Tht' Hlad; Hill.. Ill' :-;otlth Daknt1i and thl' Had. <br />Janns 01 :\orth Dakola art' two uniqllt' topogmphi{' <br />are-as in lilt' sllhhasin. TIll! majilfit\. 01 tht' suhha"in is <br />of a prairie grassland t'co~...,..lf"m. Exlt'nsj"e rlryli1nd <br />farming of t he crop fall"w typt' ha\'t> dt>\'t']opt'ri in west. <br />t'rn :'\orth ()Hkotll. <br /> <br />The majllrit.... 01 lht' ~\Jbhasin art'a is located in <br />;-";"rth and Soulh Ilakptil. Smilll parIs r\ft' a!sl1ll1{'Rted <br />in \fontana, \ryoming and :\'t'hrnska, H<tl1ching and <br />larming arf' !hf' prf'dominatf' t'conomic ~t'{.tors. Tour. <br />I,..m I,.. al~" an impllrtanl ,..{-'{'tor of tht, t'conom..... The <br />pronu{'\wn of enert.:.- hw]" from l'tlfll and lignite de-. <br />pl''''lt~, a,.. we-II a,.. the prl'duetioll of crudtO' oil and nat. <br />ura] ga... prp\'idt' signifil'llnl t'{'onomir <lI'ti\'ity. Gold <br />mint.d in Tilt' Hhwk Hill~ ;l{'('IIUllt,.. for <l high percent <br />01 \hl' naliollil] productioll. (;round water resource'" <br />aTe IUnlted I1nd gPIWTil]h- <Ir(, ,)f poor qualit..... <br /> <br />~urlan. waler ~uppli(-.; in t1H' tributary Slr('am~ lirt' <br />tht, ft'~ult of "'prmg ....now melt and ~t1mlller thunder. <br />"howt'f.;. :h a n'~lllt, ....treaml1ow;; In the trihutary <br />..trt'<lm~ ate ('xtremt,l.... variable from ....l'ar to ....ear. Th(' <br />~urfilt'e ",ater nlltl1tlw pomt -..e]e{'ted for Ihi."'- subba"in <br />I." Ihi' l--,,(~~ g-<lj!t' numher O(H~l;\n110 I..cated 011 the <br />\11~~ollri Hi\'('r .'II Furt Randall Dam, :'nuth Dakota. <br />Tht, drainagt' area ;ih/l\(' thaI pllin! i~ apptoximatt.l.... <br />~1;~,i)n(J square milt''''-. For the 19-H to 197", period of <br />record. Ihe .'I\eragt' recorded ~tre<lmnnw at that point <br />was about :!."dil-l c.L~.. or \'';.6 milliun acre. feet an. <br />nualh. <br /> <br />At thi,.. timp Ihert' are- no impllrls l.lr {'Xports of water <br />to or from this sllhha",-in. <br /> <br />Four major fl,,..t't\Hir,.. ha\e he-t'n cnnt-truct('d 1l11h(' <br />.;uhhasll1, all on tht, \Ii.'>souri main ..tern. In tt>rm" of <br />normal capanty tht, Oaht> re..er\'oir at 19.3 million <br />ill're.je-('t I~ the Iflrgbt. Cllrn"nn Dam and jt~ l.ake <br /> <br />:H <br />