Laserfiche WebLink
<br />A community flash flood reporting n~twork of river <br />and rainfell stations and a flood warning program developed and <br />operated in connection with the 24_hour Weather Bureau facilities <br />could minimize 10s3 of life and movable property in the event of <br />a major flOOd. Such an arrangement would require that local river <br />and rainfall reports be communicated promptly by responsible local <br />officials to the Weather Bureau forecast Offioe for evaluation and <br />analysis. If availsble, this data and analysis would be used by <br />the Weather Bureau to mOre accurately forewarn community repre- <br />eentativea of potential storm and flood conditions. This type of <br />network is preeently in effect in portions of ths Arkansas River <br />basin and, to an extremely limited degroe, in othor tributary areas. <br /> <br />WILD HORSC-DRY CRCEK <br /> <br />, <br />, <br />I <br /> <br />The Strea~ and Its Valley <br />~'ild Hotse..ory C.eek is a north_b"nk tributary of <br />the Arkansas Rive.. The watershed, approximat~ly 17 miles long <br />as measured from tho head~ete.s to the Arkansao River confluence <br />at P~eblo and aV8faging 5 miles wioe, hae a drainage erea of B2.8 <br />equare miles. Within the roughly rectangular ~atershed, eleva_ <br />tions vary from 6,000 feet nesr the headwaters to 4,700 faet at <br />thamouth. <br /> <br />I <br />I <br />i <br />. <br />, <br />; <br />I <br />i <br /> <br />The separate ephema.al streams, Wild Horse Creek and <br />Dry Creek, originate in the foothills of the frontal range north_ <br />west of Pueblo and flow in a southeaste.ly ditection to join nsa. <br />the ~ild KO~S8 subdivision community located approximately 2 m.les <br />northwest of the city. Belo~ thi5 junction point, the combined <br />~ild Korse_D~y Creek st.aa~ chBnnel pBsses under the U.S. Highway <br />50 bridge and, flowing i.r>e more southerly direction, receives <br />d1s~hargeg from lIHiliarn" [,aek at i'1il.. 2.64 abo'A 0.6 ~ilee down- <br />Sh8~~ froln thE! btidge. Continuing a hBlf-mile f'arthet, the str.."", <br />ente.s Pueblo's northwcGt fQ~idantial erea and then proceeds <br />th.ough the "xisting ccno"arcial ~nd railroad development c","plex <br />to discherge into the Arkansas River. <br />The headwaters of the resp~ctive creeks are fed f.orn <br />"no,.m~l.. ,,'OJ rainfall runoff during t,,~ late rall, ",inta" and <br />~a.ly Bp.ing. During the summB. month8, the flo~s are the result <br />of thunder.torms or gener~l .ain~ over the entire w~tetshed. <br />The scrub vegntation growing in the higher olev~ti~no <br />is typical of southern Colorado's foothill tsgione where fairly <br />.ough, b.ok~n terrain ueuolly prevail~. At lower elevations. the <br />creeks travers A high pl~i"s covar~d with sparse vegetetion of <br />eemi-~rid type--p.edominantly sage brush, cactus. and native graso. <br />The study rRoch e~tenoe from tha ~outh of Wild Koroe_ <br />0'.1 C."e~ "t the AI'ka"5"s River confluDnce to P;ile ~. 'Ie on the Dry <br /> <br />" <br /> <br />" <br />