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FLOOD00475
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Last modified
1/29/2010 10:15:21 AM
Creation date
10/4/2006 9:17:22 PM
Metadata
Fields
Template:
Floodplain Documents
Designation Number
157
County
Adams
Arapahoe
Douglas
Community
Denver Metro Region
Stream Name
Bear Creek
Title
Flood Hazard Area Delineation - Bear Creek
Date
12/1/1979
Designation Date
3/1/1980
Floodplain - Doc Type
Floodplain Report/Masterplan
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<br />I <br /> <br />I <br /> <br />I <br /> <br />feet. A large flooding area upstream of South Wadswor,th Boulevard <br /> <br /> <br />is caused by backwater from the bridge crossing. The water ponds <br /> <br /> <br />up behind South Wadsworth Boulevard, reaching depths of 1 to 2 feet <br /> <br /> <br />before flowing over the road just south of the channel. Very little <br /> <br /> <br />development exists in this area, and therefore very few structures <br /> <br />are in the floodplain. <br /> <br /> <br />In the reach from South Estes Street to South Kipling Street, <br />floodplain limits are approximately 400 to 500 feet in width and <br />are mostly confined to undeveloped land. There are, however, a <br />few structures upstream of the South Kipling Bridge which would <br />be inundated by the 100-year floodplain. <br /> <br />From South Kipling Street to the end of the study at Bear <br />Creek Dam, the floodplain narrows down to widths between 100 and <br />300 feet. Land in this area for the most part is undeveloped. <br />No structures are in the floodplain along this reach. <br /> <br />The floodway data presented show floodway widths to the right <br />and left of the channel centerline, along with the floodway eleva- <br />tion and total width of the floodway. <br /> <br />I <br /> <br />I <br /> <br />- FLOOD VELOCITIES - <br /> <br />I <br /> <br />Maximum flow velocities characteristic of a 100-year flood <br />event on Bear Creek are tablulated at typical cross sections on <br />the water profile sheets. <br /> <br />The flow velocity in the channel generally ranges between <br />5 fps and 15 fps. Velocity in the overbanks would range between <br />2 fps and 7 fps. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />- FLOODPLAIN AND FLOODWAY DATA - <br /> <br />Water velocities greater than 6 to 8 feet per second can <br />cause severe erosion of stream banks, and are capable of trans- <br />porting large rocks and debris. Velocities in this range can <br />also erode fill around bridge abutments, causing possible bridge <br />failure. Lower velocities of approximately 2 fps or less will <br />deposit debris and silt. <br /> <br />I <br /> <br />I <br /> <br />The Flood Hazard Area Delineation Maps show the outline of <br /> <br /> <br />the 100-year flood event for fully developed basin conditions and <br /> <br /> <br />present channel conditions. The maps are supplemented by Table II, <br /> <br />"Floodplain and Floodway R~ference Data." <br /> <br />- SUMMARY - <br /> <br />I <br /> <br />The tables contain a listing of potential 100-yoar flood dis- <br /> <br /> <br />charges, streambed elevation, 100-year Cloed elL'vation "nd 100- <br /> <br /> <br />year floodplain width for cross sections utilized in this study. <br /> <br />This report has identified the probable flooding limits of <br />a potential 100-year flood event in the lower Bear Creek drainage <br />basin below the Bear Creek Dam. <br /> <br />I <br /> <br />I <br /> <br />The flooc1wuy data cont.uin.(~d in this tdbJe dt.'Filh~::-; :1 flt'l\\' ,11't.~,1 <br /> <br /> <br />required to convQY the 100-yo<1r l'vellt wi [ltout InCI-,'"'' I nq t-It" <br /> <br />IOO-year W.J.tPI- ~:::;urfLlcc by more th<l11 {)..~} f-t'l'l. '['Ill' :"ll)lhl\\".l)' 1 ~~ ,\ <br /> <br /> <br />high hazard .:J.r0t1 char(JctcrlzC'd by doc'>p w,lh'l' ,-[tld hiqll \','ll)I.'ity <br /> <br /> <br />flow clurinq flood cv('nt~;, and should l'c,t\I;lill l-l"I.'I.' elj ,\11\' dl'\'l'l,,!'!\\,'td <br /> <br />which would obstruct flow. <br /> <br />The floodplain limits are based on (1) planned future devel- <br />opment in the lower basin; (2) existing, mapped floodplain condi- <br />tions; and, (3) hydraulic calculations assuming no blockage of <br />existing bridge structures. Even with these assumptions, floods <br />of greater magnitude can and will occur in which the limits of <br />flooding will exceed those shown in this report. <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />For thc "caclt of <br />furUwr n,strietr'd by <br />inchc':;.. 'I.'h(,30 ar{~ I-he' <br /> <br />Bc:ar' Cr'('('k 111 Ill'I1Vl'l- 1.)[11')', Illl' t-l{){)l!\\!.l~' I:; <br /> <br /> <br />illCll1dinq Zlll dl-{',l W!H't-C d{'flll1:; 1.':':'l'I.'I.',! l~; <br /> <br />.:ldordC'd cl-jtct"i;l fOt" !h(' l'il~' ()! l~l'lt\'I.'l-. <br /> <br />Presently there are sections of Bear Creek in which extensive <br />flooding may occur. The preservation of the floodplain will serve <br />at least to limit flood damage potential at its present level while <br />any improvements will serve to minimize or reduce the flood damage <br />potential. <br /> <br />I <br /> <br />-7- <br /> <br />I <br />
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