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Last modified
1/29/2010 10:12:01 AM
Creation date
10/5/2006 3:10:10 AM
Metadata
Fields
Template:
Floodplain Documents
County
Elbert
El Paso
Community
Elbert and El Paso Counties
Stream Name
Kiowa Creek, Bijou Creek
Basin
South Platte
Title
Flood Problems and Conditions in the Kiowa, Bijou, and Boxelder Creeks
Date
8/11/1949
Prepared For
State of Colorado
Prepared By
CWCB
Floodplain - Doc Type
Floodplain Report/Masterplan
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<br />, <br /> <br />STATEMENT <br />Of <br />James Price <br /> <br />Byers, Colorado <br />AlJiwt 8, 1949 <br /> <br />To Whom It May Concern I <br /> <br />"\ <br /> <br />Why should water of the Kiowa and Bijous be controlled? <br /> <br />1" <br />~ <br />", <br />\ <br /> <br />This article has to do with the Bijous which are similar to the Kiowa <br />creek. The informant has lived all his life on the Bijous and has watched <br />the destruction for the past fifty years. <br /> <br />I have seen valuable hay meadows and pastures of thousands of acres <br />ruined completely. I have known of hundreds of cattle and other livestock <br />washed away. Peoples' lives have been in jeopardy. while their homes were <br />washed away. Millions of dollars worth of railroad property, highway and <br />county bridges have been destroyed. Thousands of miles of fences have been <br />washed down stream with from 40 to 60 per cent sediment water flooding into <br />the South Platte ruining irrigation water with sediment that is a detriment <br />into even Nebraska. <br /> <br />~ <br /> <br />These streams are sediment-laden and destructive because the soil is a <br />sand and gravel and adobe formation a type that washes easily due to the fall <br />per mile. This fall is estimated all the way from 30 to 60 feet levelling <br />off to from 10 to 15 feet in the flatter country. A series of minor floods <br />happen regularly reaching different points dovmstream, all carrying a certain <br />amount of erosion. Then along comes the "Daddy" flood, sweeping it all with <br />increased amount that it brings along. This rolline, boiling, large flood <br />separates the gravel and sand from the adobe~ The ~a~d stops in the stream <br />making the treacherous quicksartd, and later blows from the bed by the prevail- <br />ing west and northwest winds which accounts for the sand dunes and hills that <br />are on the east side of the streams. The adobe is settled in the flats on the <br />west side to make the rich soil of the Antelope Flats. This land is being <br />developed to pump irrigation. This large flat area has been subjected to big <br />floods through the times which have built up the soil. These flats are <br />roughly five to six miles wide and fifty miles long some 275 square miles on <br />175,000 acres. <br /> <br />^ <br /> <br />;, <br />I' <br /> <br />. <br /> <br />What can be done to stop this awful destruction of sediment laden flood <br />water? I have the Owens reservoir to cite as an example of the kind that <br />would answer our problems if there were enough of them in different sizes. <br /> <br />The Owens dam was put in some sixty years ago by the late C. S. Owens <br />at the mouth of a large draw just before it empties into the Bijou. This <br />reservoir takes care of any flood that happens in this draw. Then it has a <br />feeder ditch that takes water out of the Bijou some four or five miles above <br />for storage. Any sediment is deposited in the bottom of the ditch and ~ery <br />little reaches the reservoir. This sediment is removed from time to time from <br />the ditch. The sediment would not be so much on ditches above or closer to <br />the source as the Owens project is downstream - just above Byers. <br /> <br />-2- <br /> <br />
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