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Last modified
1/25/2010 6:49:39 PM
Creation date
10/5/2006 1:39:46 AM
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Floodplain Documents
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Title
Ephemeral Streams Hydraulic Factors and Their Relation to the Drainage Net
Date
1/1/1956
Prepared For
State of Colorado
Prepared By
USGS
Floodplain - Doc Type
Educational/Technical/Reference Information
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<br /> <br />IS <br /> <br />PHYSIOGRAPIDC AND HYDRAULIC STUDIES OF RIVERS <br /> <br /> cr 10,000 <br /> w <br /> 0 <br /> cr <br /> -I 0 <br /> z y <br /> w <br /> > <br /> i3 <br /> "- . <br /> 0 <br /> y V) <br /> . '" 1000 <br /> << <br /> :,;. '" <br /> cr <br /> >-- <br /> V) <br /> "- <br /> v. 0 <br /> cr <br /> y . W <br /> <Il <br /> '" <br /> . . ::J <br /> Z <br /> 100 <br />. . . <br />o/I .\ <br />y <br />. <br /> . <br /> 10 \ <br /> \ <br /> \ <br /> I <br /> 6 8 9 10 II I 2 3 4 ,-~ 6 7 8 9 10 II <br /> STREAM ORDER <br /> <br />EXPLANATION <br /> <br />o Average values, Arroyo Calienle <br /> <br />. Arroyo de losFrijoles <br /> <br />" Arroyo de las Trampas to Rio Santa Fe <br /> <br />. Rio Santa Fe, Rio Galisteo, and <br />Canada Ancha (del oriente) <br /> <br />'100 <br /> <br /> <br /> <br />10 <br /> <br />if) <br />w <br />--' <br />'" <br />:;;:: <br />:r:- <br />>-- <br />'-"I <br />Z <br />w <br />--' <br /> <br />'" <br /><< <br />w <br />cr <br />>-- <br />V) <br /> <br />.1 <br /> <br /> <br />o <br /> <br />01 <br />~ <br /> <br />.010 <br /> <br /> <br />2 <br /> <br />3 <br /> <br />4 <br /> <br />1,000,000 <br /> <br />100,000 <br /> <br /> <br />r:r- <br /> <br /> <br />o <br /> <br /> <br /> <br /> <br />FlGl'RE 13.-Relation of stream length and number of streams to stream order in basins or 11th order in central .:-:rew Mexico. Left, stream length plotted against st.ream <br />order; right, number of individual streSl.lliS of a given order plotted against order, <br /> <br />This same general procedure was followed for several <br />other sample drainage basins. Order 11 was the highest <br />found, this being for the main stem of Rio Galisteo. <br />The number and average length of streams in each order <br />were determined and the results are included in <br />figure 13, <br />It will be noted that the plots of stream order against <br />stream length and stream order against number of <br /> <br />streams are straight lines on semilogarithmic paper, as <br />Horton discovered. Lengths range from about 50 feet <br />for the 1st order tributaries to 54 miles for the Rio <br />Galisteo. <br />In order to visualize better the types of channels <br />studied and their relation to stream order, the reader is <br />referred to the phot()graphs in figure 14, which show <br />first-order tributaries in the basin of Arroyo Caliente, <br />
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