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Last modified
1/26/2010 3:14:17 PM
Creation date
10/12/2006 4:27:49 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8270.100
Description
Colorado River Basin Water Quality/Salinity -- Misc Water Quality
Basin
Colorado Mainstem
Water Division
5
Date
1/1/1971
Author
USDOI
Title
Quality of Water - Colorado River Basin - Progress Report No. 5 - January 1971
Water Supply Pro - Doc Type
Report/Study
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<br />DESCRIPTION OF BASIN <br /> <br />Q <br />c:n <br />-..1 <br />"n <br /> <br />are reddish brown in color and have <br />lying formations or adjacent areas. <br />soils, but in many areas topogra;phy <br /> <br />no resemblance to either the under- <br />These are excellent agricultural <br />makes agriculture difficult. <br /> <br />C. Climate <br /> <br />The Colora'lo River Basin has climatic extremes, ranging between <br />year-round snow cover and heavy precipitation on the high peaks of the <br />Rocky Mountains to desert conditions with very little rain in the south- <br />ern part of the basin. This wide r8-Qge of climate is caused by differ- <br />ences in altitu'le, latitude, and by the configuration of .the high moun- <br />tain r8-Qges. The encircling mountain ranges o~struct a~d deflect the <br />air m'3.sses to such an extent that storm ;:>atterns are more erratic than <br />in most other parts of the United States. Most of the moisture for pre- <br />cipitation on the Upper Basin is derived from the Pacific Ocean and the <br />Gulf of Mexico. T1le Pacific source predominates generally from Octo~er <br />through April and the Gulf source during the late spring a:.1d ea!'ly <br />SUrmner. <br /> <br />In the n::Jrthern part of the basin most precipitation falls in the <br />form of winter snoWS a:.'li spring rains. Summer storms are infrequent <br />but are sometimes of cload.b-JX'st intensity in localized areas. In the <br />m)re arid soathern portion the principal rainy season is in the winter <br />months with occasional localized cloudbursts in the su~er roll fall. <br /> <br />Extremes of temperature in the basin r8-'lge from 500 F. below zero to <br />1300 F. above zero. The northern po~tion ::Jf the basin is characterized <br />by short, warm summers and long, cold winters, and cwny mO'J.ntain areas <br />are blanketed by deep snow all winter. 1>1e southern p::J~ion of the basin <br />has long, hot s\L'llI1lers, practically continuous sanshine, and almost co:n- <br />plete absence of freezing temperatures. <br /> <br />Nevertheless, the entire ~asin is arid except in the extremely high <br />altituies of the headwaters a!'eas. Rainfall averages as low as 2.5 <br />inc:hes in the southern end. of the basin while total precipitatio!l in the <br />high moantains may range from 40 to 60 inches annually. <br /> <br />D. Vegetation <br /> <br />Areas of higher elevation are covered with forests of pine, fir, <br />spruce, and silver-stemned aspens, broken by small glaies and moantain <br />meadows. Pin::Jn a:.1d jlmiper trees, intersperse.l with scrub oak, mountain <br />mahog8-QY, rabbit bl'ush, .bLillCh grasses, and similar plants grad' in the <br />intermediate elevations of the mesa and plateau regions. Large areas in <br />the upper Basin are d~minated by big sagebrush aQl related .vegetatio!l. <br />Many of the streams are bordered by cottonwoods, willows, a~d salt ced~r. <br /> <br />9 <br /> <br />
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