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WSPC04168
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Last modified
1/26/2010 11:38:09 AM
Creation date
10/9/2006 4:28:21 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8040.950
Description
Section D General Studies - General Water Studies
State
CO
Basin
Statewide
Date
9/14/1979
Author
Unknown
Title
High Plains Study - Six-State High Plains-Ogallala Aquifer Area Study
Water Supply Pro - Doc Type
Report/Study
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<br />OOJ33J '''~:Jr~.. <br />:'LJ,i~>i,:( <br />i "'It"": \1 <br />,I ., <br />. , <br />For each of the above, the outcomes or impacts can be measured in t.rins'of <br />(a) changes in agricultural production, income and employment induced by the change <br />in available water supplies, both on the farm and in the agribusiness industrial sec- <br />tor, and (b) the nonagricultural production, income and employment necessary to meet <br />shortfalls in continued regional economic growth and vitality. Outcomes and 'impacts <br />will be evaluated and compared at the national, regional. , state and subregional lev- <br />els. This procedure will allow the High Plains Council and the Secretaries of Com- <br />merce and Army to develop policies and plans involving combinations of strategies <br />at the state and subregional level, as appropriate to differing situations and sub- <br />regions over time. <br /> <br />These are the alternatives as originally presented in the interim report to the <br />Congress forwarded on January 15, 1979, however, minor modifications have been <br />made as a result of study developmemt to date. <br /> <br />Regional Basin <br /> <br />The High Plains area extends over parts of Colorado, Kansas, Nebraska, <br />New Mexico, Oklahoma and Texas in the Great Plains land resource region of mid- <br />continental America as shown on Figure 2. Much of the High Plains is underlain by <br />the Ogallala Formation, a major aquifer supplying most of the water needs of the <br />area's large agricultural economy. <br /> <br />The Ogallala Formation is an unconsolidated remnant of vast deposits of <br />gravel, sand, and silt eroded from the Rockies. Erosion has reduced the area of <br />the extensive deposits that once covered all of the Great Plains region, leaving <br />the Ogallala as the principal geologic unit associated with the High Plains today. <br /> <br />The specific area encompassed by this study includes 180 counties in the <br />six-state region underlain in whole or in part by the Ogallala Formation, an area <br />of about 225 thousand square miles. As a part of the overall study, the related <br />economies of nearby cities including Denver, Oklahoma City, Tulsa, Kansas City, <br />Albuquerque, and Lincoln and Omaha must be considered. Peripheral aquifers which <br />are interrelated with the Ogallala must be taken into account. The interbasin transfer <br />studies will consider potential sources of water outside the study area. <br /> <br />, <br /> <br />Colorado's Basin <br /> <br />The Colorado portion of the Ogallala-High Plains aquifer lies in the east- <br />central and southeast part of the state in two separate basins. This portion of the <br />aquifer lies beneath all or part of eleven Colorado counties and covers approxi- <br />mately 6.9 million acres. The northern Colorado basin lies between the drainages <br />of the South Platte and Arkansas Rivers and covers a triangular area that could be <br />described as extending from a point east of Limon in a northeasterly direction to <br />the Colorado-Nebraska state line at a point a few miles south of Julesburg and <br />from this same point east of Limon in a southeasterly direction to the Colorado- <br />Kansas state line southeast of Sheridan Lake. The southern basin which covers <br />the southeastern part of Prowers County, most of Baca County, and the south- <br />eastern corner of Las Animas County could best be described as that part of the <br />state lying southeast of a line running roughly from Cheney Center in a south- <br /> <br />-3- <br /> <br />, <br />'t <br /> <br />- <br /> <br />
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