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Last modified
1/26/2010 12:29:17 PM
Creation date
10/11/2006 10:09:51 PM
Metadata
Fields
Template:
Water Supply Protection
File Number
8112.600
Description
Arkansas White Red Basins Interagency Committee - AWRBIAC -- Reports
Basin
Arkansas
Water Division
2
Date
6/1/1977
Title
Specific Problem Analysis Summary Report - 1975 National Assessment of Water and Related Land Resources - Part 2 of 2
Water Supply Pro - Doc Type
Report/Study
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<br />o <br />[;j <br />~ <br />w <br />(0 <br />(.ll <br /> <br />The area is drained by two major str~ams, the North Canadian <br />(Beaver) River and the Cimarron River, both of which are tributaries <br />to the Arkansas River. The total drainag~ area within these coun- <br />ties is 6,700 square miles with ,runoff of 10,400 acre-feet per year. <br /> <br />The Ogallala formation of the tertitary age consists of a <br />heterogenous mixture of sand, gravel, silt, clay, caliche, and <br />local beds cemented with calcium carbonate. It is the principal <br />source of water in the Oklahoma Panhandle. This formation wss <br />deposited over the entire Oklahoma Panhandle, but has been re- <br />moved locally by stream erosion and has been truncated completely <br />by erosion, a short distance east of Beaver County. <br /> <br />The maximum thickness of the Ogsllala is about 650 feet, but <br />it thins along major drainsgewsys and oV~r bedrock highs. Sand <br />and gravel of the Ogallala Formation are the principal sources of <br />water. Well yields range from a few gallons per minute to more <br />than 2,000 gallons per minute. Wells yielding less than 300 gpm <br />are usually not completed for irrigation wells. <br /> <br />Water from the Ogallala is generally chemically suitable for <br />most purposes. Total hardness is usually more than 180 mg/l with <br />some wells in the lower zones of the Ogallala containing dissolved <br />solids in excess of 5,000 mg/l. <br /> <br />The average groundwater gradient is eastward at 14 feet per <br />mile. Because of this eastern gradient, no large volumes of <br />water enter or leave the area from Kansas or Texas and only small <br />quantities are entering from New Mexico border becuase the Ogallala <br />is above the water table except in the extreme southwestern corner <br />of Cimarron County. <br /> <br />The Panhandle region of Oklahoma was called No Man'. Land <br />until 1890 wh~n it became' Oklahoma's seventh county. Development <br />to this point had been slow and was further retarded by the Dust <br />Bowl Era. <br /> <br />The 1970 population totaled 26,779 with projected population <br />of 33,200 in 2020. Employment records of the total labor force <br />show 31% in agriculture and the remaining 69% in domestic services, <br />self-employed and unpaid fsmily works, manufacturing, wholesale <br />and retail trade, government, construction, mining, finance, in- <br />surance, real estate and other services. Municipalities in the <br />area with populations over 1,000 in 1970 are: <br /> <br />City <br />BeaVer <br />Boise Ci ty <br />Goodwell <br />Guymon <br />Hooker <br /> <br />1970 Population <br />1,853 <br />1,993 <br />1,467 <br />7 J 640 <br />1,615 <br /> <br />111 <br /> <br /> I <br /> I <br />- ---~ <br /> I <br /> I <br /> I <br /> I <br />---- <br /> I <br /> I <br /> I <br /> I <br /> I <br /> I <br /> I <br /> I <br /> I <br /> I <br /> I <br /> I <br /> I <br />
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