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Ground-water resources of Greeley and Wichita counties, Western Kansas Ground-water resources of Greeley and Wichita counties, Western Kansas

Unconsolidated deposits of sand, silt, clay, and gravel compose the principal aquifer in Greeley and Wichita Counties. The deposits are as much as 300 feet (91 m) 2/ thick, of which as much as 145 feet (44 m) is saturated. In 1972, there were about 1,040 large-capacity wells--yielding 100 gallons per minute (6.3 1/s) or more--in the counties, mostly for irrigation supplies. The wells...
Authors
Steven E. Slagle, Edward C. Weakly

Ground water in the Grand (Neosho) River basin, Kansas and Oklahoma Ground water in the Grand (Neosho) River basin, Kansas and Oklahoma

Ground water in the Grand (Neosho) River basin occurs in both consolidated rocks and unconsolidated deposits. Water for domestic and stock supplies generally can be obtained from wells in either of the above deposits. Water for municipal, industrial, and irrigation supplies generally can be obtained in limited quantities from the unconsolidated deposits of sand and gravel and in adequate
Authors
Robert B. Morton, Stuart W. Fader

Ground water in the middle Arkansas River basin, Kansas and Oklahoma Ground water in the middle Arkansas River basin, Kansas and Oklahoma

Ground water in the Middle Arkansas River basin occurs in consolidated rocks and unconsolidated deposits. Wells for domestic and stock supply generally can be drilled successfully in consolidated rocks. Wells for large-scale municipal, industrial, and irrigation supplies generally are successful in areas underlain by saturated unconsolidated deposits of sand and gravel. Unconsolidated...
Authors
Stuart Wesley Fader, Robert B. Morton

Ground water in the Verdigris River basin, Kansas and Oklahoma Ground water in the Verdigris River basin, Kansas and Oklahoma

Ground water in the Verdigris River basin occurs in consolidated rocks and unconsolidated deposits ranging in age from Mississippian to Quaternary. Water for municipal, industrial, and irrigation supplies generally can be obtained in limited quantities from the alluvial deposits in the stream valleys. Except for water in the alluvial deposits in the stream valleys and in the outcrop...
Authors
Stuart Wesley Fader, Robert B. Morton

Water development for irrigation in northwestern Kansas Water development for irrigation in northwestern Kansas

Northwestern Kansas, an area of 8,050 square miles (21,000 square kilometres), is a flat to gently rolling plain that is dissected by the Smoky Hill and Republican Rivers. Loessial soils underlying the plain are ideal for cultivation. The climate is semiarid with the mean annual precipitation ranging from 16 to 21 inches (41 to 53 centimetres). Precipitation occurring mainly as...
Authors
Edward D. Jenkins, Marilyn E. Pabst

Water resources of Gove, Logan, and Wallace Counties, west-central Kansas Water resources of Gove, Logan, and Wallace Counties, west-central Kansas

This atlas presents information on the geology and water resources of a three-county area in west-central Kansas (index map). The report is intended promarily as a guide to the availability of ground water, which is the main source of supply for domestic, stock, inductrial, irrigation, and municipal uses.
Authors
Thomas J. McClain, Edward D. Jenkins, Katherine M. Keene, Marilyn E. Pabst

Water resources data for Kansas, water year 1974; Part 1, Surface water records Water resources data for Kansas, water year 1974; Part 1, Surface water records

Water resources data for the 1974 water year for Kansas including records of stream-flow or reservoir storage at gaging stations, partial-record stations, and miscellaneous sites are given in this report. Records are included for 163 gaging stations of which 143 are streamflow discharge stations and 20 are reservoir or lake stations; also are included records for 23 low-flow partial...
Authors
Water Resources Division U.S. Geological Survey

Application of statistical techniques to the estimation of ground-water withdrawals in northwestern Kansas Application of statistical techniques to the estimation of ground-water withdrawals in northwestern Kansas

This study was made to determine the accuracy of using readily available data with certain statistical techniques to estimate ground-water withdrawals in western Kansas. The data used in the investigation were from a sample of wells chosen from the total inventoried irrigation wells in nine counties in northwestern Kansas; they can be considered as being typical of the data generally...
Authors
William M. Kastner

Floods of June 1965 in Arkansas River basin, Colorado, Kansas, and New Mexico Floods of June 1965 in Arkansas River basin, Colorado, Kansas, and New Mexico

Maximum discharges during the floods of June 1965 in the Arkansas River basin in Colorado, Kansas, and New Mexico were greater than those previously known at 49 of the 137 locations where flood information was obtained. Property damage exceeded $60 million, and 16 lives were lost. At many sites, peak discharges exceeded by severalfold the discharges that may be expected, on the average...
Authors
R.J. Snipes

Ground water in Finney County, southwestern Kansas Ground water in Finney County, southwestern Kansas

No abstract available.
Authors
Edwin D. Gutentag, D.H. Lobmeyer, H.E. McGovern, W.A. Long
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