Publications
Publications
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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
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
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
Ground water in Haskell County, southwestern Kansas Ground water in Haskell County, southwestern Kansas
No abstract available.
Authors
Edwin D. Gutentag, Lloyd E. Stullken
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
Water resources data for Kansas, water year 1973; Part 1, Surface water records Water resources data for Kansas, water year 1973; Part 1, Surface water records
Surface-water records for the 1973 water year for Kansas, including records of streamflow or reservoir storage at gaging stations and partial-record stations, are given in this report. The locations of the stations are on figures 1 and 2. Records for a few pertinent gaging stations in bordering States also are included. These data represent that part of the National Water Data System...
Authors
M.L. Thompson, R. E. Curtis
Water resources of Hamilton County, southwestern Kansas Water resources of Hamilton County, southwestern Kansas
According to records of the National Weather Service (formerly the U.S. Weather Bureau) for a station near Syracuse, the average annual precipitation in Hamilton County is about 16 inches. Of this amount, 83 percent occurs during the growing season (March 15 to October 15). A part of the precipitation runs off as surface flow, part is evaporated, part is used by vegetation, and a small...
Authors
David H. Lobmeyer, C. G. Sauer
Ground water in Gray County, southwestern Kansas Ground water in Gray County, southwestern Kansas
No abstract available.
Authors
Harold E. McGovern, W.A. Long
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
Water resources data for Kansas, water year 1973; Part 2, Water quality records Water resources data for Kansas, water year 1973; Part 2, Water quality records
Water-resources data for the 1973 water year for Kansas include records of data for the chemical and physical characteristics of surface and ground water. Data on the quality of surface water (chemical, microbiological, temperature, and sediment) were collected from designated sampling sites at predetermined intervals such as once daily, weekly, monthly, or less frequently, and at some...
Authors
A.M. Diaz, C.D. Albert
Fluvial sediment characteristics of the Kansas River at Wamego, Kansas, 1957-70 Fluvial sediment characteristics of the Kansas River at Wamego, Kansas, 1957-70
Fluvial-sediment samples have been collected from the Kansas River at Wamego from 1957-70 by the U.S. Geological Survey in cooperation with the Kansas Water Resources Board. During this period. the stream-runoff pattern of the basin has been altered by constructions of Tuttle Creek and Milford Reservoirs. An analysis of data shows that the reduction of suspended sediment discharge has...
Authors
C.D. Albert