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Saline ground-water discharge to the Smoky Hill River between Salina and Abilene, central Kansas Saline ground-water discharge to the Smoky Hill River between Salina and Abilene, central Kansas
Saline water discharges from the alluvial aquifer into the Smoky Hill and Solomon Rivers between New Cambria and Sand Springs, Kansas. During relatively stable base flow in 1976-77, the discharge was about 32 cubic feet per second. Chloride concentrations at base flow increased about 800 milligrams per liter in the Smoky Hill River and 550 milligrams per liter in the Solomon River. The...
Authors
Joe B. Gillespie, Gerald D. Hargadine
Water-resources investigations of the U.S. Geological Survey in Kansas; fiscal years 1979 and 1980 Water-resources investigations of the U.S. Geological Survey in Kansas; fiscal years 1979 and 1980
Activities of the U.S. Geological Survey in Kansas include the systematic collection and analysis of data to describe the framework of hydrologic systems, assess the water resources, define existing or potential problems in the quantity or quality of water, and provide information for optimum development and management of resources. Streamflow studies are made to determine availability...
Authors
Harold E. McGovern, L. J. Combs
January 1981 water levels, and data related to water-level changes, western and south-central Kansas January 1981 water levels, and data related to water-level changes, western and south-central Kansas
This report provides hydrologic data related to water-level measurements in observation wells in western and south-central Kansas during January 1981. Annual water-level measurements are made by personnel from the Division of Water Resources, Kansas State Board of Agriculture, and from the U.S. Geological Survey . State-agency support for this cooperative program is provided by the...
Authors
Marilyn E. Pabst
Ground-water hydrology of the Mormon Island Crane Meadows wildlife area near Grand Island, Hall County, Nebraska Ground-water hydrology of the Mormon Island Crane Meadows wildlife area near Grand Island, Hall County, Nebraska
The Platte River in south-central Nebraska flows generally eastward in a broad, flat valley. The river banks and many areas adjacent to the river support thick stands of cottonwood and willow trees. Brush, grass, pasture land, and cultivated fields occupy most of the remaining area. This is the habitat for many types of wildlife that live in the area or stop over in the area during...
Authors
R. Theodore Hurr
Hydrology and model of North Fork Solomon River Valley, Kirwin Dam to Waconda Lake, north-central Kansas Hydrology and model of North Fork Solomon River Valley, Kirwin Dam to Waconda Lake, north-central Kansas
The alluvial valley of the North Fork Solomon River is an important agricultural area. Reservoir releases diverted below Kirwin Dam are the principal source of irrigation water. During the 1970'S, severe water shortages occurred in Kirwin Reservoir and other nearby reservoirs as a result of an extended drought. Some evidence indicates that surface-water shortages may have been the result...
Authors
Donald G. Jorgensen, Lloyd E. Stullken
Results of a reconnaissance water-quality sampling program of the Ogallala aquifer in Colorado, Kansas, Nebraska, Oklahoma, South Dakota, and Texas Results of a reconnaissance water-quality sampling program of the Ogallala aquifer in Colorado, Kansas, Nebraska, Oklahoma, South Dakota, and Texas
Results of a reconnaissance water-quality sampling program of the Ogallala aquifer indicates the water generally is suitable for most uses. Fluoride and selenium were the only chemical constituents found to exceed the National Interim Primary Drinking Water Regulations in water from some of the wells. Unusually large silica concentrations in many of the water samples probably were due to...
Authors
Gerald L. Feder, Noel C. Krothe
Hydrologic maps of Ogallala Aquifer, west-central Kansas Hydrologic maps of Ogallala Aquifer, west-central Kansas
No abstract available.
Authors
Lloyd E. Dunlap, Joseph M. Spinazola
Water-level and saturated-thickness changes, predevelopment to 1980, in the High Plains aquifer in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming Water-level and saturated-thickness changes, predevelopment to 1980, in the High Plains aquifer in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming
No abstract available.
Authors
Richard R. Luckey, Edwin D. Gutentag, John B. Weeks
Map of water table in Graham County, northwestern Kansas, March 1979 Map of water table in Graham County, northwestern Kansas, March 1979
A map of the water table in Graham County, prepared in collaboration with the U.S. Bureau of Reclamation, provides current (1980) information on water levels in the unconsolidated deposits. Graham County, an area of 900 square miles in northwestern Kansas, is within the rolling, moderately to well-dissected terrain on the eastern edge of the High Plains. The eastward-flowing South Fork...
Authors
Joseph M. Spinazola
Water resources data for Kansas, water year 1980--Volume 1. Missouri River Basin Water resources data for Kansas, water year 1980--Volume 1. Missouri River Basin
No abstract available.
Authors
Water Resources Division U.S. Geological Survey
Floods in Kansas City, Missouri and Kansas, September 12-13, 1977 Floods in Kansas City, Missouri and Kansas, September 12-13, 1977
The storms of Sept. 12-13, 1977, delivered as much as 16 in. of rain, with average rainfall exceeding 10 in. in the Kansas City metropolitan area. Twenty-five lives were lost, many were left homeless, and damages exceeded $80 million. Data obtained by the National Weather Service and the U.S. Geological Survey indicate that two record-setting rainstorms occurred within 24 hours. The...
Authors
L.D. Hauth, W. J. Carswell, E.H. Chin
Location of sampling sites and available information on wells sampled in the Kansas ground-water-quality monitoring network, 1976-80 Location of sampling sites and available information on wells sampled in the Kansas ground-water-quality monitoring network, 1976-80
No abstract available.
Authors
T.B. Spruill, J. F. Kenny