Water Resources Division, U.S. Geological Survey
1982, Open-File Report 82-550
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Page 4826, results 120626 - 120650
Publication Extents
Not all publications have extents, not all extents are completely accurateG. L. Barr, George R. Schiner
1982, Open-File Report 82-1011
A September 1982 potentiometric surface map of the Southwest Florida Water Management District depicts the annual high water-level period. Water levels in most wells measured in September 1982 were higher than in May 1982. Levels averaged about 12 feet higher in the southern part of the area and about 5...
Nairn Albert
1982, Open-File Report 82-141
No abstract available....
Fernando Gómez-Gómez, Senen Guzman-Rios
1982, Open-File Report 82-332
Gary W. Levings
1982, Open-File Report 82-562
The potentiometric surface of the Judith River Formation is mapped at a scale of 1:1,000,000. The map is one of a series produced as part of a regional study of aquifers of Cenozoic and Mesozoic age in the northern Great Plains of Montana. The contour interval is 200 feet. Water...
Gary Wayne Levings
1982, Open-File Report 82-563
The potentiometric surface of water in the lower Cretaceous Lakota Formation and equivalent units (Cut Bank Sandstone Member , Sunburst Sandstone Member, and Moulton Member of Kootenai formation; Third Cat Creek sandstone of Kootenai Formation; Pryor Conglomerate Member of Kootenai Formation) is shown on a base at a scale of...
John S. Havens
1982, Open-File Report 82-100
The High Plains aquifer in Oklahoma is part of a regional aquifer system extending from South Dakota on the north through Wyoming, Colorado Nebraska Kansas, and Oklahoma to Texas and New Mexico on the south (index map) . The principal aquifer, the Ogallala Formation of Tertiary age, is hydraulically connected...
George R. Schiner, Eugene C. Hayes
1982, Open-File Report 83-30
This map presents the potentiometric surface of the Floridan aquifer in the St. Johns River Water Management District and vicinity for September 1982. The Floridan aquifer is the principal source of potable water in the area. Water-level measurements were made on approximately 1,000 wells and on several springs. The potentiometric...
Robert L. Klausing
1982, Open-File Report 82-515
This preliminary map is the first product of the ground-water resources study of Logan County, which has an area of 1,015 mi2 (2,629 km2) in south-central North Dakota (see location map). This study is part of a statewide program to determine the...
Donald G. Hadley
1982, Open-File Report 82-288
The Wadi Dhahaban quadrangle (sheet 18/41 D) lies between lat 18?00? and 18?30' N. and long 41?30' and 42?00' E. and encompasses an area of 2,937 km2 located along the Red Sea coast and includes part of the escarpment-mountains province. The geologic formations exposed in the quadrangle are comprised of...
Richard Goldsmith, D.J. Milton, J. Wright Horton Jr.
1982, Open-File Report 82-56
No abstract available....
Gary W. Hill, John L. Chin
1982, Open-File Report 82-824
No abstract available....
David M. Miller, Joel D. Schneyer
1982, Open-File Report 83-725
No abstract available....
Edward J. Young
1982, Open-File Report 82-601
Gary W. Levings
1982, Open-File Report 82-564
The potentiometric surface of water in the Upper Cretaceous Fox Hills-lower Hell Creek aquifer is shown on a base map at a scale of 1:1,000,000. The map is one of a series produced as part of regional study of aquifers of Cenozoic and Mesozoic age in the northern Great Plains...
Water Resources Division, U.S. Geological Survey
1982, Open-File Report 82-66
Water Resources Division, U.S. Geological Survey
1982, Open-File Report 82-1084
Gary W. Levings
1982, Open-File Report 82-565
The potentiometric surface of water in the Upper Cretaceous Eagle Sandstone and equivalent units (Virgelle Sandstone and Telegraph Creek Formation) is shown on a base map at a scale of 1:1,000,000. The map is one of a series of maps produced as part of a regional study of aquifers of...
John S. Havens
1982, Open-File Report 82-275
The High Plains aquifer in Oklahoma is part of a region~l aquifersystem extending from South Dakota on the north through Wyoming, Colorado,Nebraska, Kansas, and Oklahoma to Texas and New Mexico o~ the south.(index map). The principal aquifer, the Ogallala F?rmat1on of :ert1aryage, is hydraulically connected with other unconsolidated ~eposits, .principally...
Robert Mills Chapman, Warren Yeend, W. P. Brosge, H. N. Reiser
1982, Open-File Report 82-734
No abstract available....
Craig L. Sprinkle
1982, Water-Resources Investigations Report 81-1103
INTRODUCTION The tertiary limestone aquifer system of the southeastern United States is a sequence of carbonate rocks referred to as the Floridan aquifer in Florida and the principal artesian aquifer in Georgia, Alabama, and South Carolina. More than 3 billion gallons of water are pumped daily from the limestone aquifer; and...
Paul S. Hampson, Eugene C. Hayes
1982, Open-File Report 81-907
Data collected from 1976 to 1979 indicate large water-quality variations in the upper 300 feet of the Floridan aquifer in St. Johns County, Florida. Chloride concentrations range from less than 10 milligrams per liter in the northwestern part of the county to more than 1,000 milligrams per liter in the...
Charles R. Meissner Jr., B.S. Hackman, John C. Ossi
1982, Open-File Report 82-452
James J. Rytuba, D. B. Vander Meulen, T. L. Vercoutere, S.A. Minor, M.E. Caress, B.J. Kriens
1982, Open-File Report 82-1127
Marilyn E. Pabst, Lloyd E. Stullken
1982, Open-File Report 82-449
The High Plains aquifer in Kansas is a part of a regional system that extends South Dakota to Texas. The aquifer in Kansas underlies an area of 31,000 square miles in the western and south-central part. This aquifer is a hydraulically connected assemblage of unconsolidated water-bearing deposits of Tertiary and...