Keith A. Kvenvolden
1983, Open-File Report 83-822
No abstract available....
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Page 4747, results 118651 - 118675
Publication Extents
Not all publications have extents, not all extents are completely accurateSherwood E. Frezon (compiler), Thomas M. Finn
1983, Open-File Report 83-919
Rick M. Spechler
1983, Water-Resources Investigations Report 83-4101
The Floridan aquifer is the principal source of freshwater to wells in most of St. Johns County. The aquifer consists of a thick sequence of interbedded limestone and dolomite of Eocene age. The top of the Floridan aquifer, which is irregular throughout St. Johns County, ranges from less than 90...
Harry George Rodis, D.A. Munch
1983, Water-Resources Investigations Report 83-4176
The Floridan aquifer supplies most of the fresh groundwater for municipal, industrial, and agricultural uses within the 12,400 sq mi St. Johns River Water Management District. Because of the growing demand for water and the variation in rainfall, resource managers need timely information on short-term and long-term changes in the...
D. L. Leach, D.M. Hopkins, J. A. Domenico, H. E. Dawson
1983, Open-File Report 83-307
William A. Lawson, Russell C. Evarts
1983, Open-File Report 83-392
No abstract available....
M. E. Cooley
1983, Open-File Report 83-935
This map is one of a series of linear-features maps compiled for the U.S. Geological Survey's Northern Great Plains Regional Aquifer System Analysis (U.S. Geological Survey, 1979). This map shows the linear features that were recognized in Wyoming. Other maps in the series cover South Dakota (Cooley, 1983a), Montana (Cooley,...
William W. Patton Jr., Elizabeth J. Moll
1983, Open-File Report 80-811-G
M. E. Cooley
1983, Open-File Report 83-548
D. L. Leach, D.M. Hopkins, J. A. Domenico, H. E. Dawson
1983, Open-File Report 83-304
Paul A. Schneider Jr.
1983, Water-Resources Investigations Report 83-4058
Shallow ground water may limit the location of construction and excavation projects in parts of the Front Range Urban Corridor. A shallow water table occurs from 0 to 50 feet below the land surface principally in the alluvial deposits along the streams and rivers in the Boulder-Fort Collins-Greeley area. This...
M. E. McCallum, W.K. Camp, M. L. Griswold
1983, Open-File Report 83-579
No abstract available....
D. L. Leach, D.M. Hopkins, J. A. Domenico, R.J. Goldfarb
1983, Open-File Report 83-309
No abstract available....
D. L. Leach, D.M. Hopkins, J. A. Domenico, R.J. Goldfarb
1983, Open-File Report 83-308
John Stewart Kelley
1983, Open-File Report 84-152
Daphne Darden
1983, Water-Resources Investigations Report 83-4133
Water levels were measured in about 500 wells in the Mississippi River valley alluvial aquifer in northwestern Mississippi during September 13-24, 1982. The water-level change from September 1981 to September 1982 showed some recovery, but the depth-to-water map showed areas of continual water-level decline in the central part of the...
Michael J. Blaskowski, J. S. Loen, James E. Elliott
1983, Open-File Report 83-414
Victoria R. Todd
1983, Open-File Report 83-781
G.L. Prost, Michael E. Brownfield
1983, Open-File Report 83-633
John B. Cathrall, G.W. Day, J. D. Hoffman, S.K. McDanal
1983, Open-File Report 83-420-W
Bruce T. Brady
1983, Open-File Report 79-303
No abstract available....
Bruce T. Brady
1983, Open-File Report 79-306
No abstract available....
Donald Clarence Ross (compiler)
1983, Open-File Report 83-231
Donald Clarence Ross
1983, Open-File Report 83-904
No abstract available....
E. A. Du Bray
1983, Open-File Report 83-840
This 1:500,000-scale compilation shows the distribution of felsic plutonic rocks, lithologic types, and associated mineralization in an area between lat 21° and 24°30’ N., long 43°30’ and 46° E. It is part of a shieldwide compilation being done within the framework of Saudi Arabian Deputy Ministry for Mineral Resources projects...