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Publications

Publications from USGS science centers throughout the Southeast Region.

Filter Total Items: 10383

Saline-water intrusion related to well construction in Lee County, Florida Saline-water intrusion related to well construction in Lee County, Florida

Ground water is the principle source of water supply in Lee County, Florida where an estimated 30,000 wells have been drilled since 1990. These wells ranges in depth from about 10 to 1,240 feet and tap the water table aquifer or one or more of the artesian water-bearing units or zones in the Tamiami Formation, the upper part of the Hawthorn Formation, the lower part of the Hawthorn...
Authors
Durward Hoye Boggess, T.M. Missimer, T.H. O’Donnell

Geohydrology of Muscatine Island, Muscatine County, Iowa Geohydrology of Muscatine Island, Muscatine County, Iowa

Muscatine Island is a wide segment of the west bank of the Mississippi River flood plain that covers about 50 square miles in Muscatine and Louisa Counties; the project area encompasses the 30 square miles in Muscatine County. The flood plain is underlain by thick, permeable alluvial deposits that comprise a water-table aquifer that is developed extensively for water supplies in the area...
Authors
R.E. Hansen, W. L. Steinhilber

Techniques for Estimating Flood-Depth Frequency Relations on Natural Streams in Georgia Techniques for Estimating Flood-Depth Frequency Relations on Natural Streams in Georgia

Regional relations are defined for estimating the depth of floods having recurrence intervals of 10, 50, and 100 years on streams with natural flow in Georgia. Multiple-regression analysis of station data is used to define the relations between flood depths and frequency for streams draining from 1 to 1,000 square miles, and for 10 climatological and physical basin characteristics. The...
Authors
McGlone Price

Selected water-level records for western Oklahoma, 1975-1976 Selected water-level records for western Oklahoma, 1975-1976

A systematic program to collect water-level records in Oklahoma began in 1937. The objectives of this program are (1) to provide long-term records of water-level fluctuations in representative wells, (2) to facilitate the prediction of water-level trends and indicate future availability of ground-water supplies, and (3) to provide information for use in basic research. Water-level data...
Authors
Robert L. Goemaat

Stratigraphic and hydrogeologic framework of part of the coastal plain of Texas Stratigraphic and hydrogeologic framework of part of the coastal plain of Texas

The subsurface delineation of hydrogeologic units of Miocene and younger age and stratigraphic units of Paleocene to Holocene age establishes and interrelationship of these units statewide across much of the Coastal Plain of Texas. The 11 dip sections and 1 strike section, which extend from the land surface to 7 ,600 feet below sea level, provide continuity of correlation from the...
Authors
E.T. Baker

Approximate areas of recharge to the Chicot and Evangeline aquifer systems in the Houston-Galveston area, Texas Approximate areas of recharge to the Chicot and Evangeline aquifer systems in the Houston-Galveston area, Texas

The purpose of this report is to show the general geographic areas of recharge to the Chicot and Evangeline aquifers in the Houston area, Texas (fig. 1). The areas of recharge shown on the map were determined by interpretations of subsurface hydrology, soil surveys of Harris County, and surface and subsurface geology.
Authors
R.K. Gabrysch

Hydrologic data for Mountain Creek, Trinity River basin, Texas, 1975 Hydrologic data for Mountain Creek, Trinity River basin, Texas, 1975

Mountain Creek drains the northeast corner of Johnson County, the northwest corner of Ellis County, the southeast corner of Tarrant County, and part of the southwest corner of Dallas County, Tex. The basin is 30 miles long and averages 10 miles in width. The total drainage area at the mouth is 304 sq mi. Basin outflow for the 1975 water year was 146,400 acre-feet which is 68,880 acre...
Authors
H.D. Buckner

Ground-water resources along the Blue Ridge Parkway, North Carolina Ground-water resources along the Blue Ridge Parkway, North Carolina

The best areas to develop ground water along the Blue Ridge Parkway in North Carolina are in broad draws and in stream valleys where draws open to the valleys. Saprolite thickness in these places can exceed 50 feet and provide adequate ground-water storage; draws are topographic expressions of fracture zones in the underlying bedrock, which transmit water from the overlying saprolite to...
Authors
M. D. Winner
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