Water Resources Division, U.S. Geological Survey
1978, Open-File Report 78-536
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Page 5229, results 130701 - 130725
Publication Extents
Not all publications have extents, not all extents are completely accurateRobert D. Hettinger
1978, Open-File Report 78-702
Robert G. Hobbs
1978, Open-File Report 78-401
The Geological Survey conducted a seven-hole core-drilling program in the Recluse Geologic Analysis Area, northern Campbell County, Wyoming, in 1975. The purpose was to acquire rock and coal samples to further evaluate the surface-minable coals of this area. In 1976 the Bureau of Land Management defined a portion of this...
John J. Hickey
1978, Open-File Report 78-853
Lithologic, hydraulic, geophysical, and water-quality data were collected at the Bear Creek subsurface-injection test site at St. Petersburg, FL. The data were collected to determine the feasibility of subsurface injection of storm runoff. An exploratory hole and five observation wells were constructed between October 1974 and April 1976. The lithology...
R. W. Hartz
1978, Open-File Report 78-406
No abstract available....
Thomas D. Hessin, P. M. Taufen, J. C. Seward, S. J. Quintana, A. L. Clark, Donald Grybeck, J. M. Hoare, W. L. Coonrad
1978, Open-File Report 78-9-N
No abstract available....
Jack Hardee, Robert A. Miller, Harold C. Mattraw Jr.
1978, Open-File Report 78-612
Rainfall, stormwater discharge, and water-quality data for both rainfall and runoff are summarized for a highway area near Pompano Beach, Florida. Loads for 20 water-quality constituents were computed for the runoff from 41 storms between April 1975, and July 1977. The basin of 58.3 acres contains a 3,000 ft segment...
Ray J. Hoffman
1978, Open-File Report 78-735
The Merced River originates on the western slope of the Sierra Nevada and flows through Yosemite National Park. The river drains 1,276 square miles before joining the San Joaquin River near Stevinson, Calif. Data were collected to permit descriptions of the river's quality during a hydrologic cycle, the natural and...
Thomas E. Fumal
1978, Open-File Report 78-1067
To identify geologic units with distinctly different seismic responses for the purposes of seismic zonation, compressional and shear wave velocities have been measured in boreholes at 59 sites in the San Francisco Bay region in a wide range of near-surface (0-30m) geologic materials. Several physical parameters, which can be readily...
Vincent J. Flanigan
1978, Open-File Report 78-150
J. Thomas Hanley
1978, Open-File Report 78-550
Deborah S. Hammond, Ralph C. Heath, Roger Milton Waller
1978, Open-File Report 78-710
Ground water in the Hudson River basin occurs in unconsolidated deposits and consolidated rock. Sand and gravel units of the unconsolidated deposits, which occur principally in valley bottoms, form the best aquifers and commonly provide well yields of several hundred gallons per minute. Carbonate aquifers are the most productive consolidated...
John J. Hickey
1978, Open-File Report 78-575
One exploratory hole, a test injection well, and nine monitor wells were constructed at the South Cross Bayou test-injection site between January 1973 and October 1975. At the test site, the first 125 feet below land surface is predominantly limestone and clay; from 125 to 3,280 feet it is mostly...
Mark A. Hardy
1978, Open-File Report 78-202
Data collected for a wide range of flow conditions from September 8, 1975, to July 13, 1976, reveal that human and animal waste loading of streams and pesticide use in the watershed are probably the most significant water-quality problems. Generally, the type(s) of water in tributary streams in the south...
John S. Havens
1978, Open-File Report 78-857
J.D. Hudson
1978, Open-File Report 78-238
Tijeras Canyon is located at the eastern edge of Albuquerque, New Mexico and extends about 15 miles to the east. The canyon is the construction site of a new east-west interstate highway. This basic-data report contains surface and ground-water data collected prior to and during highway construction. Well and spring...
Water Resources Division, U.S. Geological Survey
1978, Open-File Report 78-185
Richard I. Grauch
1978, Open-File Report 78-949
Uraninite of Precambrian age occurs locally in and around a massive sulfide deposit at Camp Smith, Westchester and Putnam Counties, New York. The host rocks are believed to be part of a sequence of marine sediments and submarine volcanogenic rocks that were metamorphosed to leucogneisses, amphibolites, and amphoholite gneisses in...
Water Resources Division, U.S. Geological Survey
1978, Open-File Report 78-278
William Craven Culbertson, L. N. Robinson, T. M. Gaffke
1978, Open-File Report 78-653
H. W. Sundelius, A. A. Stromquist
1978, IMAP 1082
Thomas L. Holzer
1978, Open-File Report 78-1016
Modern surface faulting along the Picacho fault, east of Picacho, Arizona, has been attributed to ground-water withdrawal. In September 1977, three exploratory test holes were drilled 5 km east of Picacho and across the Picacho fault to investigate subsurface conditions and the mechanism of the faulting. The holes were logged...
William Kam
1978, Open-File Report 78-492
Percolation of contaminants from the controlled land application of domestic anaerobic digested liquid sludge has affected the quality of ground water in the highly permeable unconfined Miocene Cohansey Sand aquifer at Colliers Mills and Webbs Mill areas of the Pine Barrens region in Ocean County, New Jersey.The sludge, containing five...
James M. Frazee Jr., Charles P. Laughlin
1978, Open-File Report 78-189
Benjamin Gildersleeve
1978, Geologic Quadrangle 1316