Lynn Harmsen
1977, Open-File Report 77-221
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Publication Extents
Not all publications have extents, not all extents are completely accurateVirginia Carter, Frederic Billingsley, Jeannine Lamar
1977, Open-File Report 77-414
Glenn Allen Miller
1977, Open-File Report 77-728
The hydrologic system in Death Valley is probably in a steady-state condition--that is, recharge and discharge are equal, and net changes in the quantity of ground water in storage are not occurring. Recharge to ground water in the valley is derived from interbasin underflow and from local precipitation. The two...
George A. Desborough
1977, Open-File Report 77-341
R.F. Carter
1977, Open-File Report 77-408
Richard W. Casteel, C.K. Beaver, D.P. Adam, J.D. Sims
1977, Open-File Report 77-639
Melville Rhodes Mudge, Robert L. Earhart, Dudley D. Rice, Lawrence Y. Marks
1977, Open-File Report 77-95
The proposed Great Bear wilderness has a good potential for oil and gas (mainly gas), and a moderate potential for submarginal resources of copper and silver in a belt 25 miles (40 km) long and about 1 mile (1.6 km) wide that is partly within the study area along the...
Sergio Garza
1977, Open-File Report 77-219
Regional decline of aquifer head due to ground-water withdrawal in the Houston area has caused extensive land-surface subsidence. The NASA-Johnson Space Center (NASA-JSC) in southeastern Harris County, Texas, was about 13 to 19 feet above mean sea level in 1974 and sinking at a rate of more than 0.2 foot...
M. O. Fretwell
1977, Open-File Report 77-128
This report describes the quality of the surface and ground waters of the Yakima Indian Reservation in south-central Washington, during the period November 1973-October 1974. The average dissolved-solids concentrations ranged from 48 to 116 mg/L (milligrams per liter) in the mountain streams, and from 88 to 372 mg/L in the...
F. Allan Hills
1977, Open-File Report 77-55
The Estes Conglomerate, which is exposed in the Nemo District on the northeastern flank of the Black Hills, South Dakota, is inferred to be of early middle Precambrian age (early Precambrian X or Paleoaphebian) and to be resting on late early Precambrian (late Precambrian W) granitic continental crust. The Estes...
F. E. Senftle, A.B. Tanner, P. W. Philbin, G. R. Boynton, C.W. Schram
1977, Open-File Report 77-162
John W. Hillhouse
1977, Open-File Report 77-457
Paleomagnetic inclinations of the Late Quaternary sediments of South San Francisco Bay were determined from bore hole samples collected near Dumbarton Bridge. The sediments consist of estuarine muds and nonmarine sand deposits, floored by bedrock of the Mesozoic Franciscan Formation. - Beneath Dumbarton Bridge the entire sedimentary fill is normally...
Philip Thayer Hayes, Thomas A. Ryer, L.W. Kiteley, J. R. Hatch, F. W. Osterwald, C.R. Dunrud, J. J. Connor
1977, Open-File Report 77-513
Bruce D. Smith, C.J. Zablocki, F.C. Frischknecht, V. J. Flanigan
1977, Open-File Report 77-59
Paul C. Lyons
1977, Open-File Report 77-816
Timothy L. Miller, Stuart W. McKenzie
1977, Open-File Report 77-799
Charles G. Cunningham, Thomas August Steven
1977, Open-File Report 77-568
Gary M. Edson, Cathy L. Barnosky
1977, Open-File Report 77-866
Eight holes were drilled in that part of T. 24 S., R. 5 E. which is in the Willow Springs 7 1/2-minute quadrangle, Emery and Sevier Counties, Utah (fig. 1). This drilling was done from June 15 to July 14, 1977, to obtain information on the thickness and extent of...
Robert L. Goemaat
1977, Open-File Report 77-238
The objectives of the observation-well 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 the future availability of ground-water supplies, and (3) to provide information for use in basic research. These selected records serve as a...
J. Thomas Nash
1977, Open-File Report 77-787
Red granites of the St. Francois Mountains are highly radioactive and contain 4 to 34 parts per million (ppm) uranium. The most radioactive is the Graniteville Granite which contains an average of 16.9 ppm U and 42.6 ppm Th. The Butler Hill and Breadtray Granites also contain anomalous amounts, averaging...
Wilfred P. Hasbrouck
1977, Open-File Report 77-600
Joseph Moses Botbol, Richard Sinding-Larsen, R.B. McCammon, G. B. Gott
1977, Open-File Report 77-349
Robert L. Goemaat
1977, Open-File Report 77-73
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...
Robert L. Goemaat
1977, Open-File Report 77-239
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...
Jules D. Friedman, David Frank
1977, Open-File Report 77-599
Surface thermal features occur in an area of 9700 m2 at Mt. Hood, on the basis of an aerial line-scan survey made April 26, 1973. The distribution of the thermal areas below the summit of Mt. Hood, shown on planimetrically corrected maps at 1:12,000, suggests structural control by a fracture...