Permit requirements for energy and other natural resources for the State of Mississippi
Berry Lawson Associates
1981, Open-File Report 81-1266
Assessment of conventionally recoverable petroleum resources of southeastern Mexico, northern Guatemala, and Belize
Charles D. Masters, James A. Peterson
1981, Open-File Report 81-1144
Corrensite; mineralogical ambiguities and geologic significance
P. L. Hauff
1981, Open-File Report 81-850
Lithologic log: Shell-Sloan No. 34-1, Okeechobee County, Florida
Barbara H. Lidz
1981, Open-File Report 81-453
Appendices to Geology of contaminants in coal; Phase I, report on investigations
C. B. Cecil, R.W. Stanton, F.T. Dulong
1981, Open-File Report 81-953-B
Geologic data for borehole ERDA-6, Eddy County, New Mexico
C.L. Jones
1981, Open-File Report 81-468
Assessment of conventionally recoverable petroleum resources of Persian Gulf basin and Zagros fold belt (Arabian-Iranian Basin)
Charles D. Masters
1981, Open-File Report 81-986
Report on microearthquake monitoring in the vicinity of Auburn Dam, California: November 1976-March 1977
Jerry P. Eaton, C.A. McHugh, F.W. Lester
1981, Open-File Report 81-244
A model of uranium mineralization in the Dripping Spring Quartzite, Gila County, Arizona
Connie J. Nutt
1981, Open-File Report 81-524
Geologic data for borehole ERDA-9, Eddy County, New Mexico
C.L. Jones
1981, Open-File Report 81-469
Permit requirements for energy and other natural resources for the State of Missouri
Radian Corporation
1981, Open-File Report 81-1265
Water use in Ohio, 1975
R. Michael Hathaway, Michael Eberle
1981, Water-Resources Investigations Report 81-17
The estimated water use in Ohio for all purposes in 1975 was 16 ,431 million gallons per day. Of this total, 15,321 were taken from surface water while the remaining 1,110 represent ground-water withdrawals. Totals by category are as follows (in million gallons per day): Thermoelectric power generation, 12 ,404;...
Proceedings of the Symposium on Mineral Deposits of the Pacific Northwest: Geological Society of America, Cordilleran Section meeting at Corvallis, Oregon, March 20-21, 1980
Miles L. Silberman, C. W. Field, Anne L. Berry
1981, Open-File Report 81-355
Stratiform and volcanogenic zinc-lead-barium deposits occur within the pelagic Kagvik sequence in the Red Dog Creek and Drenchwater Creek areas in the DeLong Mountains and Howard Pass quadrangles. The sulfide deposits occur together with barite, tuff, sandstone, shale, chert, and keratophyre flows and sills. The three main occurrences of the...
Estimates of undiscovered recoverable conventional resources of oil and gas in the United States
G.L. Dolton, K.H. Carlson, Ronald R. Charpentier, A. B. Coury, R. A. Crovelli, S. E. Frezon, A. S. Khan, J.H. Lister, R. H. McMullin, R. S. Pike, R. B. Powers, E. W. Scott, K. L. Varnes
1981, Circular 860
Effects of volcanism on the glaciers of Mount St. Helens
Melinda M. Brugman, Austin Post
1981, Circular 850-D
The cataclysmic eruption of Mount St. Helens May 18, 1980, removed 2.9 km2 (about 0.13 km3) of glacier snow and ice including a large part of Shoestring, Forsyth, Wishbone, Ape, Nelson, and all of Loowit and Leschi Glaciers. Minor eruptions and bulging of the volcano from March 27 to May...
Toxicity of Mount St. Helens ash leachate to a blue-green alga
Diane M. McKnight, Gerald L. Feder, Eric A. Stiles
1981, Circular 850-F
During several periods of volcanic-ash eruption at Mount St. Helens, Wash., (March 30, May 25-26, May 30-June 2, and June 12-13, 1980) strong winds from the north occurred at high altitudes. As a result, the volcanic ash fell some 50 miles to the south in the Bull Run watershed, the...
Altitude and configuration of the water table in the High Plains aquifer in Kansas, 1980
Marilyn E. Pabst, Lloyd E. Stullken
1981, Open-File Report 81-1004
The High Plains aquifer in Kansas is part of a regional system that extends into Colorado, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming. The aquifer in Kansas underlies an area of 31,000 square miles in the western and south-central part of the State. This aquifer is a hydraulically...
Tests of a hole-to-hole acoustic pulse measurement system
James H. Scott
1981, Open-File Report 81-1087
An analysis of strong-motion data from a severely damaged structure, the Imperial County Services Building, El Centro, California
Christopher Rojahn, P. N. Mork
1981, Open-File Report 81-194
Water-quality reconnaissance of Cretaceous aquifers of the southeastern Coastal Plain
Gerald L. Feder, Roger W. Lee
1981, Open-File Report 81-696
Multi-saline sample distillation apparatus for hydrogen isotope analyses: Design and accuracy
Afifa Afifi Hassan
1981, Water-Resources Investigations Report 81-25
A distillation apparatus for saline water samples was designed and tested. Six samples may be distilled simultaneously. The temperature was maintained at 400 C to ensure complete dehydration of the precipitating salts. Consequently, the error in the measured ratio of stable hydrogen isotopes resulting from incomplete dehydration of hydrated salts...
Surficial geology of part of Westdale quadrangle, Oswego County, New York
Todd S. Miller
1981, Open-File Report 81-147
The location and extent of seven kinds of surficial deposits in part of Westdale quadrangle, Oswego County, N.Y., are mapped on a 7.5-minute U.S. Geological Survey topographic map. The map was compiled to indicate the lithology and potential for groundwater development at any specific location....
Manchester quadrangle, Carroll County, Maryland: Hydrogeology
E. G. Otton
1981, Open-File Report 81-126
Data on depths to the upper Mya zone of the San Joaquin Formation in the Kettleman City area, San Joaquin Valley, California
R. W. Page
1981, Open-File Report 81-699
Reconnaissance of water availability and quality in abandoned coal mines near Roslyn, Kittitas County, Washington
F. A. Packard
1981, Open-File Report 80-955
The recoverable volume of ground water in abandoned coal mines near Roslyn, Wash., is estimated to be 20,000 acre-feet. During times of drought, pumping this water into the Cle Elum and Yakima Rivers for use in irrigation downstream should present few major water-quality problems. Wells at seven locations should be...