Ground water in the Piedmont upland of central Maryland
Claire A. Richardson
1982, Water Supply Paper 2077
This report, describing ground-water occurrence in a 130-square-mile area of the central Maryland Piedmont, was originally designed for use by the U.S. Environmental Protection Agency in replying to a request for designation of the aquifers to be the sole or principal source of ground water. However, the information contained in...
Plankton studies in San Francisco Bay; IV, Phytoplankton abundance and species composition, January 1980 - February 1981
R.L. Wong, J. E. Cloern
1982, Open-File Report 82-443
Data are presented on the phytoplankton species composition and abundance in San Francisco Bay from January 1980 through February 1981. Phytoplankton were identified and enumerated in surface samples collected approximately every two weeks at selected stations in the main channel of the Bay, and at shoal stations in the central...
Evaluation of earthquake-induced ground failure
J.M. Ferritto
1982, Open-File Report 82-880
Water-quality and hydrogeologic data for three phosphate industry waste-disposal sites in central Florida, 1979-80
Ronald L. Miller, Horace Sutcliffe Jr.
1982, Water-Resources Investigations Report 81-84
This report is a complilation of geologic, hydrologic, and water-quality data and information on test holes collected in the vicinity of gypsum stack complexes at two phosphate chemical plants and one phosphatic clayey waste disposal pond at a phosphate mine and beneficiation plant in central Florida. The data were collected...
Stratigraphic notes, 1980-1982
Water Resources Division, U.S. Geological Survey
1982, Bulletin 1529-H
No abstract available....
Appraisal of ground-water quality near wastewater-treatment facilities, Glacier National Park, Montana
Joe A. Moreland, Wayne A. Wood
1982, Water-Resources Investigations Report 82-4
Water-level and water-quality data were collected from monitoring wells at wastewater-treatment facilities in Glacier National Park. Five additional shallow observation wells were installed at the Glacier Park Headquarters facility to monitor water quality in the shallow ground-water system.Water-level, water-quality, and geologic information indicate that some of the initial monitoring wells...
Reconnaissance of ground-water quality, eastern Snake River basin, Idaho
D. J. Parliman
1982, Water-Resources Investigations Report 82-4004
Water-quality, geologic, and hydrologic data were collected for 165 wells in the eastern Snake River basin, Idaho. Water-quality characteristics analyzed include specific conductance, pH, water temperature, major dissolved cations and anions, and coliform bacteria. Ground water from aquifers in all rock units is generally composed of calcium, magnesium, and bicarbonate...
AQUBIO : a computer code for simulating fast-transient, three-dimensional concentrations of biota in aquatic environments for assessment of entrainment losses at power plants -- Vol. III, computer listing, example input and output
Kenneth H. Kim
1982, FWS/OBS 82/41.3
Summary chart of geological data from Amoco Tierney Unit 1 well, SW 1/4, SE 1/4, Sec. 15, T 20 N., R. 94 W., Sweetwater County, Wyoming
D.J. Markovchick, R.E. Lanham, H.G. Bucurel, B. E. Law
1982, Oil and Gas Investigation Chart 116
No abstract available....
Geology and ground-water resources of Oswego County, New York
Todd S. Miller
1982, Water-Resources Investigations Report 81-60
Unconsolidated deposits of Pleistocene and Holocene age form a nearly continuous cover in Oswego County. Pleistocene deposits consist of lodgment and ablation tills, outwash, kame, beach and wave-delta sand and gravel, and lacustrine sand, silt, and clay. Holocene deposits consist of peat and muck deposited in wetlands , and alluvial...
Sedimentology and stratigraphy of the Kanayut Conglomerate, central Brooks Range, Alaska: Report of 1980 field season
T. H. Nilsen, Thomas E. Moore, D. F. Balin, S. Y. Johnson
1982, Open-File Report 82-199
The Upper Devonian Kanayut Conglomerate crops out along the crest of the Brooks Range of northern Alaska for a distance of almost 1000 km. It ranges in thickness from 2600 m in the Atigun River area to 700 m south of Anaktuvuk Pass and has been subdivided into four regionally...
Life history requirements of selected finfish and shellfish in Mississippi sound and adjacent areas
Norman Gustaf Benson, editor(s)
1982, FWS/OBS 81/51
No abstract available....
Water resources data, New York, water year 1981, volume 3, western New York
Water Resources Division, U.S. Geological Survey
1982, Water Data Report NY-81-3
No abstract available. ...
Viking Lander 1 rectified photomosaics evening scene; camera 1, Mars
Water Resources Division, U.S. Geological Survey
1982, IMAP 1368
Viking Lander 1 rectified photomosaics evening scene; camera 2, Mars
Water Resources Division, U.S. Geological Survey
1982, IMAP 1367
Heavy-mineral variability in beach and dune sands in the vicinity of the mouth of the Columbia River
Gretchen Luepke
1982, Open-File Report 82-1091
Land use and land cover, 1972-76, Alabama; Tennessee
Water Resources Division, U.S. Geological Survey
1982, Land Use and Land Cover 90
Detailed bathymetric map of the United States continental slope between Lindenkohl Canyon and Toms Canyon, offshore New Jersey
J.R. Kirby, James M. Robb, J.C. Hampson Jr.
1982, Miscellaneous Field Studies Map 1443
Thermal springs in the Salmon River basin, central Idaho
H.W. Young, R.E. Lewis
1982, Open-File Report 82-104
The Salmon River basin drains approximately 13,000 square miles in central Idaho underlain by the Idaho batholith. Geologic units in the basin include igneous, sedimentary, and metamorphic rocks and granitic rocks predominate. Water from thermal springs ranges in temperature from 20.5 degrees to 94.0 degrees Celsius. The waters are slightly...
Controlled photomosaic of the Mare Tyrrhenum Southwest Quadrangle of Mars
Water Resources Division, U.S. Geological Survey
1982, IMAP 1471
Organic geochemistry of sediments on the flanks of Tanner and Cortes banks offshore from southern California
J. B. Rapp, K.A. Kvenvolden
1982, Open-File Report 82-829
Holocene sediment, composed mainly of foram tests, occurs on the flanks of the Tanner and Cortes Banks, offshore southern California. The organic matter in this sediment differs in content and composition from the organic matter in nearby basins. Two sources of hydrocarbons are indicated: terrestrial plants and biodegraded or immature...
Algal conditions in the Caloosahatchee River (1975-79), Lake Okeechobee to Franklin Lock, Florida
Benjamin F. McPherson, Henry R. La Rose
1982, Water-Resources Investigations Report 81-81
Maximum numbers of suspended algae occurred in late spring and early summer, in each of the years 1975-79, in the Caloosahatchee River. Numbers exceeded 100,000 cells per milliliter at all stations sometime during the study. Concentrations decreased during late summer and autumn and were low during winter, except in January...
Maps showing locations and descriptions of radiocarbon-dated samples from central and northern California
Carol A. Price
1982, Miscellaneous Field Studies Map 1321
This compilation includes radiocarbon dates and other pertinent information about samples from northern and central California, principally north of latitude 36°, drawn largely from Radiocarbon, Science, unpublished data of U.S. Geological Survey geologists, and other published and unpublished data brought to the author's attention as of January 1981. It includes...
Landslides and related features, Kentucky and Tennessee, Corbin 1° x 2° sheet
Alfred R. Taylor, Roger E. Thomas
1982, Open-File Report 82-653
No abstract available....
Geologic map and oil shale deposits of the Elko East quadrangle, Elko County, Nevada
Barry J. Solomon, Steven W. Moore
1982, Miscellaneous Field Studies Map 1421
