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Page 5861, results 146501 - 146525

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Sulfides associated with the Salton Sea geothermal brine
Brian J. Skinner, Donald E. White, Harry J. Rose, Robert E. Mays
1967, Economic Geology (62) 316-330
Concentrated saline brine tapped by a deep well drilled for geothermal power near the Salton Sea, California, deposited metal-rich siliceous scale at the rate of 2 to 3 tons per month. The iron-rich opaline scale contains an average of 20% Cu and up to 6% Ag present in bornite, digenite,...
Standards for water quality
Luna B. Leopold
1967, Conference Paper, World petroleum congress proceedings
The quality which is necessary depends on the use to which the water will be put. Because uses vary, so also must quality standards. Maintaining any level of quality presents a problem of cost and depends on variations in natural water characteristics, in time and space, and variations in volume...
Insecticide residues in big game mammals of South Dakota
Raymond J. Greenwood, Y.A. Greichus, E.J. Hugghins
1967, Journal of Wildlife Management (31) 288-292
An analysis was made of eight insecticide residues in the renal fat tissue of 23 white-tailed deer (Odocoileus virginianus), 13 mule deer (O. hemionus), 9 pronghorns (Antilocapra americana), and 2 elk (Cervus canadensis) collected in South Dakota during the fall of 1964. Identification and quantitative analysis of the insecticide residues...
Relative toxicity of lead and selected substitute shot types to game farm mallards
Harold D. Irby, Louis N. Locke, George E. Bagley
1967, Journal of Wildlife Management (31) 253-257
The acute toxicity of lead, three types of plastic-coated lead, two lead-magnesium alloys, iron, copper, zinc-coated iron, and molybdenum-coated iron shot were tested in year-old male game farm mallards. Mallards (Anus platyrhynchos) were fed eight number 6 shot of each type and observed for a period of 60 days. Ducks...
Stump and tree nesting by mallards and black ducks
Lewis M. Cowardin, G.E. Cummings, P.B. Reed Jr.
1967, Journal of Wildlife Management (31) 229-235
Studies conducted 1961-65 at the Montezuma National Wildlife Refuge in New York demonstrated that mallards (Anas platyrhynchos) and black ducks (Anas rubripes) make extensive use of stumps and dead snags for nest sites. Nest densities in timbered habitats compared favorably with those in untimbered habitats. Nest success was generally higher...
Plans of the U.S.Geological Survey, water resources division for research, investigations, and data collection in ground water
J. E. Upson
1967, Groundwater (5) 13-19
The Geological Survey has been the foremost agency in the investigation of ground‐water resources in the United States beginning about 1910. Most of the basic principles of modern ground‐water hydrology were developed in the Survey's program of cooperative investigations. Use of ground water in the United States in 1960 was about 17½ percent of all water uses, excluding water power. The use will probably increase, though at a decreasing rate. Although amount of use may level off, the...
Plans of the U.S.Geological Survey, water resources division for research, investigations, and data collection in ground water
J. E. Upson
1967, Groundwater (5) 13-19
The Geological Survey has been the foremost agency in the investigation of ground‐water resources in the United States beginning about 1910. Most of the basic principles of modern ground‐water hydrology were developed in the Survey's program of cooperative investigations. Use of ground water in the United States in 1960 was about 17½ percent of all water uses, excluding water power. The use will probably increase, though at a decreasing rate. Although amount of use may level off, the...
Post-paleozoic radiometric ages and their relevance to fault movements, Northern Southeastern Alaska
R. A. Loney, David A. Brew, Marvin A. Lanphere
1967, GSA Bulletin (78) 511-526
Recently determined lead-alpha and potassium-argon ages from northern southeastern Alaska indicate major plutonic events in the Paleozoic, Mesozoic, and Tertiary; in contrast, previous studies suggested that only one complex Jurassic and Cretaceous event occurred. The ages presented in this paper indicate the following Mesozoic and Tertiary plutonic events: Middle or...
Artificial Recharge at Valley City, North Dakota, 1932 to 1965
T. E. Kelly
1967, Groundwater (5) 20-25
Valley City, North Dakota, has an average daily water use of 750,000 gallons, which is obtained from wells tapping pattly confined gravel deposits in the Sheyenne River valley. These deposits at Valley City have a maximum thickness of more than 50 feet and an areal extent of approximately 1 square...
Mineral appraisal of the Harney Lake and Malheur Lake candidate areas of the Malheur National Wildlife Refuge, north-central Harney County, Oregon
George Walton Walker, Donald Swanson
1967, Open-File Report 890
The Harney Lake and Malheur Lake candidate areas are in the Malheur National Wildlife Refuge, north-central Harney County, Oreg. The two areas occupy the shallow center of the Harney Basin, a broad structural and physiographic depression filled by several varieties of silicic to mafic volcanic rocks, sedimentary rocks, and unconsolidated...
Aurorite, argentian todorokite, and hydrous silver-bearing lead manganese oxide
Arthur S. Radtke, Charles M. Taylor, D. F. Hewett
1967, Economic Geology (62) 186-206
During a study of hypogene manganese minerals, three silver-bearing manganese oxides were identified in "black calcite" associated with silver ores at the Aurora mine (Treasure Hill), Hamilton, Nevada. Specifically these are: (1) argentian chalcophanite (aurorite) (Ag 2 Ba,Ca,Pb,-K 2 ,Cu,Mn (super +2) )Mn 3 (super +4) O 7 . 3H 2 O; (2) argentian todorokite (Ag 2 ,K 2 ,Ca,Ba,-Na 2 ,Cu,Pb)Mn 4 (super +4) O 9 . 5H 2 O; and...
The porphyry copper deposit exposed in the Liberty open-pit mine near Ely, Nevada; Part 2, The formation of hydrothermal alteration zones
Robert O. Fournier
1967, Economic Geology (62) 207-227
In the southwest part of the Liberty pit a large porphyry body exhibits a zonal alteration pattern related to fissures and pyrite-bearing veins. The outermost zone contains unaltered K-feldspar, kaolinite after plagioclase, and black biotite after hornblende. An intermediate zone contains reconstituted K-feldspar, phlogopitic biotite, and muscovite or muscovite plus...
Belt of sigmoidal bending and right-lateral faulting in the western great basin
John P. Albers
1967, GSA Bulletin (78) 143-156
Betweeen the northwest-trending Sierra Nevada and the north-northeast-trending ranges that characterize most of the Great Basin section of the Basin and Range province is a belt of confused and divergent topographic forms, which is approximately 50 miles wide and 300 miles long. Along the eastern part of this belt is...
The role of olivine in the crystallization of the prehistoric Makaopuhi tholeiitic lava lake, Hawaii
James G. Moore, B.W. Evans
1967, Contributions to Mineralogy and Petrology (15) 202-223
On eruption, the tholeiitic basalt lava of the prehistoric Makaopuhi lake contained nearly seven percent euhedral olivine phenocrysts of approximately Fa14 composition. In the center of the 225 foot vertical section of the lake, the lava became more than 90 percent solid at 1000° C after about 30 years. At the...
Temperature and water-quality conditions for the period July 1963 to December 1965, Patuxent River Estuary, Maryland
Robert L. Cory, Jon W. Nauman
1967, Report
Graphs and tables obtained from continuous records of surface-water temperature from five stations for the period july 1963 through December 1965 and of surface, salinity, dissolved oxygen, turbidity, tide-stage, wind data and bottom temperature from a single station are presented herein. Effects of powerplant cooling water on water temperature were...
Prospecting for gold in the United States
Water Resources Division, U.S. Geological Survey
1967, Report
Prospecting for gold is something that probably everyone dreams of trying at least once. To the person who is mainly concerned with this activity as a vacation diversion, prospecting offers a special excitement. There is a constant hope that the next pan of sediment may be "pay dirt," and no...
Mineral appraisal of the Flattery Rocks, Quillayute Needles, and Copalis National Wildlife Refuges, Washington
Albert Edward Weissenborn, Parke Detweiler Snavely Jr.
1967, Open-File Report 879
The Flattery Rocks, Quillayute Needles, and Copalis National Wildlife Refuges lie off the Pacific coast of the Olympic Peninsula between Cape Flattery and Grays Harbor. They have a total land area of 247 acres and consists of numerous small islands, sea stacks and rocks that rise above a wave-cut platform....
Water resources data for Indiana, 1966
Water Resources Division, U.S. Geological Survey
1967, Water Data Report IN-66-1
The surface-water records for the 1966 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of Indiana are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering states. The quality-of-water investigations of the U.S. Geological Survey are...
Results of the second phase of the drought-disaster test-drilling program near Morristown, N.J.
John Vecchioli, William D. Nichols, Bronius Nemickas
1967, New Jersey Division of Water Policy and Supply Water Resources Circular 17
The continued drought in northeastern New Jersey through the summer of 1966 with its attendant water-supply problems resulted in an extension of the drought-disaster test-drilling program originally requested by the Office of Emergency Planning on August 30, 1965. Authorization to continue test drilling was fiven by the Office of Emergency...
Mountains and plains Denver's geologic setting
Water Resources Division, U.S. Geological Survey
1967, Report
A slice of geologic history is exposed to view in the Denver, Colorado area. Denver is situated on the High Plains near the east front of the Rocky Mountains. As one travels westward from Denver toward the mountains, successively older rocks are crossed from the geologically young rocks of the...