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Page 6039, results 150951 - 150975

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Manganese deposits in the Drum Mountains, Juab and Millard Counties, Utah
Max D. Crittenden Jr., John A. Straczek, Ralph Jackson Roberts
1961, Bulletin 1082-H
The Drum Mountains are in west-central Utah 30 miles northwest of Delta, between the Sevier Desert on the east and Whirlwind Valley on the west. It is a typically barren desert range comprising a westward-tilted structural unit in which is exposed as much as 9,000 feet of quartzite (Cambrian and...
Geology and mineral deposits of the Carlile quadrangle, Crook County, Wyoming
M.H. Bergendahl, R. E. Davis, G. A. Izett
1961, Bulletin 1082-J
The Carlile quadrangle-is along the northwestern flank of the Black Hills uplift in Crook County, Wyo. The area-is primarily one of canyons and divides that are a result of downcutting by the Belle Fourche River and its tributaries through an alternating succession of sandstone, siltstone, and mudstone or shale beds....
Water resources of the Raft River basin, Idaho-Utah
Raymond L. Nace
1961, Water Supply Paper 1587
Much arable land in the Raft River basin of Idaho lacks water for irrigation, and the potentially irrigable acreage far exceeds the amount that could be irrigated with the estimated total supply of water. Therefore, the amount of uncommitted water that could be intercepted and used within the basin is...
Water requirements of the copper industry
Orville Durey Mussey
1961, Water Supply Paper 1330-E
The copper industry in 1955 used about 330 million gallons of water per day in the mining and manufacturing of primary copper. This amount is about 0.3 percent of the total estimated withdrawals of industrial water in the United States in 1955. These facts were determined by a survey, in...
Effect of reforestation on streamflow in central New York
William Joseph Schneider, Gordon Roundy Ayer
1961, Water Supply Paper 1602
Hydrologic data have been collected since 1932 in central New York State to determine the effect of reforestation on streamflow. Data are available for three small partly reforested areas and for one nonreforested control area. From 35 to 58 percent of the 3 areas were reforested, mostly with species of...
Recharging ground-water reservoirs
George H. Taylor
1961, Open-File Report 60-139
Successful artificial recharge of a ground-water reservoir depends upon many factors. Some factors are very complicated and technical. This paper will deal briefly with some of them. For a more comprehensive description of ground-water reservoirs and their artificial recharge, the publications listed at the end of this paper should be...
Salinity and hydrology of closed lakes
Walter Basil Langbein
1961, Professional Paper 412
Lakes without outlets, called closed lakes, are exclusively features of the arid and semiarid zones where annual evaporation exceeds rainfall. The number of closed lakes increases with aridity, so there are relatively few perennial closed lakes, but "dry" lakes that rarely contain water are numerous.Closed lakes fluctuate in level to...
Floods in Arkansas, magnitude and frequency
James L. Patterson
1961, Open-File Report 62-99
This report presents methods by which the magnitude and frequency of expected floods for most streams in Arkansas may be determined. Flood data have been used to define flood-frequency curves applicable to the State.Composite frequency curves have been defined showing the relation of the mean annual flood to floods having...