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Page 6193, results 154801 - 154825

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Saline-water resources of Texas
Allen George Winslow, Lester Ray Kister
1956, Water Supply Paper 1365
Large quantities of saline water are available in the world, both on the surface and underground; however, these waters have not been studied extensively as sources of potable water. Saline water is defined herein as water containing more than 1,000 parts per million of dissolved solids, or, with certain mineralized irrigation...
Ground-water resources of the Ainsworth unit, Cherry and Brown Counties, Nebraska
James G. Cronin, Thomas G. Newport, R. A. Krieger
1956, Water Supply Paper 1371
The Ainsworth unit, so named by the U. S. Bureau of Reclamation, is in north-central Nebraska and is in the drainage basin of the Niobrara River. It is an area of about 1,000 square miles in the east-central part of Cherry County and northern part of Brown County. The east-west...
Reservoirs in the United States
N.O. Thomas, G. Earl Harbeck Jr.
1956, Water Supply Paper 1360-A
Reservoir storage facilities in the United States play an important part in the national economy. Storage facilities have enabled the country to utilize to a much fuller extent one of the most valuable natural resources: water. During recent years the construction of reservoirs has continued at a high rate. This...
Hydrology of Indiana lakes
Joseph Irving Perrey, Don Melvin Corbett
1956, Water Supply Paper 1363
Indiana's lakes are a valuable resource for both recreational use and their industrial potential. Some lakes are used for water supply. The natural lakes are glacial in origin and are most concentrated in northeastern Indiana. Many of the lakes were drained by the early settlers. The natural processes of sedimentation ad...
U.S. Geological Survey exploration program in the Trixie area, East Tintic mining district, Utah County, Utah
H. T. Morris, A.E. Disbrow, Thomas Seward Lovering
1956, Open-File Report 56-84
The Trixie area is in the south central part of the East Tintic mining district, Utah, and is believed to include the intersections of several mineralized pebble dike-fissure zones and a major, easterly trending fault. The fissure-fault intersections, which are considered to be favorable ore-locallizing structures, are concealed by lavas...