Howard W. Lorenz, R. G. McMurtrey, Herbert A. Swenson
1956, Water Supply Paper 1360-C
No abstract available....
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Publication Extents
Not all publications have extents, not all extents are completely accurateWater Resources Division, U.S. Geological Survey
1956, Water Supply Paper 1336
Water Resources Division, U.S. Geological Survey
1956, Water Supply Paper 1270
Water Resources Division, U.S. Geological Survey
1956, Water Supply Paper 1322
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...
Edward Joseph Harvey
1956, Water Supply Paper 1356
Alfred E. Torrey, F. A. Kohout, Herbert A. Swenson
1956, Water Supply Paper 1355
No abstract available....
B. R. Colby, C. H. Hembree, F. H. Rainwater
1956, Water Supply Paper 1373
This report gives results of an investigation by the U. S. Geological Survey of chemical quality of surface waters and sedimentation in the Wind River Basin, Wyo. The sedimentation study was begun in 1946 to determine the quantity of sediment that is transported by the streams in the basin; the...
Water Resources Division, U.S. Geological Survey
1956, Water Supply Paper 1272
Water Resources Division, U.S. Geological Survey
1956, Water Supply Paper 1271
Water Resources Division, U.S. Geological Survey
1956, Water Supply Paper 1338
Raymond Lavern Schreurs, Frank Hays Rainwater
1956, Water Supply Paper 1358
No abstract available....
Water Resources Division, U.S. Geological Survey
1956, Water Supply Paper 1249
Water Resources Division, U.S. Geological Survey
1956, Water Supply Paper 1342
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...
Water Resources Division, U.S. Geological Survey
1956, Water Supply Paper 1325
Water Resources Division, U.S. Geological Survey
1956, Water Supply Paper 1323
Edward Bradley, F. Rainwater
1956, Water Supply Paper 1368
No abstract available....
Donald Frazier Eschman, Joseph H. Hartshorn
1956, Open-File Report 56-45
This brief report outlines the surface geology along the proposed relocation of a segment of Route 2, and indicates areas of sand and gravel suitable for select borrow.A reconnaissance geologic map was prepared and is included as a part of this report (see attached map).Field work was done in 1953...
J. F. Robertson
1956, Open-File Report 56-102
George Plafker
1956, Open-File Report 56-95
Geologic conditions at Sheep Creek, Carlson Creek, and Turner Lake are discussed in relation to possible plans for hydroeletric power development. The proposed sites are on the rugged mainland of Southeastern Alaska along Gastineau Channel and Taku Inlet near Juneau. Bedrock in the area consists of a coastal strip of...
W. J. Mapel, Charles Sherwood Robinson
1956, Open-File Report 56-77
No abstract available....
Garn Arthur Rynearson, R.M. Hutchinson
1956, Open-File Report 56-105
No abstract available....
Samuel L. Moore
1956, Open-File Report 56-82
A large body of zinc and copper mineralization is exposed in a line of low hills about 5 kilometers east of the small village of Vazante in the northwestern part of the state of Minas Gerais, Brazil. The Vazante area can be reached by roads leading north from the State...
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...