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Page 6306, results 157626 - 157650

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Electrical resistivity studies of subsurface conditions near Antigo, Wisconsin
H. Cecil Spicer
1952, Circular 181
Resistivity measurements are reported for the glaciated area near Antigo, Wis., to locate buried sand and gravel deposits in the glacial drift, which might be developed as aquifers, and to determine depths to the pre-Cambrian bedrock. The results of the resistivity study are presented both as cross sections and as...
Geology and ground-water resources of Comal County, Texas
William Owsley George, Seth D. Breeding, Warren W. Hastings
1952, Water Supply Paper 1138
The purpose of this report on the geology and ground-water resources of Comal County in central Texas is to determine the sources of the waters that supply Comal Springs, the largest springs in the Southwest, and other springs and wells. Comal County has an area of about 559 square miles...
The bauxite deposits of Floyd, Bartow, and Polk counties of northwest Georgia
Walter S. White, N.M. Denson
1952, Circular 193
Most of the bauxite deposits ipf northwest Georgia are in the Hermitage, Bobo, and Cave Spring districts in Floyd, Bartow, and Polk Counties. The region has produced in the neighborhood of 400,000 tons of bauxite from about 65 small mines, but the known reserves of high grade bauxite are very...
Hydrologic reconnaissance of the Green River in Utah and Colorado
H. E. Thomas
1952, Circular 129
The Green River, rising in Wyoming and draining high mountains in that state, northeast Utah and northwest Colorado, is a major tributary of the Colorado River. In the late summer, after the snow has melted from these mountains, the flow in the Green River reaches its minimum for the year....
Geologic map of the Barnes Hill talc prospect, Waterbury, Vermont
A.H. Chidester, G. W. Stewart, D.C. Morris
1952, Miscellaneous Field Studies Map 7
The Barnes Hill talc prospect is in northeastern Waterbury township, Washington County, Vermont, about 2.2 miles N. 35° E. of the road triangle at Waterbury Center.  The deposit occurs in a body of ultramafic rock that crops out between the altitudes of 1,150 and 1,190 feet above sea level, near...