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Page 2686, results 67126 - 67150

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Geology and ground-water resources of Cedar City and Parowan Valleys, Iron County, Utah
H. E. Thomas, G.H. Taylor
1946, Water Supply Paper 993
Cedar City Valley and Parowan Valley are situated in the eastern part of Iron County, in southwestern Utah. Both valleys are traversed by United States Highway 91, which skirts the west base of the High Plateaus of Utah. The sparse population of the valleys is chiefly dependent upon agricultural products...
Ground water in the High Plains of Texas
W. N. White, W. L. Broadhurst, Joseph W. Lang
1946, Water Supply Paper 889-F
The High Plains of Texas occupy an area of about 35,000 square miles, extending from the northern boundary of the Panhandle southward about 300 miles, and from the New Mexico line eastward an average distance of about 120 miles. This region is divided into two segments by the Canadian River...
Cloudburst floods in Utah, 1850-1938
Ralf R. Woolley, Ray E. Marsell, Nathan C. Grover
1946, Water Supply Paper 994
Five years after the first settlement was made in Utah, at Salt Lake City in 1847, it became manifest to the settlers both there and at Manti that "cloudbursts" were of common occurrence in this region. Other settlements were made and gradually expanded on the steep alluvial fans of the...
Quartz crystal in Brazil
W. D. Johnston Jr., R.D. Butler
1946, GSA Bulletin (57) 601-650
The peak production of Brazilian quartz crystal was reached in 1943 when 2411 metric tons were exported. Minas Gerais, Goiaz, and Bahia are the principal producing states. Minor quantities are obtained from Espirito Santo and Northeastern Brazil.Primary veins and pegmatites yield secondary deposits of eluvial, colluvial, and alluvial origin. The...
Notes on determining the effective distance to a line of recharge
R.G. Kazmann
1946, Eos, Transactions, American Geophysical Union (27) 854-859
Increasing emphasis has been given in recent years to the installation of wells in sand and gravel deposits along perennial streams. Under favorable conditions water enters the aquifer from the adjacent stream so that the safe yield is not limited by recharge from local precipitation [see “References” at end of...
Appendix A—Report of the subcommittee on permeability
C. E. Jacob
1946, Eos, Transactions, American Geophysical Union (27) 245-256
The Subcommittee on Permeability of the Permanent Research Committee on Ground Water of the Section of Hydrology, was organized in 1943 to provide for the open discussion of the terminology relating to permeability with a view toward the elimination of conflicting usages and the clarification and standardization of acceptable terms....
Appendix B—Notes on the permeability coefficient and its units
V.C. Fishel
1946, Eos, Transactions, American Geophysical Union (27) 256-269
In the development of terms and units for a new science such as ground‐water hydrology, which is based on physics, it would seem fitting to adopt the terminology that has become standard in other branches of physics such as heat and electricity. Darcy's law has its counterpart in similar laws...