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Publication Extents

Not all publications have extents, not all extents are completely accurate
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...
Appendix E—List of current publications concerning ground water
Jean M. Berdan
1946, Eos, Transactions, American Geophysical Union (27) 274-278
Alexander, W. H., Jr., Broadhurst, W. L., and White, W. N., Progress report on ground water In the High Plains in Texas, Tex. State Bd. Water Engrs., 12 pp., 7 tigs. (mimeogranhedl May 1944.Ashley, George H.,and Graham, Jack B., Groundwater investigations in Pennsylvania Pa. Dep. Internal Affairs, Monthly Bull., v....
Report of Committee on Ground Water—1944–1945
S. W. Lohman
1946, Eos, Transactions, American Geophysical Union (27) 236-245
Because of war‐imposed responsibilities of most agencies and individuals this year, no new programs were undertaken by the Committee, but the work of the Subcommittee on Permeability was continued, and a substantial progress report by C. E. Jacob, Acting Chairman, and by members of this Subcommittee follows this report as...
Report of the Research Committee on Runoff, 1945–46
R. W. Davenport
1946, Eos, Transactions, American Geophysical Union (27) 876-878
The variety of usage and even the confusion in the nomenclature and terminology of some fields of hydrology have been often remarked. The Committee on Runoff conceived the idea that it would be profitable to consider some of the terms which are especially pertinent to the field of runoff. That...
A generalized graphical method for evaluating formation constants and summarizing well‐field history
H.H. Cooper, C. E. Jacob
1946, Eos, Transactions, American Geophysical Union (27) 526-534
The capacities of a water‐bearing formation to transmit water under a hydraulic gradient and to yield water from storage when the water table or artesian pressure declines, are generally expressed, respectively, in terms of a coefficient of transmissibility and a coefficient of storage. Determinations of these two constants are almost...
General principles of artificial ground-water recharge
O. E. Meinzer
1946, Economic Geology (41) 191-201
The natural subterranean reservoirs formed by the porous and permeable rocks differ from surface reservoirs chiefly in that they have complex structure and great internal resistanc• to the How of water. Their full utilization requires systematic development based on the geology and hydrology of the aquifer and the principles of...
Artificial recharge of artesian limestone at Orlando, Florida
A.G. Unklesbay, H.H. Cooper
1946, Economic Geology (41) 293-307
The principal aquifer in the Orlando area consists of 900 feet or more of permeable artesian limestones of upper and middle Eocene age. As in most other parts of the Florida peninsula, these limestones are overlain by the Hawthorn formation of Miocene age which contains relatively impervious beds. The Hawthorn...
Artificial recharge of productive ground-water aquifers in New Jersey
H.C. Barksdale, G.D. DeBuchananne
1946, Economic Geology (41) 726-737
Artificial recharge by water spreading is practiced in several places in New Jersey. Rates of recharge ranging from 3,000 to 125,000 gallons per acre per day have been measured at the Perth Amboy Water Works, where artificial recharge of the Old Bridge sand, of upper Cretaceous age, has been practiced...
Geology and ground-water resources of the island of Hawaii
Harold T. Stearns, Gordon A. Macdonald
1946, Bulletin 9
Hawaii, the largest island in the Hawaiian group, is 93 miles long, 76 miles wide, and covers 4,030 square miles. Mauna Loa Volcano is 13,680 feet high and Mauna Kea is 13,784 feet high. Plate 1 shows the geology, wells, springs, and water-development tunnels. Plate 2 is a map and...
Industrial limestones and dolomites in Virginia: northern and central parts of the Shenandoah Valley
R.S. Edmundson
1945, Book, Virginia Division of Mineral Resources Bulletin
The area described in this report includes the northern and central parts of Shenandoah Valley in Virginia extending from the West Virginia line southwestward to the vicinity of Greenville, Augusta County. It contains extensive deposits of high-calcium limestone averaging more than 97 per cent calcium carbonate. The Mosheim limestone, composed...
The Ogden Valley artesian reservoir
H. E. Thomas
1945, Technical Publication 2
Ogden Valley, in Weber County, Utah, contains an artesian reservoir from which the city of Ogden obtains all except a small part of its municipal water supply. A detailed investigation of the ground-water resources of Ogden Valley, and particularly of this artesian reservoir, was made by the Geological Survey, United...
Columnaris as a disease of cold-water fishes
1945, Transactions of the American Entomological Society (73) 32-36
A natural outbreak of columnaris disease among wild adult and hatchery-reared fingerling salmon in the State of Washington is described. The disease is identified by the recovery of the causative organism, Bacillus columnaris Davis, which may be readily identified by its characteristic action in forming columns on the surfaces of...