Geochemistry of ground water in mine drainage problems
Ivan Barnes, F.E. Clarke
1964, Professional Paper 473-A
Water-table, surface-drainage, and engineering soils map of the Sharptown area, Delaware
John K. Adams, Durward H. Boggess
1964, Hydrologic Atlas 84
Water-table, surface-drainage, and engineering soils map of the Seaford East quadrangle, Delaware
John K. Adams, Durward H. Boggess, O. J. Coskery
1964, Hydrologic Atlas 106
Water-table, surface-drainage, and engineering soils map of the Lewes area, Delaware
John K. Adams, Durward H. Boggess, Christian F. Davis
1964, Hydrologic Atlas 103
Water-table, surface-drainage, and engineering soils map of the Hickman area, Delaware
John K. Adams, Durward H. Boggess
1964, Hydrologic Atlas 100
Water-table, surface-drainage, and engineering soils map of the Harbeson quadrangle, Delaware
John K. Adams, Durward H. Boggess
1964, Hydrologic Atlas 108
Availability of ground water in the Elva quadrangle, Kentucky
J. H. Morgan
1964, Hydrologic Atlas 117
Availability of ground water in the Kirksey quadrangle, Kentucky
J. H. Morgan
1964, Hydrologic Atlas 113
Availability of ground water in the Farmington quadrangle, Kentucky
J. H. Morgan
1964, Hydrologic Atlas 92
Preliminary evaluation of hydrologic situation in Everglades National Park, Florida
J.H. Hartwell, Howard Klein, B.F. Joyner
1964, Open-File Report 64-74
Field investigation of mine waters in the northern anthracite field, Pennsylvania
Ivan Barnes, W.T. Stuart, D.W. Fisher
1964, Professional Paper 473-B
Availability of ground water in the Oak Level quadrangle, Kentucky
J. H. Morgan
1964, Hydrologic Atlas 116
Availability of ground water in the Briensburg quadrangle, Kentucky
L.M. MacCary
1964, Hydrologic Atlas 114
Availability of ground water in the Hardin quadrangle, Kentucky
L.M. MacCary
1964, Hydrologic Atlas 115
Availability of ground water in Hall County, Nebraska
Charles Franklin Keech, V. H. Dreeszen
1964, Hydrologic Atlas 131
Short papers in geology and hydrology, articles 122-172
Water Resources Division, U.S. Geological Survey
1964, Professional Paper 475-D
No abstract available....
Hidden Recharge
J. H. Feth
1964, Ground Water (2) 14-17
“Hidden recharge” is defined as subsurface percolation of water from basin‐margin mountains directly into aquifers of the valley basins. It is an important, and sometimes neglected, item in hydrologic equations. Locally, geologic conditions permit inter‐basin circulation of ground water. The concept that ground‐water basins necessarily terminate at the contact between...
The international hydrological decade
R. L. Nace
1964, Eos, Transactions, American Geophysical Union (45) 413-421
Work toward establishing a program of international cooperative studies in scientific hydrology began about 4 years ago, and the IHD (International Hydrological Decade) will begin under international auspices in January 1965. This program will be highly important for hydrology and hydrologists, and it should contribute greatly to human welfare in the future. Fortuitously, the opening year...
Geohydrologic analogies between the Jordan Valleys of Utah and the holy land
Edward Bradley
1964, International Association of Scientific Hydrology - Bulletin (9) 12-23
The biblical Jordan River Valley, which extends from Lake Tiberias (the Sea of Galilee) to the Dead Sea, is decidedly similar to the Jordan River Valley of Utah, which joins Lake Utah and Great Salt Lake. Both Jordan Rivers drain relatively large fresh-water lakes and also are major sources of discharge into large salty lakes that have no outlets to the ocean.The...
The father of modern ground water hydrology
O. M. Hackett
1964, Groundwater (2) 2-5
No abstract available. ...
Tritium-hydrologic research: Some results of the U.S. Geological Survey Research Program
C.W. Carlston
1964, Science (143) 804-806
In general tritium is of limited usefulness as a tool in hydrologic studies because the tritium content of ground water, as a result of radioactive decay, becomes too low to be detectable after about 50 years. Nevertheless, a unique study was made of the hydrologic cycle of small stream basins...
Sedimentology: general introduction and definitions : fluvial sediment and channel morphology
Roger G. Wolff, Paul C. Benedict
1964, Report
Sedimentology, the study of sedimentary rocks and the processes by which they are formed, includes and is related to a large number of phenomena. Sedimentology includes the five fundamental processes defined by the term sediaentation --weathering, erosion, transportation, deposition and diagenesis. Sedimentology shares with geomorphology the study of the surface...
Soil mechanics and soil physics symbols and nomenclature useful in hydrologic studies
A.I. Johnson
1964, Report
The study of hydrology requires an interdisciplinary approach, incorporating knowledge from fields such as engineering, geology, chemistry, and agriculture. With increasing frequency, the hydrologist finds it necessary to study the literature of the soil mechanics and soil physics disciplines for assistance in the solution of hydrologic problems. Because of the inter-relation between hydrology and soil mechanics...
Hydrologic factors pertinent to ground‐water contamination
R. Brown
1964, Groundwater (2) 5-12
Predictions of where and how a fluid waste may travel from disposal site to the water table require detailed information on the physical characteristics, location, and extent of all pervious and impervious materials in the unsaturated zone. Principles concerning the flow system in the unsaturated zone indicate the importance of choice of...
Hydrologic factors pertinent to ground‐water contamination
R. Brown
1964, Groundwater (2) 5-12
Predictions of where and how a fluid waste may travel from disposal site to the water table require detailed information on the physical characteristics, location, and extent of all pervious and impervious materials in the unsaturated zone. Principles concerning the flow system in the unsaturated zone indicate the importance of choice of...