Climate and streamflow of Puerto Rico
E.V. Giusti, M. A. Lopez
1967, Caribbean Journal of Science (7) 87-93
The presently available data on streamflow, runoff rainfall, and temperature of Puerto Rico are evaluated, although the period of record is very short, with a view to contributing to the knowledge of hydrology of tropical islands. The average annual streamflow in Puerto Rico is 45 percent of the annual rainfall, or 15 percent more than in the eastern piedmont of...
Test hold in aquifer with many water-bearing zones at Jacksonville, Florida
G.W. Leve, D. A. Goolsby
1967, Groundwater (5) 18-22
One of the deepest water‐exploration wells in the southeastern United States was completed in 1966 at Jacksonville, Florida. It was drilled to a depth of nearly 2,500 feet to supply geologic and hydrologic information on the deeper unexplored part of the Floridan aquifer. This aquifer consists of a series of water producing zones separated by nonproducing zones. An important new fresh‐water producing zone was found, and the contact between...
Compilation of surface water records of Nepal through December 31, 1965
Nepal Hydrological Survey Department.
1967, Book
No Abstract available ...
Compilation of hydrologic data Green Creek, Brazos River basin, Texas, 1967
1967, Report
The U.S. Soil Conservation Service is actively engaged in the installation of flood and soil erosion reducing measures in Texas under the authority of "The Flood Control Act of 1936 and 1944" and "Watershed Protection and Flood Prevention Act" (Public Law 566), as amended. The Soil Conservation Service has found...
Applications of factor analysis in study of chemistry of groundwater quality, Mojave River Valley, California
D.R. Dawdy, J. H. Feth
1967, Water Resources Research (3) 505-510
Factor analysis is applied to results of chemical analyses of 103 water samples from wells in the Upper and Middle Mojave River valley, San Bernardino County, California. Chemical analyses showed that there are three principal chemical types of water, calcium bicarbonate, sodium sulfate, and sodium chloride, as well as many...
Standards for water quality
Luna B. Leopold
1967, Conference Paper, World petroleum congress proceedings
The quality which is necessary depends on the use to which the water will be put. Because uses vary, so also must quality standards. Maintaining any level of quality presents a problem of cost and depends on variations in natural water characteristics, in time and space, and variations in volume...
Plans of the U.S.Geological Survey, water resources division for research, investigations, and data collection in ground water
J. E. Upson
1967, Groundwater (5) 13-19
The Geological Survey has been the foremost agency in the investigation of ground‐water resources in the United States beginning about 1910. Most of the basic principles of modern ground‐water hydrology were developed in the Survey's program of cooperative investigations. Use of ground water in the United States in 1960 was about 17½ percent of all water uses, excluding water power. The use will probably increase, though at a decreasing rate. Although amount of use may level off, the...
Plans of the U.S.Geological Survey, water resources division for research, investigations, and data collection in ground water
J. E. Upson
1967, Groundwater (5) 13-19
The Geological Survey has been the foremost agency in the investigation of ground‐water resources in the United States beginning about 1910. Most of the basic principles of modern ground‐water hydrology were developed in the Survey's program of cooperative investigations. Use of ground water in the United States in 1960 was about 17½ percent of all water uses, excluding water power. The use will probably increase, though at a decreasing rate. Although amount of use may level off, the...
An electrical analog study of the geometry of limestone solution
M. S. Bedinger
1967, Groundwater (59) 24-24
This study of the geometry of limestone solution is based on the following conditions: (1) the limestone is impermeable but contains and transmits water in joints, fractures, bedding‐plane partings, and solution channels; (2) at depth, the limestone aquifer is underlain by impermeable rock; (3) ground water in the limestone is under water‐table conditions; (4) recharge to the limestone is by infiltration of precipitation through the overlying rock...
Availability of ground water in the Cayce quadrangle, Jackson Purchase region, Kentucky-Tennessee
Arnold J. Hansen
1967, Hydrologic Atlas 180
No abstract available....
Serial publications commonly cited in technical bibliographies of the United States Geological Survey
Water Resources Division, U.S. Geological Survey
1967, Report
This compilation is a listing of the serial publications cited in the following publications of the United States Geological Survey: Geophysical Abstracts, Abstracts of North American Geology, Bibliography of North American Geology, and Bibliography of Hydrology of the United States. A supplement of publications added since the main list was...
Northern part, Ten Mile and Taunton River basins
John R. Williams, Richard E. Willey
1967, Massachusetts Hydrologic - Data Report 10
The northern part of the Ten Mile and Taunton River basins is an area of about 195 square miles within Norfolk, Plymouth, and Bristol Counties in southeastern Massachusetts. The northern boundary of the area (plate 1) is the drainage divide separating these basins from that of the Charles, Neponset, and...
Hydrologic applications of lithofacies clastic-ratio maps
Wayne A. Pettyjohn, Phillip G. Randich
1967, Conference Paper, Proceedings, South Dakota Academy of Science
No abstract available....
Hydrology of the Valley-fill and carbonate-rock reservoirs, Pahrump Valley, Nevada-California
Glenn T. Malmberg
1967, Water Supply Paper 1832
This is the second appraisal of the water supply of Pahrump Valley, made 15 years after the first cooperative study. In the first report the average recharge was estimated to be 23,000 acre-feet per year, only 1,000 acre-feet more than the estimate made in this report. All this recharge was...
Hydrologic and climatologic data, 1966, Salt Lake County, Utah
A. G. Hely, Reed W. Mower, C. A. Horr
1967, Utah Basic-Data Release 13
An investigation of the water resources of Salt Lake County, Utah, was undertaken by the Water Resources Division of the U.S. Geological Survey in July 1963. This investigation is a cooperative project financed equally by the State of Utah and the Federal Government in accordance with an agreement between the...
Ground-water research in the U.S.A.
C. L. McGuinness
1967, Earth-Science Reviews (3) 181-202
Ground-water reservoirs and the overlying unsaturated zone-collectively, the "subsurface"-have an enormous capacity to supply water to wells and useful plants, to store water to meet future needs for the same purposes, and, under suitable precautions, to accept wastes. This capacity can be exploited on a maximum scale, however, only on...
Bibliography of U.S. Geological Survey water-resources reports for Utah
1966, Utah Division of Water Rights Information Bulletin 17
This bibliography contains a complete listing to December 1966 of reports relating to the water resources of Utah prepared by personnel of the U.S. Geological Survey. Discussions of the related subjects of geology, hydrology, and chemical quality of the water are included in many of the reports. The reports were,...
A study of some effects of urbanization on storm runoff from a small watershed
William Howard Espey Jr., Carl W. Morgan, Frank D. Masch
1966, Report 23
The evaluation of the effects of urbanization on the runoff characteristics of a small watershed is a problem that can be studied by either a short-range or a long-range investigation. Because the long-range type of investigation would require several years for hydrologic data accumulation, it cannot provide any immediate information...
The Alaska earthquake, March 27, 1964: effects on hydrologic regimen
Roger M. Waller, R. W. Coble, Austin Post, Arthur McGarr, Robert C. Vorhis
1966, Professional Paper 544
This is the fourth in a series of six reports that the U.S. Geological Survey published on the results of a comprehensive geologic study that began, as a reconnaissance survey, within 24 hours after the March 27, 1964, Magnitude 9.2 Great Alaska Earthquake and extended, as detailed investigations, through several...
Hydrogeologic data in the Quinebaug River basin, Connecticut
Chester E. Thomas Jr., Allan D. Randall, Mendall P. Thomas
1966, Connecticut Water Resources Bulletin 9
This report presents hydrologic and geologic data collected by the U.S. Geological Survey during an investigation of water resources in the Quinebaug River basin of Connecticut in cooperation with the Connecticut Water Resources Commission. The Quinebaug River basin occupies about 425 square miles in the northeastern part of the State,...
Summary of hydrologic and physical properties of rock and soil materials, as analyzed by the hydrologic laboratory of the U.S. Geological Survey, 1948-60
D. A. Morris, A.I. Johnson
1966, Report
The Hydrologic Laboratory was established in 1948 to serve as the central laboratory for the Ground Water Branch, Water Resources Division, of the U.S. Geological Survey. During the period it has been in existence, numerous samples of rock and soil materials have been analyzed. Analysis data on samples from 42...
Effects of the March 1964 Alaska earthquake on the hydrology of south-central Alaska
Roger M. Waller
1966, Professional Paper 544-A
The earthquake of March 27, 1964, greatly affected the hydrology of Alaska and many other parts of the world. Its far-reaching effects were recorded as water-level fluctuations in gages operated on water wells and streams. The close-in effects were even more striking, however; sediment-laden ground water erupted at the surface,...
Effects of the March 1964 Alaska earthquake on the hydrology of the Anchorage area, Alaska
Roger M. Waller
1966, Professional Paper 544-B
The Anchorage hydrologic system was greatly affected by the seismic shock. Immediate but temporary effects included increased stream discharge, seiche action on lakes, and fluctuations in ground-water levels. Generally, ground-water levels were residually lowered after the initial period of fluctuation. This lowering is attributed either to changes in the discharge...
Effects of the earthquake of March 27, 1964, in the Homer area, Alaska
Roger M. Waller, Kirk W. Stanley
1966, Professional Paper 542-D
The March 27, 1964, earthquake shook the Homer area for about 3 minutes. Land effects consisted of a 2- to 6-foot subsidence of the mainland and Homer Spit, one earthflow at the mouth of a canyon, several landslides on the Homer escarpment and along the sea bluffs, and minor fissuring...
Hydrologic reconnaissance of Point Reyes National Seashore area, California
R. H. Dale, S. E. Rantz
1966, Open-File Report 66-22
This report summarizes the results of a hydrologic reconnaissance of the Point Reyes National Seashore area, the primary purpose of which was to appraise potential sources of water supply at park sites where visitor accommodations are proposed. Point Reyes National Seashore is a peninsular area on the California coast about...