Water resources of the Utica-Rome area, New York
Henry N. Halberg, O. P. Hunt, F. H. Pauszek
1962, Water Supply Paper 1499-C
The Utica-Rome area is along the Mohawk River and New York State Erie (Barge) Canal about midway between Lake Ontario and Albany. It encompasses about 390 square miles centered around the industrial cities of Utica and Rome. The Mohawk River, its tributary West Canada Creek, and a system of reservoirs...
The effect of bed roughness on depth-discharge relations in alluvial channels
Daryl B. Simons, E.V. Richardson
1962, Water Supply Paper 1498-E
Reconnaissance of ground-water resources in the Eastern Coal Field Region, Kentucky
William E. Price, D. S. Mull, Chabot Kilburn
1962, Water Supply Paper 1607
In the Eastern Coal Field region of Kentucky, water is obtained from consolidated sedimentary rocks ranging in age from Devonian to Pennsylvanian and from unconsolidated sediments of Quaternary age. About 95 percent of the area is underlain by shale, sandstone, and coal of Pennsylvanian age. Principal factors governing the availability...
Saline-water resources of New Mexico
J. W. Hood, Lester Ray Kister
1962, Water Supply Paper 1601
No abstract available....
Rainwater as a chemical agent of geologic processes; a review
Dorothy Carroll
1962, Water Supply Paper 1535-G
Chemical analyses of the rainwater collected at several localities are given to show the variations of the principal constitutents. In rock weathering and soil-forming processes, the chemical composition of rainwater has an important effect which has been evaluated for only a few arid areas. In humid regions the important amounts...
Salinity of the Delaware Estuary
Bernard Cohen, Leo T. McCarthy Jr.
1962, Water Supply Paper 1586-B
The purpose of this investigation was to obtain data on and study the factors affecting the salinity of the Delaware River from Philadelphia, Pa., to the Appoquinimink River, Del. The general chemical quality of water in the estuary is described, including changes in salinity in the river cross section and...
The ground-water flow system in the Snake River Plain, Idaho — An idealized analysis
Herbert E. Skibitzke, Jose Alves Da Costa
1962, Water Supply Paper 1536-D
No abstract available....
Beach-area water supplies between Ocean City, Maryland and Rehoboth Beach, Delaware
Turbit H. Slaughter
1962, Water Supply Paper 1619-T
Solutes in small streams draining single rock types, Sangre de Cristo Range, New Mexico
John P. Miller
1962, Water Supply Paper 1535-F
Subsidence in the Santa Clara Valley, California: A progress report
J. F. Poland, J. H. Green
1962, Water Supply Paper 1619-C
No abstract available....
Ground-water geology and hydrology of the Maynard area, Massachusetts
Nathaniel M. Perlmutter
1962, Water Supply Paper 1539-E
No abstract available....
Summary of floods in the United States during 1955
J. V. B. Wells
1962, Water Supply Paper 1455-B
Methods of measuring soil moisture in the field
A.I. Johnson
1962, Water Supply Paper 1619-U
For centuries, the amount of moisture in the soil has been of interest in agriculture. The subject of soil moisture is also of great importance to the hydrologist, forester, and soils engineer. Much equipment and many methods have been developed to measure soil moisture under field conditions. This report discusses...
Ground-Water Reconnaissance at Pinnacles National Monument, California
R. E. Evenson
1962, Water Supply Paper 1475-K
Ground-water supplies at Pinnacles National Monument have been obtained from springs that occur in fractures and along bedding planes of volcanic flows and deposits, and from springs discharged from perched water in a sedimentary fanglomerate formation. The spring-water yield is barely adequate to supply existing camp facilities, and therefore a...
Ground-water resources of Cow Valley, Malheur County, Oregon
Stuart G. Brown, Reuben Clair Newcomb
1962, Water Supply Paper 1619-M
No abstract available....
Surface water of Mariana, Caroline and Samoa Islands through June 1960
E. L. Hendricks
1962, Water Supply Paper 1751
Surface water supply of the United States, 1960, part 2-B, South Atlantic slope and Eastern Gulf of Mexico Basins, Ogeechee River to Pearl River
E. L. Hendricks
1962, Water Supply Paper 1704
Ground-water provinces of Brazil
Robert Schneider
1962, Water Supply Paper 1663-A
As part of a study of the status of investigations and development of ground water in Brazil, made under the auspices of the United States International Cooperation Administration and with the cooperation of the Government of Brazil, the country was divided into seven ground-water provinces. The identification and delineation of...
Theory of aquifer tests
J.G. Ferris, D.B. Knowles, R. H. Brown, R.H. Stallman
1962, Water Supply Paper 1536-E
The development of water supplies from wells was placed on a rational basis with Darcy's development of the law governing the movement of fluids through sands and with Dupuit's application of that law to the problem of radial flow toward a pumped well. As field experience increased, confidence in the...
Observations of tidal flow in the Delaware River
Everett George Miller
1962, Water Supply Paper 1586-C
Surface water supply of the United States, 1960, Part 7, lower Mississippi River Basin
E. L. Hendricks
1962, Water Supply Paper 1711
Waterpower resources near Petersburg and Juneau, southeastern Alaska : a discussion of potential development of power on 12 Alaskan streams
Fred A. Johnson
1962, Water Supply Paper 1529
Availability of Additional Water for Chiricahua National Monument, Cochise County, Arizona
Phillip W. Johnson
1962, Water Supply Paper 1475-H
The Chiricahua National Monument is in the eastern part of Cochise County, Ariz. The monument is about 35 miles southeast of Wilicox in the north end of the Chiricahua Mountains which border Sulphur Springs Valley on the west. The area is drained by two intermittent washes, one in Bonita and...
Water-supply possibilities at Capitol Reef National Monument, Utah
I. Wendell Marine
1962, Water Supply Paper 1475-G
A water supply of 50 gpm (gallons per minute) is estimated to be sufficient to supply the present and future water demand at the monument. The Coconino sandstone of Permian age seems to be capable of yielding this quantity to a well between 1,500 and 2,700 feet deep in the...
Water in the Coconino sandstone for the Snowflake-Hay Hollow area, Navajo County, Arizona
Phillip W. Johnson
1962, Water Supply Paper 1539-S
No abstract available....
