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Page 2380, results 59476 - 59500

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Regional impact of water resource investments in an developing area
Emil Attanasi
1975, Journal of the American Water Resources Association (11) 69-76
Regional development and industrialization patterns are investigated and related via regression analysis to water resource investments for the island of Puerto Rico. Although results of this study indicate such investments have little immediate or short‐term impact, significant relationships and variations in regional responses appear over longer time periods. This is...
Mechanism of Formation of Pillow Lava
James G. Moore
1975, American Scientist (63) 269-277
Much of the ocean floor is covered by lava of a distinctive character. The lava appears to be made up of closely packed ellipsoidal masses about the size and shape of pillows - hence the term pillow lava. Only within the last few years has the abundance of pillow lava...
A brief history of the U.S. Geological Survey
Water Resources Division, U.S. Geological Survey, Mary C. Rabbitt
1975, Report
Established by an Act of Congress in 1879 and charged with responsibility for "classification of the public lands, and examination of the geological structure, mineral resources, and products of the national domain," the U. S. Department of the Interior's Geological Survey has been the Nation's principal source of information about...
Geohydrology and water quality of the Mississippi River alluvial aquifer, northeastern Louisiana
Merrick S. Whitfield Jr.
1975, Water Resources Technical Report 10
The Mississippi River alluvial aquifer in northeastern Louisiana is in the alluvium of the Mississippi, Arkansas, and Ouachita Rivers and underlies approximately 5,000 square miles (13,000 square kilometers) in the Mississippi River valley. The aquifer, of Pleistocene age, is a southeastward-thickening wedge of sand and gravel that ranges in thickness...
Lakes of Oregon, Volume 3: Hood River, Multnomah, Washington and Yamhill Counties
M.V. Shulters
1975, Report
An inventory of lakes and reservoirs of Oregon is essential for a complete evaluation of the total surface-water supply of the State and to provide a basis for answering questions about Oregon's lakes. Much of the information on lakes and reservoirs previously collected by Federal and State agencies has never...
The EROS Data Center
Water Resources Division, U.S. Geological Survey
1975, Report
The EROS Data Center, 16 miles (25 km) northeast of Sioux Falls, South Dakota, is operated by the EROS Program to provide access to NASA's LANDSAT [formerly Earth Resources Technology Satellite (ERTS)] imagery, aerial photography acquired by the U.S. Department of the Interior, and photography and imagery acquired by the...
Water-resources investigations of the U.S. Geological Survey in the northern Great Plains coal region of Wyoming, Montana, and North Dakota, 1975
Water Resources Division, U.S. Geological Survey
1975, Report
The Geological Survey's Water Resources Division has for many years maintained a program of water-resources investigations that includes the coal regions of Wyoming, Montana, and North Dakota. These programs have been supported by State and local agencies and by other agencies of the Federal government, largely to provide data for...
History of irrigation and characteristics of streamflow in northern Nebraska
F.B. Shaffer
1975, Open-File Report 7501
Five streams drain the northern part of Nebraska and are tributaries to the Missouri River above Yankton, S. Dak. This report presents statistical data at 29 gaging sites on four of the streams, namely, White River, Ponca Creek, Niobrara River, and Bazile Creek. The fifth stream, Hat Creek, drains a...
Water-quality changes during a salmon run in an interior Alaskan stream
Jon W. Nauman, Donald R. Kernodle
1975, Journal of Research of the U.S. Geological Survey (3) 103-106
Increased activity at sunset of sockeye (red) salmon (Oncorhynchus nerka) in an Alaskan stream resulted in increases in carbon dioxide, turbidity, suspended chlorophyll a, and drift invertebrates, and a decrease in pH and dissolved oxygen....
Summary of hydrologic data collected during 1974 in Dade County, Florida
J.E. Hull
1975, Open-File Report FL 75-012
This report is ninth in a series documenting the annual hydrologic conditions in Dade County, Florida. The hydrologic conditions in Dade County for the 1974 water year (October 1, 1973 to September 30, 1974) except for rainfall are summarized in tables, graphs, and maps. The locations of ground-water data-collection stations...
Norman Creek, a source of recharge to Maramec Spring, Phelps County, Missouri
E. E. Gann, E. J. Harvey
1975, Journal of Research of the U.S. Geological Survey (3) 99-102
Rhodamine WT dye was used to trace the subsurface movement of water from Norman Creek, a losing Ozark stream, to Maramec Spring, a straight-line distance of 8.7 mi (14.0 km). Grab samples and activated charcoal packets were used to check possible emergent points of the dye. The leading edge of...
Changes in concentration of certain constituents of treated waste water during movement through the Magothy Aquifer, Bay Park, New York
Henry F. H. Ku, John Vecchioli, Stephen E. Ragone
1975, Journal of Research of the U.S. Geological Survey (3) 89-92
Approximately 7 million gallons (27 million litres) of tertiary-treated sewage (reclaimed water) was injected by well into the Magothy aquifer and was subsequently pumped out. As the reclaimed water moved through the aquifer, concentrations of certain dissolved constituents decreased as follows: Total nitrogen, 7 percent; methylene blue active substances, 49...
Mobilization of iron in water in the Magothy aquifer during long-term recharge with tertiary-treated sewage, Bay Park, New York
Stephen E. Ragone, Henry F. H. Ku, John Vecchioli
1975, Journal of Research of the U.S. Geological Survey (3) 93-98
Tertiary-treated sewage (reclaimed water) has been recharged by well into the Magothy aquifer at Bay Park, N. Y., intermittently since 1968. The longest of 13 recharge tests, the subject of this report, lasted 84.5 days. This was sufficient time for the reclaimed water to reach an observation well 200 ft...
Topographic maps
Water Resources Division, U.S. Geological Survey
1975, Report
A topographic map is a graphic representation of selected manmade and natural features of a part of the earth's surface plotted to a definite scale. The distinguishing characteristic of a topographic map is the portrayal of the shape and elevation of the terrain....