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Page 5061, results 126501 - 126525

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Trace metals in Suisun Bay, California: A preliminary report
S. N. Luoma, P. V. Cascos, R. M. Dagovitz
1984, Water-Resources Investigations Report 84-4170
A 5-month partial study (February to July 1983) was completed in Suisun Bay, a shallow embayment of San Francisco Bay, Calif., to determine characteristic heavy metal concentrations present in sediments and organisms (Corbicula clams) prior to possible discharge of San Luis Drain irrigation tile return water. Preliminary results show sediments...
Gazetteer of hydrologic characteristics of streams in Massachusetts — Hudson River basin
S. William Wandle Jr.
1984, Water-Resources Investigations Report 83-4250
The Hudson River basin includes streams draining the Hoosic River (205 square miles), Kinderhook Creek (20.9 square miles), and Roeliff Jansen Kill (13.3 square miles) basins in western Massachusetts, eastern New York, and southern Vermont. Drainage areas, using the latest available 1:24,000 scale topographic maps, are re-computed for data-collection sites...
Geophysical interpretation of the gneiss terrane of northern Washington and southern British Columbia, and its implications for uranium exploration
John W. Cady, Kenneth F. Fox
1984, Professional Paper 1260
The Omineca crystalline belt of northeastern Washington and southern British Columbia has a regional Bouguer gravity high, and individual gneiss domes within the terrane are marked by local gravity highs. Models of crustal structure that satisfy the limited available seismic-refraction data and explain the gravity high over the gneiss terrane...
Land subsidence in the Santa Clara Valley, California as of 1980
J. F. Poland, R. L. Ireland
1984, Open-File Report 84-818
From 1916 to 1966 in the San Jose area of Santa Clara Valley, California, deficient rainfall and runoff was accompanied by a fourfold increase in groundwater withdrawals. In response the artesian head declined 180-240 ft. The land surface subsided 12.7 ft in San Jose, due to compaction of the fine-grained...