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Page 5125, results 128101 - 128125

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Water resources data for Michigan, water year 1978
Water Resources Division, U.S. Geological Survey
1979, Water Data Report MI-78-1
Water resources data for the 1978 water year for Michigan consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels and water temperature of ground water. This report contains discharge records for 187 gaging stations; stage only...
Depth determination of Colvocoresses Reef, Indian Ocean (EC-68-Landsat)
Alden P. Colvocoresses
1979, Open-File Report 79-726
The depth to the subject reef has been estimated at a nominal 10 n by three independent analyses based on Landsat and (in two cases) comparisons.: to measured depths of submerged features in the same area. Fathometer readings made in 1979 confirm the 1O-m reading....
Ground-water levels in alluvium on the South coast of Puerto Rico, February 1978
Jose R. Diaz
1979, Open-File Report 79-1272
Ground-water levels in the alluvial aquifer of the south coast of Puerto Rico in February 1978 were similar to or slightly higher than those of February 1977. Water levels rose about 2 to 3 meters in the northern section near the foothills in the coastal plain area from Salinas to...
Texture, clay mineralogy, trace metals, and age of cored sediments from the North Atlantic Outer Continental Shelf
Michael H. Bothner, E.C. Spiker, W.M. Ferrebee, D.L. Peeler
1979, Open-File Report 79-842
The concentration of 9 trace metals in sediment cores collected from the Continental Shelf off the northeastern United States are generally uniform with sediment depth and are low compared to average crustal abundances. No evidence for the accumulation of anthropogenic metals was found in these samples.The sediment texture on Georges...
Ground water in Dale Valley, New York
Allan D. Randall
1979, Water-Resources Investigations Report 78-120
Dale Valley is a broad valley segment, enlarged by glacial erosion, at the headwaters of Little Tonawanda Creek near Warsaw , New York. A thin, shallow alluvial aquifer immediately underlies the valley floor but is little used. A deeper gravel aquifer, buried beneath many feet of lake deposits, is tapped...