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Page 306, results 7626 - 7650

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Not all publications have extents, not all extents are completely accurate
Stratigraphy, structure, and palinspastic synthesis of the western Brooks Range, northwestern Alaska
Charles F. Mayfield, Irvin L. Tailleur, Inyo Ellersieck
1983, Open-File Report 83-779
This report is an effort to describe and decipher the mid-Paleozoic to Lower Cretaceous stratigraphy and the orogenic evolution of the western Brooks Range. The western Brooks Range primarily is composed of stacks of complexly deformed thrust sheets that contain mostly coeval sequences of rocks with slightly different lithologic facies....
The Alaska Mineral Resource Assessment Program: Background information to accompany folio of geologic and mineral resource maps of the Ambler River quadrangle, Alaska
Charles F. Mayfield, I.L. Tailleur, N. R. Albert, Inyo Ellersieck, Donald Grybeck, S. W. Hackett
1983, Circular 793
The Ambler River quadrangle, consisting of 14,290 km2 (5,520 mi2) in northwest Alaska, was investigated by an interdisciplinary research team for the purpose of assessing the mineral resource potential of the quadrangle. This report provides background information for a folio of maps on the geology, reconnaissance geochemistry, aeromagnetics, Landsat imagery,...
The Alaska Mineral Resource Assessment Program: Guide to information contained in folio of geologic and mineral resource maps of the Philip Smith Mountains quadrangle, Alaska
H. N. Reiser, W. P. Brosge, T. D. Hamilton, D.A. Singer, W. D. Menzie II, K. J. Bird, J. W. Cady, J. R. Le Compte, J. B. Cathrall
1983, Circular 759
The geology and mineral resources of the Philip Smith Mountains quadrangle were virtually unexplored until the investigations for oil began in northern Alaska. Construction of the Trans-Alaskan Pipeline System has now made the quadrangle accessible by road. In 1975 and 1976 a team of geologists, geochemists, and geophysicists investigated the...
Floods from small drainage basins in Alaska
Stanley H. Jones
1983, Open-File Report 83-258
Flood peak-stage and associated discharge data collected since 1963 in small (generally less than 100 square miles) drainage areas in Alaska are presented in tabular and graphical form. The report also contains table of computed magnitudes of floods at selected recurrence intervals (2, 5, 10, 25, and 50 years) for...
Sediment transport in the Tanana River near Fairbanks, Alaska, 1982
P.E. Harrold, R.L. Burrows
1983, Water-Resources Investigations Report 83-4213
Suspended-sediment and bedload-transport rates for the Tanana River near Fairbanks can be related to water discharge, and annual sediment loads can be computed using these relations. For a site at Fairbanks the annual loads in 1982 were 26.1 million metric tons of suspended sediment and 227,000 metric tons of bedload....
Trace metals in surface water and stream sediments of Healy and Lignite Creek basins, Alaska
Bruce Parks
1983, Water-Resources Investigations Report 83-4173
Water quality and streamflow in the Russian River basin during low-flow seasons (May to October), were studied for water years 1973-78 to document water-quality and streamflow conditions in the basin, and to determine the extent and cause of any water-quality impairment. The most important factors affecting surface-water quality and streamflow...