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164468 results.

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Page 5885, results 147101 - 147125

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Plant microfossils from the Lakota Formation
Robert H. Tschudy, Sharon D. Van Loenen
1966, Open-File Report 66-134
As a part of continuing studies to provide palynological data from critical sequences for comparative biostratigraphic studies, the microfossils found in a sample of "Pine Needle" coal have been examined and photographed. The assemblage is presented on one plate....
Plant microfossils from the Fort Union Formation
Robert H. Tschudy, Sharon D. Van Loenen
1966, Open-File Report 66-133
As a part of continuing studies to provide palynological data from critical sequences for comparative biostratigraphic studies, the microfossils found in two Paleocene samples have been examined and photographed....
Gravity survey and regional geology of the Prince William Sound epicentral region, Alaska
J. E. Case, D.F. Barnes, George Plafker, S. L. Robbins
1966, Professional Paper 543-C
Sedimentary and volcanic rocks of Mesozoic and early Tertiary age form a roughly arcuate pattern in and around Prince William Sound, the epicentral region of the Alaska earthquake of 1964. These rocks include the Valdez Group, a predominantly slate and graywacke sequence of Jurassic and Cretaceous age, and the Orca...
Floods of November and December 1965 in southern California
E. R. Hedman, E.G. Pearson
1966, Open-File Report 66-61
Severe flooding occurred in southern California in late November and late December 1965 as a result of three heavy storms. Rain occurred on most days during the period November 13-26 and December 28-31, with major amounts distributed in three periods: November 13-19, 21-26, and December 28-31. More than 12 inches...
Slide-induced waves, seiching and ground fracturing caused by the earthquake of March 27, 1964 at Kenai Lake, Alaska
David S. McCulloch
1966, Professional Paper 543-A
The March 27, 1964, earthquake dislodged slides from nine deltas in Kenai Lake, south-central Alaska. Sliding removed protruding parts of deltas-often the youngest parts-and steepened delta fronts, increasing the chances of further sliding. Fathograms show that debris from large slides spread widely over the lake floor, some reaching the toe...