G. H. Nelson Jr., C. O. Ming
1983, Open-File Report 84-54
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Page 4743, results 118551 - 118575
Publication Extents
Not all publications have extents, not all extents are completely accurateS. A. Hoffman, K. L. Wetzel
1983, Open-File Report 83-941
K. L. Wetzel, S. A. Hoffman
1983, Open-File Report 83-940
Fernando Gómez-Gómez, Rafael Dacosta, Miguel Orona
1983, Open-File Report 83-689
K. A. Dickinson, J.E. Morrone, M. E. Roberts
1983, Open-File Report 83-169
G. R. Schiner, E. C. Hayes
1983, Open-File Report 83-869
This potentiometric map highlights: the altitude at which water level would stay in tightly cased wells; wells; springs; state water management district boundaries and sub-basin boundaries. (Lantz-PTT)...
Michael P. Foose, C.M. Sears
1983, Open-File Report 83-839
Senen Guzman-Rios
1983, Open-File Report 83-683
No abstract available....
Richard B. Waitt
1983, Open-File Report 83-671
In deposits of Pleistocene glacial lakes in northern Idaho and Washington, beds comprising 20 to 55 varves (average = 35-40) separate each successive graded gravel or sand bed that was swiftly emplaced by a catastrophic flood from glacial Lake Missoula. The floodlaid beds are similar to rhythmic successions of 40...
Water Resources Division, U.S. Geological Survey
1983, Open-File Report 83-610
G. F. Embree, R. D. Hoggan, E.J. William
1983, Open-File Report 83-599
R. S. Ballantyne
1983, Open-File Report 83-559
Remaining recoverable reserves of oil* and gas in the Outer Continental Shelf off Southern California are estimated to be 968 million barrels of oil and 1,851 billion cubic feet of gas as of December 31, 1982. These reserves are attributed to 14 fields. Original recoverable reserves from these fields are...
Alden P. Colvocoresses
1983, Open-File Report 83-558
Henry R. Schmoll, Richard P. Emanuel
1983, Open-File Report 83-479
No abstract available....
Brian F. Atwater
1983, Open-File Report 83-456
Kenneth W. King, W. W. Hays, P. J. McDermott
1983, Open-File Report 83-452
Little strong-motion data exists for seismic motions in the Intermountain seismic belt. Measurements of low-strain ground motions at 82 different locations in the urban areas of the Intermountain seismic belt were made to investigate the variations of ground-motion characteristics of a seismic data base for ground-motion hazards study. The low-strain...
John F. Windolph Jr.
1983, Open-File Report 83-446
No abstract available. ...
James D. Bliss
1983, Open-File Report 83-433-B
James D. Bliss
1983, Open-File Report 83-433-A
GEOTHERM, a computerized information system now off-line, was used to maintain data on the geology, geochemistry and hydrology of geothermal sites primarily within the United States. The system was proposed at the First Geothermal Implementation Conference in New Zealand in 1974 (Swanson, 1977) and was active until 1983. The primary...
James D. Bliss
1983, Open-File Report 83-431-B
James D. Bliss
1983, Open-File Report 83-428-B
John B. Cathrall, G.W. Day, J. D. Hoffman, S.K. McDanal
1983, Open-File Report 83-420-U
Sylvester Theodore Algermissen, B. L. Askew, P.C. Thenhaus, D. M. Perkins, S. Hanson, B.L. Bender
1983, Open-File Report 83-358
John S. Pallister
1983, Open-File Report 83-332
The Harrat Tuffil quadrangle, sheet 20/39 B, is located between lat 20°30’ and 21°00’ N. and long 39°30’ and 40°00’ E. about 50 km southeast of Jiddah. A western belt of Proterozoic metapelites and related rocks, defined as the Sa’diyah formation, structurally underlies and locally is interlayered with Proterozoic metabasaltic...
John B. Townshend, J.E. Papp, E.A. Sauter, P.A. Franklin, L.Y. Torrence
1983, Open-File Report 83-300-L
The preliminary geomagnetic data included here is made available to scientific personnel and organizations, as part of a cooperative effort and on a data exchange basis because of the early need by some users. To avoid delay, all of the data is copied from original forms processed at the observatory;...