George V. Keller
1960, Bulletin 1083-D
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Page 6823, results 170551 - 170575
Publication Extents
Not all publications have extents, not all extents are completely accurateJ. W. Clarke, D.B. Vitaliano, V.S. Neuschel, and others
1960, Bulletin 1116-B
R.A. Bagnold
1960, Professional Paper 282-E
W.C. Overstreet, Henry Bell
1960, Miscellaneous Field Studies Map 235
Howard Dale Gower
1960, Geologic Quadrangle 129
No abstract available....
P.R. Wood
1960, Water Supply Paper 1491
Roger B. Colton
1960, Geologic Quadrangle 137
No abstract available....
John B. Reeside Jr., William Aubrey Cobban
1960, Professional Paper 355
J. V. B. Wells
1960, Water Supply Paper 1565
Water Resources Division, U.S. Geological Survey
1960, Water Supply Paper 1453
Edward Huntington Cobb
1960, Mineral Investigations Resource Map 11
M. H. Krieger
1960, IMAP 500
John Tilton Hack, John C. Goodlett
1960, Professional Paper 347
The area studied, mostly in the headwaters of the Shenandoah River, Augusta and Rockingham Counties, Va., includes about 55 square miles of densely forested mountain land and has an average relief of about 1,500 feet. It is part of an area that in June 1949 was subjected to a violent...
Harry L. Baldwin Jr., David P. Hill
1960, Open-File Report 60-11
During the early summer of 1959, a total of 1,187 gravity stations were occupied on the western part of the Snake River plain in Idaho. An area of 2,000 square miles extending from Glenns Ferry, Idaho, to Caldwell, Idaho, was covered with a station density of one station per two...
W. Storrs Cole
1960, Professional Paper 374-A
Charles F. Withington, Marion Charlotte Jaster
1960, Bulletin 1105
Richard A. Bramkamp, Leon F. Ramirez
1960, IMAP 201-B
Prepared by the U.S. Geological Survey and the Arabian American Oil Company under the joint sponsorship of the Kingdom of Saudi Arabia and the U.S. Department of State....
Richard A. Bramkamp, Leon F. Ramirez
1960, IMAP 202-B
Prepared by the U.S. Geological Survey and the Arabian American Oil Company under the joint sponsorship of the Kingdom of Saudi Arabia and the U.S. Department of State....
N. Herz, C. V. Dutra
1960, Geochimica et Cosmochimica Acta (21) 81-98
Thirty-nine samples of granitic rocks from the Quadrilátero Ferrifero, Minas Gerais, Brazil, representing "mixed" ages and at least three distinct Pre-Cambrian ages were analysed for seventeen minor elements. The rocks are placed in five groups:, (1) 2400 million year old group;, (2) Bacao complex younger, a group of mixed rocks...
R.G. Henderson
1960, Geophysics (25) 569-585
In the interpretation of magnetic and gravity anomalies, downward continuation of fields and calculation of first and second vertical derivatives of fields have been recognized as effective means for bringing into focus the latent diagnostic features of the data. A comprehensive system has been devised for the calculation of any or all of these...
W. I. Jensen, Jack P. Allen
1960, Conference Paper, Natural resources and american citizenship: Transactions of the twenty-fifth North American wildlife and natural resources conference
No abstract available....
G.H. Davis
1960, Bulletin of the Geological Society of America (71) 1727-1728
Hamilton (1959) concluded that in most sediments excess pore-water pressure is equal to zero - that is, the hydrostatic pressure is at atmospheric pressure. This note points out that in terrestrial environments the occurrence of artesian water (excess pore-water pressure) is commonplace and widespread and that such excess pressure is the...
M.W. Busby, M. A. Benson
1960, International Association of Scientific Hydrology - Bulletin (5) 32-36
The basin characteristics Σal or L ca are useful in hydrologic studies, but existing methods of determining them are either tedious or somewhat inaccurate. The grid method presented herein lessens the amount of tedious labor and provides an accurate measure of either Σal or L ca . An adaptation of the method could be used to compute the...
L. C. Pakiser
1960, Bulletin of the Geological Society of America (71) 153-160
In the Owens Valley region of California, volcanic activity of Cenozoic age was confined mainly to three areas near the ends of important faults. The volcanic eruptions seemingly took place in regions of relative tension, if the horizontal movement along these faults was left lateral. The deep depression of Owens Valley may have...
L. D. Clark
1960, Bulletin of the Geological Society of America (71) 483-496
A large fault system, here named the Foothills fault system, is the dominant structural feature of the western Sierra Nevada. The steeply dipping to vertical component faults trend northwestward through an area about 200 miles long and 30 miles wide north of 37°30' north latitude. The faulted Paleozoic and Mesozoic...