Reuben James Ross, William B. N. Berry
1963, Bulletin 1134
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Publication Extents
Not all publications have extents, not all extents are completely accurateA. M. Pommer
1963, Professional Paper 386-C
Water Resources Division, U.S. Geological Survey
1963, Bulletin 1155
Gilbert H. Espenshade
1963, Bulletin 1142-I
Water Resources Division, U.S. Geological Survey
1963, Professional Paper 475-A
B. R. Colby
1963, Bulletin 1181-A
This paper presents a broad but undetailed picture of fluvial sediments in streams, reservoirs, and lakes and includes a discussion of the processes involved in the movement of sediment by flowing water. Sediment is fragmental material that originates from the chemical or physical disintegration of rocks. The disintegration products may...
Max D. Crittenden Jr.
1963, Professional Paper 454-E
No abstract available....
David Marcel Larrabee
1963, Open-File Report 63-80
David Marcel Larrabee
1963, Open-File Report 63-81
Stanley Alfred Schumm
1963, Professional Paper 454-H
No abstract available....
D.A. Livingstone
1963, Professional Paper 440-G
C. L. Pillmore, W. J. Mapel
1963, Bulletin 1121-E
James Bachelder Cathcart
1963, Bulletin 1142-D
R. B. Colton, R.V. Cushman
1963, IMAP 402
James F. Pepper, Gail M. Everhart
1963, IMAP 380
The ocean realm, which covers more than 70 percent of the earth's surface, contains vast areas that have scarcely been touched by exploration. The best known parts of the sea floor lie close to the borders of the continents, where numerous soundings have been charted as an aid to navigation....
Watson Hiner Monroe
1963, Geologic Quadrangle 191
S. W. Lohman
1963, IMAP 404
J. R. Henderson, J. L. Vargo
1963, Geophysical Investigations Map 352
W.J. Dempsey, M. E. Hill
1963, Geophysical Investigations Map 419
No abstract available....
Leon F. Ramirez, E.L. Elberg Jr., H.H. Helley
1963, IMAP 219-A
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....
Charles Warren Merriam
1963, Professional Paper 408
The Inyo Mountains near Cerro Gordo comprise strongly folded and faulted sedimentary rocks ranging in age from Ordovician to Middle Triassic. These were intruded by granitic bodies, aplite dikes, and by innumerable andesitic and dacitic dikes of later age. Though largely nonfoliated, the sedimentary rocks have undergone varying degrees of...
Leonard Gene Schultz
1963, Bulletin 1147-C
L. A. Anderson, R. W. Bromery, N.S. Tyson
1963, Geophysical Investigations Map 376
Thomas E. Mullens, Glen Arthur Izett
1963, Geologic Quadrangle 185
Robert W. Schnabel
1963, Bulletin 1063-F