Elver J. McClelland
1964, Open-File Report 64-168
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Page 6004, results 150076 - 150100
Publication Extents
Not all publications have extents, not all extents are completely accurateG.E. Becraft
1964, Miscellaneous Field Studies Map 283
Joseph Edwin Upson, Charles Winthrop Spencer
1964, Professional Paper 454-M
No abstract available....
D.L. Durham, R. F. Yerkes
1964, Professional Paper 420-B
Manuel G. Bonilla
1964, Open-File Report 64-16
No abstract available....
Henry Rowland Cornwall, Frank J. Kleinhampl
1964, Professional Paper 454-J
No abstract available....
T. W. Dibblee Jr.
1964, IMAP 427
James Franklin McAllister
1964, Open-File Report 64-108
No abstract available....
T. W. Dibblee Jr.
1964, IMAP 431
Patrick James Barosh
1964, Open-File Report 64-10
The Permian section near Ely, Nevada, consists of, in ascending order: Riepe Spring Limestone, a bluff-forming limestone with abundant corals, and Reipetown Sandstone, a buff to red very coarse-grained siltstone with minor carbonates, both formations of Steele (1960); Arcturus Formation, divisible into a Lower Member composed of alternating medium-bedded limestone...
B. F. Leonard, A. F. Buddington
1964, Professional Paper 377
R. F. Yerkes, Russell H. Campbell, J. E. Schoellhamer
1964, Open-File Report 64-166
No abstract available....
T. W. Dibblee Jr.
1964, IMAP 426
T. W. Dibblee Jr.
1964, IMAP 430
No abstract available....
Charles Brian Read, Sergius H. Mamay, Grace C. Keroher
1964, Professional Paper 454-K
No abstract available....
U.S. Geological Survey
1964, Report
The United States Geological Survey was established by Congress in 1879 to make a systematic study of the geology and natural resources of the United States. To provide the essential base maps for these studies, the Survey immediately began a program of topographic mapping. In 1882 a general plan was adopted for a standard series...
Water Resources Division, U.S. Geological Survey
1964, Report
The surface-water records for the 1964 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of Indiana are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering States. The records were collected and computed by the...
C. F. Withington
1964, Report
No abstract available....
C. A. Kaye, E.S. Barghoorn
1964, Geological Society of America Bulletin (75) 63-80
The compression of peat beneath its own weight (autocompaction) is discussed, and it is shown that because of this process radiocarbondated samples of salt-marsh peat or peaty sediment, other than very thin samples cut from the base of the deposit, cannot be correlated with sea level without construction of a...
C. A. Kaye
1964, Geological Society of America Bulletin (75) 233-236
Pebbles of silicified gymnospermous wood occur widely in the drift of southeastern Massachusetts. An investigation of the distribution of these pebbles shows the bedrock source of the wood to be tuffaceous beds that apparently overlie older granite in the Middleboro-Plympton area, Massachusetts, and are at the base of the Carboniferous...
L. Marek, E. L. Yochelson
1964, Science (146) 1674-1675
An unusually well-preserved Ordovician fossil from Czechoslovakia shows that the enigmatic paired structures once thought to be outgrowths of the operculum of Hyolithes are really independent structures lying between the operculum and the aperture of the shell. The find seems to provide conclusive proof of the morphologic uniqueness of hyolithids....
Vernon J. Hurst
1964, Report
White County is in the Northeast Georgia Highland. It comprises 243 square miles and has abouit 7,000 Inhabitants. The county seat is Cleveland.Although the scene of considerable mining activity in the past, White County now has few operating mines: a small production of clay1 for the manufacture of miscellaneous potter...
U.S. Bureau of Sport Fisheries and Wildlife
1964, Wildlife Leaflet 464
No abstract available....
U.S. Bureau of Sport Fisheries and Wildlife
1964, Wildlife Leaflet 463
No abstract available....
J.W. Allingham
1964, Geophysics (29) 537-552
This study shows that aeromagnetic anomalies of less than 200 gammas are associated with topographic relief of exposed Precambrian granitic and volcanic rocks of the St. François Mountains. Anomalies resulting from hills coarsely crystalline granite are as high as 100 gammas in amplitude, whereas anomalies over comparable hills of fine-grained rocks, such as granophyre or devitrified volcanic rock, are...