C. E. Meinzer
1918, Journal of the Washington Academy of Sciences (8) 411-412
No abstract available....
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Publication Extents
Not all publications have extents, not all extents are completely accurateArthur Jackson Ellis
1917, Water Supply Paper 416
The use of a forked twig, or so-called divining rod, in locating minerals, finding hidden treasure, or detecting criminals is a curious superstition that has been a subject of discussion since the middle of the sixteenth century and still has a strong hold on the popular mind, even in this...
V. H. Barnett
1917, Bulletin 641-H
No abstract available....
Robert Bradford Marshall
1917, Bulletin 654
C.J. Hares
1917, Bulletin 641-I
No abstract available....
J. A. Bownocker, F. R. Clark
1917, Professional Paper 100-B
No abstract available....
H.S. Washington
1917, Professional Paper 99
Water Resources Division, U.S. Geological Survey
1917, Water Supply Paper 434
Gaillard Sherburne Rogers
1917, Bulletin 653
Adolph Knopf
1917, Bulletin 640-G
No abstract available....
E. L. Jones Jr.
1917, Bulletin 640-E
No abstract available....
D. E. Winchester
1917, Bulletin 641-F
No abstract available....
W. R. Calvert
1917, Bulletin 641-G
No abstract available....
A.E. Fath
1917, Bulletin 641-E
No abstract available....
O. B. Hopkins
1917, Bulletin 641-D
No abstract available....
J. T. Pardee
1917, Bulletin 640-K
No abstract available....
W. T. Lee, F. H. Knowlton
1917, Professional Paper 101
No abstract available....
Charles W. Gilmore
1917, Professional Paper 103
The fossils on which this paper is based were collected by me and my assistant, Mr. J. F. Strayrer, during the summer of 1913, while working under the auspices of the United States Geological Survey on the Blackfeet Indian Reservation, in northwestern Montana. The specimens were obtained from exposures of...
Carroll H. Wegemann
1917, Professional Paper 108-D
Northeastern Wyoming is occupied by a broad structural basin opening to the north and bounded on the east, south, and west by three mountain uplifts - the Black Hills, the Laramie Mountains, and the Big Horn Mountains. (See fig. 16.) Throughout much of this basin the surface rocks are of...
Edward Wilber Berry
1917, Professional Paper 108-E
The presence of erosion intervals at several horizons in the Eocene of the Gulf States has been pointed out in a recent paper, and the evidence of an erosion interval between the period of deposition of the sediments of the Wilcox group (lower Eocene) and that of the Claiborne group...
G. R. Mansfield, P. V. Roundy
1917, Professional Paper 98-G
In the detailed geologic mapping of the Wayan and Montpelier quadrangles, in south-eastern Idaho and adjacent territory, it has been found necessary to apply new names to strata hitherto referred to the Beckwith and Bear River formations or to portions of the Laramie as mapped by the Hayden Survey. The...
L. F. Noble, J. Fred Hunter
1917, Professional Paper 98-I
The field work upon which this article is based was done in March and April, 1914. From Garnet Canyon, near the west end of the Granite Gorge, the route followed the Tonto trail along the so-called lower plateau, or Tonto platform, to Red Canyon, at the east end of the...
M. R. Campbell
1917, Professional Paper 100-A
No abstract available....
Bertrand L. Johnson
1917, Professional Paper 98-C
The Barry Glacier, in the northwest corner of Prince William Sound (fig. 6), was first described by Glenn, Castner, and Mendenhall. It was more extensively studied by the Harriman Alaska expedition in 1899; by Grant in 1905; by Grant and Higgens in 1908 and 1909; and by Martin in 1910....
W.B. Hicks
1917, Professional Paper 98-A
The bed of crystalline salts known as Searles Lake, in southeastern California, contains the most valuable potash-bearing brine known in the United States. This salt body has an exposed surface area estimated at 11 or 12 square miles and an average depth of about 70 feet. For the most part...