Lester Hood Woolsey, Ralph Webster Richards, Charles Thomas Lupton
1917, Bulletin 647
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184617 results.
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Page 7289, results 182201 - 182225
Publication Extents
Not all publications have extents, not all extents are completely accurateF. C. Calkins
1917, Bulletin 640-D
No abstract available....
T. W. Stanton
1917, Professional Paper 98-R
C.J. Hares
1917, Bulletin 641-I
No abstract available....
V. H. Barnett
1917, Bulletin 641-H
No abstract available....
O. B. Hopkins
1917, Bulletin 641-D
No abstract available....
E. L. Jones Jr.
1917, Bulletin 640-E
No abstract available....
A.E. Fath
1917, Bulletin 641-E
No abstract available....
W. R. Calvert
1917, Bulletin 641-G
No abstract available....
D. E. Winchester
1917, Bulletin 641-F
No abstract available....
Eugene Stebinger
1917, Bulletin 641-C
No abstract available....
J. T. Pardee
1917, Bulletin 640-K
No abstract available....
Adolph Knopf
1917, Bulletin 640-G
No abstract available....
F. W. Clarke, W. C. Wheeler
1917, Professional Paper 102
Water Resources Division, U.S. Geological Survey
1917, Water Supply Paper 406
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....
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...
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...
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...
A.C. Spencer
1917, Professional Paper 96
No abstract available....
D. Dale Condit
1917, Professional Paper 98-O
The information set forth in this chapter was obtained in field work during the seasons of 1913 and 1915. During 1913 the writer was engaged in the detailed mapping of the phosphate beds of the Ember formation on the northeast slope of the Wind River Mountains and in the Owl...
Charles W. Gilmore
1917, Professional Paper 98-Q
The presence of dinosaurian fossil remains near Ojo Alamo, in the northwestern part of the San Juan Basin, N.Mex., was first reported by George Pepper, of the Hyde Exploring Expedition, in 1902....
M. R. Campbell
1917, Professional Paper 100-A
No abstract available....
F. H. Knowlton
1917, Professional Paper 108-F
This paper deals with a small but important fossil flora, now known to be of Colorado age, from the vicinity of Cumberland, Lincoln County, Wyo. It was for many years thought to be of Jurassic age, and only within the last decade has its stratigraphic position been established. Although small...
Water Resources Division, U.S. Geological Survey
1917, Water Supply Paper 407