Spirit leveling in California, 1896-1923: 36 degrees to 37 degrees latitude, 119 degrees to 120 degrees longitude
Claude Hale Birdseye
1925, Bulletin 766-CC
Spirit leveling in California, 1896-1923: 37 degrees to 38 degrees latitude, 117 degrees to 118 degrees longitude
Claude Hale Birdseye
1925, Bulletin 766-FF
Spirit leveling in California, 1896-1923: 36 degrees to 37 degrees latitude, 120 degrees to 121 degrees longitude
Claude Hale Birdseye
1925, Bulletin 766-DD
Spirit leveling in California, 1896-1923: 36 degrees to 37 degrees latitude, 121 degrees to 122 degrees longitude
Claude Hale Birdseye
1925, Bulletin 766-EE
Mineral resources of Alaska: Report on progress of investigations in 1923
Alfred H. Brooks
1925, Bulletin 773
No abstract available....
Spirit leveling in California, 1896-1923: 40 degrees to 41 degrees latitude, 122 degrees to 123 degrees longitude
Claude Hale Birdseye
1925, Bulletin 766-UU
Spirit leveling in California, 1896-1923: 40 degrees to 41 degrees latitude, 123 degrees to 124 degrees longitude
Claude Hale Birdseye
1925, Bulletin 766-VV
Spirit leveling in California, 1896-1923: 40 degrees to 41 degrees latitude, 124 degrees to 125 degrees longitude
Claude Hale Birdseye
1925, Bulletin 766-WW
Continuity of some oil-bearing sands of Colorado and Wyoming
W. T. Lee
1925, Bulletin 751-A
No abstract available....
Water power and irrigation in the Madison River basin, Montana
J.F. Deeds, W. N. White
1925, Water Supply Paper 560-A
Additional ground-water supplies for the city of Enid, Oklahoma
B. C. Renick
1925, Water Supply Paper 520-B
Power resources of Snake River between Huntington, Oregon and Lewiston, Idaho: Chapter C in Contributions to the hydrology of the United States, 1923-1924
William Glenn Hoyt
1925, Water Supply Paper 520-C
Thousands of people are familiar with that part of Snake River where it flows for more than 300 miles in a general westward course across the plains of southern Idaho, but few have traversed the river where it flows northward and for 200 miles forms the boundary between Idaho and...
The artesian water supply of the Dakota sandstone in North Dakota, with special reference to the Edgeley quadrangle
Oscar E. Meinzer, Herbert A. Hard
1925, Water Supply Paper 520-E
The Dakota sandstone and the overlying dense plastic shales form the most remarkable artesian basin in the United States with respect to its great extent, the long distances through which its water has percolated from the outcrops of the sandstone in the western mountains to the areas of artesian flow,...
Some floods in the Rocky Mountain region: Chapter G in Contributions to the hydrology of the United States, 1923-1924
Robert Follansbee, Paul V. Hodges
1925, Water Supply Paper 520-G
In 1923 severe floods occurred on the larger streams in Wyoming and a number of cloudburst floods on small streams in Wyoming and especially in Colorado. An investigation of the principal floods in each State was made, and the results are given in this paper, together with descriptions of two...
Index of analyses of natural waters in the United States
W. D. Collins, C. S. Howard
1925, Water Supply Paper 560-C
Variation in annual run-off in the Rocky Mountain region: Chapter A in Contributions to the hydrology of the United States, 1923-1924
Robert Follansbee
1925, Water Supply Paper 520-A
Records of run-off in the Rocky Mountain States since the nineties and for a few stations since the eighties afford a means of studying the variation in the annual run-off in this region. The data presented in this report show that the variation in annual run-off differs in different areas...
Discovery of a Balkan fresh-water fauna in the Idaho formation of Snake River Valley, Idaho
W.H. Dall
1925, Professional Paper 132-G
In 1866 Gabb described Melania taylori and Lithasia antiqua "from a fresh-water deposit on Snake River, Idaho Territory, on the road from Fort Boise to the Owyhee mining country. Collected by A. Taylor." He states that a small bivalve, perhaps a Sphaerium, was associated with them....
Origin of the boghead coals
Reinhardt Thiessen
1925, Professional Paper 132-I
The bituminous rocks of sedimentary origin may be classified roughly under two main heads - coals and bituminous shales. In a strict sense no definite line can be drawn between these two groups, because coals may be insensibly grade into bituminous shales. Chemically the boghead coals are preeminently bituminous....
A new fauna from the Colorado group of southern Montana
John B. Reeside Jr.
1925, Professional Paper 132-B
This paper describes a small but interesting fauna collected in 1921 by W. T. Thorn, Jr., Gail F. Moulton, T. W. Stanton, and K. C. Heald in the Crow Indian Reservation in southern Montana. The locality is in sec. 36, T. 6 S., R. 32 E., Big Horn County, and...
Surface water supply of the United States, 1921, Part IX, Colorado River basin
Water Resources Division, U.S. Geological Survey
1925, Water Supply Paper 529
Surface water supply of the New-Kanawha River basin, West Virginia, Virginia, and North Carolina
N.C. Grover, Albert Howard Horton, Guy Clarke Stevens
1925, Water Supply Paper 536
Contributions to the hydrology of the United States, 1925
Nathan Clifford Grover
1925, Water Supply Paper 560
Contributions to the hydrology of the United States, 1923-1924
Nathan Clifford Grover
1925, Water Supply Paper 520
Geology and possible oil and gas resources of the faulted area south of the Bearpaw Mountains, Montana
Frank Reeves
1925, Bulletin 751-C
No abstract available....
Contributions to economic geology (short papers and preliminary reports), 1923-1924, Part I, Metals and nonmetals except fuels. Deposits of magnesia alum near Fallon, Nevada
D. F. Hewett
1925, Bulletin 750-E