The evolution and disintegration of matter
Frank Wigglesworth Clarke
1925, Professional Paper 132-D
In any attempt to study the evolution of matter it is necessary to begin with its simplest known forms, the so-called chemical elements. During a great part of the nineteenth century many philosophical chemists held a vague belief that these elements were not distinct entities but manifestations of one primal...
Temperature of water available for industrial use in the United States: Chapter F in Contributions to the hydrology of the United States, 1923-1924
W. D. Collins
1925, Water Supply Paper 520-F
The importance of water supply as a limiting factor in industrial development is becoming more evident each year. The limitation in a particular instance may be the quantity of water available, the quality determined by the mineral matter in solution or in suspension or by organic pollution, or the temperature...
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...
Contributions to the geography of the United States, 1923-1924. Pedestal rocks in stream channels
Kirk Bryan
1925, Bulletin 760-D
No abstract available....
Relations of the Wasatch and Green River formations in northwestern Colorado and southern Wyoming, with notes on oil shale in the Green River formation
J. D. Sears, W. H. Bradley
1925, Professional Paper 132-F
No abstract available....
Contributions to economic geology (short papers and preliminary reports), 1923-1924, Part II, Mineral fuels. Continuity of some oil-bearing sands of Colorado and Wyoming
W. T. Lee
1925, Bulletin 751-A
No abstract available....
Surface water supply of the United States, 1922, Part VII, Lower Mississippi River basin
Water Resources Division, U.S. Geological Survey
1925, Water Supply Paper 547
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,...
Water power and flood control of Colorado River below Green River, Utah
Eugene Clyde La Rue, Hubert Work, Nathan C. Grover
1925, Water Supply Paper 556
The purpose of this report is to present the facts regarding available water supply and all known dam sites on Colorado River between Cataract Canyon, Utah, and Parker, Ariz., and to show the relative value of these dam sites. To determine the relative value of the dam sites, a comprehensive...
Spirit leveling in California, 1896-1923: 36 degrees to 37 degrees latitude, 117 degrees to 118 degrees longitude
Claude Hale Birdseye
1925, Bulletin 766-AA
Spirit leveling in California, 1896-1923: 38 degrees to 39 degrees latitude, 121 degrees to 122 degrees longitude
Claude Hale Birdseye
1925, Bulletin 766-OO
Mineral resources of Alaska, report on progress of investigations in 1923. Alaska's mineral resources and production, 1923. An early Tertiary placer deposit in the Yentna District, Alaska. Mineral resources of Alaska, 1923; administrative report
Alfred H. Brooks, Stephen Reid Capps
1925, Bulletin 773-A
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
Spirit leveling in California, 1896-1923: 37 degrees to 38 degrees latitude, 120 degrees to 121 degrees longitude
Claude Hale Birdseye
1925, Bulletin 766-II
Contributions to economic geology (short papers and preliminary reports), 1923-1924, Part I, Metals and nonmetals except fuels. New and known minerals from the Utah-Colorado carnotite region
F. L. Hess
1925, Bulletin 750-D
Spirit leveling in California, 1896-1923: 34 degrees to 35 degrees latitude, 115 degrees to 116 degrees longitude
Claude Hale Birdseye
1925, Bulletin 766-L
Contributions to economic geology (short papers and preliminary reports), 1923-1924: Part II. - Mineral fuels
K. C. Heald, W. T. Thom Jr.
1925, Bulletin 751
Contributions to economic geology (short papers and preliminary reports), 1923-1924, Part II, Mineral fuels. Geologic structure of San Juan Canyon and adjacent country, Utah
H. D. Miser
1925, Bulletin 751-D
No abstract available....
Spirit leveling in California, 1896-1923: 37 degrees to 38 degrees latitude, 122 degrees to 123 degrees longitude
Claude Hale Birdseye
1925, Bulletin 766-KK
Spirit leveling in California, 1896-1923: 38 degrees to 39 degrees latitude, 118 degrees to 119 degrees longitude
Claude Hale Birdseye
1925, Bulletin 766-LL
Spirit leveling in California, 1896-1923: 38 degrees to 39 degrees latitude, 119 degrees to 120 degrees longitude
Claude Hale Birdseye
1925, Bulletin 766-MM
Spirit leveling in California, 1896-1923: 37 degrees to 38 degrees latitude, 118 degrees to 119 degrees longitude
Claude Hale Birdseye
1925, Bulletin 766-GG
Spirit leveling in California, 1896-1923: 37 degrees to 38 degrees latitude, 119 degrees to 120 degrees longitude
Claude Hale Birdseye
1925, Bulletin 766-HH
Spirit leveling in California, 1896-1923: 33 degrees to 34 degrees latitude, 118 degrees to 119 degrees longitude
Claude Hale Birdseye
1925, Bulletin 766-J
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
