Surface water supply of the United States, 1932 : Part 12. North Pacific slope basins : A. Pacific slope basins in Washington and upper Columbia River basin
Water Resources Division, U.S. Geological Survey
1934, Water Supply Paper 737
Gold-quartz veins south of Libby, Montana
Russell Gibson
1934, Circular 7
The area described in this paper is one of rugged mountains, composed chiefly of folded and faulted sedimentary rocks of the Belt series. In the nearby region the beds are intruded by diorite sills and granitic stocks. Glacial drift, including silt deposited in a lake, covers much of the lower...
Artesian water in Somervell County, Texas
Albert George Fiedler
1934, Water Supply Paper 660
Somervell County is part of the Grand Prairie region of north-central Texas. An excellent supply of artesian water is available from the Trinity reservoir at no great depth. The first flowing well in Somervell County was drilled in 1880, and the first flowing well in Glen Rose, the county seat,...
Bibliography of North American geology, 1931 and 1932
John M. Nickles
1934, Bulletin 858
A flora of Pottsville age from the Mosquito Range, Colorado
C.B. Read
1934, Professional Paper 185-D
Core drilling for coal in the Moose Creek area, Alaska
Gerald Ashley Waring
1934, Bulletin 857-E
No abstract available....
The Curry district, Alaska
Ralph Tuck
1934, Bulletin 857-C
No abstract available....
Geology and ore deposits of the Breckenridge mining district, Colorado
T. S. Lovering
1934, Professional Paper 176
Surface water supply of Hawaii : July 1, 1931 to June 30, 1932
Nathan C. Grover, Max H. Carson
1934, Water Supply Paper 740
Paleozoic formations of the Mosquito Range, Colorado
J. H. Johnson
1934, Professional Paper 185-B
Mineral and fuel resources, report on progress of investigations in 1933. Mineral industry of Alaska in 1933
Philip Sidney Smith
1934, Bulletin 864-A
Surface water supply of the United States, 1932, Part I, North Atlantic slope basins
Water Resources Division, U.S. Geological Survey
1934, Water Supply Paper 726
Fifty-fifth annual report of the Director of the Geological Survey
Walter Curran Mendenhall
1934, Annual Report 55
From the point of view of the geologists of this continent, the important event of the year was the meeting in Washington, in July, of the sixteenth session of the International Geological Congress. The only other session held in the United States was the fifth, in 1891....
Geologic and structure contour map of the southern half of the Cedar Creek anticline, Fallon County, Montana and Bowman County, North Dakota
C. E. Dobbin, R. M. Larsen
1934, Report
No abstract available....
Progressive regional metamorphism of the lower kittanning coal bed of western Pennsylvania
T. Stadnichenko
1934, Economic Geology (29) 511-543
No abstract available. ...
Field evidence about the viscosity of lavas
Clarence S. Ross
1934, Eos, Transactions, American Geophysical Union (15) 255-257
There appears to be surprisingly little definite information on the viscosity of lavas. With few exceptions writers content themselves with such general and indefinite terms as “mobile”, “viscous”, or “highly viscous”. Apparently the only attempts to actually calculate viscosity have been made on Hawaiian lavas. ...
The Rôle of volatiles in the formation of Virginia titanium deposits
C. S. Ross
1934, Eos, Transactions, American Geophysical Union (15) 245-245
The feldspathic rock with which the titanium deposits of Virginia are associated appears to be an anorthosite, although the plagioclase is somewhat more sodic than in normal anorthosites. That is, this rock shows evidence of having been introduced as a mush‐like mass of crystals and intersititial magma, and of undergoing...
Relation of stream‐flow to ground‐water levels
L.L. Harrold
1934, Eos, Transactions, American Geophysical Union (15) 414-416
In recent years the Water Resources Branch of the United States Geological Surrey has given considerable attention to the relation of ground‐water to stream‐flow. One locality in which this relation is being studied is about 13 miles from Washington, near Colesvllle, Maryland, where a Kinnison float‐gage is being maintained in a well In connection with the operation of a...
A study of salt‐water encroachment in the Galveston Area, Texas
Samuel F. Turner, Margaret D. Foster
1934, Eos, Transactions, American Geophysical Union (15) 432-435
A survey of the ground‐water resources of the region in which Houston and Galveston are situated was started in December 1930 by the United States Geological Survey in cooperation with the Texas Board of Water Engineers. In connection with this survey a special study is being made of the geochemical relations of the ground‐waters of an area about 25 miles wide and 90 miles long, extending from Galveston northwestward through Houston. This study considers the influence...
Rare chemical constituents of amelia (Virginia) pegmatite dikes, and their mineral sources
Jewell J. Glass
1934, Eos, Transactions, American Geophysical Union (15) 234-237
Students of Igneous phenomena have long since become familiar with the occurrence of rare minerals in pegmatitic bodies. The great local concentration of rare elements in pegmatite minerals provides a remarkably good opportunity for the Investigation of deep-seated rock constituents, for it is reasonable to suppose that these same elements...
Report of the committee on underground‐water, 1933–34
D. G. Thompson
1934, Eos, Transactions, American Geophysical Union (15) 312-316
The by‐laws adopted at the meeting of the Section of Hydrology in 1933 provided that the membership of research committees should be reconstituted every three years. There have, accordingly, been some changes in the membership of the Committee on Underground‐Water. Certain members have retired because of pressure of other duties or because they are no...
The transmission of pressure in artesian aquifers
R.M. Leggette, G.H. Taylor
1934, Eos, Transactions, American Geophysical Union (15) 409-413
The water in artesian aquifers is confined under pressure. Under ideal conditions in a perfectly rigid artesian reservoir a change of pressure in one part of the reservoir should produce a corresponding change of pressure in all other parts of the reservoir. Theoretically, the transmission of pressure should take place rapidly and without any movement of water other than the small amount resulting from the compressibility of water. However,...
Ablation of snow‐fields at high altitudes by radiant solar heat
F. E. Matthes
1934, Eos, Transactions, American Geophysical Union (15) 380-385
Snow‐fields and the so‐called névés of glaciers on lofty mountains often present a peculiar, honeycombed appearance, the surface being pitted with deep cell‐like hollows a foot or two feet in diameter and from a few inches to several feet in depth. When typically developed these hollows are closely spaced, the divides...
Appendix A—permeability
O. E. Meinzer
1934, Eos, Transactions, American Geophysical Union (15) 316-317
In the paper entitled “The measurement of the permeability of porous media for homogeneous fluids” by R. D. Wyckoff and others [42] a unit of permeability is proposed which is based on centimeters, seconds, and atmospheres of pressure (76 centimeters of mercury).In 1923, when the Hydrologic Laboratory of the United...
Report of the committee on chemistry of natural waters, 1933–34
C. S. Howard
1934, Eos, Transactions, American Geophysical Union (15) 322-325
The personnel of this Committee during the past year, practically the same as during the previous year, has been as follows: C. S. Howard, Chairman—United States Geological Survey, Washington, D.C. L. C. Case—Gypsy Oil Company, Tulsa, Oklahoma. W. D. Collins—United States Geological Survey, Washington, D.C. H. F. Flynn—United States Engineer Office, 35...