Surface water supply of the United States, 1931 : Part 11. Pacific slope basins in California
Water Resources Division, U.S. Geological Survey
1932, Water Supply Paper 721
Surface water supply of the United States, 1930, Part VIII, Western Gulf of Mexico basins
Water Resources Division, U.S. Geological Survey
1932, Water Supply Paper 703
Surface water supply of the United States, 1930, Part III, Ohio River basin
Water Resources Division, U.S. Geological Survey
1932, Water Supply Paper 698
Surface water supply of the United States, 1929, Part VIII, Western Gulf of Mexico basins
Water Resources Division, U.S. Geological Survey
1932, Water Supply Paper 688
Surface water supply of the United States, 1930, Part IX, Colorado River basin
Water Resources Division, U.S. Geological Survey
1932, Water Supply Paper 704
Geology and ground-water resources of the Dalles region, Oregon
A. M. Piper
1932, Water Supply Paper 659-B
No abstract available....
Outline of methods for estimating ground-water supplies
O. E. Meinzer
1932, Water Supply Paper 638-C
No abstract available....
A Miocene flora from Grand Coulee, Washington
E. W. Berry
1932, Professional Paper 170-C
Contributions to economic geology (short papers and preliminary reports), 1931-32 : Part II. - Mineral fuels
Hugh D. Miser
1932, Bulletin 831
No abstract available....
Geology and ore deposits of the Pioche district, Nevada
L.G. Westgate, Adolph Knopf
1932, Professional Paper 171
LOCATION AND SURFACE FEATURES The Bristol Range, Highland, and Ely Range quadrangles make up the larger part of a. rectangular area 35 miles north and south by 24 miles east and west, which lies 19 miles west of the Nevada-Utah line and about 250 miles southwest of Salt Lake...
Physiography and glacial geology of eastern Montana and adjacent areas
W. C. Alden
1932, Professional Paper 174
Quality of water of the Colorado River in 1928-1930
C. S. Howard
1932, Water Supply Paper 638-D
This report gives the results obtained in the continuation of a study of the Colorado River begun in 1925.1 The analyses represent composites of daily samples collected by the observers at the gaging stations on the Colorado River at Cisco, Utah, and Lees Ferry and Grand Canyon, Ariz.; on the...
Contributions to the hydrology of the United States 1931
Nathan C. Grover
1932, Water Supply Paper 638
No abstract available....
Surface water supply of the United States, 1929, Part II, South Atlantic slope and eastern Gulf of Mexico basins
Water Resources Division, U.S. Geological Survey
1932, Water Supply Paper 682
The Lake Clark-Mulchatna region
S. R. Capps
1932, Bulletin 824-C
No abstract available....
Mining in the Circle district
J.B. Mertie Jr.
1932, Bulletin 824-D
No abstract available....
Surface water supply of the United States, 1929, Part V, Hudson Bay and upper Mississippi River basin
Water Resources Division, U.S. Geological Survey
1932, Water Supply Paper 685
Surface water supply of the United States, 1929 : Part 10, The Great Basin
Water Resources Division, U.S. Geological Survey
1932, Water Supply Paper 690
Contributions to the hydrology of the United States, 1932
Nathan C. Grover
1932, Water Supply Paper 659
Relation of disease to wildlife cycles
R.G. Green, J.E. Shillinger
1932, Conference Paper, Transactions of the nineteenth American Game Conference
No abstract available....
On glaciers
F. E. Matthes
1932, Eos, Transactions, American Geophysical Union (13) 287
The changes in the sizes of glaciers has for long attracted the attention of glacialists on account of the scientific interest and the development of water‐power from the streams issuing from the glaciers.The International Congress of Geologists, at its Zurich meeting in 1894, appointed a committee, with members from many...
On underground water
David G. Thompson
1932, Eos, Transactions, American Geophysical Union (13) 298-305
No abstract available....
Investigations of the fluctuations of the ground‐water table in Pennsylvania
S.W. Lohman
1932, Eos, Transactions, American Geophysical Union (13) 373-375
Hydraulic engineers are interested in ground‐water as a source of water supply and also as it affects stream‐flow. The stream‐flow is especially valuable at low stages and it is at the low stages that it is most closely related to the ground‐water conditions. For several years the Pennsylvania Topographic and Geologic Survey and the United States Geological Survey have...
Recent investigations of Thiem's method for determining permeability of water‐bearing materials
L.K. Wenzel
1932, Eos, Transactions, American Geophysical Union (13) 313-317
This paper presents results obtained in an investigation of the ground-water resources of the Platte River Valley that is being conducted in cooperation between the Conservation and Survey Department of the University of Nebraska and the United States Geological Survey.Most quantitative ground-water studies are concerned with the amount of water...
Investigations of the fluctuations of water‐levels in observation‐wells in Virginia
R.C. Cady
1932, Eos, Transactions, American Geophysical Union (13) 370-373
An automatic water‐stage recorder has been maintained on an observation‐well in Arlington County, Virginia, about 1‐½ miles from the United States Weather Bureau, in Washington, D.C., since June, 1928, but there are a few interruptions in the record. This is a dug well, about 28 feet deep and extends through terrace deposits of gravelly silt or loam. It has not...