Surface water supply of the United States, 1933 : Part 12, North Pacific drainage basins ; B. Snake River basin
Water Resources Division, U.S. Geological Survey
1935, Water Supply Paper 753
Surface water supply of the United States, 1933 : Part 12, North Pacific drainage basins ; A. Pacific drainage basins in Washington and upper Columbia River basin
Water Resources Division, U.S. Geological Survey
1935, Water Supply Paper 752
No abstract available....
Geology and ground-water resources of Atascosa and Frio Counties, Texas
John T. Lonsdale
1935, Water Supply Paper 676
Atascosa and Frio Counties are in southwestern Texas and form a part of the Winter Garden district. The purpose of the investigation here recorded was to determine the source, quantity, and quality of the ground water used for irrigation and other purposes in the area....
Water utilization in the Snake River Basin
William Glenn Hoyt, Herman Stabler
1935, Water Supply Paper 657
The purpose of this report is to describe the present utilization of the water in the Snake River Basin with special reference to irrigation and power and to present essential facts concerning possible future utilization. No detailed plan of development is suggested. An attempt has been made, however, to discuss...
Geology of Big Horn County and the Crow Indian Reservation, Montana, with special reference to the water, coal, oil, and gas resources
William Taylor Thom Jr., George Martin Hall, Carroll H. Wegemann, G. F. Moulton
1935, Bulletin 856
No abstract available....
Surface water supply of the United States, 1933, IX, Colorado River basin
Water Resources Division, U.S. Geological Survey
1935, Water Supply Paper 749
Surface water supply of the United States, 1934 : Part 10, The Great Basin
Water Resources Division, U.S. Geological Survey
1935, Water Supply Paper 765
Ground water in part of southeastern Utah and southwestern Colorado
Gerald A. Waring, Maxwell M. Knechtel
1935, Open-File Report 35-1
No abstract available....
Surface water supply of the United States, 1934, Part VI, Missouri River basin
Water Resources Division, U.S. Geological Survey
1935, Water Supply Paper 761
Surface water supply of the United States, 1933, Part V, Hudson Bay and upper Mississippi River basin
Water Resources Division, U.S. Geological Survey
1935, Water Supply Paper 745
Surface water supply of the United States, 1933, Part II, South Atlantic slope and eastern Gulf of Mexico basins
Water Resources Division, U.S. Geological Survey
1935, Water Supply Paper 742
Geology and ground-water resources of the island of Oahu, Hawaii
Harold T. Stearns, Knute N. Vaksvik
1935, Bulletin 1
Oahu, one of the islands of the Hawaiian group, lies in the Mid-Pacific 2,100 miles southwest of San Francisco. The principal city is Honolulu. The Koolau Range makes up the eastern part of the island, and the Waianae Range the western part. Both are extinct basaltic volcanoes deeply dissected by...
Further tests of permeability with low hydraulic gradients
V.C. Fishel
1935, Eos, Transactions, American Geophysical Union (16) 499-503
Many of the water‐bearing formations in the United States have hydraulic gradients of much less than 20 feet to the mile, and some may have gradients of less than one foot to the mile, whereas most laboratory‐tests of permeability are made with much higher gradients. An investigation was therefore undertaken by the writer, under the direction of 0. E....
The Piezometric surface of artesian water in the Florida peninsula
V. T. Stringfield
1935, Eos, Transactions, American Geophysical Union (16) 524-529
The ground‐water of the Florida Peninsula constitutes one of its most valuable natural resources and is of importance as a source of water‐supplies throughout the area. The problems relating to the development of ground‐water supplies are both quantitative and qualitative. They include such problems as the decline in yield of wells in areas of large withdrawals of water and salt‐water contamination of ground‐water supplies. In order...
Bank storage‐loss and recovery of Missouri River discharge during drought of 1934
H.C. Beckman
1935, Eos, Transactions, American Geophysical Union (16) 513-515
Whenever measurements show that the discharge of a stream becomes smaller as it passes downstream to a considerably larger drainage-area and no diversions of water are known to exist between the places of measurement, curiosity is always aroused as to the cause, and a question may be raised as to...
Report of the Committee on Underground Waters, 1934–35
David G. Thompson
1935, Eos, Transactions, American Geophysical Union (16) 433-437
The annual report this year consists almost wholly of a brief summary of investigations in progress in different parts of the country. It is by no means complete, and the Chairman of the Committee will be glad to receive information in regard to investigations that have not been mentioned.The outstanding...
The need for a nation‐wide program of observation‐wells
O. E. Meinzer
1935, Eos, Transactions, American Geophysical Union (16) 498-499
During the severe droughts of recent years almost the only water‐supplies available throughout large areas of the United States have been those obtained from underground sources. Consequently, a great interest has developed in the ground‐water resources of the country and there has been much concern lest the declining water‐levels in wells and the diminished...
Appendix B—Active ground‐water projects in California, Oregon, and Washington
Arthur M. Piper
1935, Eos, Transactions, American Geophysical Union (16) 441-443
General Pumping from wells for irrigation—The Division of Irrigation, Bureau of Agricultural Engineering, United States Department of Agriculture, is investigating the economics and practice of pumping from wells for irrigation in the western United States. The study is under the...
Occurrence of enargite and wulfenite in ore deposits of northern Arkansas
E.T. McKnight
1935, Economic Geology (30) 61-66
One of the several contrasting features between zinc and lead deposits of the Mississippi Valley type and those of the Cordilleran type is the mineralogic simplicity of the Mississippi Valley ores. Because the usual ore and gangue minerals are few in kind and are those that can conceivably be carried...
Annotated bibliography and index of geology and water supply of the island of Oahu, Hawaii
Norah D. Stearns
1935, Bulletin 3
No abstract available...
Some general considerations of plankton and plankton problems with reference to water supplies
Hilary J. Deason
1935, Conference Paper, Papers presented at Ninth Annual Michigan Conference on Water Purification
No abstract available....
Stream measurement work: Appendix 4 in Nineteenth biennial report of the State Engineer to the governor of Utah: 1933-1934
A.B. Purton
1934, Utah State Engineer Biennial Report 19-Appendix 4
Stream measurement work under the usual co-operative agreement between the U.S. Geological Survey and the State Engineer continued during the biennium for the purpose of determining the water resources of the State. This work in Utah is part of the general plan for a systematic determination of the water resources...
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,...
Mineral-water supply of the Mineral Wells area, Texas
Samuel Foster Turner
1934, Circular 6
No abstract available....
Quicksilver deposits of southwestern Oregon
Francis Gerritt Wells, Aaron Clement Waters
1934, Bulletin 850