Appendix E—List of current publications concerning ground water
Jean M. Berdan
1946, Eos, Transactions, American Geophysical Union (27) 274-278
Alexander, W. H., Jr., Broadhurst, W. L., and White, W. N., Progress report on ground water In the High Plains in Texas, Tex. State Bd. Water Engrs., 12 pp., 7 tigs. (mimeogranhedl May 1944.Ashley, George H.,and Graham, Jack B., Groundwater investigations in Pennsylvania Pa. Dep. Internal Affairs, Monthly Bull., v....
Report of Committee on Ground Water—1944–1945
S. W. Lohman
1946, Eos, Transactions, American Geophysical Union (27) 236-245
Because of war‐imposed responsibilities of most agencies and individuals this year, no new programs were undertaken by the Committee, but the work of the Subcommittee on Permeability was continued, and a substantial progress report by C. E. Jacob, Acting Chairman, and by members of this Subcommittee follows this report as...
Report of the Research Committee on Runoff, 1945–46
R. W. Davenport
1946, Eos, Transactions, American Geophysical Union (27) 876-878
The variety of usage and even the confusion in the nomenclature and terminology of some fields of hydrology have been often remarked. The Committee on Runoff conceived the idea that it would be profitable to consider some of the terms which are especially pertinent to the field of runoff. That...
A generalized graphical method for evaluating formation constants and summarizing well‐field history
H.H. Cooper, C. E. Jacob
1946, Eos, Transactions, American Geophysical Union (27) 526-534
The capacities of a water‐bearing formation to transmit water under a hydraulic gradient and to yield water from storage when the water table or artesian pressure declines, are generally expressed, respectively, in terms of a coefficient of transmissibility and a coefficient of storage. Determinations of these two constants are almost...
General principles of artificial ground-water recharge
O. E. Meinzer
1946, Economic Geology (41) 191-201
The natural subterranean reservoirs formed by the porous and permeable rocks differ from surface reservoirs chiefly in that they have complex structure and great internal resistanc• to the How of water. Their full utilization requires systematic development based on the geology and hydrology of the aquifer and the principles of...
Artificial recharge of artesian limestone at Orlando, Florida
A.G. Unklesbay, H.H. Cooper
1946, Economic Geology (41) 293-307
The principal aquifer in the Orlando area consists of 900 feet or more of permeable artesian limestones of upper and middle Eocene age. As in most other parts of the Florida peninsula, these limestones are overlain by the Hawthorn formation of Miocene age which contains relatively impervious beds. The Hawthorn...
Artificial recharge of glacial sand and gravel with filtered river water at Louisville, Kentucky
W.F. Guyton
1946, Economic Geology (41) 644-658
Records obtained by the Geological Survey, United States Department of the Interior, and the Geological Division, Kentucky Department of Mines and Minerals, indicate that industries at Louisville pumped about 62 million gallons of water per day from wells in 1943. This was over 20 million gallons a day more than...
Artificial recharge of productive ground-water aquifers in New Jersey
H.C. Barksdale, G.D. DeBuchananne
1946, Economic Geology (41) 726-737
Artificial recharge by water spreading is practiced in several places in New Jersey. Rates of recharge ranging from 3,000 to 125,000 gallons per acre per day have been measured at the Perth Amboy Water Works, where artificial recharge of the Old Bridge sand, of upper Cretaceous age, has been practiced...
Ground water in the Fargo-Moorhead area, North Dakota and Minnesota
A.C. Byers, L.K. Wenzel, Wilson M. Laird, P.E. Dennis
1946, Report
No abstract available....
Ground-water resources of the southwestern part of the Louisville area, Kentucky
Matthew Irvin Rorabaugh
1946, Report
No abstract available....
Geology and ground-water resources of the island of Hawaii
Harold T. Stearns, Gordon A. Macdonald
1946, Bulletin 9
Hawaii, the largest island in the Hawaiian group, is 93 miles long, 76 miles wide, and covers 4,030 square miles. Mauna Loa Volcano is 13,680 feet high and Mauna Kea is 13,784 feet high. Plate 1 shows the geology, wells, springs, and water-development tunnels. Plate 2 is a map and...
Ground water in beach deposits of glacial Lake Agassiz near Mountain, Pembina County, North Dakota
P.D. Akin
1946, North Dakota Ground Water Studies 2
No abstract available....
Industrial limestones and dolomites in Virginia: northern and central parts of the Shenandoah Valley
R.S. Edmundson
1945, Book, Virginia Division of Mineral Resources Bulletin
The area described in this report includes the northern and central parts of Shenandoah Valley in Virginia extending from the West Virginia line southwestward to the vicinity of Greenville, Augusta County. It contains extensive deposits of high-calcium limestone averaging more than 97 per cent calcium carbonate. The Mosheim limestone, composed...
The Ogden Valley artesian reservoir
H. E. Thomas
1945, Technical Publication 2
Ogden Valley, in Weber County, Utah, contains an artesian reservoir from which the city of Ogden obtains all except a small part of its municipal water supply. A detailed investigation of the ground-water resources of Ogden Valley, and particularly of this artesian reservoir, was made by the Geological Survey, United...
Columnaris as a disease of cold-water fishes
1945, Transactions of the American Entomological Society (73) 32-36
A natural outbreak of columnaris disease among wild adult and hatchery-reared fingerling salmon in the State of Washington is described. The disease is identified by the recovery of the causative organism, Bacillus columnaris Davis, which may be readily identified by its characteristic action in forming columns on the surfaces of...
Record of wells in Suffolk County, N.Y., Supplement 1
C.M. Roberts, M.L. Brashears Jr.
1945, Bulletin GW-9
Correlation of ground-water levels and precipitation on Long Island, New York
C. E. Jacob
1945, Bulletin GW-14
No abstract available....
The water table in the western and central parts of Long Island, New York
C. E. Jacob
1945, Bulletin GW-12
Geology and ground-water resources of Thomas County, Kansas
J.C. Frye
1945, Kansas Geological Survey Bulletin (59)
Some recent publications on management and propagation of waterfowl
R. B. Nestler
1945, Wildlife Leaflet 267
No abstract available....
Plant-food resources for waterfowl in the Pacific Northwest
T.H. Scheffer, N. Hotchkiss
1945, Washington Department of Game, Biological Bulletin No. 7
The aquatic and marsh vegetation of Minnesota and its value to waterfowl
J.B. Moyle, N. Hotchkiss
1945, Technical Bulletin No. 3.
Water facts for Oklahoma
Water Resources Division, U.S. Geological Survey
1945, Open-File Report 45-110
Water descends from the clouds, and forms rivers, lakes, and seas. It is delivered to the earth absolutely free, not in accordance with man-made specifications or orders but at the caprice of the elements. Hence man to realize fully the benefits of this incomparable and recurring resource must have full...
Water utilization in the Nooksack River, Washington
R.O. Helland
1945, Open-File Report 45-24
The primary purpose of the investigation of the water resources of the Nooksack River was land classification. The Nooksack basin lies largely within the Mt. Baker National Forest and a considerable area of public lands will be involved in any plan for the ultimate development of its water power. Surveys on a scale of 1:24,000...
Water levels and artesian pressure in observation wells in the United States, 1943, Part 6, Southwestern States and Hawaii
Water Resources Division, U.S. Geological Survey
1945, Water Supply Paper 991
