Water levels and artesian pressures in observation wells in the United States, 1950, Part 1, Northeastern States
Water Resources Division, U.S. Geological Survey
1953, Water Supply Paper 1165
Water levels and artesian pressures in observation wells in the United States, 1950, Part 2, Southeastern States
Water Resources Division, U.S. Geological Survey
1953, Water Supply Paper 1166
Water levels and artesian pressures in observation wells in the United States, 1950, Part 6, Southwestern States and Hawaii
Water Resources Division, U.S. Geological Survey
1953, Water Supply Paper 1170
Ground-water conditions in the Milwaukee-Waukesha area, Wisconsin
Frank Clingan Foley, W.C. Walton, W.J. Drescher
1953, Water Supply Paper 1229
Three major aquifers underlie the Milwaukee-Waukesha area: sandstones of Cambrian and Ordovician age, Niagara dolomite of Silurian age, and sand and gravel deposits of Pleistocene age. The Maquoketa shale of Ordovician age acts as a more or less effective seal between the Pleistocene deposits and Niagara dolomite above and the...
Surface water supply of the United States, 1950, Part XIII, Snake River basin
Water Resources Division, U.S. Geological Survey
1953, Water Supply Paper 1183
Irrigation and streamflow depletion in Columbia River basin above The Dalles, Oregon
Wilbur Douglas Simons
1953, Water Supply Paper 1220
The Columbia River is the largest stream in western United States. Above The Dalles, Oregon, it drains an area of 237,000 square miles, of which 39,000 square miles is in Canada. This area is largely mountainous and lies between the Rocky Mountains and the Cascade Range. The Kootenai, Pend Oreille,...
Geology and ground-water resources of the Egbert-Pine Bluffs-Carpenter area, Laramie County, Wyoming
J. R. Rapp, D. A. Warner, Arthur Mitchell Morgan
1953, Water Supply Paper 1140
No abstract available....
Surface water supply of the United States, 1950, Part VI, Missouri River basin
Water Resources Division, U.S. Geological Survey
1953, Water Supply Paper 1176
Quality of surface waters of the United States, 1949 : Parts 1 -6
C. G. Paulsen
1953, Water Supply Paper 1162
Quality of surface waters of the United States, 1949 : Parts 7 -14
Water Resources Division, U.S. Geological Survey
1953, Water Supply Paper 1163
Surface water supply of the United States, 1950, Part 12, Pacific slope basins in Washington and upper Columbia River basin
Carl Gustave Paulsen
1953, Water Supply Paper 1182
Surface water-supply of the United States, 1951, Part II-A, South Atlantic slope and eastern Gulf of Mexico basins, James River to Savannah River
Water Resources Division, U.S. Geological Survey
1953, Water Supply Paper 1203
Stratigraphic relationships of Cretaceous and early Tertiary rocks of a part of northwestern San Juan basin
Elmer Harold Baltz Jr.
1953, Open-File Report 53-8
The Bridge Timber Mountain area in south-central La Plata County, southwestern Colorado lies mostly in the northwestern part of the Central San Juan Basin but contains a segment of the bounding Hogback 'monocline' and Four-Corners platform. The area contains rocks of late Cretaceous through early Eocene age, as well as...
Water, frost, and frost resistance of natural and artificial building stones
H. Breyer, S. H. Britt (translator)
1953, Open-File Report 54-33
The worst enemy of construction engineering and of construction material is uncontrollable water, whether it be ground-, seepage-, rainwater, water of condensation, or melting snow and ice, exerting objectionable pressure upon tracks and roads. this applies as well to structures above the ground as to bridge piers and foundations, road...
Stratigraphy and structure of the Miners Mountain area, Wayne County, Utah
Robert G. Luedke
1953, Open-File Report 53-161
The Miners Mountain area includes about 85 square miles in Wayne County, south-central Utah. The area is semiarid and characterized by cliffs and deep canyons. Formations range in age from Permian to Upper Jurassic and have an aggregate thickness of about 3,500 feet. Permian formations are the buff Coconino sandstone and...
Marine geology of the Near Islands Shelf, Alaska
Philip Challacombe Scruton
1953, Open-File Report 53-245
During the summer of 1950 on the insular shelf surrounding the Near Islands, Alaska, 193 oceanographic stations were occupied from aboard the U. S. Geological Survey vessel EIDER. Bottom character and temperature observations were made at these stations. The composition and size distribution characteristics of the bottom samples have been...
Public and industrial water supplies of the Jackson Purchase region, Kentucky
Henry Louis Pree, William Harry Walker
1953, Circular 287
The industrial utility of public water supplies in the New England States, 1952
E. W. Lohr, Walter Finch White
1953, Circular 288
The industrial utility of public water supplies in the South Atlantic States, 1952
E. W. Lohr, F. H. Pauszek, P.G. Connor, W.L. Lamar, E.F. McCarren
1953, Circular 269
Potential industrial sites in the Lynn Canal area, Alaska
Arthur Johnson, William Stephens Twenhofel
1953, Circular 280
Full development of a proposal to divert the headwaters of the Yukon River drainage from Canada into the Taiya River valley of Alaska would make available more than a half million kilowatts of electrical energy. Utilization of this block of power, for which there is at present no local market,...
Sedimentation in small reservoirs on the San Rafael Swell, Utah
Norman Julius King, Mervyn M. Mace
1953, Circular 256
Movement of sediment from upland areas and eventually into main drainages and rivers is by no means through continuous transportation of material from the source to the delta. Instead it consists of a series of intermittent erosional and depositional phases that present a pulsating movement. Hence, sediment carried off upland...
Water-power resources of Crystal River, Colorado
Fred Forrest Lawrence
1953, Circular 292
The Crystal River drains the western slope of the Elk Mountains, a relatively small range in the southern Rocky Mountain province, and flows into the Roaring Fork 13 miles southeast of Glenwood Springs, Colo. The lower 7 miles of the valley is cultivated, but upstream from this stretch the valley...
Annotated bibliography of U.S. Geological Survey reports on water-power resources, including floods and droughts
Loyd L. Young, Benjamin Earl Jones
1953, Circular 200
Occurrence and development of ground water in permafrost regions
Dagfin John Cederstrom, Paul McKelvey Johnston, Seymour Subitzky
1953, Circular 275
Chemical quality of water and sedimentation in the Moreau River drainage basin, South Dakota
Bruce R. Colby, C. H. Hembree, E. R. Jochens
1953, Circular 270
This report gives the results of an investigation by the U. S. Geological Survey of the sediments and dissolved minerals that are transported by the Moreau River. The Moreau River drainage basin is a narrow basin in northwestern South Dakota that covers about 5, 360 square miles of rolling, grassy plains,...