Geologic map of the Smelterville and vicinity quadrangle, Idaho
Water Resources Division, U.S. Geological Survey
1953, Open-File Report 53-29
No abstract available. ...
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...
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....
Geology and geography of the Henry Mountains region, Utah
Charles B. Hunt, Paul Averitt, Ralph L. Miller
1953, Professional Paper 228
The Henry Mountains region in southeastern Utah is one of the classic areas in geology because of the study made there by Grove Karl Gilbert in 1875 and 1876. His report on the geology of the mountains was the first to recognize that intrusive bodies may deform their host rocks...
A geologic and geophysical reconnaissance of the Doney Park-Black Bill Park area, Arizona, with reference to ground water, with a section on geophysics
John Henry Frederick Feth, Coyd Bickley Yost
1953, Circular 233
No abstract available....
Trace elements research quarterly progress report - April 1 to June 30, 1952
Water Resources Division, U.S. Geological Survey
1953, Trace Elements Investigations 280
General availability of ground water and depth to water level in the Arkansas, White, and Red River basins
Stanley William Lohman, V. M. Burtis
1953, Hydrologic Atlas 3
No abstract available....
Areas of principal ground-water investigations in the Arkansas, White, and Red River basins
Stanley William Lohman, V. M. Burtis
1953, Hydrologic Atlas 2
Low-water study, Gasconade River basin, Missouri
Harry C. Bolon
1953, Open-File Report 53-24
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...
The molybdenum blue reaction and the determination of phosphorus in waters containing arsenic, silicon, and germanium
Harry Levine, Jack James Rowe, F. S. Grimaldi
1953, Trace Elements Investigations 379
A brief report on the progress of the Manatee County, Florida, ground-water investigation
R.B. Anders, R.C. Heath
1953, Open-File Report 53-4
Fifth progress report on the cooperative investigation of springs and streamflow in the Tecolote Tunnel area of Santa Barbara County, California
Walter Hofmann
1953, Open-File Report 53-121
This report is the fifth in a continuing series of annual progress reports giving the results of discharge measurements made at more than 120 selected sites in the "Tecolote Tunnel Area" of the Santa Ynez Mountains. This area derives its name from the tunnel now being built by the Bureau...
Water power of the coast streams of Oregon
Randolph O. Helland
1953, Open-File Report 53-109
Chlorine contamination of a well at New Bern, North Carolina
H. E. LeGrand
1953, Open-File Report 53-152
Reconnaissance of the geology and ground-water resources of the La Prele area, Converse County, Wyoming, with a section on the chemical quality of the ground water
John Richard Rapp, W. H. Durum
1953, Circular 243
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
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
Water resources of the Minneapolis-St. Paul area, Minnesota
Charles Henry Prior, Robert Schneider, W. H. Durum
1953, Circular 274
The water supply of the Minneapolis-St. Paul area is adequate to satisfy present requirements and requirements for many years to come if the area continues to develop at about the present rate. The flow of -the Mississippi River at the Twin Cities is more than sufficient to meet the demands of...
Remarks on the program of the Water Resources Division, U. S. Geology Survey, and water problems in California, made before the Association of American State Geologists, Feb. 14, 1953, Los Angeles, California
J. F. Poland
1953, Open-File Report 53-218
Floods of March-April 1951 in Alabama and adjacent states
Water Resources Division, U.S. Geological Survey
1953, Water Supply Paper 1227-A
No abstract available....
Surface water supply of the United States, 1951, Part XI, Pacific slope basins in California
Water Resources Division, U.S. Geological Survey
1953, Water Supply Paper 1215
Surface water supply of the United States, 1951, Part IV, St. Lawrence River basin
Water Resources Division, U.S. Geological Survey
1953, Water Supply Paper 1207
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,...
Floods of 1950 in the upper Mississippi River and Lake Superior basins in Minnesota
C. G. Paulsen
1953, Water Supply Paper 1137-G
In areal coverage and magnitude of peak discharge the floods of April-May 1950 in the Missouri River Basin in North and South Dakota were unprecedented in the area. These floods were characterized by an extremely late spring breakup of ice, by great flood peaks resulting from snow melt, and by...