G.H. Taylor
1953, Open-File Report 53-254
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Publication Extents
Not all publications have extents, not all extents are completely accurateG.H. Taylor
1953, Open-File Report 53-253
F. A. Swenson
1953, Open-File Report 53-252
Allen and others Sinnott
1953, Open-File Report 53-248
C.B. Simmons, G.A. LaRocque Jr.
1953, Open-File Report 53-247
R. C. Newcomb, and others
1953, Open-File Report 53-199
Two seismic cross sections were run with a refraction seismograph near Spokane, Wash., in Hay and June 1951. One section trended north-south across the Spokane River valley plain Just east of the Idaho-Washington boundary; the other trended east-west across the strath just north of the Hillyard section of Spokane. Each section...
M.J. Mundorff
1953, Open-File Report 53-197
Walter MacDonald Jr.
1953, Open-File Report 53-163
Pat H. Holland
1953, Open-File Report 53-122
No abstract available....
C. S. Howard
1953, Open-File Report 53-133
N.D. Hoy
1953, Open-File Report 53-134
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 Resources Division, U.S. Geological Survey
1953, Open-File Report 53-29
No abstract available. ...
U.S. Fish and Wildlife Service
1953, Special Scientific Report - Wildlife 21
J. R. Rapp, D. A. Warner, Arthur Mitchell Morgan
1953, Water Supply Paper 1140
No abstract available....
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...
C. G. Paulsen
1953, Water Supply Paper 1137-F
The flood of November-December 1950 in the Central Valley basin was the greatest in most parts of the basin since the turn of the century and probably was exceeded in the lower San Joaquin River basin only by the historic flood of 1862. In respect to monetary loss, the 1950...
Water Resources Division, U.S. Geological Survey
1953, Water Supply Paper 1137-D
Four floods occurred in southeast Nebraska during the period of May to July 1950. Two of these were the greatest known in the State if the size of the drainage areas is considered, and the other two were not so spectacular but were of notable size and of possible hydrologic...
Randolph O. Helland
1953, Open-File Report 53-109
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 Resources Division, U.S. Geological Survey
1953, Open-File Report 53-138
Water Resources Division, U.S. Geological Survey
1953, Water Supply Paper 1227-A
No abstract available....
Water Resources Division, U.S. Geological Survey
1953, Water Supply Paper 1207
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,...
Water Resources Division, U.S. Geological Survey
1953, Water Supply Paper 1215