T. G. Payne
1954, Open-File Report 54-231
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Publication Extents
Not all publications have extents, not all extents are completely accurateSaul Aronow
1954, Open-File Report 54-12
T. G. Payne
1954, Open-File Report 54-232
Eugene Brown
1954, Open-File Report 54-40
Margaret K. Robinson
1954, Professional Paper 260-D
Martin Wiggo Johnson
1954, Professional Paper 260-F
U.S. Fish and Wildlife Service
1954, Special Scientific Report - Wildlife 25
Water Resources Division, U.S. Geological Survey
1954, Water Supply Paper 1194
Gordon H. Wood Jr., R. B. Johnson, G. H. Dixon
1954, Open-File Report 54-337
No abstract available....
R. W. Mower
1954, Open-File Report 54-217
Investigations by the United States Geological Survey of Ground Water in the Southern border area of the Snake Rive Plain, south of the Snake River, a re concerned at the present time with delineation of the principal ground-water districts, the extent and location of existing ground-water developments, the possibilities for...
James E. May
1954, Open-File Report 54-193
The proposed relocation of Route 128 in Dedham, Mass. requires a grade separation with long approach cuts at its crossing with Route 1A. In order to obtain information on the configuration and depths of the bedrock surfaces, and on the nature of the overlying material, a geologic study was made...
Harold Burns Lindeman
1954, Circular 235
H.N. Loeblich
1954, Open-File Report 54-169
M. D. Mangus
1954, Open-File Report 54-181
H.N. Loeblich
1954, Open-File Report 54-170
H.D. Wilson Jr.
1954, Open-File Report 54-336
Ruth Todd, Rita Post
1954, Professional Paper 260-N
I. J. Witkind
1954, Trace Elements Investigations 340
During the summers of 1951 and 1952 the U.S. Geological Survey mapped the geology and uranium deposits in three 15-minute quadrangles on the Navajo Indian Reservation in Apache and Navajo Counties, northeastern Arizona. Exposed sedimentary rocks range in age from the Halgaito tongue of the Cutler formation (Permian) to the Salt Wash...
Jerry C. Olson, Stewart R. Wallace
1954, Trace Elements Investigations 353
Thorium has been found since 1949 in at least 33 deposits in an area 6 miles wide and 20 miles long in the Powderhorn district, Gunnison County, Colo. The district is composed largely of pre-Jurassic metamorphic and igneous rocks, which are chiefly if not entirely pre-Cambrian in age. The metamorphic...
Herbert A. Swenson
1954, Report
This paper is a general discussion of the quality and chemical character of surface and ground waters in the Pacific Northwest as shown by the available data. Previous quality of water studies reported in the literature are reviewed. The composition of natural waters is considered as to the source and...
Irving A. Breger, James M. Schopf
1954, Trace Elements Investigations 496
Microscopic study of black, vitreous, carbonaceous material occurring in the Chattanooga shale in Tennessee and in the Cleveland member of the Ohio shale in Ohio has revealed coalified woody plant tissue. Some samples have shown sufficient detail to be identified with the genus Callixylon. Similar material has been reported in...
George W. Walker, Tom G. Lovering
1954, Trace Elements Investigations 229
Reconnaissance examination by Government geologists of many areas, mine properties, and prospects in California during the period between 1948 and 1953 has confirmed the presence of radioactive materials in place at more than 40 localities. Abnormal radioactivity at these localities is due to concentrations of primary and secondary uranium minerals,...
P. C. Bateman, W. P. Irwin
1954, California Division of Mines and Geology Bulletin 170
No abstract available....
W.E. Wrather
1954, Science (119) 3A-3A
No abstract available. ...
Randolph W. Chapman
1954, Geological Society of America Bulletin (65) 97-114
The alkaline stock at Mount Monadnock, Vermont, described briefly by Wolff (1929), has been restudied in detail. Its petrography and structure are discussed here and conclusions are drawn as to its mode of emplacement. The stock consists of plutonic and hypabyssal rocks which intrude folded Ordovician (?) schist and quartzite. The longer axis, trending north-northwest across the strike of the country...