Coal resources of Virginia
Andrew Brown, Henry L. Berryhill Jr., Dorothy A. Taylor, James V. A. Trumbull
1952, Circular 171
The U. S. Geological Survey and the Virginia Geological Survey have cooperated in preparing this reappraisal of the coal resources of Virginia, which is based on a study of all information" on the reserves of the State available in the publications and files of the two organizations, supplemented by mine...
Geologic map of the Barnes Hill talc prospect, Waterbury, Vermont
A.H. Chidester, G. W. Stewart, D.C. Morris
1952, Miscellaneous Field Studies Map 7
The Barnes Hill talc prospect is in northeastern Waterbury township, Washington County, Vermont, about 2.2 miles N. 35° E. of the road triangle at Waterbury Center. The deposit occurs in a body of ultramafic rock that crops out between the altitudes of 1,150 and 1,190 feet above sea level, near...
Fourth progress report on the cooperative investigation of springs and streamflow in the Tecolote Tunnel area of Santa Barbara County, California
C.E. Burgess
1952, Open-File Report 52-21
This is a continuation of annual progress reports giving the results of discharge measurements made in the Santa Ynez Mountains between Refugio Canyon on the west to San Marcos Pass and the Painted Cave area on the east. This portion of Santa Barbara County has been designated as the "Tecolote...
Ground-water recharge in the East Shore area, Utah
P.E. Dennis
1952, Open-File Report 52-32
No abstract available....
Geology of the Alaska-Juneau lode system, Alaska
William Stephens Twenhofel
1952, Open-File Report 52-160
The Alaska-Juneau lode system for many years was one of the worlds leading gold-producing areas. Total production from the years 1893 to 1946 has amounted to about 94 million dollars, with principal values in contained gold but with some silver and lead values. The principal mine is the Alaska-Juneau mine,...
Quicksilver deposit areas near Aleknagik, Nushagak district, southwestern Alaska
Wallace Martin Cady
1952, Open-File Report 52-22
The deposit here described is on Marsh Mountain, three miles due east of the village of Aleknagik (Mosquito Point), near the foot of Wood River Lakes (see-fig. 1)....
Geologic structure map of the Beetown lead-zinc area, Grant County, Wisconsin
Allen V. Heyl Jr., Erwin J. Lyons, John J. Theiler
1952, Miscellaneous Field Studies Map 3
The Beetown area, in Grant County, Wisconsin, in the northwestern part of the Upper Mississippi Valley zinc-lead district, lies in the western part of T. 4 N., R. 4 W., and the eastern part of T. 4 N., R. 5 W. The village of Beetown is at about its center. Recent...
Geology and hydrology of dam sites on the island of St. Croix, Virgin Islands
R. R. Meyer
1952, Open-File Report 52-98
The Virgin Islands Corporation plans to build a series of small earth dams along some of the streams on the island of St. Croix, and field studies involving the selection and hydrology of possible sites was carried on by the Geological Survey during the months of August and September 1951....
Floods of 1950 in the Red River of the North and Winnipeg River basins
Water Resources Division, U.S. Geological Survey
1952, Water Supply Paper 1137-B
The floods of April-July 1950 in the Red River of the North and Winnipeg River Basins were the largest that have occurred in several decades and caused the greatest damage that the flooded area has ever sustained. Five lives were lost in the United States, owing to causes directly connected...
The Permian phosphorite deposits of western United States
V.E. McKelvey, Roger Warren Swanson, Richard Porter Sheldon
1952, Open-File Report 53-166
The Permian marine phosphorite deposits of the western United States were laid down in the Phosphoria formation and its partial stratigraphic equivalents over an area of about 135,000 square miles in Montana, Idaho, Wyoming, Utah, and Nevada. The deposits in the eastern part of the field lie on the western...
A magnetic anomaly near Bear Lake, Houghton County, Michigan
James C. Wright
1952, Open-File Report 52-169
A large magnetic anomaly of unknown origin occurs about 1 1/2 miles east of Bear Lake, Houghton County, Michigan, in secs. 24 and 258 T. 56 N., R. 34 W. The occurrence is isolated in an area of very weakly magnetic rocks and has special geologic interest because it is...
Surface water supply of the United States, 1950, Part II, South Atlantic slope and eastern Gulf of Mexico basins
Water Resources Division, U.S. Geological Survey
1952, Water Supply Paper 1172
The coal deposits of the Alkali Butte, the Big Sand Draw, and the Beaver Creek fields, Fremont County, Wyoming
Raymond M. Thompson, Vincent L. White
1952, Circular 152
Large coal reserves are present in three areas located between 12 and 20 miles southeast of Riverton, Fremont County, central Wyoming. Coal in two of these areas, the Alkali Butte coal field and the Big Sand Draw coal field, is exposed on the surface and has been developed to some...
Total intensity aeromagnetic and geologic map of east-central St. Louis County, Minnesota
J. L. Meuschke, John R. Henderson Jr.
1952, Geophysical Investigations Map 92
No abstract available....
Geologic setting of the Mountain Pass rare earth deposits, San Bernardino County, California
Jerry Chipman Olson
1952, Open-File Report 52-110
The Mountain Pass district is in a block of pre-Cambrian metamorphic rocks bounded on the east and south by the alluvium of Ivanpah Valley. This block is separated from Paleozoic and Mesozoic sedimentary and volcanic rocks on the west by the Clark Mountain normal fault, and the northern boundary of...
Structural geology of the Crazy Mountain syncline-Beartooth Mountain border east of Livingston, Montana
Paul W. Richards
1952, Open-File Report 52-127
No abstract available....
The industrial utility of public water supplies in the east south central states, 1952
E. W. Lohr, G. A. Billingsley, J.W. Geurin, W.L. Lamar
1952, Circular 197
The location of industrial plants is dependent on an ample water supply of suitable quality. Information relating to the chemical characteristics of the water supplies is not only essential to the location of many plants but also is an aid in the manufacture and distribution of many commodities. Public water...
Sedimentary volumes in Gulf Coastal Plain of the United States And Mexico: Part I: Volume of Mesozoic Sediments In Florida and Georgia
Paul Livingston Applin
1952, Geological Society of America Bulletin (63) 1159-1164
Mesozoic sedimentary rocks are present throughout Florida and the Coastal Plain of Georgia, but chiefly in the subsurface in an area of approximately 93,500 square miles. The Mesozoic rocks in this area belong, for the most part, to the Gulf and Comanche series of the Cretaceous system. Rocks tentatively classified...
Late quaternary geology and frost phenomena along Alaska Highway, Northern British Columbia and Southeastern Yukon
Charles Storrow Denny
1952, Geological Society of America Bulletin (63) 883-922
Reconnaissance field work along the Alaska Highway in northern British Columbia and southeastern Yukon furnishes preliminary data on the later Quaternary history of the region, and on the processes and results of intensive frost action. Extensive erosion surfaces were developed prior to glaciation, such as the Alberta Plateau of northeastern British Columbia and the Yukon Plateau in southern Yukon. In the region from Dawson Creek to Fort Nelson, British Columbia, the drift is dominantly...
Stratigraphy and structure of some selected localities in the eastern Brooks Range, Alaska
William P. Brosge, J. Thomas Dutro Jr., Marvin D. Mangus, Hillard N. Reiser
1952, Geological Investigations, Naval Petroleum Reserve No. 4, Alaska 42
No abstract available....
Glaciation and drainage changes in the fish Lake Plateau, Utah
Clyde T. Hardy, S. Muessig
1952, Geological Society of America Bulletin (63) 1109-1116
The Fish Lake Plateau, nearly centrally located among the High Plateaus of Utah, exhibits glacial and other geomorphic features of regional significance. The plateau is divided into two areas by Fish Lake and the wide valley of Sevenmile Creek. The Fish Lake trough is a structural basin; Sevenmile Valley may be largely erosional. Volcanic rocks of Tertiary age underlie most of the plateau;...
Pimpled plains of Eastern Oklahoma
M. M. Knechtel
1952, Geological Society of America Bulletin (63) 689-700
Patterns formed by the networks of furrows separating the natural mounds of pimpled plains in eastern Oklahoma are regarded as attributable to shrinkage-polygon systems of coarse texture comparable to those occurring (1) in mound-studded parts of the northwestern United States that are underlain by vertically jointed basalt, (2) in tracts of Alaskan tundra that are occupied...
Radioactivity at the Copper Creek copper lode prospect, Eagle district, east-central Alaska
Helmuth Wedow, Gene Edward Tolbert
1952, Trace Elements Investigations 195
Investigation of radioactivity anomalies at the Copper Creek copper lode prospect, Eagle district, east-central Alaska, during 1949 disclosed that the radioactivity is associated with copper mineralization in highly metamorphosed sedimentary rocks. These rocks are a roof pendant in the Mesozoic "Charley River" batholith. The radioactivity is probably all due to...
Preliminary report on the White Canyon area, San Juan county, Utah
William E. Benson, Albert F. Trites Jr., Ernest P. Beroni, John A. Feeger
1952, Trace Elements Memorandum 325
The White Canyon area, in the central part of San Juan County, Utah, consists of approximately two 15-minute quadrangles. Approximately 75 square miles have been mapped by the Geological Survey on a scale of 1 inch equals 1 mile, using a combined aerial photography-plane table method. Structure contours were drawn...
Uranium occurrence on the No. 8 claim, east side of the Thomas Range, Juab County, Utah
Herman L. Bauer Jr., Mortimer H. Staatz
1951, Trace Elements Memorandum 220
No abstract available....