Charles Reynolds Warren
1970, Geologic Quadrangle 871
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Publication Extents
Not all publications have extents, not all extents are completely accurateJ. Hiram Smith
1970, Geologic Quadrangle 867
Clyde Wahrhaftig
1970, Geologic Quadrangle 809
Clyde Wahraftig
1970, Geologic Quadrangle 807
Charles Reynolds Warren
1970, Geologic Quadrangle 848
Clyde Wahrhaftig
1970, Geologic Quadrangle 811
Edward Huntington Cobb
1970, Mineral Investigations Resource Map 52
No abstract available....
Clyde Wahraftig
1970, Geologic Quadrangle 806
John B. Roen
1970, Geologic Quadrangle 838
Roger Warren Swanson
1970, Geologic Quadrangle 860
Jeffrey T. Armbruster
1970, Open-File Report 70-11
An evaluation of the available streamflow data in South Carolina was made to provide guidelines for planning future surface-water data programs. The basic elements in the evaluation procedure were (1) establishment of objectives and goals of the program, (2) examination and analysis of all available data to determine which goals...
Howard Klein
1970, Open-File Report 70-188
No abstract available....
Wilbur C. Ballance
1970, Open-File Report 70-16
Hole UA-1 was center punched (a small-diameter exploratory hole drilled ahead of the large-diameter emplacement hole) from 1,524.0 to 1,981.2 meters (5,000 to 6,500 feet) and hydraulically tested to determine an ideal location for mining a chamber. Fifteen zones were tested; minor amounts of water bypassed the packers during five...
D. A. Goolsby, B. F. McPherson
1970, Open-File Report 71-124
David Schleicher, editor(s)
1970, Open-File Report 70-287
Because complex data that are presented orally and extemporaneously are far easier to study from a written record than from the oral description alone, during the Apollo 11 mission the Lunar Geology Experiment (LGE) team prepared a transcript of all communication between the LM and the Capcom during descent and...
R. L. Knutilla
1970, Open-File Report 70-189
No abstract available....
Robert L. Earhart, Mustafa M. Mawad
1970, Open-File Report 70-116
The Wadi Bidah district in southwest Saudi Arabia contains several ancient mines and mineral-prospects. The Precambian rocks of the district are steeply dipping and highly folded and faulted. They are divided into three major units: (1) older metavolcanic rocks, (2) metasedimentary rocks, and (3) younger metavolcanic rocks. Massive sulfide-type deposits...
James Bachelder Cathcart
1970, Open-File Report 70-60
B. F. McPherson
1970, Open-File Report 71-199
Water quality in the Shark River estuary was strongly influenced by seasonal patterns of rainfall, water level and temperature. During the rainy season (summer and early fall) the salinity in the 20-mile long estuary ranged from that of fresh water to half that of sea water while concentrations of...
B. F. McPherson
1970, Open-File Report 70-210
No abstract available....
Charles R. Meissner Jr.
1970, Open-File Report 70-220
J.W. Mercer, E.G. Lappala
1970, Open-File Report 70-222
E. G. Crosthwaite, C.A. Thomas, K.L. Dyer
1970, Open-File Report 70-93
The Big Lost River basin occupies about 1,400 square miles in south-central Idaho and drains to the Snake River Plain. The economy in the area is based on irrigation agriculture and stockraising. The basin is underlain by a diverse-assemblage of rocks which range, in age from Precambrian to Holocene. The...
J.E. Hull, C.F. Galliher
1970, Open-File Report 70-167
Glen L. Faulkner
1970, Open-File Report 70-121
The Cross-Florida Barge Canal route commences at Palatka on the St. Johns River, about 75 miles upstream from the Atlantic Ocean, and extends 110 miles southwestward across Peninsular Florida into deep water in the Gulf of Mexico near Yankeetown. The canal will be equipped with five locks, each 600 feet...