R.W. Stallman
1950, Open-File Report 50-97
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Publication Extents
Not all publications have extents, not all extents are completely accurateH.A. Whitcomb
1950, Open-File Report 50-106
T.B. Dover
1950, Open-File Report 50-69
Pure water does not exist in nature. Because water is a powerful solvent, every drop of rain water carries dissolved or suspended material - dust, pollen, and smoke, as well as the atmospheric gases, oxygen, nitrogen and carbon dioxide. When rain falls, the water running over the rocks and percolating...
Judith Weiss Frondel, Michael Fleischer
1950, Trace Elements Investigations 103
Elizabeth B. Jaffe
1950, Trace Elements Investigations 132
Michael Fleischer
1950, Trace Elements Investigations 128
Dagfin John Cederstrom
1950, Water Supply Paper 1067
No abstract available....
John Edward Johnston, W. A. Heck
1950, Coal Map 5
This preliminary report on the coal in the Hyden quadrangle, Kentucky, presents data on two of the principal commercial coals. The Fire Clay is the most valuable commercial coal in the quadrangle, and locally the Whitesburg bed is of minable thickness. Special emphasis has been placed on determining the thickness,...
Ralph L. Miller, William Peters Brosge
1950, Oil and Gas Investigation Map 104
Constance Leatherock
1950, Oil and Gas Investigation Chart 40
James F. Pepper, Wallace De Witt Jr.
1950, Oil and Gas Investigation Chart 37
Delmar W. Berry
1950, Open-File Report 50-54
Ground-water studies in the Missouri River Basin were begun by the U.S. Geological Survey during the fall of 1945 as a part of the program for development of the resources of the basin by the U.S. Bureau of Reclamation and other Federal agencies. The studies of the ground-water resources in...
George C. Taylor Jr., Remy C. Lemoine
1950, Report
The Gonaives Plain lies in northern Haiti at the head of the Gulf of Gonaives. Ground water in the plain is used widely for domestic and stock purposes but only to limited extent for irrigation. The future agricultural development of the plain will depend in large measure on...
Hirosi Kawasumi
1950, Report
In the latter half of this period the seismology in Japan was so much affected by the war that retrogressions in the instrumental seismology became very remarkable. Much regretted three leading seismologists, professors Ishimoto, Sezawa, and Inamura died in this period. But the seismic activities in this well-known land of...
C.W. Carlston
1950, Geological Society of America Bulletin (61) 1119-1130
Following its deposition, the late Pliocene or early Pleistocene Citronelle formation was entrenched by consequent streams and then tilted toward the Gulf. Submergence in waters 190 to 210 feet above present sea level then resulted in a compound shore line and marine erosion of the Coharie terrace. Four other marine...
Harry Clifford Granger, Herman Louis Bauer
1950, Trace Elements Memorandum 119
No abstract available....
Karen Duttweiler Kelley, M. C. Lachenbruch, A.H. Lachenbruch
1950, Geological Investigations, Naval Petroleum Reserve No. 4, Alaska 35
No abstract available....
I.L. Tailleur, Bion H. Kent
1950, Geological Investigations, Naval Petroleum Reserve No. 4, Alaska 34
No abstract available....
Charles L. Whittington, Steven J. Blazewicz
1950, Geological Investigations, Naval Petroleum Reserve No. 4, Alaska 33
U. S. Geological Survey Party No. 4 mapped the stratigraphy and structure of parts of the Carbon Creek and Ketik anticlines during the summer of 1950. The area, which lies in quadrangles I-19 and I-20 is shown in figure 1. Large-scale maps, compiled from plane-table surveys, give a more detailed...
Robert M. Chapman, G. Donald Eberlein, Charles D. Reynolds
1950, Geological Investigations, Naval Petroleum Reserve No. 4, Alaska 32
No abstract available....
William P. Brosge, Hillard N. Reiser
1950, Geological Investigations, Naval Petroleum Reserve No. 4, Alaska 31
Location: - This report describes sections of the Lisburne limestone studied in the foothills and northern mountains of the Brooks Range, Alaska. The area covered extends along the front of the range from Sagavanirktok Lake (68°28' N. - 149°25' W.) west to the head of the Kukpowruk River (68°25' N....
A. Samuel Keller
1950, Geological Investigations, Naval Petroleum Reserve No. 4, Alaska 30
Structural and stratigraphic studies of the rocks in the Siksikpuk and Nanushuk Rivers area were conducted by Navy Oil Unit party No. 2 during the summer field season of 1950. The field party consisted of six men: two geologists; two field assistants; a cook; and a weasel mechanic. Three weasels...
Marvin D. Mangus
1950, Geological Investigations, Naval Petroleum Reserve No. 4, Alaska 29
U. S. Geological Survey Navy Oil Unit Party I examined the surface geology of the area of the upper Utukok River and east fork of the Kokolik River from June 28 to September 3, 1950. The party consisted of six men: E. G. Sable and M. D. Mangus, geologists; C....
William A. Fischer
1950, Geological Investigations, Naval Petroleum Reserve No. 4, Alaska 27
The following report presents in tabulated form the location, structure, and stratigraphy of various anticlines in the Maybe Creek area which are presently considered to be reasonably favorable drilling sites, References to mere complete sources of information for each anticline are listed.The accompanying diagram (Fig. 1) presents a generalized stratigraphic...
E.G. Sable, M. D. Mangus
1950, Geological Investigations, Naval Petroleum Reserve No. 4, Alaska 28
No abstract available....