O. E. Meinzer, L.K. Wenzel
1938, Water Supply Paper 840
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Publication Extents
Not all publications have extents, not all extents are completely accurateSamuel Grossman Lasky
1938, Bulletin 885
Philip Sidney Smith
1938, Bulletin 897-A
John George Staack
1938, Bulletin 888
N. W. Bass, L. E. Kennedy, W. R. Dillard, Otto Leatherock, J. H. Hengst
1938, Bulletin 900-A
No abstract available....
Water Resources Division, U.S. Geological Survey
1938, Bulletin 898-C
Ralph Tuck
1938, Bulletin 897-B
No abstract available....
W. Ayvazoglou (compiler)
1938, Bulletin 895-D
Water Resources Division, U.S. Geological Survey
1938, Bulletin 898-A
Water Resources Division, U.S. Geological Survey
1938, Bulletin 898-D
Water Resources Division, U.S. Geological Survey
1938, Bulletin 898-B
P.D. Trask
1938, Professional Paper 186-N
W.W. Rubey
1938, Professional Paper 189-E
John C. Reed, Francis Gerritt Wells
1938, Bulletin 886-C
Harvey B. Kinnison, L.F. Conover, B. L. Bigwood
1938, Water Supply Paper 836-A
Water Resources Division, U.S. Geological Survey
1938, Water Supply Paper 834
Harold T. Stearns, Lynn Crandall, Willard G. Steward
1938, Water Supply Paper 774
A. Peter, Severine Britt (translator)
1938, Open-File Report 49-23-B
No abstract available....
W. Ayvazoglou (compiler)
1938, Bulletin 895-C
Water Resources Division, U.S. Geological Survey
1938, Water Supply Paper 806
Water Resources Division, U.S. Geological Survey
1938, Water Supply Paper 833
Water Resources Division, U.S. Geological Survey
1938, Water Supply Paper 810
C. Milton, W. D. Johnston Jr.
1938, Economic Geology (33) 749-771
Seventeen representative samples of supergene sulphates from old workings on the Comstock Lode are described. They range from simple minerals such as gypsum and epsomite to complex aggregates of four or more distinct species. All are well known species except a mineral of the copper (chalcanthite) or magnesium sulphate pentahydrate...
Charles Frederick Park
1938, Economic Geology (33) 709-729
The replacement ore bodies of the Metaline zinc-lead district, in northeastern Washington are limited to the greatly disturbed fault block through which the Pend Oreille River flows and are associated with the major faults but are not in them. They are mostly near the top of the Metaline limestone, of...
U.S. Bureau of Biological Survey
1938, Wildlife Leaflet 121
No abstract available....