Water Resources Division, U.S. Geological Survey
1943, Water Supply Paper 937
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Publication Extents
Not all publications have extents, not all extents are completely accurateWater Resources Division, U.S. Geological Survey
1943, Bulletin 930-D
Water Resources Division, U.S. Geological Survey
1943, Bulletin 930-C
S. W. Hobbs
1943, Open-File Report 43-16
Cordell Durrell, Thomas P. Thayer
1943, Open-File Report 43-81
R. J. Roberts
1943, Open-File Report 43-89
J. W. Parker III, W.C. Stoll
1943, Open-File Report 43-71
Carl Fries Jr., A.P. Butler Jr.
1943, Open-File Report 43-1
D.M. Lemmon, D.G. Wyant, F. M. Byers
1943, Open-File Report 43-87
J.J. Norton
1943, Open-File Report 43-93
W.C. Stoll
1943, Open-File Report 43-3
C.J. Vitaliano, A.J. Bodenlos, G. T. Faust
1943, Open-File Report 43-94
L. R. Page, A.R. Kinkel, L.C. Pray, R.H. Porter
1943, Open-File Report 43-86
Water Resources Division, U.S. Geological Survey
1943, Open-File Report 43-92
W.C. Stoll, J. W. Parker III
1943, Open-File Report 43-72
J. C. Olson
1943, Open-File Report 43-70
J.J. Page, J.J. Norton, V.C. Fryklund
1943, Open-File Report 43-77
A. C. Waters, Randall E. Brown, Robert R. Compton, George W. Walker, Lloyd W. Staplese, Howell Willians
1943, Open-File Report 43-25
Lowell S. Hilpert, James B. Cathcart
1943, Open-File Report 43-82
No abstract available. ...
Walter S. White
1943, Bulletin 940-E
Manganiferous rocks are found in two areas in eastern Aroostook County, Maine, one west and northwest of Presque Isle and the other south of Houlton. The manganiferous deposits are sedimentary lenses, up to 150 feet thick and half a mile long, in middle Silurian argilllte. The rocks of both areas...
Allen P. Agnew, Allen V. Heyl Jr.
1943, Open-File Report 43-11
Walter S. White
1943, Open-File Report 42-1
Walter S. White, John H. Eric, Thomas William Amsden
1943, Open-File Report 79-352
No abstract available....
J.F. Smith Jr. , L.L. Ray
1943, Geological Society of America Bulletin (54) 891-924
In north-central New Mexico the rugged Cimarron Range marks the eastern margin of the Southern Rocky Mountains, abruptly rising more than 5000 feet above the adjacent Great Plains. Structurally the range is a northward-plunging anticline with a core of pre-Cambrian crystalline rocks. Faulting along the eastern and western margins of...
H.S. Davis
1943, Journal of Parasitology (29) 385-386
No abstract available. ...