F. G. Poole, J.C. Roller
1960, Open-File Report 60-113
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Publication Extents
Not all publications have extents, not all extents are completely accurateValentine E. Zadnik
1960, Open-File Report 60-162
Petrographic investigation of the Upper Cambrian dolomites along the Delaware River in Warren County, New Jersey, has led to the distinction of six different microfacies each representing a specific sedimentary environment. In order of decreasing relative depth these microfacies are: dololutite, dolarenite, oolitic dolarenite, dolorudite, cryptozoan dolomite and desiccation dolorudite....
Randolph Wilson Bromery, G. L. Zandle, and others
1960, Geophysical Investigations Map 260
F. N. Houser, F. G. Poole
1960, IMAP 328
Robert O. Castle
1960, Open-File Report 60-26
A. B. Gibbons
1960, Open-File Report 60-56
Robert O. Castle
1960, Open-File Report 60-25
E. A. Merewether (compiler)
1960, IMAP 311
Charles F. Withington, Marion Charlotte Jaster
1960, Bulletin 1105
J. V. B. Wells
1960, Water Supply Paper 1561
J. V. B. Wells
1960, Water Supply Paper 1624
Wilbur Nathaniel Palmquist Jr., Wilbur Francis Ramey Hall
1960, Hydrologic Atlas 22
No abstract available....
Wilbur Nathaniel Palmquist Jr., Francis Ramey Hall
1960, Hydrologic Atlas 16
No abstract available....
Wilbur Nathaniel Palmquist, Francis Ramey Hall
1960, Hydrologic Atlas 25
No abstract available....
M. S. Griffin, E.N. Clark
1960, Open-File Report 60-61
Reuben Kachadoorian
1960, IMAP 307
Randolph Wilson Bromery, K.O. Emery, J. R. Balsley Jr.
1960, Geophysical Investigations Map 211
No abstract available....
H. L. Berryhill Jr.
1960, IMAP 318
No abstract available....
E. H. Herrick
1960, Open-File Report 60-67
Alfred H. Harder
1960, Water Supply Paper 1488
Large quantities of fresh ground water are available in Calcasieu Parish. Fresh water is present in sand of Recent, Pleistocene, Pliocene, and Miocene ages, although locally only small supplies for rural or stock use can be obtained from the shallow sand lenses of Recent and Pleistocene ages. The principal fresh-water-bearing...
Nancy C. Pearre, Allen V. Heyl Jr.
1960, Bulletin 1082-K
The Piedmont Upland in Maryland, Pennsylvania, and Delaware is about 160 miles long and at the most 50 miles wide. Rocks that underlie the province are the Baltimore gneiss of Precambrian age and quartzite, gneiss, schist, marble, phyllite, and greenstone, which make up the Glenarm series of early Paleozoic (?)...
Robert E. Matson
1960, Open-File Report 60-96
The Smoky Butte intrusives are located in T. 18 N., R. 36 E. Garfield County, Montana on the extreme eastern edge of the petrographic province of Central Montana. They consist of dikes and plugs arranged in linear, en-echelon pattern with a northeast trend and intrude the Tullock member (Paleocene age)...
Jerry C. Olson, E. Neal Hinrichs
1960, Bulletin 1082-D
Pegmatite occurs widely in Nevada and northwestern Arizona, but little mining has been done for such pegmatite minerals as mica, feldspar, beryl, and lepidolite. Reconnaissance for beryl-bearing pegmatite in Nevada and in part of Mohave County, Ariz., and detailed studies in the Dawley Canyon area, Elko County, Nev., have shown...
Dorothy B. Vitaliano, and others
1960, Bulletin 1106-E
Arthur B. Campbell
1960, Bulletin 1082-I
The St. Regis-Superior area occupies about 300 square miles in northwestern Montana and includes parts of the Squaw Peak Range and Coeur d'Alerie Mountains of the northern Rocky Mountains physiographic province. Nearly 50,000 feet of metasedimentary rocks of the Precambrian Belt series, chiefly varieties of quartzite and argillite, underlies most...