William Peters Brosge
1960, Open-File Report 60-21
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Page 6079, results 151951 - 151975
Publication Extents
Not all publications have extents, not all extents are completely accurateJ.R. Cooper
1960, Miscellaneous Field Studies Map 231
P.E. Hotz, Ronald Willden
1960, Miscellaneous Field Studies Map 161
T. S. Lovering
1960, Miscellaneous Field Studies Map 230
No abstract available....
Carl E. Dutton
1960, Open-File Report 60-46
No abstract available. ...
G.E. Becraft
1960, Miscellaneous Field Studies Map 171
D. G. Adolphson
1960, Open-File Report 60-1
No abstract available....
C. M. Bunker
1960, Open-File Report 60-22
Vance C. Kennedy, S. W. Hobbs
1960, Bulletin 1098-A
No abstract available....
C. Ervin Brown, Jesse W. Whitlow
1960, Bulletin 1123-A
No abstract available....
Dorothy B. Vitaliano, and others
1960, Bulletin 1106-E
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...
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 (?)...
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...
Richard Kenneth Hose, Charles Albert Repenning, Joseph I. Ziony
1960, Open-File Report 60-73
No abstract available....
William Peters Brosge
1960, Open-File Report 60-20
Luna Bergere Leopold
1960, Circular 414-B
In a sandy, riverside location in Wisconsin my family has a farm, once abandoned by a previous owner because it would not produce much corn. By the time we bought it for a pittance, only a few remnants of white pine remained from the magnificent stands made famous by Paul...
Louis W. Currier
1960, Circular 426
Luna Bergere Leopold
1960, Circular 414-C
Forsaking his inheritance and its assurance of a comfortable existence, Guatama Buddha adopted the life of a pauper to seek the intellectual joys of pure contemplation. Under a mulberry tree, it is said, he propounded a 12-point program of ethical conduct stressing the development of a disinterested outlook in each...
M. W. Skougstad, C. Albert Horr
1960, Circular 420
The regions where the stable strontium content of surface waters is relatively low (less than 0.50 ppm) include the Pacific Northwest, Northeastern United States, and the Central Lowlands, Particularly the Lower Mississippi basin and the Western Gulf Coast area. Moderate concentrations of strontium (0.50 to 1.5 ppm) are found in...
Howard Dale Gower
1960, Geologic Quadrangle 129
No abstract available....
J. V. B. Wells
1960, Water Supply Paper 1637
Joseph Haffty
1960, Water Supply Paper 1540-A
A spectrographic method is described for the quantitative analysis of many minor elements in natural water. The excitation of the water residue using a direct-current arc provides a method for the detection of elements present in very low concentrations. The concentration of the elements is determined in percent of the...
L. F. Emmett
1960, Open-File Report 60-50
C.L. Jones
1960, Open-File Report 60-83
Between Project Gnome site and the International Minerals and Chemical. Corporation's plant site, in central eastern Eddy County, N. Mex., unconsolidated deposits of Quaternary age and redbeds of Triassic age attain a thickness of about 700 feet, and rest unconformably on evaporites of late Permian age. The upper Permiau evaporites...