William Peters Brosge
1960, Open-File Report 60-20
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Publication Extents
Not all publications have extents, not all extents are completely accurateP. B. King, H. W. Ferguson, Warren Hamilton
1960, Professional Paper 311
No abstract available....
United States Geological Survey
1960, Open-File Report 82-7
No abstract available. ...
T. W. Dibblee Jr.
1960, Bulletin 1089-B
C.E. Price
1960, Open-File Report 60-115
G.E. Becraft
1960, Miscellaneous Field Studies Map 171
T. W. Dibblee Jr.
1960, Miscellaneous Field Studies Map 232
Henry Bell, W.C. Overstreet
1960, Miscellaneous Field Studies Map 234
T. W. Dibblee Jr.
1960, Miscellaneous Field Studies Map 76
Edwin R. Landis
1960, Bulletin 1087-G
T. W. Dibblee Jr.
1960, Miscellaneous Field Studies Map 229
T. W. Dibblee Jr.
1960, Miscellaneous Field Studies Map 227
G. W. Weir, W. D. Carter, W.P. Puffett, J. L. Gualtieri
1960, Miscellaneous Field Studies Map 150
Thomas Daniel Murphy
1960, Bulletin 1072-L
T. W. Dibblee Jr.
1960, Miscellaneous Field Studies Map 233
J. R. Rapp
1960, Open-File Report 60-117
William H. Kiel Jr.
1960, Special Scientific Report - Wildlife 49
No abstract available....
Peter Zubovic
1960, Open-File Report 60-165
Spectrographic analyses for 15 elements of 249 block samples of coal are reported here. These samples represent 28 localities of beds 5 and 6 of Illinois and their correlatives in Indiana and western Kentucky.Comparison with the coals of the Northern Great Plains province shows a similarity in the total amount...
T. W. Dibblee Jr.
1960, Miscellaneous Field Studies Map 226
Everett D. Jackson
1960, Open-File Report 60-79
This paper presents some results of work done between 1951 and 1955 as a part of a comprehensive investigation of the stratigraphy, geochemistry, and petrography of the Ultramafic zone of the Stillwater complex by the U. S. Geological Survey. Detailed mapping of the chromite deposits of the complex was done...
Kenneth S. Soward
1960, Open-File Report 60-128
Knowles and Perma damsites, at river miles 3 and 11 respectively, are alternates for developing the lower Flathead River. A high dam with a flow line at altitude 2,705 feet would back water to Kerr Dam at river mile 72 and would produce a hydraulic head of 235 feet at...
R. L. Smith
1960, Professional Paper 354-F
Welded tuffs are recognized as special parts of ash flows, other pyroclastic flows, or, more rarely, air-fall deposits. Ash flows may be emplaced at any temperature below a maximum eruption temperature. Those emplaced above a minimum welding temperature may show any and all degrees of welding and crystallization. ...
C. B. Sherwood, Howard Klein
1960, Open-File Report 60-124
E.M. MacKevett Jr.
1960, Bulletin 1087-F
Richard Quintin Lewis, Willis H. Nelson, Howard Adorno Powers
1960, Bulletin 1028-Q