Frank Walter Kennon
1966, Water Supply Paper 1839-C
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Page 5917, results 147901 - 147925
Publication Extents
Not all publications have extents, not all extents are completely accurateJ. L. Vargo, F. C. Smith, A. J. Petty
1966, Geophysical Investigations Map 557
No abstract available....
G. R. Boynton, D.R. Pittillo, G. L. Zandle
1966, Geophysical Investigations Map 554
No abstract available....
Glenn C. Prescott
1966, Hydrologic Atlas 225
No abstract available....
George Edward Manger
1966, Bulletin 1203-D
P. W. Philbin, C. W. Smith
1966, Geophysical Investigations Map 595
No abstract available....
G. R. Boynton, D.R. Pittillo, G. L. Zandle
1966, Geophysical Investigations Map 569
No abstract available....
E.F. Pashley Jr.
1966, Open-File Report 66-95
Jack Edward Harrison
1966, Open-File Report 68-120
Kenneth John Englund, A.O. DeLaney
1966, Geologic Quadrangle 522
Water Resources Division, U.S. Geological Survey
1966, Water Data Report NV-65-1
Robert L. Rioux, Robert J. Hite, John R. Dyni, Willard C. Gere
1966, Open-File Report 66-112
No abstract available....
P. W. Philbin, F. P. Gilbert
1966, Geophysical Investigations Map 560
J. L. Meuschke, J. A. Pitkin, C. W. Smith
1966, Geophysical Investigations Map 574
Frank R. Moore
1966, Geologic Quadrangle 560
R.N. Doolittle
1966, Open-File Report 66-26
Alfred R. Taylor
1966, Geologic Quadrangle 562
Robert Hadley Moench, Avery Drake Jr.
1966, Open-File Report 66-87
The Idaho Springs mining district forms an important segment of the Front Range mineral belt, a northeast-trending zone of coextensive intrusive rocks and hydrothermal ore deposits of early Tertiary age. This belt, which is about 50 miles long, extends from the region just west of Boulder southwestward across the Front...
C.B. Crawford Jr., R. W. Page, R.A. LeBlanc
1966, Open-File Report 66-20
Peter W. Lipman
1966, Geologic Quadrangle 489
S. G. Robson, F.W. Glessner
1966, Open-File Report 66-116
John Mark Cattermole
1966, Geologic Quadrangle 514
Clemens Arvid Nelson
1966, Geologic Quadrangle 528
David S. Harwood
1966, Open-File Report 66-57
The Cupsuptic quadrangle, in west-central Maine, lies in a relatively narrow belt of pre-Silurian rocks extending from the Connecticut River valley across northern New Hampshire to north-central Maine. The Albee Formation, composed of green, purple, and black phyllite with interbedded-quartzite, is exposed in the core of a regional anticlinorium overlain...
D.L. Hart
1966, Hydrologic Atlas 223