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Publication Extents

Not all publications have extents, not all extents are completely accurate
Locations and descriptions of lode mines and prospects in the Fairbanks district, Alaska
Robert Mills Chapman, Robert Lutz Foster
1967, Open-File Report 67-44
This report has been compiled from data gathered in the field in September and October, 1966, and from a detailed survey of the various geologic and mining reports on the Fairbanks lode mining district. A number of people who are familiar with mining in this district have provided some additional...
Dictionary of Alaska place names
Donald J. Orth
1967, Professional Paper 567
This work is an alphabetical list of the geographic names that are now applied and have been applied to places and features of the Alaska landscape. Principal names, compiled from modem maps and charts and printed in boldface type, generally reflect present-day local usage. They conform to the principles of...
Iron in the United States, exclusive of Alaska and Hawaii
Martha S. Carr, Philip White Guild, W.B. Wright
1967, Mineral Investigations Resource Map 51
The iron-ore deposits in the United States (exclusive of Alaska and Hawaii) are shown on the accompanying map; many iron-bearing deposits that are of lesser or only potential value are also shown. Because these deposits range widely in extent, two general categories of symbols are used, each of which is...
Effects of the earthquake of March 27, 1964, on air and water transport, communications, and utilities systems in south-central Alaska
Edwin B. Eckel
1967, Professional Paper 545-B
The earthquake of March 27, 1964, wrecked or severely hampered all forms of transportation, all utilities, and all communications systems over a very large part of south-central Alaska. Effects on air transportation were minor as compared to those on the water, highway, and railroad transport systems. A few planes were...
Surface faults on Montague Island associated with the 1964 Alaska earthquake
George Plafter
1967, Professional Paper 543-G
Two reverse faults on southwestern Montague Island in Prince William Sound were reactivated during the earthquake of March 27, 1964. New fault scarps, fissures, cracks, and flexures appeared in bedrock and unconsolidated surficial deposits along or near the fault traces. Average strike of the faults is between N. 37° E....
The Alaska earthquake, March 27, 1964: effects on transportation, communications, and utilities
Malcolm H. Logan, Lynn R. Burton, Edwin B. Eckel, Reuben Kachadoorian, David S. McCulloch, Manuel G. Bonilla
1967, Professional Paper 545
This is the forth in a series of six reports that the U.S. Geological Survey published on the results of a comprehensive geologic study that began, as a reconnaissance survey, within 24 hours after the March 27, 1964, Magnitude 9.2 Great Alaska Earthquake and extended, as detailed investigations, through several...
Devonian rocks of the Yukon-Porcupine Rivers area and their tectonic relation to other Devonian sequences in Alaska
Michael Churkin Jr., Earl E. Brabb
1967, Conference Paper, International Symposium of the Devonian system: Papers
Devonian rocks along the Yukon River near the Alaska-Yukon boundary comprise 250 feet of limestone and shale and 800 feet of chert and siliceous shale, all referred to the McCann Hill Chert of Early to Late Devonian age; about 3,000 feet of non-marine chert-pebble conglomerate, graywacke, and shale of...
Viscosity and finite strength of the mantle as determined from water and ice loads
Max D. Crittenden Jr.
1967, Geophysical Journal International (14) 261-279
Some recent examples of transient Earth loads (Lake Bonneville, Utah; Glacier Bay, Alaska; northeast Greenland) indicate that both the viscosity and finite strength of the mantle are lower than is commonly presumed. A time constant (1/e) of 4000 years is estimated for Lake Bonneville, and of 1000 years for...
Post-paleozoic radiometric ages and their relevance to fault movements, Northern Southeastern Alaska
R. A. Loney, David A. Brew, Marvin A. Lanphere
1967, GSA Bulletin (78) 511-526
Recently determined lead-alpha and potassium-argon ages from northern southeastern Alaska indicate major plutonic events in the Paleozoic, Mesozoic, and Tertiary; in contrast, previous studies suggested that only one complex Jurassic and Cretaceous event occurred. The ages presented in this paper indicate the following Mesozoic and Tertiary plutonic events: Middle or...