T. L. Pewe
1954, Bulletin 989-F
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Page 420, results 10476 - 10500
Publication Extents
Not all publications have extents, not all extents are completely accurateAlaska Geology Branch
1954, Open-File Report 54-1
Alaskan Geology Branch
1954, Open-File Report 54-2
Edward J. Webber
1954, Open-File Report 54-330
Alaskan Geology Branch
1954, Open-File Report 54-4
Alaskan Geology Branch
1954, Open-File Report 54-5
Alaskan Geology Branch
1954, Open-File Report 54-6
W. W. Patton Jr.
1954, Open-File Report 54-226
W. W. Patton Jr., A.S. Keller
1954, Open-File Report 54-228
Reuben Kachadoorian, David Moody Hopkins, D.R. Nichols
1954, Open-File Report 54-137
Alaskan Geological Branch
1954, Open-File Report 54-9
R. M. Thompson, W. L. Barksdale
1954, Open-File Report 54-312
No abstract available....
R. F. Thurrell Jr.
1954, Open-File Report 54-313
Frank W. Trainer
1954, Open-File Report 54-315
The Matanuska Valley is a part of the lowland lying north of the Chugach Range in south-central Alaska. The valley of Matanuska River and the lowland extending westward from it to the Susitna River are in the Matanuska and Wasilla districts as defined by P.S. Smith (1939, pl. 3). The...
Edward J. Webber, R.L. Detterman
1954, Open-File Report 54-331
M. D. Mangus, R.L. Detterman, M.C. Lachenbruch Jr., A.H. Lachenbruch
1954, Open-File Report 54-182
Arthur Edward Nelson, Walter S. West, John J. Matzko
1954, Trace Elements Investigations 292
Reconnaissance for radioactive deposits was conducted in selected areas of eastern Alaska during 1952. Examination of copper, silver, and molybdenum occurrences and of a reported nickel prospect in the Slana-Nabesna and Chisana districts in the eastern Alaska Range revealed a maximum radioactivity of about 0.003 percent equivalent uranium. No appreciable...
F.W. Trainer
1954, Science (119) 356
[No abstract available]...
Helmuth Wedow Jr.
1953, Trace Elements Investigations 56
R.A. Eckhart
1953, Bulletin 989-C
R.R. Coats
1953, Bulletin 989-A
Irvin L. Trailleur, Bion H. Kent
1953, Open-File Report 54-305
This report was prepared to assist in the planning of seismic profiles to be run across the anticlinorium in the vicinity of the Kiligwa River. The stratigraphy and structure of the mapped area south of the anticlinorium are reviewed. Two facies of the Lisburne formation, a calcarenite-hydroclastic limestone facies and...
Walter S. West
1953, Trace Elements Investigations 53
Farrell F. Barnes
1953, Open-File Report 53-10
The Little Susitna district, as defined in this report, occupies an area roughly 25 miles long and 3 miles wide on the north side of the lower (western) extremity of the Matanuska Valley in south-central Alaska (fig. 1). The district is bounded on the north by the Talkeetna Mountains, on...
Arthur Johnson, William Stephens Twenhofel
1953, Circular 280
Full development of a proposal to divert the headwaters of the Yukon River drainage from Canada into the Taiya River valley of Alaska would make available more than a half million kilowatts of electrical energy. Utilization of this block of power, for which there is at present no local market,...