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Page 430, results 10726 - 10750

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Not all publications have extents, not all extents are completely accurate
Geology of the Arctic slope of Alaska
Thomas G. Payne, W.W. Dana, W. A. Fischer, George Gryc, E. H. Lathram, R. H. Morris, H.N. Tappan, S.T. Yusler
1951, Oil and Gas Investigation Map 126
No abstract available....
Preliminary report on the stratigraphy and structure of the Shaviovik and upper Sagavanirktok Rivers area, Alaska
A. Samuel Keller, Robert L. Detterman
1951, Geological Investigations, Naval Petroleum Reserve No. 4, Alaska 36
During the 1951 field season, U. S. Geological Survey Navy Oil Unit party 1 conducted stratigraphic and structural studies of the rocks in the area between the westernmost fork of the Shaviovik River and the East Kuparuk River. This area is drained by the Sagavanirktok River and its major tributaries;...
Stratigraphy and structure of the southern foothills section between the Etivluk and Kiligwa Rivers
Irvin L. Tailleur, Bion H. Kent
1951, Geological Investigations, Naval Petroleum Reserve No. 4, Alaska 43
The part of the Southern Foothill section, Arctic foothills province, that lies beteween the Etivluk and Kiligwa Rivers was investigated by Navy Oil Unit party 6 during the 1950 field season, A belt about 16 miles wide and 60 miles long (approximately 800 square miles) was mapped in considerable detail...
Stratigraphy and structure of the upper Siksikpuk - Nanushuk Rivers area
William W. Patton Jr., A. Samuel Keller
1951, Geological Investigations, Naval Petroleum Reserve No. 4, Alaska 42
Structural and stratigraphic studies of tha rocks in the Siksikpuk and Nanushuk Rivers area were conducted by Navy Oil Unit party 2 during the summer field season of 1950. The field party consisted of two geologists, two field assistants, a cook, and a weasel mechanic. Three weasels were used for...
Gypsiferous deposits on Sheep Mountain, Alaska
Richard A. Eckhart
1950, Open-File Report 51-62
Gypsiferous deposits occur on the south side of Sheep fountain, 112 miles northeast of Anchorage via the Glenn Highway. Sheep Mountain is a high east trending, ridge, approximately 10 miles long and 3 miles wide. It is bordered on the west by Caribou Creek and on the east by Tahneta...
Reconnaissance of Lake Chackachamna, Alaska
Arthur Johnson
1950, Open-File Report 50-112
The purpose of this brief investigation was to obtain general information on Lake Chackachamna and its water-power possibilities which would serve as a guide in planning and executing future studies. Field investigation consisted of a flight to the lake in a small float plane (see Plate I-B) by the writer...
Water power resources of Scenery Creek near Petersburg, Alaska
Fred F. Lawrence
1950, Open-File Report 50-113
Due to high unit runoff, a good storage site, and a high concentration of fall, Scenery Lake presents a favorable power site. By building a tunnel three miles long from Scenery Grove to tap Scenery Lake at elevation 900 feet and a dam to raise Scenery Lake to elevation 1020...
Trace elements reconnaissance in the Jakolof Bay area, southern Alaska
Robert M. Moxham, Arthur E. Nelson
1950, Trace Elements Investigations 74-A
As a result of inquiries by prospectors in 1948 concerning radioactive ores in the vicinity of Jakolof Bay on the Kenai Peninsula in southern Alaska, the Geological Survey conducted a brief investigation during 1949. No radioactive material was found. Possibly a chromite stockpile in this locality was mistaken for pitchblende....