Gravity survey and regional geology of the Prince William Sound epicentral region, Alaska
J. E. Case, D.F. Barnes, George Plafker, S. L. Robbins
1966, Professional Paper 543-C
Sedimentary and volcanic rocks of Mesozoic and early Tertiary age form a roughly arcuate pattern in and around Prince William Sound, the epicentral region of the Alaska earthquake of 1964. These rocks include the Valdez Group, a predominantly slate and graywacke sequence of Jurassic and Cretaceous age, and the Orca...
Potential effects of Project Chariot on local water supplies, northwestern Alaska
Arthur M. Piper
1966, Professional Paper 539
The Alaska earthquake, March 27, 1964: Field investigations and reconstruction effort
Wallace R. Hansen, Edwin B. Eckel, William E. Schaem, Robert E. Lyle, Warren George, Genie Chance
1966, Professional Paper 541
One of the greatest geotectonic events of our time occurred in southern Alaska late in the afternoon of March 27, 1964. Beneath a leaden sky, the chill of evening was just settling over the Alaskan countryside. Light snow was falling on some communities. It was Good Friday, schools were closed,...
Geologic map of the Fairbanks quadrangle, Alaska
T. L. Pewe, Clyde Wahraftig, F. R. Weber
1966, IMAP 455
Geologic map of the Kwiguk and Black quadrangles, western Alaska
J. M. Hoare, W. H. Condon
1966, IMAP 469
Regional geology of the Kateel River quadrangle, Alaska
W. W. Patton Jr.
1966, IMAP 437
Regional geologic map of the Hughes quadrangle, Alaska
W. W. Patton Jr., T. P. Miller
1966, IMAP 459
Outcrop/geologic maps of the Nuka-Etivluk region, northern Alaska
I.L. Tailleur, B.H. Kent Jr., H. N. Reiser
1966, Open-File Report 66-128
Geomorphic effects of the earthquake of March 27, 1964 in the Martin-Bering Rivers area, Alaska
Samuel J. Tuthill, Wilson M. Laird
1966, Professional Paper 543-B
The Alaska earthquake of March 27, 1964, caused widespread geomorphic changes in the Martin-Bering Rivers area-900 square miles of uninhabited mountains, alluvial flatlands, and marshes north of the Gulf of Alaska, and east of the Copper River. This area is at lat 60°30’ N. and long 144°22’ W., 32 miles...
Geology of the Umiat-Maybe Creek region, Alaska. Part 3, areal geology
W. P. Brosge, R. H. Morris
1966, Professional Paper 303-H
No abstract available....
Geologic effects of the March 1964 earthquake and associated seismic sea waves on Kodiak and nearby islands, Alaska
George Plafker, Reuben Kachadoorian
1966, Professional Paper 543-D
Kodiak Island and the nearby islands constitute a mountainous landmass with an aggregate area of 4,900 square miles that lies at the western border of the Gulf of Alaska and from 20 to 40 miles off the Alaskan mainland. Igneous and metamorphic rocks underlie most of the area except for...
Effects of toxaphene on fishes and bottom fauna of Big Kitoi Creek, Afognak Island, Alaska
William R. Meehan, William L. Sheridan
1966, Investigations in Fish Control 8
Phytoecology of a greenstone habitat at Eagle, Alaska
Hansford T. Shacklette
1966, Bulletin 1198-F
Tertiary stratigraphy and paleobotany of the Cook Inlet region, Alaska
J. A. Wolfe, D.M. Hopkins, E. B. Leopold
1966, Professional Paper 398-A
No abstract available....
Proceedings of the first international scientific meeting on the polar bear
Bureau Of Sport Fisheries And Wildlife, University Of Alaska
1966, Resource Publication 16
No abstract available....
Map of geologic materials, Anchorage and vicinity, Alaska
Ernest Dobrovolny, Henry R. Schmoll
1966, Open-File Report 66-25
Effects of toxaphene on fishes and bottom fauna of Big Kitoi Creek, Afognak Island, Alaska
William R. Meehan, William L. Sheridan
1966, Resource Publication 12
No abstract available....
Geologic map and stratigraphic sections, Porcupine River Canyon, Alaska
W. P. Brosge, H. N. Reiser, J.T. Dutro Jr., Michael Churkin Jr.
1966, Open-File Report 66-10
Micropaleontology of the Mesozoic rocks of northern Alaska
H. R. Bergquist
1966, Professional Paper 302-D
Magnetic data on the structure of the central Arctic Region
E. R. King, I. Zietz, L.R. Alldredge
1966, Geological Society of America Bulletin (77) 619-646
A study of 23,000 miles of total intensity aeromagnetic profiles in the central Arctic has been made by the U. S. Geological Survey and the U. S. Coast and Geodetic Survey. The profiles were flown at 20,000 feet above sea level and cover approximately 1,350,000 square miles of the Arctic Ocean between the North Pole...
Exposure of basement rock on the continental slope of the Bering Sea
D.W. Scholl, E. C. Buffington, D.M. Hopkins
1966, Science (153) 992-994
Profiles of repetitive seismic reflections reveal that the Bering continental slope, outer shelf, and rise overlay an acoustically reflective "basement" which extends at least 750 kilometers parallel to the trend of the slope. This acoustic basement is usually covered by several hundred meters of stratified sediments at the top and...
Water resources data for Alaska
Water Resources Division, U.S. Geological Survey
1966, Report
No abstract available....
Evidence for an early recent warm interval in northwestern Alaska
David S. McCulloch, David M. Hopkins
1966, Geological Society of America Bulletin (77) 1089-1108
A warm interval that began at least 10,000 years ago and lasted until at least 8300 years ago is recorded in the coastal tundra covered area of northwestern Alaska by the presence of fossil wood of tree size or tree species, fossil beaver-gnawed wood found beyond the modern range of beaver, evidence of ice-wedge melting, buried soils, and soils that...
Effects of toxaphene on fishes and bottom fauna of Big Kitoi Creek, Afognak Island, Alaska
W.R. Meehan, W.L. Sheridan
1966, Investigations in Fish Control 8
Abstract not submitted to date...
Tertiary plants from the Cook Inlet region, Alaska
J. A. Wolfe
1966, Professional Paper 398-B
No abstract available....
