Adsorption equilibria between earth materials and radionuclides, Cape Thompson, Alaska
J.H. Baker, W.A. Beetem, J.S. Wahlberg
1964, Open-File Report 64-5
The concept and the derivation of a distribution coefficient are developed. Ion exchange and the nature of competition among cations are given. Distribution coefficients for carrier-free cesium, strontium, and iodine were determined on 17 samples collected during July, 1961, in the vicinity of Cape Thompson, northwestern Alaska. High percentage uptake...
Geology of the Killik-Etivluk Rivers region, Alaska
R.M. Chapman, R.L. Detterman, M. D. Mangus
1964, Professional Paper 303-F
Quaternary geology of the Kenai Lowland and glacial history of the Cook Inlet region, Alaska
Thor N. V. Karlstrom
1964, Professional Paper 443
The Kenai Lowland is part of the Cook Inlet Lowland physiographic subprovince that borders Cook Inlet, a major marine reentrant along the Pacific Ocean coastline of south-central Alaska. The Cook Inlet Lowland occupies a structural trough underlain by rocks of Tertiary age and mantled by Quaternary deposits of varying thicknesses....
Gubik Formation of Quaternary age in northern Alaska
R. F. Black
1964, Professional Paper 302-C
Preliminary geologic map of the Charley River quadrangle, east-central Alaska
Earl E. Brabb, Michael Churkin
1964, Open-File Report 64-23
Pre-tertiary orogenic and plutonic intrusive activity in central and northeastern Oregon
T. P. Thayer, C. E. Brown
1964, Geological Society of America Bulletin (75) 1255-1261
Pre-Tertiary rocks of the Blue Mountain region of central and northeastern Oregon comprise three major sedimentary and volcanic sequences and two distinct intrusive magma series. The ages of the sedimentary-volcanic sequences are Paleozoic, Late Triassic-Late Jurassic, and middle Cretaceous (Albian to Cenomanian), respectively. The earlier intrusive magma series ranges in composition from peridotite to albite granite and was emplaced during the major...
Magnetic disturbances preceding the 1964 Alaska earthquake
George W. Moore
1964, Nature (203) 508-509
THROUGH a fortunate circumstance, a recording magnetometer was operating in the city of Kodiak, 30 km north-west of the surface trace of a fault zone along which movement occurred at the time when the earthquake occurred in Alaska on March 27, 1964. Fortunately, too, the instrument...
Apparent right-lateral separation on Chatham Strait Fault, southeastern Alaska
Ernest H. Lathram
1964, GSA Bulletin (75) 249-252
Right-lateral separation of about 120 miles along Chatham Strait Fault is suggested by apparent displacement of major geologic features on opposite sides of the fault....
Oil and gas fields of the United States, exclusive of Alaska and Hawaii
Sophie D. Vlissides, Barbara A. Quirin
1964, Report
No abstract available....
Mineral resources of Alaska, 1959-63
1964, Bulletin 1108
No abstract available....
Bouguer gravity anomaly map of the United States (exclusive of Alaska and Hawaii)
American Geophysical Union, U.S. Geological Survey
1964, Report
No abstract available....
Stratigraphy and petrography of the Pybus-Gambier area, Admiralty Island, Alaska
R. A. Loney
1964, Bulletin 1178
No abstract available....
Potassium-argon and lead-alpha ages of plutonic rocks, Bokan Mountain area, Alaska
M. A. Lanphere, E.M. MacKevett Jr., T. W. Stern
1964, Science (145) 705-707
Most of the granitic rocks in the Bokan Mountain area, southeastern Alaska, are early Paleozoic (probably Ordovician) judged by potassium-argon and lead-alpha age measurements. The Bokan Mountain Granite, the youngest intrusive unit in the area, belongs to a Mesozoic plutonic episode. These age measurements are the first direct evidence for...
Preliminary geologic map of the McCarthy C-5 quadrangle, Alaska
E.M. MacKevett Jr.
1963, IMAP 406
Geology of the Imuruk Lake area, Seward Peninsula, Alaska
David Moody Hopkins
1963, Bulletin 1141-C
Beryllium deposits of the western Seward Peninsula, Alaska
C.L. Sainsbury
1963, Circular 479
Deposits of beryllium ore in the Lost River area of the western Seward Peninsula, Alaska, consist of replacement veins, pipes, and stringer lodes is limestone in a zone about 7 miles long and 2 to 3 miles wide which is faulted and intruded by dikes and stocks. The ores are...
An aeromagnetic reconnaissance of the Cook Inlet area, Alaska
Arthur Grantz, Isidore Zietz, G.E. Andreasen
1963, Professional Paper 316-G
No abstract available....
Reconnaissance geology of northern Baranof Island, Alaska
Henry C. Berg, D.W. Hinckley
1963, Bulletin 1141-O
Geology of the eastern part of the Mount Fairweather quadrangle, Glacier Bay, Alaska
Darwin L. Rossman
1963, Bulletin 1121-K
Geology and petrology of two stocks of layered gabbro in the Fairweather Range, Alaska
Darwin L. Rossman
1963, Bulletin 1121-F
Preliminary geologic map of the Umiat-Maybe Creek region, Alaska
William Peters Brosge, Charles L. Whittington
1963, Open-File Report 63-10
No abstract available....
Field guide to halobiid and monotid pelecypods of the Alaskan Triassic
Norman J. Silberling
1963, Open-File Report 63-119
Geology and ore deposits of the Bokan Mountain uranium-thorium area, southeastern Alaska
E.M. MacKevett Jr.
1963, Bulletin 1154
Principal lakes of the United States
Conrad D. Bue
1963, Circular 476
The United States has about 250 fresh-water lakes that are known to have surface areas of 10 square miles or more. Nearly 100 of these are in Alaska, and 100 in Minnesota, Wisconsin, Michigan, New York,, and Maine. Thirty-four fresh-water lakes, exclusive of the Great Lakes, are known to have maximum...
Ground-water resources of the Fairbanks area, Alaska
Dagfin John Cederstrom
1963, Water Supply Paper 1590
