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11322 results.

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Page 401, results 10001 - 10025

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Publication Extents

Not all publications have extents, not all extents are completely accurate
Geomagnetic polarity epochs: Nunivak Island, Alaska
A. Cox, G. B. Dalrymple
1967, Earth and Planetary Science Letters (3) 173-177
New paleomagnetic and potassium-argon dating measurements have been made of basalt flows from Nunivak Island, Alaska, with the following results. (1) The best estimate of the age of the Brunhes/Matuyama polarity epoch boundary is found to be 0.694 m.y. (2) The best...
The Alaska earthquake of 1964
W. R. Hansen
1967, Nature (215) 348-351
Now that the dust has settled it is possible to assess the long term effects of the Alaskan earthquake on March 27, both on the activities of man and on the wild life of the State....
The Alaska earthquake, March 27, 1964: effects on hydrologic regimen
Roger M. Waller, R. W. Coble, Austin Post, Arthur McGarr, Robert C. Vorhis
1966, Professional Paper 544
This is the fourth 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...
Bald eagle pesticide relations
L.F. Stickel, N.J. Chura, P.A. Stewart, C. M. Menzie, R. M. Prouty, W. L. Reichel
1966, Conference Paper, Transactions of the North American Wildlife and Natural Resources Conference
No abstract available....
Effects of the March 1964 Alaska earthquake on the hydrology of south-central Alaska
Roger M. Waller
1966, Professional Paper 544-A
The earthquake of March 27, 1964, greatly affected the hydrology of Alaska and many other parts of the world. Its far-reaching effects were recorded as water-level fluctuations in gages operated on water wells and streams. The close-in effects were even more striking, however; sediment-laden ground water erupted at the surface,...
Effects of the earthquake of March 27, 1964, in the Copper River Basin area, Alaska
Oscar J. Ferrians Jr.
1966, Professional Paper 543-E
The Copper River Basin area is in south-central Alaska and covers 17,800 square miles. It includes most of the Copper River Basin and parts of the surrounding Alaska Range and the Talkeetna, Chugach, and Wrangell Mountains. On March 27, 1964, shortly after 5:36 p.m. Alaska standard time, a great earthquake having...
Effects of the earthquake of March 27, 1964, in the Homer area, Alaska
Roger M. Waller, Kirk W. Stanley
1966, Professional Paper 542-D
The March 27, 1964, earthquake shook the Homer area for about 3 minutes. Land effects consisted of a 2- to 6-foot subsidence of the mainland and Homer Spit, one earthflow at the mouth of a canyon, several landslides on the Homer escarpment and along the sea bluffs, and minor fissuring...
Effects of the earthquake of March 27, 1964, at Valdez, Alaska
Henry Welty Coulter, Ralph R. Migliaccio
1966, Professional Paper 542-C
Valdez is situated on the seaward edge of a large outwash delta composed of a thick section of saturated silty sand and gravel. The earthquake of March 27, 1964, triggered a massive submarine slide, involving approximately 98 million cubic yards of material that destroyed the harbor facilities and nearshore installations....
Effects of the March 1964 Alaska earthquake on the hydrology of the Anchorage area, Alaska
Roger M. Waller
1966, Professional Paper 544-B
The Anchorage hydrologic system was greatly affected by the seismic shock. Immediate but temporary effects included increased stream discharge, seiche action on lakes, and fluctuations in ground-water levels. Generally, ground-water levels were residually lowered after the initial period of fluctuation. This lowering is attributed either to changes in the discharge...
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...
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,...
Slide-induced waves, seiching and ground fracturing caused by the earthquake of March 27, 1964 at Kenai Lake, Alaska
David S. McCulloch
1966, Professional Paper 543-A
The March 27, 1964, earthquake dislodged slides from nine deltas in Kenai Lake, south-central Alaska. Sliding removed protruding parts of deltas-often the youngest parts-and steepened delta fronts, increasing the chances of further sliding. Fathograms show that debris from large slides spread widely over the lake floor, some reaching the toe...
Reservoirs in the United States
R.O.R. Martin, Ronald L. Hanson
1966, Water Supply Paper 1838
This report summarizes the storage capacities and related data of reservoirs and controlled natural lakes for the contermimous United States, Alaska, Hawaii, and the Commonwealth of Puerto Rico. Data are given for all storage facilities having a usable capacity of 5,000 acre-feet or more and completed or under construction as...