Publications
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Erosion and deposition on a beach raised by the 1964 earthquake Montague Island, Alaska Erosion and deposition on a beach raised by the 1964 earthquake Montague Island, Alaska
During the 1964 Alaska earthquake, tectonic deformation uplifted the southern end of Montague Island as much as 33 feet or more. The uplifted shoreline is rapidly being modified by subaerial and marine processes. The new raised beach is formed in bedrock, sand, gravel, and deltaic bay-head deposits, and the effect of each erosional process was measured in each material. Fieldwork was...
Authors
M. J. Kirkby, Anne V. Kirkby
Tectonics of the March 27, 1964, Alaska earthquake Tectonics of the March 27, 1964, Alaska earthquake
The March 27, 1964, earthquake was accomp anied by crustal deformation-including warping, horizontal distortion, and faulting-over probably more than 110,000 square miles of land and sea bottom in south-central Alaska. Regional uplift and subsidence occurred mainly in two nearly parallel elongate zones, together about 600 miles long and as much as 250 miles wide, that lie along the...
Authors
George Plafker
Geologic structure between the Murray fracture zone and the Transverse Ranges Geologic structure between the Murray fracture zone and the Transverse Ranges
The Murray fracture has been thought to extend ashore into the Transverse Ranges of California, but a geophysical study shows no evidence of structural continuity between these features. Instead, basement morphology typical of the Murray fracture zone ends where its known magnetic and bathymetric expression dies out. Similarly, east-west Transverse Range structures change direction so...
Authors
Roland E. von Huene
The Alaska earthquake, March 27, 1964: Effects on communities The Alaska earthquake, March 27, 1964: Effects on communities
This is the second 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 field seasons. The 1964 Great Alaska earthquake was the largest earthquake...
Authors
Wallace R. Hansen, Reuben Kachadoorian, Henry W. Coulter, Ralph R. Migliaccio, Roger M. Waller, Kirk W. Stanley, Richard W. Lemke, George Plafker, Edwin B. Eckel, Lawrence R. Mayo
Effects of the Alaska earthquake of March 27, 1964, on shore processes and beach morphology Effects of the Alaska earthquake of March 27, 1964, on shore processes and beach morphology
Some 10,000 miles of shoreline in south-central Alaska was affected by the subsidence or uplift associated with the great Alaska earthquake of March 27, 1964. The changes in shoreline processes and beach morphology that were suddenly initiated by the earthquake were similar to those ordinarily caused by gradual changes in sea level operating over hundreds of years, while other more...
Authors
Kirk W. Stanley
Surface seismic measurements of the Project GASBUGGY explosion at intermediate distance ranges Surface seismic measurements of the Project GASBUGGY explosion at intermediate distance ranges
Project GASBUGGY was an experiment performed by the Atomic Energy Commission, the El Paso Natural Gas Company, and the Bureau of Mines, U.S. Department of the Interior, to determine the effectiveness of a method for increasing the recovery of natural gas by large-scale fracturing of a gas-bearing formation with an underground nuclear explosion. The Project GASBUGGY nuclear explosive of...
Authors
David H. Warren, W. H. Jackson
Seismic seiches from the March 1964 Alaska earthquake Seismic seiches from the March 1964 Alaska earthquake
Seismic seiches caused by the Alaska earthquake of March 27, 1964, were recorded at more than 850 surface-water gaging stations in North America and at 4 in Australia. In the United States, including Alaska and Hawaii, 763 of 6,435 gages registered seiches. Nearly all the seismic seiches were recorded at teleseismic distance. This is the first time such far-distant effects have been...
Authors
Arthur McGarr, Robert C. Vorhis
Effects of the earthquake of March 27, 1964, on the Alaska highway system Effects of the earthquake of March 27, 1964, on the Alaska highway system
The great earthquake that struck Alaska about 5:36 p.m., Alaska standard time, Friday, March 27, 1964 (03:36:1.3.0, Greenwich mean time, March 28, 1964), severely crippled the highway system in the south-central part of the State. All the major highways and most secondary roads were impaired. Damage totaled more than $46 million, well over $25 million to bridges and nearly $21 million to...
Authors
Reuben Kachadoorian
The Alaska earthquake, March 27, 1964: effects on transportation, communications, and utilities The Alaska earthquake, March 27, 1964: effects on transportation, communications, and utilities
This is the forth 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 field seasons. The 1964 Great Alaska earthquake was the largest earthquake...
Authors
Malcolm H. Logan, Lynn R. Burton, Edwin B. Eckel, Reuben Kachadoorian, David S. McCulloch, Manuel G. Bonilla
Effect of the earthquake of March 27, 1964, on the Eklutna Hydroelectric Project, Anchorage, Alaska, with a section on television examination of earthquake damage to underground communication and electrical systems in Anchorage Effect of the earthquake of March 27, 1964, on the Eklutna Hydroelectric Project, Anchorage, Alaska, with a section on television examination of earthquake damage to underground communication and electrical systems in Anchorage
The March 27, 1964, Alaska earthquake and its associated aftershocks caused damage requiring several million dollars worth of repair to the Eklwtna Hydroelectric Project, 34 miles northeast of Anchorage. Electric service from the Eklutna powerplant was interrupted during the early phase of the March 27 earthquake, built was restored (intermittently) until May 9,1964, when the plant was...
Authors
Malcolm H. Logan, Lynn R. Burton
Effects of the earthquake of March 27, 1964, at Seward, Alaska Effects of the earthquake of March 27, 1964, at Seward, Alaska
Seward, in south-central Alaska, was one of the towns most devastated by the Alaska earthquake of March 27, 1964. The greater part of Seward is built on an alluvial fan-delta near the head of Resurrection Bay on the southeast coast of the Kenai Peninsula. It is one of the few ports in south-central Alaska that is ice free all year, and the town’s economy is almost entirely dependent upon...
Authors
Richard W. Lemke
Effects of the earthquake of March 27, 1964, on air and water transport, communications, and utilities systems in south-central Alaska Effects of the earthquake of March 27, 1964, on air and water transport, communications, and utilities systems in south-central Alaska
The earthquake of March 27, 1964, wrecked or severely hampered all forms of transportation, all utilities, and all communications systems over a very large part of south-central Alaska. Effects on air transportation were minor as compared to those on the water, highway, and railroad transport systems. A few planes were damaged or wrecked by seismic vibration or by flooding. Numerous...
Authors
Edwin B. Eckel