Spatial and temporal study of the seismicity of the hypocentral region of the Great 1964 Alaskan Earthquake

In March 28, 1964, the largest earthquake (9.2 MW) in North America occurred in south-central Alaska (SCA). The epicenter of this great earthquake was in Prince William Sound (PWS) (Figure 1). The earthquake occurred as a result of underthrusting of the Pacific plate and Yakutat Block beneath the No...

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Bibliographic Details
Main Author: De La Pena, Alejandro
Format: Text
Language:English
Published: ScholarWorks@UTEP 2007
Subjects:
Online Access:https://scholarworks.utep.edu/dissertations/AAI1444084