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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Format: | Text |
Language: | English |
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ScholarWorks@UTEP
2007
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Online Access: | https://scholarworks.utep.edu/dissertations/AAI1444084 |