Aftershock regions of Aleutian-Alaska earthquakes, 1938–2021

Carl Tape and Anthony Lomax

Journal of Geophysical Research: Solid Earth, 2022


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Supplemental materials

Previous studies of aftershock regions

AGU highlight written by JGR Editor Dr. Agnes Helmstetter

2022 EOS article led by USGS scientists

Aftershock regions for 11 mainshock earthquakes in this study. (image credit: Owen Larson, UAF/GINA)

1964-03-28 Mw 9.2

Mainshock and aftershocks of the 1964-03-28 Mw 9.2 earthquake in south-central Alaska. The large dots, colored by depth, are the relocated maximum likelihood epicenters; the small dots display the probability density function for each epicenter. Dashed lines depict the aftershock regions from Sykes et al. (1981); solid line depicts the aftershock regions from this study. Black lines depict active faults of Koehler et al. (2012). Magenta contours show the subduction interface for Slab 2.0 (Hayes et al., 2018), from 10 to 80 km in 10 km intervals. Thick red line is the trench (Krabbenhoeft et al., 2018).

1938-11-10 Mw 8.3

Mainshock and aftershocks of the 1938-11-10 Mw 8.3 earthquake near southwestern Alaska. The large dots, colored by depth, are the relocated maximum likelihood epicenters; the small dots display the probability density function for each epicenter. Dashed outlines depict the aftershock regions published in Sykes et al. (1981); solid black outlines depict the regions determined in this study, with the 1938 region emphasized. Thick red line depicts the trench plate boundary (Bird, 2003). Magenta contours show the subduction interface for Slab 2.0 (Hayes et al., 2018), from 10 to 80 km in 10 km intervals. Maximum likelihood epicenters for the mainshocks are plotted as stars. Geographic labels include Unga Island (U), Shumagin Islands (S), and Kodiak Island (K).