Marco Aquino-Lopez Sean Bemis Peter J. Haeussler Jessalyn Ginnaty Carl Tape 2026 <p><span>The 2002 <i>M</i>_w</span><span>&nbsp;7.9 earthquake in central Alaska ruptured 340&nbsp;km on three faults—Susitna Glacier thrust fault, Denali fault, Totschunda fault—crossing both the Richardson Highway and the Alaska Pipeline. Its occurrence prompted renewed interest in historical large earthquakes that possibly originated on the Denali fault. One of these earthquakes was a <i>M</i>_s</span><span>&nbsp;7.2 event on July 7, 1912, which we revisit with two approaches: (1) probabilistic relocation of the epicenter using globally recorded arrival times, and (2) compilation and reassessment of shaking intensity reports to estimate a macroseismic epicenter. Our preferred instrumental epicenter is west of the Parks Highway and in agreement with the maximum‐reported shaking, which was from the Parker–Browne expedition of Denali. We also relocated a <i>M</i>_s</span><span>_&nbsp;6.4 aftershock, whose epicenter is 11&nbsp;km from the mainshock. Candidate faults for the 1912 earthquake include the Denali fault, the McLeod Creek thrust fault, and the Kantishna Hills thrust fault. Future analysis of active faults, paleoseismic results, 1912 instrumental data, and 1912 felt reports may help in interpreting the fault and mechanism of the 1912 earthquake.</span></p> application/pdf 10.1785/0120250150 en Seismological Society of America The 1912 Ms 7.2 earthquake in the Denali region of central Alaska article