![]() The work also indicated some notable areas of "very high" stress loading of the fault, especially in the shallower regions of the model fault plane. Modeling the Simeonof quake's stress buildup shows that the Chignik hypocenter, the location inside the earth at which an earthquake rupture begins, is embedded in an area of increased stress change, consistent with what scientists know about how earthquakes are triggered. The researchers studied data to assess the impact of the stress changes caused by the 2020 Simeonof quake, particularly as they might relate to the Chignik quake's rupture site. "This could be a case study to understand how adjacent earthquake patches could be activated by a significant release of energy that has accumulated through plate motion," Parameswaran said. No major earthquakes had been recorded in the Shumagin Gap, a space about 100 miles long in the subduction zone, until the 20 quakes. It continues along the south side of the islands and the Alaska Peninsula, curves upward across the Kenai Peninsula and encompasses the Anchorage area and Prince William Sound. That 1,900-mile subduction zone, where the Pacific tectonic plate slides under the North American plate, starts at the tip of the Aleutian Islands. The two quakes and their aftershocks occurred in the Shumagin Gap, a spot near the Shumagin Islands in a known band of historical ruptures. It registered at magnitude 8.2, was located south of the Alaska Peninsula and northeast of the Simeonof quake and ruptured eastward. The second quake, the Chignik event, occurred just over one year later on July 28, 2021. It registered at magnitude 7.8, struck near the Shumagin Islands south of the Alaska Peninsula and ruptured westward. The first of the two major quakes, known as the Simeonof event, occurred July 21, 2020. This patch then ruptures and increases the stress on the next patch in the fault, like delayed dominos," Grapenthin said. "One large earthquake increases the stress on the neighboring part of the megathrust fault. They add that their research will help scientists better understand stress transfer and earthquake triggering in the region and in general. The researchers also conclude that the two deep earthquakes on the Aleutian-Alaska megathrust fault, where the Pacific plate is sliding beneath the North American plate, may have brought shallow portions of the fault closer to failure. ![]() Parameswaran is among the four co-authors. The research was published today by the journal Science Advances in a paper jointly led by University of Alaska Fairbanks Geophysical Institute associate professor Ronni Grapenthin and Michigan State University assistant professor Julie Elliott. ![]()
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