Bluesky Facebook Reddit Email

Unraveling the physics behind Kamchatka's 73-year earthquake cycle

02.04.26 | University of Tsukuba

Apple MacBook Pro 14-inch (M4 Pro)

Apple MacBook Pro 14-inch (M4 Pro) powers local ML workloads, large datasets, and multi-display analysis for field and lab teams.

Tsukuba, Japan—In July 2025, a massive earthquake with a magnitude of 8.8-8.9 struck off the Kamchatka Peninsula, Russia. Notably, this event ruptured nearly the same region as the M9.0-class earthquake of 1952, yet the recurrence interval was only 73 years—far shorter than expected for such giant earthquakes, thereby challenging conventional seismological understanding.

In this study, the researchers estimated the rupture process of the 2025 Kamchatka earthquake using the Potency Density Tensor Inversion (PDTI) method, originally developed at the University of Tsukuba. The analysis showed that the fault slip reached 9-12 m across a broad area, substantially exceeding the ~6 m of slip deficit accumulated since 1952, and that slip accelerated twice within the large-slip zone. Following the mainshock, low-angle normal-faulting aftershocks, opposite to the direction of plate convergence, were concentrated near the plate boundary. This observation indicates that dynamic overshoot occurred during the mainshock, leading to a local reversal of shear stress. Based on these results, the team concluded that residual strain left unresolved by the 1952 earthquake combined with post-1952 strain, and that this accumulated strain was largely released during the 2025 event.

The study emphasizes that variations in rupture physics and stress release can leave substantial residual strain after a major earthquake, thereby disrupting regular recurrence intervals. These findings indicate that real-world megathrust earthquakes exhibit complex, nonperiodic behavior that cannot be fully explained by conventional seismic-cycle models. The results have important implications for long-term earthquake forecasting in subduction zones worldwide, including the Nankai Trough.

###
This research is supported by Japan Society for the promotion of Science (JSPS) Grantin-Aid for Scientific Research (B) 25K01075.

Title of original paper:
Breaking the Cycle: Short Recurrence and Overshoot of an M9-class Kamchatka Earthquake

Journal:
Seismica

DOI:
10.26443/seismica.v4i2.2012

Professor YAGI, Yuji
Institute of Life and Environmental Sciences, University of Tsukuba

Professor FUKAHATA, Yukitoshi
Disaster Prevention Research Institute, Kyoto University

TAKAGAWA, Tomohiro, PhD
Head of Tsunami and Storm Surge Research Group, Port and Airport Research Institute, National Institute of Maritime, Port and Aviation Technology

Professor TODA, Shinji
International Research Institute of Disaster Science (IRIDeS), Tohoku University

Institute of Life and Environmental Sciences

Seismica

10.26443/seismica.v4i2.2012

Breaking the Cycle: Short Recurrence and Overshoot of an M9-class Kamchatka Earthquake

30-Nov-2025

Keywords

Article Information

Contact Information

KAMOSHITA Kimio
University of Tsukuba
kohositu@un.tsukuba.ac.jp

Source

How to Cite This Article

APA:
University of Tsukuba. (2026, February 4). Unraveling the physics behind Kamchatka's 73-year earthquake cycle. Brightsurf News. https://www.brightsurf.com/news/1WROP92L/unraveling-the-physics-behind-kamchatkas-73-year-earthquake-cycle.html
MLA:
"Unraveling the physics behind Kamchatka's 73-year earthquake cycle." Brightsurf News, Feb. 4 2026, https://www.brightsurf.com/news/1WROP92L/unraveling-the-physics-behind-kamchatkas-73-year-earthquake-cycle.html.