M 7.1 - off the east coast of Honshu, Japan
- 2013-10-25 17:10:19 (UTC)
- 37.156°N 144.661°E
- 35.0 km depth
Interactive Map Regional Information Felt Report - Tell Us! 000160Responses Contribute to citizen science. Please tell us about your experience.
- Did You Feel It?
VImmi Community Internet Intensity Map - ShakeMap
IVmmi Estimated Intensity Map - PAGER
GREEN Estimated Economic Losses Estimated Fatalities Origin - Review Status
- REVIEWED
- Magnitude
- 7.1 mww
- Depth
- 35.0 km
- Time
- 2013-10-25 17:10:19 UTC
Moment Tensor Fault Plane Solution Finite Fault Cross-section of slip distribution. Tsunami U.S. Tsunami Warning System To view any current tsunami advisories for this and other events please visit https://www.tsunami.gov.
View Nearby Seismicity - Time Range
± Three Weeks - Search Radius
250.0 km - Magnitude Range
≥ 4.0
Contributors US
USGS National Earthquake Information Center, PDE
Tectonic Summary
The October 25, 2013, M 7.1 earthquake offshore of Honshu, Japan, occurred as the result of normal faulting in the shallow oceanic crust of the Pacific plate. The earthquake occurred outboard (east) of the Japan Trench, which marks the sea-floor expression of the subduction zone plate boundary between the Pacific and North America plates, and is immediately up-dip of the source region of the March 2011 M 9.0 Tohoku earthquake. At the location of this earthquake, the Pacific plate moves westward with respect to the North America plate at a rate of 83 mm/yr before subducting beneath the island of Honshu. Note that some authors divide this region into several microplates that together define the relative motions between the larger Pacific, North America and Eurasia plates; these include the Okhotsk and Amur microplates that are part of North America and Eurasia, respectively.
The location, depth, and focal mechanism solutions of the October 25, 2013, event are consistent with normal faulting rupture near the outer-arc high of the Japan Trench. Of the two possible fault orientations of the focal mechanism solution, finite-fault modeling of globally recorded seismic data is more consistent with slip on the north-northeast-striking fault. In this region, normal faulting is encouraged by the bending of the Pacific plate as it enters the subduction zone and by stresses transferred from the locked subduction thrust interface to the west. Since the March 2011 Tohoku earthquake, two large events of M 7.7 and M 7.3 have occurred in the vicinity of the October 25, 2013, earthquake. The M 7.7 event, on March 11, 2011, was also a normal faulting event near the outer-arc high and occurred 95 km north of the October 25th event. The M 7.3 event, on December 7, 2012, was a more complex earthquake resulting from thrust motion near the trench 100 km to the northwest of the October 25th earthquake. Ten additional events, ranging in magnitude from M 6.1 to 6.4, have occurred over the same time period in this region east of the Japan Trench.
Hayes et al. (2016) Tectonic summaries of magnitude 7 and greater earthquakes from 2000 to 2015, USGS Open-File Report 2016-1192. (5.2 MB PDF)
Summary Poster