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Location:
Magnitude:
7.0
Time:
20 Mar 2021 09:09:43
Depth:
43.0
M 7.0+:
There are 7 swarms found nearby.
2008
S20080614.1(99.2km)
13 Jun
3 days 16 hours
67 earthquakes
2011
PS20110309.1(38.8km)
9 Mar
7 days 12 hours
159 earthquakes
PS20110311.3(64.3km)
11 Mar
1 day 17 hours
44 earthquakes
PS20110311.8(56.8km)
11 Mar
9 hours
5 earthquakes
PS20110319.2(99.3km)
18 Mar
1 day 17 hours
8 earthquakes
2021
S20210214.1(91.8km)
13 Feb
3 days 9 hours
49 earthquakes
2022
PS20220316.1(74.0km)
16 Mar
1 hours
7 earthquakes
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Seismic Activity and Geological Context of the Ishinomaki Region, Japan

The Ishinomaki region lies along Japan's northeastern Pacific coast in Miyagi Prefecture, within the tectonically active Tohoku district. This area sits above the Japan Trench subduction zone, where the Pacific Plate converges with and subducts beneath the Okhotsk Plate at a rate of approximately 8–9 cm per year. The resulting megathrust faulting produces frequent large-magnitude earthquakes, often at depths between 20 and 50 km, along with associated tsunami hazards. A magnitude 7.0 earthquake struck 30 km east of Ishinomaki on 20 March 2021 at 09:09 local time, with a focal depth of 43 km. This event occurred within a well-documented seismic gap influenced by post-2011 stress redistribution. The region has experienced multiple strong earthquakes since 2000, underscoring its persistent activity along the subduction interface. Notable events include the magnitude 7.3 quake 57 km ENE of Namie on 16 March 2022, located 82 km from the 2021 Ishinomaki epicenter. Earlier activity featured a magnitude 7.1 event 73 km ENE of Namie on 13 February 2021 (81 km distant), a magnitude 7.1 shock 29 km ESE of Ishinomaki on 7 April 2011 (20 km distant), and the magnitude 9.1 Great Tohoku Earthquake of 11 March 2011 (65 km distant). Additional significant shocks comprise the magnitude 7.2 event 66 km ESE of Ishinomaki on 16 August 2005 (39 km distant) and the magnitude 7.0 quake 27 km SSW of Ōfunato on 26 May 2003 (44 km distant). These occurrences reflect both interplate thrust faulting and intraslab seismicity within the subducting Pacific slab. Geological studies indicate that the 2011 Tohoku mainshock altered regional stress fields, triggering aftershocks and moderate events like the 2021 sequence for years afterward. The subducting plate's variable coupling and the presence of seamounts on the incoming Pacific Plate contribute to heterogeneous rupture patterns. Historical records show recurrence intervals for magnitude 7+ events on the order of decades in this segment of the Japan Trench. Ongoing monitoring by seismic networks reveals continued low-level activity, with the 2021 event exemplifying the region's capacity for moderate-to-large earthquakes at intermediate depths. Preparedness measures, including updated building codes and tsunami defenses implemented after 2011, address the persistent risk posed by this subduction setting.

References

USGS Earthquake Catalog (events as listed in provided data)
Japan Meteorological Agency seismic reports
Geological Survey of Japan tectonic summaries