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Location:
Magnitude:
7.3
Time:
27 Aug 2012 04:37:19
Depth:
28.0
M 7.0+:
There are 4 swarms found nearby.
2001
PS20010115.1(99.9km)
14 Jan
2 days 2 hours
9 earthquakes
2012
27 Aug
1 day 4 hours
7 earthquakes
2021
S20210922.2(80.7km)
22 Sep
4 days 3 hours
50 earthquakes
2023
S20230719.1(66.7km)
18 Jul
12 days 21 hours
265 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Seismic Hazards in El Salvador: The 2012 Magnitude 7.3 Earthquake

El Salvador lies within the tectonically active Pacific Ring of Fire, where the Cocos Plate subducts beneath the Caribbean Plate along the Middle America Trench. This convergent boundary generates frequent earthquakes and volcanic activity across Central America. The region experiences both interplate thrust events at shallow depths and deeper intraslab earthquakes within the subducting slab. On 27 August 2012 at 04:37 UTC, a magnitude 7.3 earthquake struck 126 km south of Puerto El Triunfo at a depth of 28 km. This event occurred in the offshore subduction zone, consistent with the regional pattern of seismicity driven by plate convergence. A comparable magnitude 7.3 earthquake took place on 14 October 2014, located 74 km south of Intipucá and approximately 66 km from the 2012 epicenter. Both events highlight the persistent seismic productivity along this segment of the margin since 2000. Historically, El Salvador has recorded destructive earthquakes linked to the same subduction dynamics. Notable examples include the 2001 sequence, which produced widespread damage from both mainshocks and triggered landslides. The 2012 and 2014 events fit within this continuum of moderate-to-large thrust and intraslab ruptures that characterize the margin. Depths around 28 km place the 2012 hypocenter near the transition between the locked interface and the freely slipping zone, a common source region for intermediate-depth events. Ground shaking from these offshore quakes can propagate efficiently to coastal communities, prompting tsunami alerts though run-up heights have remained modest in recent decades. Ongoing GPS monitoring reveals steady convergence rates of 70–80 mm per year, underscoring the potential for future large ruptures. Seismic hazard assessments for El Salvador incorporate these subduction parameters to refine building codes and early-warning systems.

References

USGS Earthquake Catalog (events 2012-08-27 and 2014-10-14)
USGS Earthquake Hazards Program – Middle America Trench overview