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Note:This page contains AI-generated content for informational and entertainment purposes only. It may contain inaccuracies. Raw event data is from USGS and EMSC. All statistics, lists, and derived information are generated by this site. Full disclaimerFound an error?
Location:
Period:
14 Jun 2001 23:31:28 - 15 Jun 2001 06:30:20 (6 hours 58 minutes)
Volcanoes in 100km radius:
None
Earthquakes:
5
2 swarms found nearby.
2016
PS20160729.1(148.4km)
29 Jul
20 minutes
5 earthquakes
2022
PS20220708.1(10.2km)
8 Jul
6 hours
9 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Seismic Swarm in the Mariana Islands Region: June 2001

A notable seismic swarm occurred in the Mariana Islands region between 23:31 UTC on 14 June 2001 and 06:30 UTC on 15 June 2001. Over this 6-hour 58-minute period, five earthquakes were recorded. The sequence began with a magnitude 5.9 event at 23:31:28 on 14 June at a depth of 33 km. Subsequent events included a magnitude 4.6 quake at 06:14:13 on 15 June, followed by a magnitude 6.0 event at 06:17:45, a magnitude 5.1 shock at 06:22:27, and a final magnitude 5.0 earthquake at 06:30:20, all at 33 km depth.

The Mariana Islands lie along the Mariana subduction zone, where the Pacific Plate subducts beneath the Philippine Sea Plate. This tectonic setting produces frequent seismicity, including both shallow crustal events and deeper Wadati-Benioff zone activity. The region hosts the Mariana Trench, the deepest oceanic trench on Earth, reaching approximately 10,984 meters at Challenger Deep. Historical records document major earthquakes, such as the 1892 event near Guam and the 2014 magnitude 7.7 earthquake, which generated a tsunami warning. The arc's volcanic islands, including Pagan and Anatahan, result from magma generation above the subducting slab, contributing to ongoing geological hazards.

Swarm activity in subduction zones often reflects fluid migration or stress transfer along the plate interface rather than a single mainshock-aftershock sequence. The 2001 swarm clustered tightly in both time and space at intermediate depth, consistent with intraslab processes. Such episodes provide insights into fault mechanics and can precede larger ruptures, though no immediate escalation occurred in this instance.

Geological monitoring in the Mariana region relies on networks operated by the United States Geological Survey and regional partners. Updated data through 2023 confirm persistent low-to-moderate seismicity along the arc, with occasional swarms highlighting the dynamic nature of the subduction interface.

References

USGS Earthquake Catalog NOAA Pacific Tsunami Warning Center historical records Geological Society of America publications on Mariana subduction tectonics