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Location:
Period:
8 Jul 2025 02:57:36 - 26 Jul 2025 09:15:57 (18 days 6 hours 18 minutes)
Volcanoes in 100km radius:
Rainier(0km), Adams(74km), St. Helens(79km)
Earthquakes:
1304
3 swarms found nearby.
2006
S20061008.1(11.8km)
7 Oct
5 days 0 hours
103 earthquakes
2009
20 Sep
2 days 2 hours
121 earthquakes
2023
S20230828.1(15.6km)
27 Aug
3 days 10 hours
43 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Seismic Swarm VS20250708.1 Near Ashford, Washington

A seismic swarm designated VS20250708.1 occurred 22 km east-northeast of Ashford, Washington, in the Cascade Range. The sequence began at 02:57 on 8 July 2025 and concluded at 09:15 on 26 July 2025, spanning 438 hours and 18 minutes. During this period, 1,304 earthquakes were recorded.

Analysis of the first 100 events reveals predominantly low-magnitude activity. Magnitudes ranged from -0.6 to 2.1, with the majority falling between 0.0 and 0.6. Depths clustered near the surface, mostly at 0 km or -1 km, indicating very shallow foci. The largest events included a magnitude 2.1 at 09:55:59 on 8 July and a magnitude 1.6 at the same time. Subsequent events showed no significant escalation in size, consistent with typical swarm behavior rather than a mainshock-aftershock sequence.

The swarm location lies within the tectonically active Pacific Northwest, where the Juan de Fuca Plate subducts beneath the North American Plate. This setting drives volcanism along the Cascade Arc, including nearby Mount Rainier, a stratovolcano situated approximately 25 km west of the swarm epicenters. Shallow seismicity in the region often relates to volcanic processes, hydrothermal fluid movement, or minor faulting within the volcanic edifice and surrounding crust.

Mount Rainier has a well-documented history of seismic swarms linked to its magmatic and hydrothermal systems. Since 2000, only three prior swarms have been identified in the immediate area: one in 2006, one in 2009, and one in 2023. These events underscore the episodic nature of seismic unrest at the volcano, with activity typically remaining at low magnitudes and shallow depths.

The 2025 swarm aligns with established patterns observed at Mount Rainier. No surface deformation or other precursory signals beyond the recorded seismicity have been associated with this sequence. Monitoring by regional networks continues to track activity in this high-hazard volcanic zone.

References

United States Geological Survey, Volcano Hazards Program – Mount Rainier.
Pacific Northwest Seismic Network, University of Washington.
Cascades Volcano Observatory, Recent Seismicity Reports.