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Location:
Period:
27 Jul 2025 12:24:41 - 29 Jul 2025 16:27:32 (2 days 4 hours 2 minutes)
Volcanoes in 100km radius:
None
Earthquakes:
44
11 swarms found nearby.
2007
PS20071002.1(109.3km)
2 Oct
2 hours
5 earthquakes
2020
PS20200722.1(76.4km)
22 Jul
15 hours
6 earthquakes
PS20201019.2(36.7km)
19 Oct
1 day 4 hours
12 earthquakes
S20201020.1(12.8km)
19 Oct
22 days 19 hours
647 earthquakes
19 Oct
5 days 0 hours
74 earthquakes
S20201021.2(12.7km)
20 Oct
2 days 3 hours
40 earthquakes
S20201115.1(10.9km)
14 Nov
5 days 11 hours
97 earthquakes
S20201210.1(22.8km)
9 Dec
1 day 13 hours
36 earthquakes
2025
16 Jul
30 days 21 hours
1640 earthquakes
S20250716.2(25.4km)
16 Jul
1 day 7 hours
103 earthquakes
S20250717.3(14.5km)
16 Jul
7 days 2 hours
211 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Seismic Swarm S20250728.1: Analysis of Activity Near Sand Point, Alaska

Seismic swarm S20250728.1 occurred approximately 91 km south-southeast of Sand Point, Alaska, in the Aleutian Islands region. The sequence began at 12:24 on 27 July 2025 and concluded at 16:27 on 29 July 2025, spanning 52 hours and 2 minutes. During this period, 44 earthquakes were recorded, with magnitudes ranging from 1.6 to 3.4 and focal depths between 7 and 37 km.

The swarm initiated with a magnitude 3.4 event at 37 km depth. Subsequent activity included multiple events above magnitude 2.0, such as a 3.1 quake at 35 km depth and a 3.3 event at 35 km. Shallower activity appeared later in the sequence, including events at 7 km depth. The distribution showed clustering around 13–25 km depths for the majority of events, consistent with crustal processes in the overriding plate.

Sand Point lies within the tectonically active Aleutian subduction zone, where the Pacific Plate converges with the North American Plate at rates exceeding 6 cm per year. This setting produces frequent seismicity, including both interplate thrust events and intraslab earthquakes. The region also hosts active volcanoes such as Pavlof and Shishaldin, underscoring its position along the Pacific Ring of Fire. Historical records indicate persistent low-to-moderate magnitude swarms linked to fluid migration or stress adjustments along regional faults.

Since 2000, eleven swarms have been documented in the broader area. These occurred in 2007 (one swarm), 2020 (seven swarms), and 2025 (three swarms, including the current sequence). Such episodic clusters are typical in subduction environments and often do not lead to larger mainshock-aftershock sequences.

The 2025 swarm exhibited a gradual decay in both frequency and magnitude after the first 24 hours, with no events exceeding magnitude 3.0 after 28 July. Depths remained predominantly in the mid-crust, suggesting activity confined to the North American Plate rather than the deeper subducting slab.

This event aligns with established patterns of swarm behavior in the Aleutians, where short-lived clusters of small earthquakes reflect localized stress release without significant surface rupture or tsunami potential.

References
USGS Earthquake Catalog (earthquake.usgs.gov)
Alaska Earthquake Center (earthquake.alaska.edu)
SeismoSight internal swarm classification data