Location:
Period:
14 Nov 2025 18:46:28 - 17 Nov 2025 02:18:30 (2d 7h 32m)
Volcanoes in 100km radius:
Earthquakes:
36
25 swarms found nearby.
2019
S20190414.1(29.4km)
13 Apr
7 hours
28 earthquakes
2020
S20200117.2(22.8km)
17 Jan
3 days 13 hours
46 earthquakes
17 Apr
2 days 18 hours
116 earthquakes
S20200502.1(10.3km)
1 May
1 day 8 hours
30 earthquakes
6 Oct
1 day 4 hours
41 earthquakes
2021
30 Jul
9 hours
44 earthquakes
2022
6 Apr
4 hours
29 earthquakes
2023
26 Nov
20 hours
31 earthquakes
13 Dec
15 hours
24 earthquakes
2024
15 Feb
8 days 4 hours
308 earthquakes
24 Feb
6 days 6 hours
260 earthquakes
4 Mar
3 days 6 hours
47 earthquakes
3 Apr
4 days 22 hours
172 earthquakes
7 Jun
5 days 3 hours
152 earthquakes
30 Jul
4 days 8 hours
81 earthquakes
29 Nov
13 days 8 hours
239 earthquakes
2025
28 Aug
9 days 6 hours
245 earthquakes
2026
11 Mar
2 days 1 hours
47 earthquakes
21 Mar
12 days 0 hours
175 earthquakes
6 Aug
22 hours
24 earthquakes
13 Aug
21 hours
24 earthquakes
24 Aug
1 day 20 hours
31 earthquakes
26 Aug
2 days 5 hours
43 earthquakes
3 Sep
1 day 14 hours
29 earthquakes
10 Sep
1 day 16 hours
48 earthquakes
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Seismic Swarm S20251115.1 Near Milford, Utah: Characteristics and Regional Context

A seismic swarm designated S20251115.1 occurred 15 km northeast of Milford in Beaver County, Utah, between 18:46 on 14 November 2025 and 02:18 on 17 November 2025. Over 55 hours and 32 minutes, the swarm produced 36 earthquakes, all of low magnitude ranging from 0.3 to 1.6. Depths were shallow, predominantly between 1 and 2 km, with one event at 0 km.

The events clustered without a dominant mainshock, a pattern typical of swarm activity driven by fluid migration along fractures rather than sudden tectonic rupture. Magnitudes remained below levels likely to cause damage, consistent with microseismicity in the area.

Milford lies within the Basin and Range Province of western Utah, where east-west crustal extension produces north-south trending normal faults. This tectonic setting generates frequent small earthquakes across the Intermountain Seismic Belt. The specific location northeast of Milford sits near the margins of the Mineral Mountains, a range with Miocene volcanic and intrusive rocks overlying older Precambrian basement. Geothermal activity in the broader Milford area reflects ongoing heat flow and fluid circulation within fractured crystalline rock, conditions that can facilitate earthquake swarms.

Seismic swarms have occurred repeatedly in this portion of Utah since at least 2000. Records indicate 17 swarms between 2000 and 2025, with yearly counts as follows: one in 2019, four in 2020, one in 2021, one in 2022, two in 2023, seven in 2024, and one in 2025. These episodes typically involve low-magnitude events at shallow depths and are monitored for possible links to geothermal or hydrothermal processes.

The November 2025 swarm fits this regional pattern. Its brief duration and uniform depth distribution suggest a localized trigger, possibly related to transient fluid pressure changes along pre-existing faults. No larger events accompanied the sequence, and activity ceased abruptly after the final recorded shock.

Ongoing monitoring by regional seismic networks continues to track microseismicity in the Milford vicinity, providing data that improves understanding of extensional tectonics and geothermal systems in the eastern Great Basin.

References

USGS Earthquake Hazards Program. Earthquake Catalog for Utah.
Utah Geological Survey. Seismic Monitoring and Fault Studies.
University of Utah Seismograph Stations. Annual Earthquake Reports.