Location:
Period:
4 Mar 2024 02:59:32 - 7 Mar 2024 09:18:27 (3d 6h 18m)
Volcanoes in 100km radius:
Earthquakes:
47
24 swarms found nearby.
2020
S20200117.2(21.4km)
17 Jan
3 days 13 hours
46 earthquakes
17 Apr
2 days 18 hours
116 earthquakes
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
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
14 Nov
2 days 7 hours
36 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 S20240304.1: Analysis of Activity Near Milford, Utah

Seismic swarm S20240304.1 was recorded 14 km northeast of Milford, Utah, beginning at 02:59 on 4 March 2024 and concluding at 09:18 on 7 March 2024. Over 78 hours and 18 minutes, the sequence produced 47 earthquakes, all of low magnitude and shallow depth.

The events clustered tightly in both time and space, with the majority occurring at depths of 1–2 km. Magnitudes ranged from −0.8 to 1.7, indicating microseismicity typical of fluid-driven swarm behavior rather than mainshock-aftershock sequences. The largest event, magnitude 1.7, occurred at 02:28 on 5 March at 1 km depth. Activity peaked on 4 March with multiple events above magnitude 1.0, followed by a gradual decline through 6 March and only two final events on 7 March.

This swarm occurred within the Basin and Range Province, where crustal extension along normal faults produces distributed seismicity. The Milford area lies near the Mineral Mountains, a region influenced by Miocene volcanism and ongoing geothermal activity. Shallow focal depths are consistent with fluid migration along fracture networks, a common mechanism for swarm generation in this tectonic setting.

Historical records maintained by SeismoSight document ten swarms in the same locale since 1 January 2000. These episodes occurred in 2020 (4 swarms), 2021 (1), 2022 (1), 2023 (2), and 2024 (2). The recurrence pattern suggests episodic release of strain through swarm-type sequences rather than isolated large earthquakes.

The current swarm aligns with prior episodes in duration, magnitude range, and depth distribution, reinforcing the area’s characteristic low-level seismic behavior. No events exceeded magnitude 2.0, and none were reported as felt by residents.

Continued monitoring remains important given the region’s geothermal resources and proximity to infrastructure. Future swarms may follow similar spatiotemporal patterns observed in the 2000–2024 catalog.

References

SeismoSight internal swarm classification database (S20240304.1 parameters and historical swarm counts).
U.S. Geological Survey Earthquake Hazards Program – regional tectonics of the Basin and Range Province.
Utah Geological Survey – geologic framework of Beaver County and Mineral Mountains.