Location:
Period:
1 May 2020 22:45:54 - 3 May 2020 07:27:33 (1d 8h 41m)
Volcanoes in 100km radius:
Earthquakes:
30
24 swarms found nearby.
2020
S20200117.2(19.0km)
17 Jan
3 days 13 hours
46 earthquakes
17 Apr
2 days 18 hours
116 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
S20240216.1(10.0km)
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
S20241130.1(10.6km)
29 Nov
13 days 8 hours
239 earthquakes
2025
S20250829.1(10.3km)
28 Aug
9 days 6 hours
245 earthquakes
S20251115.1(10.3km)
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
S20260813.1(10.0km)
13 Aug
21 hours
24 earthquakes
S20260824.1(10.0km)
24 Aug
1 day 20 hours
31 earthquakes
S20260827.1(10.1km)
26 Aug
2 days 5 hours
43 earthquakes
3 Sep
1 day 14 hours
29 earthquakes
S20260910.2(11.1km)
10 Sep
1 day 16 hours
48 earthquakes
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Seismic Swarm S20200502.1: Analysis of Activity Near Milford, Utah

A minor seismic swarm designated S20200502.1 was recorded 19 km east-northeast of Milford in Beaver County, Utah. The sequence began at 22:45 on 1 May 2020 and concluded at 07:27 on 3 May 2020, spanning 32 hours and 41 minutes. During this interval, 30 earthquakes were detected, with magnitudes ranging from -0.8 to 1.4 and focal depths between 0 and 4 km. All events remained below the threshold for felt shaking or damage.

The swarm initiated with a series of micro-earthquakes clustered tightly in both time and space. Early events on 1 May exhibited magnitudes near or below zero and depths around 3 km. Activity continued into 2 May with slightly higher magnitudes, including peaks of 1.1 at 00:22 and 1.4 at 01:51, both at 4 km depth. The final event, magnitude 0.3 at 1 km depth, marked the end of the sequence on 3 May. The pattern shows episodic bursts separated by quiet periods, typical of fluid-driven or stress-adjustment processes rather than mainshock-aftershock sequences.

Milford lies within the Basin and Range Province, where east-west extension produces north-south trending normal faults. The area forms part of the transition between the Colorado Plateau and the Great Basin, with Quaternary basaltic volcanism in the adjacent Black Rock Desert volcanic field. Geothermal systems and young volcanic features indicate elevated crustal temperatures that can facilitate small-magnitude earthquake swarms through hydrothermal fluid migration. Historical seismicity in the region remains low to moderate, consistent with the province-wide rate of extensional faulting.

Since 1 January 2000, two swarms have been identified in the catalog for this locale, with S20200502.1 representing the earliest recorded instance. The second swarm occurred after 2020. Both episodes share similar characteristics of low magnitudes and shallow depths, underscoring the persistent but low-energy seismic behavior of the local fault network.

No larger tectonic events were associated with this swarm. Continued monitoring by regional networks provides data for refining models of strain accumulation along the dominant north-south structures near Milford.

References

USGS Earthquake Catalog
Utah Geological Survey Seismicity Reports
SeismoSight Internal Swarm Classification Database