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Note:This page contains AI-generated content for informational and entertainment purposes only. It may contain inaccuracies. Raw event data is from USGS and EMSC. All statistics, lists, and derived information are generated by this site. Full disclaimerFound an error?
Location:
Period:
9 May 2025 06:53:18 - 15 May 2025 13:35:42 (6 days 6 hours 42 minutes)
Volcanoes in 100km radius:
None
Earthquakes:
113
14 swarms found nearby.
2011
6 Nov
1 day 23 hours
31 earthquakes
2020
S20200625.1(28.9km)
24 Jun
13 hours
24 earthquakes
2023
16 Jul
2 days 11 hours
34 earthquakes
2024
3 Feb
43 days 4 hours
2981 earthquakes
18 Mar
40 days 23 hours
1378 earthquakes
28 Apr
37 days 2 hours
969 earthquakes
5 Jun
36 days 12 hours
573 earthquakes
1 Aug
3 days 3 hours
60 earthquakes
5 Aug
8 days 13 hours
84 earthquakes
28 Sep
11 days 18 hours
125 earthquakes
26 Oct
2 days 1 hours
40 earthquakes
5 Nov
6 days 12 hours
76 earthquakes
28 Nov
6 days 15 hours
139 earthquakes
2025
27 Sep
8 days 19 hours
263 earthquakes
AI-generated article — for informational and entertainment purposes only. May contain inaccuracies. Full disclaimerFound an error?

Seismic Swarm S20250510.1: Prague, Oklahoma Region

A seismic swarm designated S20250510.1 occurred 8 km northwest of Prague, Oklahoma, from 06:53 on 9 May 2025 to 13:35 on 15 May 2025. Over 150 hours and 42 minutes, the sequence produced 113 earthquakes. Analysis of the first 100 events shows magnitudes ranging from -2.0 to 3.1, with the largest event recorded at 3.1 on 10 May 2025 at a depth of 3 km. Most events clustered at depths of 4–7 km, though isolated events reached 13 km. The majority registered below magnitude 1.0, indicating predominantly microseismic activity consistent with swarm behavior rather than a mainshock-aftershock sequence. The temporal distribution revealed an initial peak in activity on 10 May, followed by a gradual decline through 13 May. Shallow focal depths align with regional basement faulting in central Oklahoma, where fluid migration along pre-existing structures can trigger slip. No events exceeded magnitude 3.1 in the initial 100, suggesting limited energy release during the early phase. Central Oklahoma lies within the stable continental interior but has experienced elevated seismicity since the early 2000s, largely linked to wastewater injection associated with oil and gas production. The Prague area sits near mapped faults of the Nemaha Uplift and Wilzetta fault system, where induced events have historically occurred at depths of 3–8 km. Historical records document 13 swarms in the region since 1 January 2000, with notable increases in frequency during 2024 (10 swarms) compared to earlier isolated episodes in 2011, 2020, and 2023. This pattern reflects broader trends in induced seismicity across the Anadarko Basin and surrounding platforms. The May 2025 swarm fits within this established framework of episodic, low-magnitude clustering. Depths and magnitudes remain typical for fluid-induced events, with no indication of deeper tectonic involvement. Continued monitoring supports improved characterization of swarm recurrence in areas of ongoing subsurface fluid management. References:
USGS Earthquake Catalog (historical Oklahoma seismicity)
Oklahoma Geological Survey annual reports on induced seismicity
SeismoSight internal swarm classification S20250510.1