Fault · Idaho
Lone Pine fault
In plain English
The two sides move less than 0.2 mm a year — under 2 cm a century. Slow faults can still produce large earthquakes, just rarely.
It has broken the ground surface within the last 150 years.
The largest earthquake recorded near it was M 4.3 in 2025 (24 km E of Clayton, Idaho) — about 89 times the energy of an M3.0, the size people start to feel. It released about 43 tons of TNT.
USGS maps it as 2 sections: unnamed northern section, unnamed southern section.
This week vs. its last ten years
0/100
quiet
0 quakes of M1.5+ within 5 km of the trace in the last 7 days — busier than 0% of weeks since 2016. A normal week: 0–0.
Computed from the USGS catalogue · a description of the past, not a forecast · method
Every year since 2016
Earthquakes of M2.5+ with an epicentre within 10 km of the mapped trace. Near is not the same as on: some will have slipped on neighbouring faults.
The big ones recorded near it
- M 4.3 24 km E of Clayton, Idaho
June 8, 2025 · epicentre 2 km from the trace
Before 1973 from the USGS ComCat historical catalogue (within 25 km; epicentres of old earthquakes are estimates). Since 2016, M4+ within 10 km.
Most recent near it
- M 3.2 25 km E of Clayton, Idaho
2025-06-08 · 1 km from the trace - M 4.3 24 km E of Clayton, Idaho
2025-06-08 · 2 km from the trace - M 2.7 20 km ENE of Clayton, Idaho
2022-08-02 · 2 km from the trace - M 2.8 32 km E of Clayton, Idaho
2019-12-25 · 5 km from the trace - M 2.6 12 km SE of Challis, Idaho
2019-09-01 · 5 km from the trace - M 2.8 8 km ESE of Challis, Idaho
2018-11-26 · 8 km from the trace
Neighbouring faults
- Lost River fault 2 km away
- Lemhi fault 30 km away
Fault trace, slip rate and age: USGS Quaternary Fault and Fold Database (public domain), simplified for the web. Earthquakes: USGS ComCat. QuakeIndex does not forecast earthquakes; a fault's history describes the past. For early warning use ShakeAlert.