Fault · Utah
Enoch graben faults
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.
Its most recent surface rupture is younger than 15,000 years.
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.
Most recent near it
- M 2.7 0 km S of Summit, Utah
2026-03-19 · 7 km from the trace - M 2.5 4 km NW of Cedar City, Utah
2025-10-14 · 8 km from the trace - M 2.9 9 km NW of Enoch, Utah
2024-06-09 · 8 km from the trace - M 2.5 9 km NW of Enoch, Utah
2024-06-09 · 7 km from the trace - M 2.5 8 km NW of Enoch, Utah
2024-06-09 · 5 km from the trace - M 2.7 1 km WSW of Summit, Utah
2024-06-03 · 5 km from the trace
Neighbouring faults
- Cedar City-Parowan monocline (and faults) 3 km away
- Hurricane fault 17 km away
- Parowan Valley faults 17 km away
- Mineral Mountains (west side) faults 32 km away
- Beaver Basin faults 38 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.