Fault · Utah
Hansel Valley 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 6.6 in 1934 (The 1934 Hansel Valley, Utah Earthquake) — about 250,000 times the energy of an M3.0, the size people start to feel. It released about 120 kilotons of TNT.
This week vs. its last ten years
Too quiet to rank: fewer than half a year's worth of weeks with any M1.5+ quake within 5 km, in ten years. A single quake here would read as "unusual", so we do not score it.
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 6.6 The 1934 Hansel Valley, Utah Earthquake
March 12, 1934 · epicentre 9 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 3.1 12 km SSW of Snowville, Utah
2026-05-28 · 8 km from the trace - M 2.8 13 km S of Snowville, Utah
2020-09-15 · 5 km from the trace - M 2.8 13 km S of Snowville, Utah
2018-10-17 · 6 km from the trace - M 2.8 13 km S of Snowville, Utah
2018-10-17 · 6 km from the trace
Neighbouring faults
- North Promontory fault 14 km away
- Great Salt Lake fault 31 km away
- Curlew Valley faults 33 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.