Fault · Nevada
Cortez Mountains 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.
Its most recent surface rupture is younger than 15,000 years.
USGS maps it as 3 sections: middle section, northeast section, southwest section.
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.
Most recent near it
- M 3.8 17 km E of Crescent Valley, Nevada
2024-03-04 · 4 km from the trace - M 2.9 18 km ESE of Crescent Valley, Nevada
2023-07-26 · 2 km from the trace - M 2.5 32 km SSW of Crescent Valley, Nevada
2022-05-10 · 4 km from the trace - M 2.7 10 km E of Crescent Valley, Nevada
2018-08-04 · 10 km from the trace
Neighbouring faults
- Simpson Park Mountains fault 4 km away
- Crescent Valley faults 4 km away
- Carico Lake Valley fault 10 km away
- Northern Simpson Park Mountains fault 20 km away
- Shoshone Range fault 33 km away
- Western Roberts Mountains fault 39 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.