Fault · Nevada
Olinghouse 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 6.5 in 1860 (East of Reno, Nevada) — about 180,000 times the energy of an M3.0, the size people start to feel. It released about 85 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
The big ones recorded near it
- M 6.5 East of Reno, Nevada
March 15, 1860 · epicentre 12 km from the trace - M 6.4 Near Fernley, Nevada
April 24, 1914 · epicentre 13 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.
Neighbouring faults
- Pyramid Lake fault 10 km away
- Northern Virginia Range fault 17 km away
- Spanish Springs Valley fault 24 km away
- Carson lineament 25 km away
- Hot Springs Mountains fault 27 km away
- Honey Lake fault 31 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.