Fault · Oregon, Washington
Cascadia megathrust
In plain English
The two sides grind past each other faster than 5 mm a year — more than half a metre (20 inches) every century.
Its most recent surface rupture is younger than 15,000 years.
The largest earthquake recorded near it was M 6.0 in 1926 (119 km SSW of Ucluelet, Canada) — about 34,000 times the energy of an M3.0, the size people start to feel. It released about 16 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 6.0 119 km SSW of Ucluelet, Canada
September 17, 1926 · epicentre 22 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 2.8 104 km W of Yachats, Oregon
2018-08-24 · 8 km from the trace
Neighbouring faults
- Cascadia fold and fault belt touching
- Alvin Canyon fault 1 km away
- Daisy Bank fault 4 km away
- South Ninitat fault 4 km away
- Coos Basin fault 4 km away
- Thompson Ridge fault 7 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.