Fault · Washington
Utsalady Point 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.
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 3.8 2 km E of Oak Harbor, Washington
2026-07-02 · 1 km from the trace - M 2.9 2 km ESE of Oak Harbor, Washington
2026-06-08 · 0 km from the trace - M 2.5 4 km ENE of Oak Bay, Canada
2025-03-26 · 10 km from the trace - M 3.3 1 km NNE of Coupeville, Washington
2024-01-18 · 7 km from the trace - M 3.4 2 km SSE of Stanwood, Washington
2023-11-17 · 9 km from the trace - M 2.6 21 km S of Friday Harbor, Washington
2023-07-07 · 2 km from the trace
Neighbouring faults
- Southern Whidbey Island fault 3 km away
- Lake Creek-Boundary Creek fault 40 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.