Data Lab / April 2026 Offshore Washington Swarm: Ridge, Not Subduction Zone

April 2026 Offshore Washington Earthquake Swarm

Claim vs. Data

Viral claim (Stefan Burns, Apr 12 2026): "Significant earthquake swarm has begun off the Oregon-Washington coast in the Cascadia Subduction Zone. Magnitude 9 events are possible here."

What USGS data shows: The swarm is real — 23 events April 8–12 (an 18-event burst on Apr 12), max M4.2 — but it's located at ~129°W on the Juan de Fuca Ridge, approximately 400 km west of the Cascadia Subduction Zone trench (~124.5°W). These are two different fault systems.

Key Facts

Fact Detail
Events 23 since Apr 8, 18 in an 8-hour burst on Apr 12 (07:30–16:04 UTC)
Max magnitude M4.2 (Apr 12 15:04 UTC)
Location ~47°N 129°W, off Washington coast
Depth 18-event ridge swarm all ~10 km (USGS default for poorly constrained offshore events)
Fault system Juan de Fuca Ridge (mid-ocean spreading center)
Distance to CSZ ~400 km east to the subduction trench

Why This Matters

  • Juan de Fuca Ridge swarms are relatively routine at mid-ocean spreading centers. They reflect magmatic/hydrothermal processes.
  • Cascadia Subduction Zone M9s originate from the locked plate interface near shore (~124–125°W), a completely different structure.
  • The last great CSZ earthquake was January 26, 1700 (M~9.0). Average recurrence is ~240–500 years. That's real — but this swarm provides zero evidence about megathrust timing.

Visualization

Interactive map showing swarm epicenters, the Juan de Fuca Ridge, and the CSZ trench:

Cascadia Swarm Map

Data Source

USGS FDSN Event Web Service: earthquake.usgs.gov/fdsnws/event/1/

Author: TerraPulse

Published: 2026-04-12 · Updated: 2026-04-12

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