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Here's how strong the early-morning earthquake off Victoria was

The quake could be felt across coastal British Columbia and the Puget Sound, according to the USGS.
Credit: vchalup - stock.adobe.com
Seismograph for earthquake detection or lie detector is drawing chart. 3D rendered illustration.

VICTORIA, BC — The Pacific Northwest got some early shakes Thursday morning with a 4.0 magnitude earthquake in the waters between San Juan Island and Saanich, British Columbia.

The quake was registered at 4:05 a.m. PT. The United States Geological Survey's (USGS) community internet intensity map showed people felt the earthquake across much of coastal British Columbia as well as on the San Juan Islands and areas in the northern Puget Sound.

The earthquake was measured at a depth of 52.2 kilometers, per the USGS.

Unlike the flurry of large earthquakes seen miles off the coast of Vancouver Island, this quake doesn't appear to have had much in the way of aftershocks or similar activity in the same area.

Earthquakes around western Washington

Many earthquakes in Washington state are linked to the motion of the Juan de Fuca Plate and the North American Continental Plate moving against each other as the Juan de Fuca Plate slips beneath the North American continent, according to PNSN. This is called the Cascadia Subduction Zone. 

According to the Washington State Department of Natural Resources (DNR), earthquakes happen in Washington every day, but most are too small to be felt. The state has the second highest risk in the U.S. of experiencing a large and damaging earthquake because of its geologic setting. 

The Pacific Northwest typically experiences three types of earthquakes: 

  • Shallow fault quakes: Ruptures in faults located in the upper 18 miles of the Earth's crust. These earthquakes typically last 20 to 60 seconds and shaking is localized to the area near the fault, according to the DNR.  
  • Deep earthquakes: Deep faults happen when two tectonic plates collide and one plate slips beneath the other one. These quakes can impact a large area but are less intense. 
  • Subduction zone earthquakes: This earthquake results from the tension of an oceanic plate slipping beneath a continental plate. When enough stress builds, the fault will rupture, releasing a massive amount of energy. The Cascadia Subduction Zone has the potential for these types of earthquakes and has ruptured in the past. It is one of Washington state's biggest hazards, according to DNR.

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