Natural Resources Canada seismologist John Cassidy said the West Coast has been experiencing "episodic tremor and slip" recently.
"Normally Vancouver Island is moving towards the mainland very slowly [but] Vancouver Island will change direction roughly every 14 or 15 months, and will slip backwards towards the ocean," Cassidy told All Points West host Robyn Burns.
"There's a very slight movement back to the west, before Vancouver Island carries on its regular direction of being squeezed towards the mainland. Vancouver Island does a little bit of a dance."
A regular occurrence
Cassidy said this occurs regularly because the West Coast is on a subduction zone where one tectonic plate (the Juan de Fuca plate) is moving under another one (the North American plate).
Episodic tremor and slip generally lasts a few weeks, and causes "thousands and thousands of tiny tremors" that are too small to be felt.
"They look almost like the recording of a train where energy will build up very slowly and shake for a few minutes , very subtly shaking, and then it rolls off again," said Cassidy.
The same phenomenon also occurs in parts of Japan, Mexico and Alaska.
Provides useful information for seismologists
Cassidy said the tremors can provide useful information about the large earthquake that is expected on the West Coast because of the plates moving under each other at the Cascadia subduction zone.
"This new information has been really very useful in helping us to identify where exactly that locked fault is, and that helps us to predict or better understand ground shaking we can expect during these future earthquakes."
Cassidy said it is unknown if the recent spate of tremors had anything to do with the Dec. 29 earthquake.
"At this point we don't know if there's a direct link," he said.
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