One explanation is that Taiwan undergoes slow earthquakes, in which
crustal faults slip over hours or days, rather than seconds, creating no seismic judders.
However, the seismic potential of
crustal faults within the forearc of the northern Cascadia subduction zone in British Columbia has remained elusive.
This article by Kristin Morell, Christine Regalla, Lucinda J. Leonard, and Vic Levson presents evidence for earthquake surface ruptures along the Leech River fault, a prominent
crustal fault near Victoria, British Columbia.
Not exact matches
By comparing the repeat - pass radar observations, scientists hope to measure any
crustal deformations that may occur between observations, allowing them to «see» the amount of strain building up on
fault lines, and giving them a clearer picture of which
faults are active and at what rates they're moving, both before earthquakes and after them.