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Earthquakes
in British Columbia
Fault
Zones
Off the
coast of southwestern British Columbia is a convergence of two tectonic
plates, which causes most of the earthquakes felt in the area.
The following
exerpt was taken from the Geological Survey of Canada,
which also provides:
Where
Earthquakes Happen
Each year, seismologists with the Geological Survey of Canada record and locate more than 1000 earthquakes in western Canada. The Pacific
Coast is the most earthquake-prone region of Canada. In the offshore region
to the west of Vancouver Island, more than 100 earthquakes of magnitude 5 or
greater (large enough to cause damage had they been closer
to land) have occurred during the past 70 years. Part of the Pacific Ring of Fire, the concentration of
earthquakes along the west coast is related to the presence of active faults,
or breaks
in the earth's crust. The surface of the earth is
always changing, as the earth's crust is made up of "plates" (like
pieces of a jigsaw puzzle) that are constantly moving relative to one another
at speed's of about 2-10 cm/year (about how fast your fingernails grow). The
plates can either slide past one another or they can collide, or they can diverge (move apart).
The west coast of Canada (click
here for cartoon) is one of the few areas in the world where all three
of these types of plate movements take place, resulting in significant earthquake
activity. Earthquakes in this region occur along the faults in the offshore
region (e.g., the M=8.1 Queen Charlotte Island earthquake of 1949); within
the subducting ocean plate (e.g., a magnitude 6.5 earthquake beneath downtown
Seattle in 1965); and within the continental crust (e.g., a magnitude 7.3
earthquake on central Vancouver Island in 1946). Moving inland
from the coast (and the active plate boundaries), the frequency and size of
the earthquakes decreases. Saskatchewan and Manitoba are the least
earthquake-prone areas in Canada.
Past
Earthquake History
The Geological
Survey of Canada provides:
Earthquake
Hazard Information You Should Know
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