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Additional
Cascadia subduction zone
English Wikipedia - The Free Encyclopedia
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Cascadia subduction zone
The
Cascadia subduction zone
(also referred to as the
Cascadia fault
) is a
convergent
plate boundary
that stretches from northern
Vancouver Island
to northern
California
. It is a very long sloping
subduction zone
fault that separates the
Juan de Fuca
and
North America
plates.
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