The Cascadia Channel refers to a geological feature in the Pacific Ocean, specifically related to the region along the Cascadia Subduction Zone, which runs from northern California up through Oregon and Washington to British Columbia, Canada. This subduction zone is characterized by the convergence of the Juan de Fuca Plate and the North American Plate. The Cascadia Channel itself may refer to a specific underwater valley or trench in this region, which can play a role in geological and oceanographic processes.
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