The Cascadia subduction zone is a convergent plate boundary that stretches from northern Vancouver Island in Canada to Northern California in the United States. It is a very long, sloping subduction zone where the Explorer, Juan de Fuca and Gorda plates move to the east and slide below the much larger mostly continental North American Plate. The zone varies in width and lies offshore beginning near Cape Mendocino, Northern California, passing through Oregon and Washington, and terminating at about Vancouver Island in British Columbia.
The Explorer, Juan de Fuca, and Gorda plates are some of the remnants of the vast ancient Farallon Plate which is now mostly subducted under the North American Plate. The North American Plate itself is moving slowly in a generally southwest direction, sliding over the smaller plates as well as the huge oceanic Pacific Plate in other locations such as the San Andreas Fault in central and southern California.
Bron: Wikipedia.org
Auteursrechten: Creative Commons 3.0
Selecteer hieronder één van de populairste activiteiten of verfijn je zoekopdracht.
Ontdek de mooiste en meest populaire routes in de buurt, zorgvuldig gebundeld in passende selecties.
Selecteer hieronder één van de populairste categorieën of laat je inspireren door onze selecties.
Ontdek de mooiste en meest populaire bezienswaardigheden in de buurt, zorgvuldig gebundeld in passende selecties.
Met RouteYou kan je eenvoudig zelf aangepaste kaarten maken. Stippel je route uit, voeg waypoints of knooppunten toe, plan bezienswaardigheden en eet- en drinkgelegenheden in en deel alles met je familie en vrienden.
Routeplanner

<iframe src="https://plugin.routeyou.com/poiviewer/free/?language=nl&params.poi.id=7673472&params.language=en" width="100%" height="600" frameborder="0" allowfullscreen></iframe>
© 2006-2026 RouteYou - www.routeyou.com