Tectonic Evolution of Western North America
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Subduction of the Farallon Plate

Subduction of the Farallon Plate
30+ MYA
Until approximately 30 million years ago (MYA), the Pacific Spreading Center operated as a continuous north-south zone, creating crust of the Pacific Plate (moving west) and the Farallon Plate (moving east). The oceanic Farallon Plate subducted under the western margin of the continental North American Plate, creating a coastal volcanic/intrusive belt similar to today's Andes or Cascades, wherein solidified granites of the Sierra Nevada, Klamath, and Peninsular Ranges. Where major oceanic fracture zones intersected the North American coast, they propagated into -- and weakened -- continental crust.


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