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The Pacific Plate is a major tectonic plate whose movements are fundamental to understanding the geology of the Pacific region. Along its boundaries, significant geological activity occurs.

In the northeastern Pacific, the Pacific Plate moves laterally alongside the North American Plate along transform faults like the San Andreas Fault. This movement causes considerable seismic activity, making California highly prone to earthquakes.1

To the west of Oregon and Washington, the Pacific Plate is spreading at the Gorda and Juan de Fuca ridges. Here, the Juan de Fuca Plate subducts beneath the North American Plate, fueling the volcanic activity in the Cascade Range.1

In the western Pacific, island arcs and deep trenches mark convergent zones where plates collide and one is subducted. Conversely, the East Pacific Rise is a spreading center where new crust is formed. The Pacific Ocean itself is the largest ocean on Earth, covering about one-third of its surface.234

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