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The boundary between the Pacific and North American plates is primarily a transform boundary, characterized by lateral sliding motion. This is most notably exemplified by the San Andreas Fault in California, where the two plates grind past each other, leading to significant seismic activity. Additionally, the boundary includes a complex interaction of geological features, such as ridges and subduction zones, contributing to the region's tectonic dynamics. These interactions result in earthquakes and other geological phenomena.

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1mo ago

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How does the transform fault boundary occur?

when two plates are slide past one another an example is the san Andreas fault California which is the boundary between the north America and pacific plates


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San Andreas Fault.


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