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Gulf of California Rift Zone

From Wikipedia, the free encyclopedia

The Gulf of California Rift Zone (GCRZ) is the northernmost extension of the East Pacific Rise which extends some 1,300 km (800 mi) from the mouth of the Gulf of California to the southern terminus of the San Andreas Fault at the Salton Sink.

The GCRZ is an incipient rift zone akin to the Red Sea Rift. In the GCRZ continental crust originally associated with the North American Plate has been pulled apart by tectonic forces and is being replaced by newly formed oceanic crust and seafloor spreading. The rifting has resulted in the transfer of the Baja California Peninsula to the Pacific Plate.

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Transcription

List of GCRZ transform faults

From north to south:

List of GCRZ rift basins

From north to south:

References

This page was last edited on 4 September 2020, at 02:31
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