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Gulf of California Rift Zone

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Northernmost extension of the East Pacific Rise

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.

List of GCRZ transform faults

From north to south:

List of GCRZ rift basins

From north to south:

References

Major seismically active faults of North America
North America
(crosses national borders)
Canada
United States
Washington and Oregon
California
Great Basin
Great Plains
Midwest
Appalachian Mountains
and Atlantic Coast
Caribbean and Mexico
Tectonic plates of Central America (Pacific plateNorth American plateCaribbean plate c
onvergence zone)
Large
Small
Faults and
rift zones
Trenches and
troughs
Other
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