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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.
The Gulf of California is divided into three faunal regions: Northern, Central, and Southern. [citation needed] One recognized transition zone is termed the Southwestern Baja California peninsula. Transition zones exist between faunal regions, and they usually vary for each individual species.
2 Gulf of California Rift Zone (GCRZ) 3 Yucatán. ... Print/export Download as PDF ... move to sidebar hide. List of seismic fault (and systems, zones) in Mexico Baja ...
List of fault zones. Add languages. ... Gulf of California, United States: ... United States and Mexico: Rift zone: Romeral Fault System: 700:
Some of the fracture zones in the western Pacific Ocean are associated with the smaller plate boundaries of the active back-arc basin spreading center of the North Fiji Basin being the Hunter fracture zone and North Fiji fracture zone. The Parece Vela Rift (Parece Vela fracture zone province) is also associated with the back-arc basin of the ...
Satellite view of the Gulf of California, between the Baja California Peninsula (left/west) and mainland northwestern Mexico (right/east). The Gulf of California — a gulf of the Pacific Ocean, part of the Pacific Coast of Mexico. Also known as the Sea of Cortez, Sea of Cortés, Vermilion Sea, Mar de Cortés, Mar Bermejo, and Golfo de California.
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Obduction zones occurs when the continental plate is pushed under the oceanic plate, but this is unusual as the relative densities of the tectonic plates favours subduction of the oceanic plate. This causes the oceanic plate to buckle and usually results in a new mid-ocean ridge forming and turning the obduction into subduction.