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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.
List of fault zones. Add languages. ... Gulf of California, United States: ... United States and Mexico: Rift zone: Romeral Fault System: 700:
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 ...
Relief map with the East Pacific Rise (shown in light blue), extending south from the Gulf of California. The East Pacific Rise (EPR) is a mid-ocean rise (usually termed an oceanic rise and not a mid-ocean ridge due to its higher rate of spreading that results in less elevation increase and more regular terrain), at a divergent tectonic plate boundary, located along the floor of the Pacific Ocean.
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.
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 ...
Hydrothermal vent diagram. Hydrothermal circulation, or the circulation of hot water, is a predominant feature of the Guaymas Basin. Hydrothermalism is mainly observed in the southern trough of the basin where hydrothermal vents make up a hydrothermal complex on the seafloor by creating mounds, chimney structures, and sediments. [7]