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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.
2 Gulf of California Rift Zone (GCRZ) 3 Yucatán. ... Print/export Download as PDF; ... List of seismic fault (and systems, zones) in Mexico Baja California Peninsula
The northwestern end of the trough starts at the San Gorgonio Pass in Riverside County and extends 115 miles (185 km) southeast to the Gulf of California. [3] Major geographical features located in the trough include the Coachella Valley , the Salton Sea , and the Imperial Valley , in the United States, and the western side of the Mexicali ...
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 ...
The NARS-Baja Seismic Array in the Gulf of California Rift Zone, Clayton, R. W., et al. (2004), Margins Newsletter; A Brief Review of Heat-Flow Studies in the Guaymas Basin, Gulf of California, Chapter 33, Part VI, Hydrothermal Processes, K. Becker, A. T. Fisher, AAPG Special Volumes, Volume M 47: The Gulf and Peninsular Province of the Californias, Pages 709–720 (1991)
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.
The Atl Fault is a right lateral-moving transform fault located on the seafloor of the southern Gulf of California. It links the Farallon Basin to the north with the Pescadero Basin to the south. All these features are part of the Gulf of California Rift Zone, the northern extension of the East Pacific Rise.
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]
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