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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; Printable version; In other projects
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]
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)
This extension of the East Pacific Rise is often referred to as the Gulf of California Rift Zone. The Gulf would extend as far as Indio, California, except for the tremendous delta created by the Colorado River. This delta blocks the sea from flooding the Mexicali and Imperial Valleys. Volcanism dominates the East Pacific Rise.
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 ...
Download as PDF; Printable version; In other projects ... It is located within the Gulf of California rift zone. It is a part of a volcanic ridge that extends from ...
The Delfin Basin (delfín is Spanish for "dolphin") is a pair of interconnected submarine depressions located on the seabed of the northern Gulf of California. [1] The northernmost of these is called the Upper Delfin Basin while the southernmost is called the Lower Delfin Basin.