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  2. Gulf of California Rift Zone - Wikipedia

    en.wikipedia.org/wiki/Gulf_of_California_Rift_Zone

    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.

  3. List of seismic faults in Mexico - Wikipedia

    en.wikipedia.org/wiki/List_of_seismic_faults_in...

    2 Gulf of California Rift Zone (GCRZ) ... Printable version; ... List of seismic fault (and systems, zones) in Mexico Baja California Peninsula ...

  4. List of fracture zones - Wikipedia

    en.wikipedia.org/wiki/List_of_fracture_zones

    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 ...

  5. Gulf of California - Wikipedia

    en.wikipedia.org/wiki/Gulf_of_California

    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.

  6. Guaymas Basin - Wikipedia

    en.wikipedia.org/wiki/Guaymas_Basin

    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]

  7. Geology of the United States - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_United_States

    The rift zone known as the mid-Atlantic ridge continued to provide the raw volcanic materials for the expanding ocean basin. [20] North America was slowly pulled westward away from the rift zone. The thick continental crust that made up the new east coast collapsed into a series of down-dropped fault blocks that roughly parallel today's coastline.

  8. List of tectonic plate interactions - Wikipedia

    en.wikipedia.org/wiki/List_of_tectonic_plate...

    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.

  9. Category:Gulf of California - Wikipedia

    en.wikipedia.org/wiki/Category:Gulf_of_California

    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.