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Farallon Basin information


The Farallon Basin is a submarine depression located on the seabed at the southern end of the Gulf of California. The basin results from the activity of one of the several spreading centers in the Gulf. The basin is linked to the Atl Fault to the south, and the Farallon Fault in the north.

The Farallon Basin has a spreading axis at its center, so the seafloor here is oceanic crust, transitioning into thin, rifted continental crust at the basin's edges. Spreading centers in the Gulf, like this one in Farallon, are different from more well known spreading axes like the Mid-Atlantic Ridge and East Pacific Rise, since they form as deep rift valleys rather than bathymetric highs.

One familiar source of terrigenous input to the Gulf is the Colorado River, which empties into the northern Gulf (though no longer consistently, as a result of overuse for irrigation). Further south, especially in the eastern Gulf, the Sierra Madre Occidental are a more important source of sediment.[1]

  1. ^ ""Information about the geography"". Archived from the original on 2011-07-11. Retrieved 2010-07-02.

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tectonic plates, the Juan de Fuca Plate is a remnant part of the once-vast Farallon Plate, which is now largely subducted underneath the North American Plate...

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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...

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Colorado River

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Range, which bound the San Juan Basin on the northeast. During the late Jurassic, continental collision of the Farallon and North American plates resulted...

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end of the Farallon Plate, a portion now known as the Kula Plate. About 85 million years ago, the Kula Plate broke off from the Farallon Plate to form...

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its western edge, the Farallon Plate has been subducting under the North American Plate since the Jurassic period. The Farallon Plate has almost completely...

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convergence rate of the Farallon and North American Plates was fast and the angle of subduction was shallow. During the Eocene the Farallon Plate subduction-associated...

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the coast of northern California, is one of the northern remnants of the Farallon Plate. It is sometimes referred to (by, for example, publications from...

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Pacific-Phoenix-Farallon triple junction. The Farallon Plate subducted under North America from the late Mesozoic, while spreading between the Pacific and Farallon plates...

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existence as an independent plate having been formed from the break-up of the Farallon Plate about 23 million years ago. The oldest rocks of the plate are about...

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subduction to a transform boundary occurred during Cenozoic time. The Farallon plate continued to be subducted beneath western North America for at least...

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