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One such batholith is the sierra nevada batholith, which is a continuous granitic formation that makes up much of the sierra nevada in california Evidence for structural controls on emplacement and volcanism. An even larger batholith, the coast plutonic complex, is found predominantly in the coast mountains of western canada
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It extends for 1,800 kilometers and reaches into southeastern alaska. ^ a b c evernden, jf The eastern boundary of the forearc basin was a volcanic arc, a chain of ancient volcanoes located where the sierra nevada is today
Batholiths and metamorphosed volcanic rocks in the sierra nevada are the geologic record of this volcanic arc.
In early triassic time, an extensive volcanic arc system called the sierran arc began to develop along the western margin of the north american continent In southern california, this volcanic arc would develop throughout the mesozoic era to become the geologic regions known as the sierra nevada batholith, the peninsular ranges batholith, (in the peninsular ranges), and other plutonic and. The vast majority of the range lies in the state of california, although the carson range spur lies primarily in nevada. The cathedral peak granodiorite (cpg) was named after its type locality, cathedral peak in yosemite national park, california
The granodiorite forms part of the tuolumne intrusive suite (tuolumne batholith), one of the four major intrusive suites within the sierra nevada It has been assigned radiometric ages between 88 and 87 million years and therefore reached its cooling stage in the. Geologic map of the merced peak quadrangle, central sierra nevada, california (map) Plutonism in the central part of the sierra nevada batholith
