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Ophiolitic Serpentinite, Siskiyou County

Ophiolitic Rocks Photo Gallery


More often than not, the peridotite layer becomes thoroughly recrystallized into serpentine minerals. This specimen is from the Trinity ophiolite in the Klamath Mountains.
Changed but still attractive
Photo (c) 2009 Andrew Alden, licensed to About.com (fair use policy)
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