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Peridots can be differentiated by size and composition. Olivine is usually found as small grains and tends to exist in a heavily weathered state, unsuitable for decorative use. Views Read Edit View history. Wikimedia Commons has media related to Peridot. Olivine is an abundant mineral, but gem-quality peridot is rather rare due to its chemical instability on Earth's surface. The largest cut peridot olivine is a carat 62 g specimen in the Smithsonian Museum in Washington, D. Olivine , of which peridot is a type, is a common mineral in mafic and ultramafic rocks , often found in lava and in peridotite xenoliths of the mantle , which lava carries to the surface; however, gem-quality peridot occurs in only a fraction of these settings.

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Olivine is an abundant mineral, but gem-quality peridot is rather rare due to its chemical instability on Earth's surface. Olivine is usually found as small grains and tends to exist in a heavily weathered state, unsuitable for decorative use. From Wikipedia, the free encyclopedia.

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