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PERIDOT
In old times, peridot was erroneously
exchanged for topaz. It is typically dragged up to the surface of the
Earth by magma and then found in the residue volcanic rock. Iron gives
peridot its fabulous green tint, with shades varying from olive green to
bright yellow green, to the most valuable dark olive green. Inclusions
may resemble lotus leaves, tiny bubbles or opaque crystals.
