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Agate Pendants

Agate was formed in mountain lavas due to intergrowth of various minerals of the silica family (SiO2), in which chalcedony is the predominant mineral. It most often has a layered structure. Alternating layers come in different colors and may have varying degrees of transparency. Due to this, in the cross-section of the stone, an original, non-repeating pattern is found.

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