Rock Identifier
Ametrine (Silicon Dioxide (SiO2) with impurities of iron) — mineral
mineral

Ametrine

Silicon Dioxide (SiO2) with impurities of iron

Hardness: 7 on Mohs scale; Color: Bicolor purple (amethyst) and yellow/orange (citrine); Luster: Vitreous (glassy); Crystal structure: Hexagonal; Cleavage: None/Conchoidal fracture; Specific gravity: 2.65

Hardness
7 on Mohs scale
Color
Bicolor purple (amethyst) and yellow/orange (citrine)
Luster
Vitreous (glassy)
Identified More mineral

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Physical properties

Hardness: 7 on Mohs scale; Color: Bicolor purple (amethyst) and yellow/orange (citrine); Luster: Vitreous (glassy); Crystal structure: Hexagonal; Cleavage: None/Conchoidal fracture; Specific gravity: 2.65

Formation & geological history

Formed in hydrothermal veins or pegmatites when temperature gradients cause iron impurities to reach different oxidation states within the same quartz crystal. Nearly all natural commercial ametrine comes from the Anahi mine in Bolivia.

Uses & applications

Primarily used in jewelry as a gemstone and for crystal healing/metaphysical collection. Smaller specimens are popular for lapidary art.

Geological facts

Ametrine is one of the rarest naturally occurring gemstone varieties in the world because it requires a very specific temperature gradient to exist during its formation. It was first introduced to Europe in the 17th century by a Spanish conquistador.

Field identification & locations

Identify by looking for the distinct, sharp transition between purple and yellow sections within a single vitreous crystal. Naturally found almost exclusively in the Santa Cruz department of Bolivia.