
mineral
Ametrine
Silicon Dioxide (SiO2) with impurities of iron
AI-generated identification · may be incorrectHardness: 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)
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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.
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Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
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Granite
Granite (Phaneritic intrusive igneous rock)
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Septarian Pebble
Septarian nodule / Concretion
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