Ametrine
Last updated: April 2026
Bicolor quartz variety with zones of purple (amethyst) and yellow-orange (citrine) in a single crystal. The zoning results from different iron oxidation states in different thermal zones during crystal growth. The Anahi mine in Bolivia produces virtually all commercial ametrine.
Ametrine has a specific gravity of 2.65 and a refractive index of 1.544–1.553, with a Mohs hardness of 7. It is uniaxial +.
Physical & Optical Properties
Measured with a polariscope, a refractometer, a hydrostatic balance, a Chelsea filter, a UV torch, a loupe, a darkfield loupe and a spectroscope — step-by-step for each.
Through the refractometer
Drawn from the refractive index above, on a 1.40–1.81 scale. How to take this reading.
Through the polariscope
Drawn from the optic character and transparency above. A polariscope separates singly refractive, doubly refractive and aggregate; the optic sign needs a conoscope. How to take this reading.
Specific gravity, and what it rules out
Drawn from the specific-gravity range above, against every other species in the table. How to take this reading.
Through the dichroscope
Drawn from the pleochroism above. Two windows that match mean either no pleochroism or the wrong angle — turn the instrument to tell. How the dichroscope compares.
Related: Quartz Varieties
Key Differentiators
- Distinct bicolor zones — purple amethyst and yellow/orange citrine in same crystal
- Quartz RI 1.544–1.553 and SG 2.65 — identical to amethyst and citrine
- Natural color boundary is curved or irregular; synthetic diffusion-bonded shows sharp planar junction
- Almost exclusively from Anahi mine, Bolivia
- Inert under both LW and SW UV fluorescence
Natural vs. Synthetic
Synthetic ametrine is commercially available (Hydrothermal growth (bicolor zones created by controlled growth conditions), Diffusion bonding (amethyst and citrine pieces joined under heat and pressure)). Distinguishing natural from synthetic typically requires microscopic examination of internal features.
- Microscopy — color boundary morphology: Natural ametrine shows an irregular, curved, or gradational color boundary between the purple and yellow zones, often with transitional mixed-color areas. Typical quartz inclusions (fluid inclusions, etch channels) present in both zones. Synthetic: Diffusion-bonded synthetic ametrine shows a sharp, planar (flat) color boundary at the junction of the two pieces — often perpendicular to the crystal axis. Hydrothermal synthetic shows straight parallel growth lines and may have a very abrupt color transition.
- RI and SG: RI 1.544–1.553; SG 2.65 — identical to all quartz. Synthetic: RI and SG are identical — these properties cannot distinguish natural from synthetic ametrine. Microscopy is essential.
Loupewise Pro includes a two-phase natural vs. synthetic testing protocol for Ametrine.
Common Simulants
- Bicolor Glass: Bicolor glass may mimic ametrine but is isotropic (no birefringence), typically shows gas bubbles or swirl marks under magnification, and RI will not match quartz range.
Treatments
- Irradiation (artificial ametrine from citrine)
- Heat Treatment (shifts/modifies color zones)
Measurement Guides
Identifying an ametrine? Loupewise walks through these tests in order — RI, SG, fluorescence, and more.
Try Loupewise Free →Studying for the GIA, FGA, or FEEG practical? Ametrine is one of the 132 species in Loupewise’s drill and exam pool — practice identifying it from its measured properties under timed exam conditions.
Practice exams →