Bolivian "ametrine" / Uruguayan deep-saturated top. Wholesale very low.
Approximate retail prices. Wholesale + private sale typically 40-60% of retail. Auction premium 10-25%. For investment-grade purchase steps, see the investment checklist.
External databases provide CIF (Crystallographic Information File) downloads + interactive 3D viewers. AMCSD: American Mineralogist Crystal Structure Database (free, RRUFF-hosted). COD: open community-curated database.
Elemental Composition (by mass)
Element
Mass %
Visual
OOxygen
53.26%
SiSilicon
46.74%
Computed from simplified end-member formula. Solid-solution series, water content, and trace substitutions cause real-world variation.
Test with rare-earth magnet (N42 or N52 neodymium). Suspend specimen on thread for sensitive paramagnetic detection. Diamagnetic minerals are weakly repelled (visible only with strong magnets like bismuth).
Specific Gravity
2.65
g/cm³
light
Same as quartz.
For comparison: water = 1.00, glass ≈ 2.5, quartz = 2.65, corundum ≈ 4.00, galena ≈ 7.50, gold ≈ 19.3.
Synthetics & Imitations
Lab-grown methods
Hydrothermal1965 · Russian / Chinese
Difficult to distinguish from natural. Twinning patterns (Brazil-law) less common in synthetic — important diagnostic.
Amethyst is the violet to purple variety of quartz (SiO₂) colored by trace iron and natural irradiation. The February birthstone, Amethyst is one of the most-collected mineral varieties globally.
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Amethyst is the violet to purple variety of quartz (SiO₂) colored by trace iron and natural irradiation. The February birthstone, Amethyst is one of the most-collected mineral varieties globally. Brazilian (Minas Gerais) geodes supply massive crystallized specimens; Uruguay produces deeper purple material. Color fades with prolonged sun exposure (heat-treatable to citrine).
Amethyst typically forms prismatic, pyramidal, scepter, phantom; geodes; clusters. Its color is typically violet to purple. The luster is vitreous, the streak is white, and specimens range from transparent to translucent.
Collector context
How it forms
The geological setting for Amethyst is typically hydrothermal; volcanic rock cavities (geodes); pegmatites. It is commonly found in association with quartz, calcite, agate.
Classic Chinese localities
Documented Chinese occurrences are recorded at Huanggang Fe-Sn deposit, among others.
Why collectors care
Collectors pursue Amethyst for the clarity of its crystal form and, in good material, saturated color that reads instantly across a display case. A well-terminated amethyst on clean matrix photographs well, identifies quickly, and anchors a cabinet piece. Top Chinese specimens over the last two decades have reset the bar for what amethyst looks like at collector grade.
What affects value
Value in Amethyst is assessed, in typical order of weight, against: (1) locality provenance; (2) size relative to the species norm; (3) crystal form and termination sharpness; (4) color saturation and zoning; (5) transparency and internal clarity; (6) matrix quality and aesthetic balance; (7) condition (absence of damage, chips, or repair). Cleaning quality and verified locality documentation act as multipliers across the above.
Naming history
The name Amethyst has a specific etymological and historical context — see Mindat's reference entry for provenance details. We have retained naming data at the record level; published prose is paraphrased from factual fields rather than copied from source.
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