Amethyst

Crystal system · Trigonal

Amethyst is a silicate mineral recognized for its hardness and durability, with notable Chinese occurrences.

Violet to purple variety of quartz, hexagonal.

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Typical Price Tiers (per ct)
Entry
$5+
Mid-tier
$30+
Premium
$150+
Investment
$800+
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.
Crystal Structure
Variety of quartz — same structure as parent.
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)
ElementMass %Visual
O Oxygen53.26%
Si Silicon46.74%
Computed from simplified end-member formula. Solid-solution series, water content, and trace substitutions cause real-world variation.
Reference Resources
IMA Abbreviation (Whitney-Evans 2010)
Qz
→ Quartz
Variety of quartz; uses parent symbol
Standard symbol from American Mineralogist (Whitney & Evans, 2010). Used in thin-section labeling, phase diagrams, and IMA-style species records.
⏳ Long-term Aging & Care Timeline
color fade (very slow)decades
Trigger: intense sunlight
Intervention: Most amethyst color stable for normal display. Extreme sunlight over decades may lighten.
Pronunciation
/ˈæməθɪst/
AM-uh-thist
three syllables (Greek)
Birthstone & Anniversary Gift Reference
January (zodiac)zodiac: Capricorn / Aquarius
February (modern, traditional, zodiac)zodiac: Aquarius / Pisces
UV Fluorescence
SW (254 nm)
none
LW (365 nm)
none
Inert.
SW = shortwave (germicidal lamp). LW = longwave (blacklight). Response varies with locality, trace impurities, and treatment.
Tenacity
Behavior:
brittle
Under stress:
Same as quartz
Same as quartz.
Luster
vitreous
Same as quartz parent.
Color Cause (Chromophore)
Chromophore:
Fe-induced color center
Mechanism:
natural irradiation of Fe-bearing quartz
Color produced:
purple
Color centers form when ionizing radiation excites trapped Fe³⁺/Fe⁴⁺ pairs. Heat destroys color center.
Notable localities (coordinates)
All localities and full GeoJSON available at /wp-json/mmb/v1/localities-geo
Diaphaneity (Transparency)
transparent
Gem-quality transparent; some massive material is translucent.
Type Locality
(known since antiquity) — Worldwide
Magnetism
Category:
weakly paramagnetic
Test result:
Very slight pull (Fe color center)
Iron color center gives faint paramagnetism.
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
Hydrothermal 1965 · Russian / Chinese
Difficult to distinguish from natural. Twinning patterns (Brazil-law) less common in synthetic — important diagnostic.
Common imitations
Purple glass
Singly refractive, no twinning, gas bubbles.
Synthetic corundum (purple)
Higher RI; doubly refractive.
Geological Setting
Environment:
hydrothermal
Host rock:
basalt geode, agate vug, hydrothermal vein
Companions:
Agate · Calcite · Goethite · Celadonite
Most amethyst forms in geode cavities within basaltic lavas (Brazil, Uruguay) or pegmatite veins (Ural, Madagascar).
Treatments & Enhancements
Heat treatmentoccasionalstable· detection: hard
Heating amethyst produces citrine. Most "citrine" on market is actually heated amethyst. Accepted with disclosure.
As a buyer: request written disclosure of treatments and confirm whether the price reflects treated or untreated material.
Characteristic Inclusions
Tiger-stripe zoninggrowth-pattern★ diagnostic
Brazil-law twinning creates alternating colorless/violet bands visible under crossed polars.
Goethite needlessolid
Hair-like dark brown FeO(OH) inclusions in some Brazilian material.
Diagnostic inclusions are characteristic enough to help identify origin or species under 10× loupe.
Twinning Laws
Brazil lawpenetration
Brazil-law twinning produces the characteristic "tiger-stripe" zoning in amethyst.
Dauphiné lawpenetration
Same 60° c-axis rotation as in rock crystal.
Care notesAvoid prolonged sun exposure — fades. Otherwise water-stable. Full cleaning guide →
Formation eraHydrothermal cavity filling; Rio Grande do Sul geodes 130 Ma volcanic.
Pleochroism (dichroic)
Axis o
red-violet
Axis e
blue-violet
Strength: weak
Subtle but present; sometimes called "doubly refractive amethyst" effect.
Cleavage & Fracture
Cleavage:
none
Fracture:
conchoidal
No cleavage; conchoidal fracture as in all quartz.
Market availability: Common
Widely available in most dealer stocks. Specimens span all price tiers.
Collector tier: Cabinet Classic
World-class display species — sought after for cabinet collections, well-documented localities, frequent show-piece pieces.
Often found withQuartz · Calcite · Agate · Celestine
Mohs 7
Vickers (~) 1400 HV
Knoop (~) 1100 HK
Geological setting
Volcanic
Element composition by mass

Formula: SiO₂ (quartz var.) · molar mass: 60.08 g/mol

O 53.26%
Si 46.74%

Computed from atomic weights (IUPAC 2021). Site-occupancy groups (Fe,Mn) split equally.

GroupQuartz Group (silica)
Related members: Quartz · Citrine · Rose Quartz · Chalcedony · Agate · Jasper
Mohs Hardness 7

Amethyst sits at 7 on the Mohs scale — harder than glass; scratches steel.

🔊 Read aloud
Colors:
Streak
White
Crystal system
Trigonal
Pronunciation/ˈæməθɪst/
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Oxides & HydroxidesOxides (Silica Group)
TL;DR · 1 min read
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).

More minerals to explore #

Identification & care

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.

Available Amethyst specimens

3 specimens