Topaz

Crystal system · Orthorhombic

Topaz is a silicate mineral valued for its hardness and gem potential, with several world-class Chinese localities.

About Topazextended article

China-iconic

China is a defining locality for Topaz · 黄玉. See the Chinese collector page →

Crystal Structure
Orthorhombic — isolated SiO₄ + Al octahedra cross-linked by F/OH.
Elemental Composition (by mass)
ElementMass %Visual
O Oxygen34.77%
Al Aluminum29.32%
F Fluorine20.65%
Si Silicon15.26%
Computed from simplified end-member formula. Solid-solution series, water content, and trace substitutions cause real-world variation.
IMA Abbreviation (Whitney-Evans 2010)
Tpz
→ Topaz
Pegmatite indicator
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
imperial topaz color fadeyears
Trigger: sunlight
Intervention: Sherry/imperial topaz may slowly lighten in sun. Blue topaz (irradiated) is generally stable.
Pronunciation
/ˈtoʊpæz/
TOH-paz
two syllables (Greek)
Lapidary & Faceting Recommendations
Recommended cut:
oval
Also seen:
pear, emerald, cushion
Typical yield:
30% of rough
Perfect basal cleavage means avoid placing table parallel to {001}. Cleavage planes must be at ≥30° to table for safe wear.
Birthstone & Anniversary Gift Reference
November (modern, traditional, zodiac)zodiac: Scorpio / Sagittarius
⚠ Safety & Handling
light-sensitivelow
Some imperial topaz fades slightly with extreme UV.
Handling: Diffused lighting OK.
Information provided in good faith. Consult local hazmat regulations for transport and disposal. Severely hazardous specimens may require special storage cabinets.
UV Fluorescence
SW (254 nm)
Yellow / orange
moderate
LW (365 nm)
Yellow
weak
Imperial topaz shows weak response; blue topaz often inert.
SW = shortwave (germicidal lamp). LW = longwave (blacklight). Response varies with locality, trace impurities, and treatment.
Famous specimens of this species
American Golden Topaz — 22892.5 ct
Largest faceted yellow topaz. 172 facets.
Origin: Minas Gerais, Brazil. Now at: Smithsonian NMNH. Recorded 1984.
El-Dorado Topaz — 31000 ct
World's largest faceted gem of any species.
Origin: Brazil. Now at: Private. Recorded 1984.
Tenacity
Behavior:
brittle (cleaves)
Under stress:
Splits along basal {001}
Perfect basal cleavage means careful handling at the parting plane.
Luster
vitreous
Bright vitreous.
Color Cause (Chromophore)
Chromophore:
color centers + Cr
Mechanism:
irradiation + heat
Color produced:
blue / yellow / pink
Imperial topaz: Cr-related color center. Blue topaz: irradiation-heat treatment.
Diaphaneity (Transparency)
transparent
Imperial, blue, and colorless topaz all transparent.
Type Locality
(ancient term) — Egypt (Topazos Island)
Source: Pliny
Magnetism
Category:
diamagnetic
Test result:
Slight repulsion
Al₂SiO₄(F,OH)₂; diamagnetic.
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).
Diagnostic Field Tests
Cleavage→ Perfect basal — careful handling
Sharp tap along c-axis can split crystals.
⚠ Use dilute HCl (~10%) only on inconspicuous spots; rinse promptly. Smell-tests should be brief and ventilated. Taste-test ONLY halite/sylvite — never lead, arsenic, or sulfur minerals.
Specific Gravity
3.49–3.57
g/cm³
medium
Heavier than quartz; lighter than corundum.
For comparison: water = 1.00, glass ≈ 2.5, quartz = 2.65, corundum ≈ 4.00, galena ≈ 7.50, gold ≈ 19.3.
Geological Setting
Environment:
pegmatite
Host rock:
granitic pegmatite, rhyolite, greisen
Companions:
Quartz · Feldspar · Cassiterite · Fluorite
Russian Urals topaz (Imperial topaz) comes from greisens around tin-tungsten deposits.
Treatments & Enhancements
Irradiation + heatuniversalstable· detection: hard
Colorless topaz irradiated then heated produces "Swiss blue", "London blue". Trade-standard, accepted.
Coatingoccasionalunstable· detection: easy
"Mystic topaz" — surface metallic coating gives rainbow color. Coating wears off with use; must be disclosed.
As a buyer: request written disclosure of treatments and confirm whether the price reflects treated or untreated material.
Characteristic Inclusions
Two-phase inclusionstwo-phase
Long needle-like cavities with liquid + bubble.
Negative crystalsnegative
Cavities mirroring host crystal habit.
Diagnostic inclusions are characteristic enough to help identify origin or species under 10× loupe.
Care notesStable but has perfect cleavage — avoid mechanical shock. No ultrasonic cleaning. Full cleaning guide →
Formation eraGranite-pegmatite + greisen; Russian Urals topaz Mesozoic.
Pleochroism (dichroic)
Axis o
colorless / paler
Axis e
characteristic body color
Strength: weak to moderate
Imperial topaz shows yellow-pink dichroism most clearly.
Cleavage & Fracture
Cleavage:
perfect 1 direction {001} — basal
Fracture:
subconchoidal
Perfect basal cleavage — important when cutting.
Market availability: Uncommon
Found at major shows and select dealers. Quality varies by locality.
Collector tier: Cabinet Classic
World-class display species — sought after for cabinet collections, well-documented localities, frequent show-piece pieces.
Often found withCassiterite · Quartz · Mica · Fluorite · Fluorapatite
Mohs 8
Vickers (~) 1650 HV
Knoop (~) 1340 HK
Nickel–Strunz 9.AF.35
Dana 52.03.01.01
Geological setting
Pegmatite
Diagnostic properties
Pyroelectric
Element composition by mass

Formula: Al2(SiO4)(F,OH)2 · molar mass: 182.05 g/mol

O 43.94%
Al 29.64%
Si 15.43%
F 10.44%
H 0.55%

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

Mohs Hardness 8
1
Talc
2
Gypsum
3
Calcite
4
Fluorite
5
Apatite
6
Orthoclase
7
Quartz
8
Topaz
9
Corundum
10
Diamond

Topaz sits at 8 on the Mohs scale — very hard; only diamond or corundum scratches it.

Colors:
Streak
White
Crystal system
Orthorhombic
Pronunciation/ˈtoʊpæz/
Type localitySchneckenstein, Saxony, Germany (classical)
Discovery First described 1737 by Johann Friedrich Henckel (Germany)
SilicatesSilicates – Nesosilicates
TL;DR · 1 min read
Topaz is the iconic Mohs-8 reference mineral and a Chinese Sichuan signature. The Xuebaoding district produces the world reference for translucent colorless and pale-blue topaz crystals on milky quartz, often paired with cassiterite and beryl.

Topaz is the iconic Mohs-8 reference mineral and a Chinese Sichuan signature. The Xuebaoding district produces the world reference for translucent colorless and pale-blue topaz crystals on milky quartz, often paired with cassiterite and beryl. Sichuan topaz – distinct from heat-treated commercial topaz – is the gem-collector standard.

Notable Varieties

  • Imperial topaz (orange-pink)
  • Sherry topaz (champagne)
  • Sky-blue topaz
  • Colorless topaz

The Chinese Angle

Xuebaoding Mine (Sichuan) is the world reference for collector-grade Chinese topaz – sharp pale-blue and colorless crystals on smoky quartz with cassiterite and beryl. Xianghualing in Hunan produces a secondary supply, often as smaller pale topaz crystals in pegmatite pockets. Both are untreated natural color.

Cite this entry
APA
MyMineralBox Editorial Team. (2026). Topaz. My Mineral Box. Retrieved May 23, 2026, from https://mymineralbox.com/mineral-encyclopedia/minerals/topaz/
MLA
MyMineralBox Editorial Team. "Topaz." My Mineral Box, 2026, https://mymineralbox.com/mineral-encyclopedia/minerals/topaz/. Accessed May 23, 2026.
Chicago
MyMineralBox Editorial Team. "Topaz." My Mineral Box. Last modified May 3, 2026. https://mymineralbox.com/mineral-encyclopedia/minerals/topaz/.
BibTeX
@misc{mmb_topaz,
 author = {{MyMineralBox Editorial Team}},
 title = {{Topaz}},
 year = {2026},
 publisher = {My Mineral Box},
 url = {https://mymineralbox.com/mineral-encyclopedia/minerals/topaz/},
 urldate = {2026-05-23}
}

About Topaz

Topaz belongs to the silicate class in the topaz group and has the chemical formula Al₂(SiO₄)(F,OH)₂. It crystallizes in the orthorhombic system and is one of the most visually varied minerals in the collector market. Its combination of structural character and global distribution make it a recognized species in both systematic and aesthetic collections.

Identification & care

Crystals commonly develop as prismatic with diamond-shaped cross-section; striated; often large crystals. Its color range is broad, including colorless, pale blue, light green, yellow, yellowish-brown, orange, pink, reddish-pink, and pale pink. The luster is vitreous, the streak is white, and specimens are typically transparent. The cleavage is perfect basal {001} — one direction, very pronounced. The fracture is conchoidal to uneven, which aids identification.

Collector context

How it forms

In terms of geology, Topaz forms in granitic pegmatites; high-temperature pneumatolytic veins; alluvial. It is commonly found in association with quartz, feldspar, tourmaline, beryl, cassiterite, fluorite.

Classic Chinese localities

Xianghualing Sn-polymetallic ore field, and Xihuashan ore field are each a benchmark source for topaz.

Why collectors care

Topaz occupies a rare position: it matters equally to specimen collectors and to the gem trade. Crisp natural crystals with saturated color and good clarity command premium pricing and are among the highest-prestige targets in any systematic collection.

What affects value

Value in Topaz is assessed, in typical order of weight, against: (1) locality provenance; (2) crystal size; (3) transparency and internal clarity; (4) color intensity and saturation; (5) crystal form and termination sharpness; (6) matrix and associated-species aesthetics; (7) gem-cutting potential. Verified locality documentation and cutting potential further elevate collector demand.

Naming history

The name Topaz 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.