Talc

Crystal system · Monoclinic

Talc is a silicate mineral prized by collectors for its exceptional color range, with notable Chinese occurrences.

About Talcextended article

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China is a defining locality for Talc · 滑石. See the Chinese collector page →

Crystal Structure
2:1 phyllosilicate — no interlayer cations (hence softness).
Elemental Composition (by mass)
ElementMass %Visual
O Oxygen46.07%
Si Silicon32.35%
Mg Magnesium21.00%
H Hydrogen0.58%
Computed from simplified end-member formula. Solid-solution series, water content, and trace substitutions cause real-world variation.
IMA Abbreviation (Whitney-Evans 2010)
Tlc
→ Talc
Soft phyllosilicate
Standard symbol from American Mineralogist (Whitney & Evans, 2010). Used in thin-section labeling, phase diagrams, and IMA-style species records.
Pronunciation
/tælk/
talk
Arabic talq
Tenacity
Behavior:
flexible
Under stress:
Soft, soapy
Mohs 1 — softest mineral; bends and crumbles.
Luster
pearlygreasy
Soapy feel; pearly to greasy.
Diagnostic Field Tests
Hardness→ Mohs 1 — softest mineral; greasy feel
Marks paper; soapy feel.
⚠ 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.
Mohs 1
Vickers (~) 1 HV
Knoop (~) 32 HK
Geological setting
Hydrothermal
Element composition by mass

Formula: Mg₃Si₄O₁₀(OH)₂ · molar mass: 379.26 g/mol

O 50.62%
Si 29.62%
Mg 19.23%
H 0.53%

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

Mohs Hardness 1

Talc sits at 1 on the Mohs scale — soft enough to be scratched by a fingernail.

Colors:
Streak
White
Crystal system
Monoclinic
SilicatesSilicates (Phyllosilicates)
TL;DR · 1 min read
Talc (Mg₃Si₄O₁₀(OH)₂) is the softest mineral on the Mohs scale (1) — defining the bottom of the hardness reference. Its greasy feel and white color are diagnostic.

Talc (Mg₃Si₄O₁₀(OH)₂) is the softest mineral on the Mohs scale (1) — defining the bottom of the hardness reference. Its greasy feel and white color are diagnostic. Talc forms by hydrothermal alteration of magnesium-rich rocks (peridotite, dolomite). Massive talc (“steatite” or “soapstone”) has been carved since prehistory. Major industrial source for cosmetics, ceramics, paper.

More minerals to explore

About Talc

Talc belongs to the silicate class in the talc-pyrophyllite group and has the chemical formula Mg3Si4O10(OH)2. It crystallizes in the monoclinic system and is one of the most visually varied minerals in the collector market.

Identification & care

Talc typically forms tabular pseudo-hexagonal plates; foliated, lamellar; massive (steatite/soapstone); granular; fine-grained. Its color range is broad, including white, grey, pale green, yellowish, rarely brown or colorless, and 'soapstone' is massive grey-green variety. The luster is waxy, pearly, greasy, the streak is white, and specimens range from transparent to translucent. The cleavage is perfect basal on {001} — flexible but not elastic plates (contrast with mica which is elastic). The fracture is micaceous (dominated by cleavage), which aids identification.

Collector context

Collector notes

Among collectors of crystallized species, Talc is a recognized reference. Documented Chinese occurrences are recorded at Dabaoshan Mine and Xikuangshan Sb deposit (Xikuangshan antimony deposit), among others.