Talc
Real mineral · common · Mg₃Si₄O₁₀(OH)₂
The softest mineral on the Mohs scale. Forms by hydrothermal alteration of olivine and pyroxene in ultramafic rocks. Its greasy feel results from a layer structure in which sheets slide easily over one another.
Identity
- Formula
- Mg₃Si₄O₁₀(OH)₂
- Chemical class
- silicate
- Also known as
- Soapstone (massive variety), Steatite
Crystallography
- Crystal system
- monoclinic
- Habits
- foliated, massive, granular
- Fracture
- uneven
Physical properties
- Mohs hardness
- 1
- Density
- 2.75 g/cm³
- Luster
- pearly, waxy, dull
- Colors
- white, gray, green, brown
- Streak
- white
- Transparency
- translucent, opaque
Geology
- Origins
- metamorphic, hydrothermal
- Host rocks
- serpentinite, dolomite, schist
- Associated minerals
- Serpentine, Chlorite, Calcite, Tremolite
- Geography
- China, India, Brazil, USA, Finland
Classification
- Rarity
- common
- Gem quality
- No
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