
mineral
Black Tourmaline
Schorl (NaFe3Al6(Si6O18)(BO3)3(OH,F)4)
AI-generated identification · may be incorrectHardness: 7-7.5 on the Mohs scale, Color: Pitch black, Luster: Vitreous to submetallic, Crystal structure: Trigonal with striated prismatic crystals, Cleavage: Indistinct, Specific gravity: 3.2-3.8
- Hardness
- 7-7
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Physical properties
Hardness: 7-7.5 on the Mohs scale, Color: Pitch black, Luster: Vitreous to submetallic, Crystal structure: Trigonal with striated prismatic crystals, Cleavage: Indistinct, Specific gravity: 3.2-3.8
Formation & geological history
Forms in pegmatites and hydrothermal veins, as well as metamorphic rocks like schists and gneisses, typically associated with cooling magmatic fluids.
Uses & applications
Widely used in jewelry, metaphysical and healing practices, and industrial applications due to its pyroelectric and piezoelectric properties.
Geological facts
Black tourmaline is known scientifically as schorl, which accounts for about 95% of all tourmaline in nature. It was historically referred to by various names like schorl until the 18th century.
Field identification & locations
Easily identified by its deep black color, vitreous luster when tumbled or polished, and striations often visible on raw prismatic faces. Found globally, notably in Brazil, Pakistan, and the USA.
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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous
Septarian Pebble
Septarian nodule / Concretion
sedimentary