
mineral
Black Tourmaline (Schorl)
NaFe3+3Al6(BO3)3Si6O18(OH)4
AI-generated identification · may be incorrectHardness: 7-7.5 Mohs. Color: Deep black. Luster: Vitreous to resinous. Crystal structure: Trigonal (often striated prismatic crystals or rough nodular aggregates). Cleavage: Indistinct. Specific gravity: 3.0-3.2.
- Hardness
- 7-7
- Color
- Deep black
- Luster
- Vitreous to resinous
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Physical properties
Hardness: 7-7.5 Mohs. Color: Deep black. Luster: Vitreous to resinous. Crystal structure: Trigonal (often striated prismatic crystals or rough nodular aggregates). Cleavage: Indistinct. Specific gravity: 3.0-3.2.
Formation & geological history
Forms primarily in pegmatites, high-grade metamorphic rocks, and hydrothermal veins during the late stages of magmatic crystallization.
Uses & applications
Popularly used for metaphysical and grounding purposes, lapidary carvings, mineral collection specimens, and historically in scientific instruments due to its pyroelectric properties.
Geological facts
Black tourmaline, known as schorl, is the most common variety of tourmaline, accounting for nearly 95% of all tourmaline found in nature. It exhibits strong piezoelectricity and pyroelectricity, generating an electrical charge under heat or pressure.
Field identification & locations
Identified by its intense black color, high hardness (scratches glass), triangular or rounded-triangular cross-section, and characteristic parallel striations along crystal faces. Commonly found in pegmatite fields worldwide, such as in Brazil, Madagascar, and Maine, 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
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
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