How to identify Black Tourmaline
Schorl
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Open the appTo correctly identify Black Tourmaline (Schorl), check each of these features in order. Many rocks and minerals look alike, so cross-reference multiple properties before deciding.
Step-by-step identification
- 1
Color
Overall color and any zoning or banding
Opaque black, sometimes with a very dark blue or brown tint.
- 2
Luster
How the surface reflects light: metallic, vitreous, dull
Vitreous to resinous, sometimes sub-metallic on fresh fracture surfaces.
- 3
Texture
Grain size and surface feel: coarse, fine, glassy
Typically forms elongated, prismatic crystals. Can also be massive or granular.
- 4
Crystal Form
Shape of visible crystals or crystal faces
Hexagonal (trigonal) system, often forming long, slender to stout prismatic crystals with characteristic vertical striations parallel to the c-axis. Cross-sections are typically triangular with rounded edges.
- 5
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
Poor to indistinct, exhibiting a conchoidal to uneven fracture rather than true cleavage.
- 6
Geological Environment
The rock formation and setting where it occurs
Granitic pegmatites, granites, aplites, high-temperature hydrothermal veins, and metamorphic rocks like schists and gneisses.
Key Facts
- Hardness
- 7-7.5 (Mohs scale)
- Specific Gravity
- 3.06-3.26 g/cm³
- Crystal System
- Trigonal
- Color
- Opaque black, sometimes with a very dark blue or brown tint
- Luster
- Vitreous to resinous
- Transparency
- Opaque
- Fracture
- Conchoidal to uneven
- Cleavage
- Poor to indistinct (no true cleavage)
- Composition
- Complex borosilicate of aluminum, iron, and other elements
Physical characteristics
- Crystal Habit: Prismatic, columnar, acicular, massive, granular. Crystals are typically elongated with vertical striations.
- Cleavage Type: None to very poor, parting may be observed along rhombohedral planes.
- Fracture Type: Conchoidal to uneven, brittle.
- Tenacity: Brittle
- Luster Type: Vitreous to resinous, sometimes sub-metallic.
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