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How to identify Black Tourmaline

Schorl (Iron Tourmaline)

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To correctly identify Black Tourmaline (Schorl (Iron Tourmaline)), 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. 1

    Color

    Overall color and any zoning or banding

    Typically opaque black, sometimes very dark blue or brownish-black.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Vitreous (glassy) to resinous.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Often found as elongated, prismatic crystals, sometimes radiating or massive. Crystals frequently exhibit prominent vertical striations on their prism faces.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Hexagonal-rhombohedral crystal system, typically forming elongated prismatic crystals with a characteristic triangular cross-section (though often appearing hexagonal due to prism faces). Terminations can be complex, often hemimorphic.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    Indistinct to poor basal cleavage, often appearing to lack cleavage. Fracture is more common than cleavage.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Most commonly found in granitic pegmatites, high-temperature hydrothermal veins, and metamorphic rocks (schists, gneisses). Can also occur in granites and other igneous rocks.

Key Facts

Hardness
7-7.5 (Mohs scale)
Specific Gravity
3.06-3.26 g/cm³ (typically around 3.1-3.2)
Crystal System
Trigonal (hexagonal-rhombohedral)
Color
Opaque black, sometimes very dark blue or brownish-black
Luster
Vitreous to resinous
Transparency
Opaque
Fracture
Conchoidal to uneven
Cleavage
Indistinct to poor basal cleavage {0001}
Composition
Complex borosilicate of aluminum, iron, and other elements. End-member formula: NaFe₃Al₆(BO₃)₃Si₆O₁₈(OH)₄

Physical characteristics

  • Crystal Habit: Prismatic, columnar, acicular, radiating, massive. Crystals often show prominent vertical striations on prism faces and a characteristic rounded triangular cross-section.
  • Cleavage Type: Indistinct to poor basal cleavage {0001}. Typically fractures rather than cleaves.
  • Fracture Type: Conchoidal to uneven.
  • Tenacity: Brittle.
  • Luster Type: Vitreous (glassy) to resinous.

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