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How to identify Bronzite

Enstatite variety

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To correctly identify Bronzite (Enstatite variety), 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

    Brownish-green to dark brown, often with golden or bronze reflections.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Submetallic to bronzy, vitreous on fresh fracture surfaces. The characteristic bronzy schiller is a key identifier.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Typically massive, granular, or lamellar. Can be found as disseminated grains or larger crystals within host rocks.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Orthorhombic system. Crystals are usually prismatic, often with a square or rectangular cross-section. Cleavage is well-developed.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    Two distinct cleavages at nearly 90 degrees (orthorhombic pyroxene cleavage), specifically {210} and {100} or {010} at 87° and 93°.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Mafic and ultramafic igneous rocks (e.g., norites, gabbros, peridotites, pyroxenites), high-grade metamorphic rocks, and occasionally in meteorites.

Key Facts

Hardness
5.5 - 6 on the Mohs scale.
Specific Gravity
3.2 - 3.3 (varies with Fe content).
Crystal System
Orthorhombic.
Color
Brownish-green to dark brown, often with a bronzy schiller.
Luster
Submetallic to bronzy, vitreous.
Transparency
Translucent to opaque.
Fracture
Uneven to conchoidal.
Cleavage
Perfect {210} and good {100} or {010} at nearly 90 degrees (87° and 93°).
Composition
Magnesium iron silicate, (Mg,Fe)SiO3, with Fe/(Mg+Fe) ratio typically between 0.1 and 0.3.

Physical characteristics

  • Crystal Habit: Prismatic, often with a square or rectangular cross-section; also massive, granular, lamellar.
  • Cleavage Type: Perfect {210} and good {100} or {010} at nearly 90 degrees (orthorhombic pyroxene cleavage).
  • Fracture Type: Uneven to conchoidal.
  • Tenacity: Brittle.
  • Luster Type: Submetallic to bronzy (schiller), vitreous.

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