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How to identify Silicon Carbide

Silicon Carbide (SiC)

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To correctly identify Silicon Carbide (Silicon Carbide (SiC)), 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

    Natural moissanite is typically colorless, pale green, or greenish-black. Synthetic SiC can be colorless, green, blue, or black, often with iridescent hues.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Adamantine to metallic, often with a sub-metallic sheen in synthetic forms.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Crystalline, often with sharp edges in synthetic forms. Natural moissanite forms small, often hexagonal, crystals.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Hexagonal (alpha-SiC, 6H-SiC, 4H-SiC) or cubic (beta-SiC, 3C-SiC). Natural moissanite typically forms small, platy hexagonal crystals.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    Poor to distinct on {0001} in hexagonal polytypes.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Natural moissanite is found in kimberlites, lamproites, and as inclusions in some meteorites. These environments are characterized by high-pressure, high-temperature conditions deep within the Earth's mantle or extraterrestrial origins.

Key Facts

Hardness
9-9.5 (Mohs scale)
Specific Gravity
3.21 g/cm³
Crystal System
Hexagonal (most common polytypes, e.g., 6H-SiC, 4H-SiC) or Cubic (3C-SiC)
Color
Colorless, pale green, greenish-black (natural); colorless, green, blue, black (synthetic)
Luster
Adamantine to metallic
Transparency
Transparent to opaque
Fracture
Conchoidal to uneven
Cleavage
Poor to distinct on {0001}
Composition
Silicon Carbide (SiC)

Physical characteristics

  • Crystal Habit: Natural: Small, platy hexagonal crystals. Synthetic: Hexagonal plates, blocky crystals, or granular aggregates.
  • Cleavage Type: Poor to distinct basal cleavage in hexagonal polytypes.
  • Fracture Type: Conchoidal to uneven, very brittle.
  • Tenacity: Brittle
  • Luster Type: Adamantine to metallic

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