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How to identify Diamond

Carbon

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To correctly identify Diamond (Carbon), 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 colorless to pale yellow or brown, but can occur in nearly any color (fancy colors) due to impurities or structural defects. Common colors include yellow, brown, green, blue, pink, red, and black.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Adamantine (diamond-like), exceptionally bright and reflective.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Rough, often greasy or waxy on unpolished surfaces; polished surfaces are extremely smooth.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Cubic system, commonly found as octahedra, dodecahedra, cubes, or combinations thereof. Macles (twinned crystals) are also common. Often exhibits trigons (triangular growth marks) on octahedral faces.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    Perfect octahedral cleavage in four directions. This means it can be split along specific planes, despite its extreme hardness.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Primarily found in kimberlite and lamproite pipes (volcanic conduits) that originate in the Earth's mantle. Also found in alluvial (placer) deposits, which are secondary deposits formed by the erosion and transport of primary kimberlite/lamproite sources.

Key Facts

Hardness
10 (Mohs scale), the hardest natural mineral.
Specific Gravity
3.50 - 3.53 g/cm³ (varies slightly with impurities).
Crystal System
Cubic (isometric).
Color
Colorless, yellow, brown, green, blue, pink, red, black, and other fancy colors.
Luster
Adamantine.
Transparency
Transparent to opaque.
Fracture
Conchoidal to uneven.
Cleavage
Perfect octahedral in four directions.
Composition
Pure carbon (C).

Physical characteristics

  • Crystal Habit: Octahedral, dodecahedral, cubic, or combinations; often rounded or distorted; also massive (bort) or radiating (carbonado).
  • Cleavage Type: Perfect, octahedral {111}.
  • Fracture Type: Conchoidal to uneven.
  • Tenacity: Brittle (despite extreme hardness, it can be fractured or cleaved by impact).
  • Luster Type: Adamantine.

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