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How to identify Shungite

Carbonaceous rock

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To correctly identify Shungite (Carbonaceous rock), 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 dull black to silvery-black.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Ranges from dull, earthy to sub-metallic or vitreous, depending on the carbon content and purity.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Can be massive, compact, or porous. Higher carbon content varieties tend to be more homogeneous and dense. Fracture surfaces are typically conchoidal to uneven.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Amorphous to cryptocrystalline; it does not form macroscopic crystals. Carbon is present as disordered, non-graphitic structures.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    None. It exhibits fracture.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Found in ancient Precambrian sedimentary basins that have undergone low-grade metamorphism, typically associated with black shales, schists, and other carbon-rich metasediments. The primary deposit is in the Shunga region of Karelia, Russia.

Key Facts

Hardness
3-4 on the Mohs scale
Specific Gravity
1.8-2.1 g/cm³ (varies with carbon content and impurities)
Crystal System
Amorphous to cryptocrystalline (no defined crystal system)
Color
Black, sometimes with a silvery sheen
Luster
Dull, earthy, sub-metallic, or vitreous
Transparency
Opaque
Fracture
Conchoidal to uneven
Cleavage
None
Composition
Primarily carbon (C), with varying amounts of silicates (SiO2, Al2O3, Fe2O3, MgO, K2O, etc.) and other trace elements. Carbon content can range from <10% to >98%.

Physical characteristics

  • Crystal Habit: Massive, compact, or porous aggregates; no distinct crystal forms.
  • Cleavage Type: Absent
  • Fracture Type: Conchoidal to uneven, sometimes splintery in lower-grade varieties.
  • Tenacity: Brittle
  • Luster Type: Dull, earthy, sub-metallic, or vitreous

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