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How to identify Chert

Chert (microcrystalline quartz)

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To correctly identify Chert (Chert (microcrystalline quartz)), 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

    Highly variable; commonly gray, white, black, brown, red, green, or tan. Color is often due to trace impurities (e.g., iron oxides for red/brown, organic matter for black).

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Dull to waxy, sometimes vitreous on freshly fractured surfaces.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Very fine-grained (cryptocrystalline), smooth to slightly granular. Feels smooth and hard.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Does not exhibit macroscopic crystal forms; composed of microscopic quartz crystals. Occurs as nodules, concretions, or bedded layers.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    None. Exhibits conchoidal fracture.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Typically found as nodules or beds within carbonate rocks (limestone, dolomite) and shales. Also occurs as bedded deposits in deep marine environments, often associated with radiolarian or diatomaceous oozes. Can be found in residual soils where carbonate host rocks have weathered away.

Key Facts

Hardness
7 (Mohs scale)
Specific Gravity
2.58 - 2.64
Crystal System
Trigonal (for individual quartz crystals, but cryptocrystalline aggregate)
Color
Highly variable: gray, white, black, brown, red, green, tan
Luster
Dull to waxy, sometimes vitreous
Transparency
Opaque to translucent
Fracture
Conchoidal
Cleavage
None
Composition
Silicon dioxide (SiO2)

Physical characteristics

  • Crystal Habit: Cryptocrystalline aggregate; no macroscopic crystal habit. Occurs as nodules, concretions, or massive beds.
  • Cleavage Type: None
  • Fracture Type: Conchoidal, producing very sharp edges.
  • Tenacity: Brittle
  • Luster Type: Dull, waxy, or subvitreous

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