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How to identify Banded Chert

Sedimentary Chert

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To correctly identify Banded Chert (Sedimentary Chert), 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, often banded with alternating colors such as white, grey, black, brown, red, green, or yellow. The colors are due to trace impurities.

  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. Non-clastic.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Cryptocrystalline aggregates of quartz; individual crystals are microscopic and not visible to the naked eye.

  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

    Deep marine environments (e.g., abyssal plains, continental slopes) where siliceous microfossils accumulate, or in shallow marine settings where silica precipitates from seawater. Also found as nodules and concretions within limestones and dolomites, and as bedded deposits in association with volcanic rocks or Banded Iron Formations.

Key Facts

Hardness
7 (Mohs scale)
Specific Gravity
2.58 - 2.64
Crystal System
Trigonal (for the constituent quartz crystals, though cryptocrystalline)
Color
Highly variable, often banded; white, grey, black, brown, red, green, yellow
Luster
Dull to waxy, sometimes vitreous
Transparency
Opaque to translucent
Fracture
Conchoidal
Cleavage
None
Composition
Primarily Silicon Dioxide (SiO2)

Physical characteristics

  • Crystal Habit: Cryptocrystalline aggregates, forming massive, nodular, or bedded structures.
  • Cleavage Type: None
  • Fracture Type: Conchoidal, producing very sharp edges.
  • Tenacity: Brittle
  • Luster Type: Dull, waxy, or sub-vitreous

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