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How to identify Fossil Coral

Fossilized Anthozoa (Coral)

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To correctly identify Fossil Coral (Fossilized Anthozoa (Coral)), 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, including white, gray, brown, black, pink, red, yellow, and blue. Often exhibits multiple colors in a single specimen due to mineral impurities during silicification.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Vitreous to waxy, depending on the degree of silicification and polish.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Smooth to slightly granular when polished. Unpolished surfaces may show rougher textures reflecting the original coral structure. Distinctive patterns of preserved coral polyps are the key identifying feature.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Cryptocrystalline (chalcedony/agate) or microcrystalline quartz, replacing the original coral structure. Does not exhibit macroscopic crystal forms of quartz.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    None, due to its cryptocrystalline nature. It fractures conchoidally.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Typically found in marine sedimentary rock formations, particularly limestones, shales, and sandstones that were deposited in ancient shallow, warm seas where coral reefs thrived. Often associated with areas of past volcanic activity that provided silica-rich solutions for replacement.

Key Facts

Hardness
6.5-7 on Mohs scale (if silicified); 3-4 (if primarily calcium carbonate)
Specific Gravity
2.58-2.64 (if silicified); 2.71 (if primarily calcite)
Crystal System
Trigonal (for chalcedony/quartz replacement); Orthorhombic (for original aragonite); Hexagonal (for original calcite)
Color
Highly variable, often multi-colored with patterns
Luster
Vitreous to waxy
Transparency
Translucent to opaque
Fracture
Conchoidal to uneven
Cleavage
None
Composition
Primarily SiO2 (silica, as chalcedony/agate) if silicified; CaCO3 (calcium carbonate, as calcite or aragonite) if un-silicified or partially replaced.

Physical characteristics

  • Crystal Habit: Cryptocrystalline or microcrystalline aggregates, pseudomorphing the original coral structure.
  • Cleavage Type: None
  • Fracture Type: Conchoidal to uneven
  • Tenacity: Brittle
  • Luster Type: Vitreous to waxy

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