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How to identify Apatite

Ca5(PO4)3(F,Cl,OH)

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To correctly identify Apatite (Ca5(PO4)3(F,Cl,OH)), 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 green, blue, yellow, brown, pink, purple, or colorless. Can also be white, gray, or black.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Vitreous to sub-resinous.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Typically crystalline, often forming hexagonal prisms. Can also be massive, granular, or botryoidal.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Hexagonal system, typically forming prismatic crystals with pyramidal terminations. Can also be tabular or acicular.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    Poor to indistinct on {0001} and {1010}.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Igneous rocks (granites, pegmatites, carbonatites), metamorphic rocks (marbles, gneisses), sedimentary rocks (phosphorites), hydrothermal veins.

Key Facts

Hardness
5 (Mohs scale)
Specific Gravity
3.16 - 3.22
Crystal System
Hexagonal
Color
Highly variable (green, blue, yellow, brown, pink, purple, colorless, etc.)
Luster
Vitreous to sub-resinous
Transparency
Transparent to translucent
Fracture
Conchoidal to uneven
Cleavage
Poor to indistinct on {0001} and {1010}
Composition
Calcium phosphate with fluoride, chloride, or hydroxyl anions

Physical characteristics

  • Crystal Habit: Prismatic, tabular, acicular, massive, granular, botryoidal
  • Cleavage Type: Poor to indistinct basal and prismatic
  • Fracture Type: Conchoidal to uneven
  • Tenacity: Brittle
  • Luster Type: Vitreous to sub-resinous

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