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How to identify Biotite

K(Mg,Fe)3AlSi3O10(OH)2

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To correctly identify Biotite (K(Mg,Fe)3AlSi3O10(OH)2), 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 dark brown, black, or greenish-black. Rarely yellowish-brown.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Vitreous to pearly on cleavage surfaces, duller on other surfaces.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Foliated, flaky, or scaly aggregates. Individual crystals are platy.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Pseudohexagonal tabular crystals, often forming books or flakes. Can also be disseminated as small flakes within rocks.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    Perfect basal cleavage (001), allowing it to be split into very thin, flexible, and elastic sheets.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Common in igneous rocks (granites, diorites, syenites, pegmatites, some volcanic rocks), metamorphic rocks (schists, gneisses, hornfels), and detrital sediments.

Key Facts

Hardness
2.5-3 on the Mohs scale
Specific Gravity
2.7-3.3 g/cm³ (varies with Fe/Mg ratio)
Crystal System
Monoclinic
Color
Dark brown, black, greenish-black
Luster
Vitreous to pearly
Transparency
Transparent to translucent in thin sheets, opaque in thicker pieces
Fracture
Uneven to splintery (rarely observed due to perfect cleavage)
Cleavage
Perfect basal cleavage (001)
Composition
Potassium iron magnesium aluminum silicate hydroxide

Physical characteristics

  • Crystal Habit: Pseudohexagonal tabular crystals, often forming 'books' or flakes; also massive, disseminated, or scaly aggregates.
  • Cleavage Type: Perfect basal cleavage (one direction), producing thin, flexible, and elastic sheets.
  • Fracture Type: Uneven to splintery, but rarely observed due to dominant cleavage.
  • Tenacity: Flexible and elastic (sheets can be bent and will return to their original shape).
  • Luster Type: Vitreous to pearly on cleavage surfaces, submetallic to dull on other surfaces.

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