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How to identify Iolite

Cordierite

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To correctly identify Iolite (Cordierite), 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 blue, violet-blue, yellowish-gray, brownish-yellow, or colorless. Strong pleochroism is a key identifier, showing different colors (e.g., deep violet-blue, pale blue, yellowish-gray) when rotated.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Vitreous (glassy) to greasy.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Often occurs as disseminated grains, anhedral to subhedral crystals, or columnar aggregates within metamorphic rocks. Gem-quality material is typically transparent to translucent.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Orthorhombic system. Crystals are typically prismatic, often with pseudohexagonal cross-sections due to twinning. Twinning is common, often cyclic or lamellar.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    Distinct to good cleavage on {010}, poor on {100} and {001}. Fracture is conchoidal to uneven.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Metamorphic rocks (schists, gneisses, hornfels) derived from aluminous sediments. Also found in some granites and pegmatites.

Key Facts

Hardness
7-7.5 (Mohs scale)
Specific Gravity
2.53-2.78 g/cm³
Crystal System
Orthorhombic
Color
Blue, violet-blue, yellowish-gray, brownish-yellow, colorless (strongly pleochroic)
Luster
Vitreous to greasy
Transparency
Transparent to translucent
Fracture
Conchoidal to uneven
Cleavage
Distinct to good on {010}, poor on {100} and {001}
Composition
Magnesium iron aluminum cyclosilicate

Physical characteristics

  • Crystal Habit: Prismatic, often pseudohexagonal due to twinning; also massive, granular, or columnar aggregates.
  • Cleavage Type: Distinct to good in one direction ({010}), poor in two others ({100}, {001}).
  • Fracture Type: Conchoidal to uneven.
  • Tenacity: Brittle.
  • Luster Type: Vitreous to greasy.

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