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How to identify Epidote

Ca2(Al,Fe)3(SiO4)3(OH)

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To correctly identify Epidote (Ca2(Al,Fe)3(SiO4)3(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

    Typically pistachio-green to yellowish-green, olive-green, or blackish-green. Less commonly brown or colorless. The intensity of the green color generally increases with higher iron content.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Vitreous (glassy) to resinous on crystal faces, sometimes dull on massive forms.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Can be massive, granular, fibrous, or in well-formed prismatic crystals. Often found as radiating aggregates.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Monoclinic, typically forming elongated, prismatic crystals, often with one direction of perfect cleavage. Crystals are commonly striated parallel to their length. Can also occur as granular aggregates or massive forms.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    Perfect cleavage on {001}, and good cleavage on {100}. This results in a splintery or step-like fracture along cleavage planes.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Metamorphic rocks (greenschist, amphibolite facies), hydrothermally altered igneous rocks (e.g., porphyry deposits), veins, skarns, and as a secondary alteration product of plagioclase.

Key Facts

Hardness
6 - 7 on the Mohs scale
Specific Gravity
3.3 - 3.5 (varies with Fe content)
Crystal System
Monoclinic
Color
Pistachio-green, yellowish-green, olive-green, blackish-green, brown, rarely colorless
Luster
Vitreous to resinous
Transparency
Transparent to translucent to opaque
Fracture
Uneven to conchoidal
Cleavage
Perfect on {001}, good on {100}
Composition
Calcium aluminum iron sorosilicate hydroxide

Physical characteristics

  • Crystal Habit: Prismatic, elongated, often striated crystals; also massive, granular, fibrous, or radiating aggregates.
  • Cleavage Type: Perfect in one direction ({001}), good in another ({100}).
  • Fracture Type: Uneven to conchoidal.
  • Tenacity: Brittle.
  • Luster Type: Vitreous (glassy) to resinous.

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