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How to identify Olivine

(Mg,Fe)2SiO4

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To correctly identify Olivine ((Mg,Fe)2SiO4), 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 olive-green, yellowish-green, or brownish-green. Can also be yellow, brown, or rarely colorless.

  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

    Granular aggregates are common. Individual crystals are typically stubby prismatic.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Orthorhombic system; typically forms stubby, equant, or tabular crystals. Often found as disseminated grains or granular masses in igneous rocks.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    Poor to indistinct in two directions at 90 degrees, often appearing as conchoidal fracture rather than true cleavage.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Mafic and ultramafic igneous rocks (basalt, gabbro, peridotite, dunite), mantle xenoliths, and some metamorphic rocks (e.g., serpentinites, marbles).

Key Facts

Hardness
6.5-7 on the Mohs scale
Specific Gravity
3.2-4.3 (increases with Fe content; forsterite ~3.2, fayalite ~4.3)
Crystal System
Orthorhombic
Color
Olive-green, yellowish-green, brownish-green, yellow, brown, rarely colorless
Luster
Vitreous to greasy
Transparency
Transparent to translucent
Fracture
Conchoidal to uneven
Cleavage
Poor to indistinct {010} and {110}
Composition
Magnesium iron silicate

Physical characteristics

  • Crystal Habit: Typically granular, massive, or as disseminated anhedral to subhedral grains. Individual crystals are usually stubby prismatic or tabular.
  • Cleavage Type: Poor to indistinct, often masked by fracture. Two directions at approximately 90 degrees.
  • Fracture Type: Conchoidal to uneven, brittle.
  • Tenacity: Brittle
  • Luster Type: Vitreous to greasy

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