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How to identify Prehnite

Ca2Al(AlSi3O10)(OH)2

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To correctly identify Prehnite (Ca2Al(AlSi3O10)(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 pale green to yellowish-green, but can also be white, gray, or colorless. The green color is often soft and apple-like.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Vitreous (glassy) to pearly, especially on cleavage surfaces.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Often forms botryoidal (grape-like) or reniform (kidney-shaped) aggregates with a smooth, waxy feel. Individual crystals, when present, are typically tabular or prismatic.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Commonly found as botryoidal, reniform, or stalactitic masses. Individual crystals are rare but can be tabular or prismatic, often with a distinct termination.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    Good cleavage in one direction ({001}), often visible as parallel lines or steps on crystal faces or fractured surfaces.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Found in veins, vugs, and amygdules within mafic igneous rocks (basalts, gabbros, diabases) that have undergone low-grade metamorphism or hydrothermal alteration. Also occurs in some granitic rocks and gneisses.

Key Facts

Hardness
6-6.5 on the Mohs scale
Specific Gravity
2.80-2.95
Crystal System
Orthorhombic
Color
Pale green, yellowish-green, white, gray, colorless
Luster
Vitreous to pearly
Transparency
Translucent to transparent
Fracture
Uneven to subconchoidal
Cleavage
Good on {001}
Composition
Hydrous calcium aluminum silicate

Physical characteristics

  • Crystal Habit: Botryoidal, reniform, stalactitic, granular, massive; rarely as tabular or prismatic crystals.
  • Cleavage Type: Good in one direction ({001}), often producing platy fragments or steps.
  • Fracture Type: Uneven to subconchoidal, meaning it breaks with irregular, rough surfaces or slightly curved, shell-like surfaces.
  • Tenacity: Brittle, meaning it breaks or crumbles easily when struck.
  • Luster Type: Vitreous (glassy) on most surfaces, becoming pearly on cleavage surfaces.

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