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How to identify Hornblende

Hornblende

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To correctly identify Hornblende (Hornblende), 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 green, dark brown, or black.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Vitreous to sub-vitreous, sometimes silky in fibrous varieties.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Prismatic, often elongated crystals. Can be massive or granular.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Monoclinic system, forming long, slender to stout prismatic crystals with a roughly hexagonal or rhombic cross-section. Often terminated by dome faces.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    Two distinct cleavage planes intersecting at approximately 56° and 124° (characteristic of amphiboles). This is a crucial diagnostic feature.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Common in intermediate to felsic igneous rocks (e.g., diorite, granodiorite, andesite) and a wide range of metamorphic rocks (e.g., amphibolite, hornblende schist, gneiss).

Key Facts

Hardness
5-6 on the Mohs scale
Specific Gravity
3.0-3.4 (variable depending on composition)
Crystal System
Monoclinic
Color
Dark green, dark brown, black
Luster
Vitreous to sub-vitreous
Transparency
Translucent to opaque
Fracture
Uneven to conchoidal
Cleavage
Perfect in two directions, intersecting at 56° and 124°
Composition
Complex calcium, magnesium, iron, aluminum silicate with hydroxyl (OH) groups. The general formula is (Ca,Na)2-3(Mg,Fe,Al)5(Al,Si)8O22(OH,F)2.

Physical characteristics

  • Crystal Habit: Prismatic, columnar, acicular, fibrous, massive, granular.
  • Cleavage Type: Perfect {110} cleavage, producing two planes at 56° and 124°.
  • Fracture Type: Uneven to conchoidal.
  • Tenacity: Brittle.
  • Luster Type: Vitreous to sub-vitreous, sometimes silky in fibrous varieties.

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