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How to identify Herkimer Diamond Quartz

Quartz (SiO2) with hydrocarbon inclusions

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To correctly identify Herkimer Diamond Quartz (Quartz (SiO2) with hydrocarbon inclusions), 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

    Colorless to transparent, occasionally with a slight brownish tint due to hydrocarbon inclusions. Black hydrocarbon inclusions are common.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Vitreous (glassy) to sub-adamantine, often exceptionally brilliant.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Smooth, naturally faceted crystal faces.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Distinctive double-terminated hexagonal prisms. This means the crystal has natural facets at both ends, unlike most quartz crystals which are typically terminated at one end and attached to a matrix at the other. The faces are typically well-formed and sharp.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    None. Quartz exhibits conchoidal fracture.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Found in vugs and cavities within dolostone formations, specifically the Little Falls Dolostone in New York. They are often extracted from weathered dolostone or directly from the rock matrix.

Key Facts

Hardness
7 on the Mohs scale
Specific Gravity
2.65 g/cm³
Crystal System
Trigonal
Color
Colorless, transparent; may contain black or brownish hydrocarbon inclusions.
Luster
Vitreous (glassy) to sub-adamantine.
Transparency
Transparent to translucent.
Fracture
Conchoidal (shell-like, curved breaks).
Cleavage
None.
Composition
Silicon dioxide (SiO2) with hydrocarbon inclusions.

Physical characteristics

  • Crystal Habit: Double-terminated hexagonal prisms, often with well-developed faces and sharp edges. Can occur as single crystals or in clusters.
  • Cleavage Type: Absent.
  • Fracture Type: Conchoidal.
  • Tenacity: Brittle.
  • Luster Type: Vitreous to sub-adamantine.

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