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How to identify Included Quartz

SiO2 with mineral inclusions

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To correctly identify Included Quartz (SiO2 with mineral 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

    Variable, depending on the host quartz and the inclusions. Host quartz can be colorless, white, smoky, purple (amethyst), yellow (citrine), or pink (rose quartz). Inclusions add their own colors: golden (rutile), black (tourmaline, hematite), green (chlorite, actinolite), red/orange (hematite, goethite).

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Vitreous (glassy) on crystal faces and fresh fractures.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Crystalline, often with visible internal structures due to inclusions. Can be massive or euhedral to anhedral crystals.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Typically hexagonal prisms terminated by rhombohedra. Inclusions are internal and do not alter the external crystal habit of the quartz, though they may outline growth zones (phantoms).

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    None, but exhibits conchoidal fracture.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Hydrothermal veins, pegmatites, igneous rocks (granites, rhyolites), metamorphic rocks (gneisses, schists), and sedimentary environments (as detrital grains). The specific type of inclusion often points to a particular formation environment (e.g., rutile in high-temperature hydrothermal veins, chlorite in lower-temperature metamorphic or hydrothermal settings).

Key Facts

Hardness
7 on the Mohs scale.
Specific Gravity
2.65 g/cm³ (for pure quartz; inclusions may slightly alter this).
Crystal System
Trigonal.
Color
Highly variable, depending on the host quartz and the type/color of inclusions.
Luster
Vitreous.
Transparency
Transparent to translucent, depending on the density and type of inclusions.
Fracture
Conchoidal.
Cleavage
None.
Composition
Silicon dioxide (SiO2) with various trapped mineral phases or fluids.

Physical characteristics

  • Crystal Habit: Prismatic, often with hexagonal cross-section, terminated by rhombohedral faces. Inclusions are internal.
  • Cleavage Type: Absent.
  • Fracture Type: Conchoidal.
  • Tenacity: Brittle.
  • Luster Type: Vitreous.

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