How to identify Included Quartz
SiO2 with mineral inclusions
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Open the appTo 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
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
Luster
How the surface reflects light: metallic, vitreous, dull
Vitreous (glassy) on crystal faces and fresh fractures.
- 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
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
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
None, but exhibits conchoidal fracture.
- 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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