How to identify Graphitic Quartz
SiO2 with C
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Open the appTo correctly identify Graphitic Quartz (SiO2 with C), 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
Typically dark gray to black due to graphite, often with translucent to opaque white or gray quartz. The graphite can appear as silvery-black flakes.
- 2
Luster
How the surface reflects light: metallic, vitreous, dull
Vitreous (glassy) for quartz, contrasting with metallic to sub-metallic or dull/earthy for graphite.
- 3
Texture
Grain size and surface feel: coarse, fine, glassy
Can be massive, granular, or foliated (schistose) if the graphite is aligned. Graphite often occurs as fine flakes or lamellae within the quartz matrix.
- 4
Crystal Form
Shape of visible crystals or crystal faces
Quartz typically forms anhedral to subhedral grains, sometimes euhedral crystals in vugs. Graphite forms hexagonal plates or flakes, often anhedral and disseminated.
- 5
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
Quartz has no true cleavage but exhibits conchoidal fracture. Graphite has perfect basal cleavage (one direction), which can be observed as flaky partings.
- 6
Geological Environment
The rock formation and setting where it occurs
Commonly found in regionally metamorphosed terrains, particularly in areas derived from carbonaceous shales, limestones, or sandstones. Also occurs in contact metamorphic aureoles and hydrothermal veins associated with carbon-rich host rocks.
Key Facts
- Hardness
- Quartz: 7 (Mohs); Graphite: 1-2 (Mohs). The overall hardness of the rock will depend on the proportion and texture of each mineral.
- Specific Gravity
- Quartz: 2.65 g/cm³; Graphite: 2.09-2.23 g/cm³. The aggregate specific gravity will be intermediate.
- Crystal System
- Quartz: Trigonal; Graphite: Hexagonal
- Color
- Dark gray to black, often with white or translucent gray areas
- Luster
- Vitreous to greasy for quartz, metallic to dull for graphite
- Transparency
- Quartz: Transparent to translucent; Graphite: Opaque
- Fracture
- Quartz: Conchoidal; Graphite: Uneven to flaky
- Cleavage
- Quartz: None; Graphite: Perfect basal (one direction)
- Composition
- Silicon dioxide (SiO2) and elemental carbon (C)
Physical characteristics
- Crystal Habit: Quartz: Prismatic, massive, granular; Graphite: Flaky, platy, massive, disseminated
- Cleavage Type: Quartz: None; Graphite: Perfect basal (0001)
- Fracture Type: Quartz: Conchoidal; Graphite: Uneven, flaky
- Tenacity: Quartz: Brittle; Graphite: Sectile, flexible (thin flakes)
- Luster Type: Quartz: Vitreous; Graphite: Metallic to sub-metallic, dull, earthy
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