How to identify Graphitic Quartz
SiO2 (Quartz) with C (Graphite)
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Open the appTo correctly identify Graphitic Quartz (SiO2 (Quartz) with C (Graphite)), 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, often with a metallic luster from the graphite. The quartz itself may be clear, white, or gray, but the graphite imparts the dominant dark coloration.
- 2
Luster
How the surface reflects light: metallic, vitreous, dull
Vitreous (glassy) for quartz, submetallic to metallic for graphite. The overall luster can be a combination, often appearing dull to submetallic due to the disseminated graphite.
- 3
Texture
Grain size and surface feel: coarse, fine, glassy
Can be massive, granular, or schistose/gneissic if part of a metamorphic rock. 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 hexagonal prisms with pyramidal terminations, though in massive forms it is anhedral. Graphite forms hexagonal plates or flakes, often anhedral when 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). The aggregate will show the fracture of quartz and the cleavage of graphite.
- 6
Geological Environment
The rock formation and setting where it occurs
Commonly found in medium to high-grade metamorphic rocks (schists, gneisses, marbles) derived from carbonaceous sediments. Also occurs in some hydrothermal veins and occasionally in igneous rocks.
Key Facts
- Hardness
- Quartz: 7 (Mohs); Graphite: 1-2 (Mohs). The overall hardness will be dominated by quartz, but graphite inclusions will be soft.
- Specific Gravity
- Quartz: 2.65 g/cm³; Graphite: 2.09-2.23 g/cm³. The aggregate's specific gravity will be between these values, depending on the proportion of each mineral.
- Crystal System
- Quartz: Trigonal; Graphite: Hexagonal
- Color
- Dark gray to black, often with a metallic sheen
- Luster
- Vitreous (quartz) to submetallic/metallic (graphite)
- Transparency
- Opaque (due to graphite) to translucent (quartz)
- Fracture
- Conchoidal (quartz), but the presence of graphite can make it more irregular.
- Cleavage
- None for quartz; Perfect basal cleavage for graphite (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 to flaky
- Tenacity: Quartz: Brittle; Graphite: Sectile
- Luster Type: Vitreous (quartz), Submetallic to metallic (graphite)
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