Rockby LogoRockby

How to identify Graphitic Quartz

SiO2 (Quartz) with C (Graphite)

Got a photo? Identify rocks instantly with the Rockby app

Open the app

To 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. 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. 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. 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. 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. 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. 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)

Explore Graphitic Quartz

Identify rocks anywhere

Free on iOS, Android, and Web. Photo identification, full database, and your personal collection.

Open in app