Rockby LogoRockby

How to identify Flint

Chert (variety of microcrystalline quartz)

Got a photo? Identify rocks instantly with the Rockby app

Open the app

To correctly identify Flint (Chert (variety of microcrystalline quartz)), 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, black, brown, or reddish-brown. Can also be tan or off-white.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Waxy to dull, sometimes vitreous on fresh fracture surfaces.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Smooth to slightly granular, very fine-grained. Feels dense and hard.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Cryptocrystalline; individual crystals are microscopic and not visible to the naked eye. Forms nodules, concretions, or beds.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    None. Exhibits a characteristic conchoidal fracture.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Most commonly found as nodules or layers within marine carbonate sedimentary rocks, particularly chalk and limestone. Also occurs in river gravels and glacial till where it has been eroded from its primary source.

Key Facts

Hardness
7 on the Mohs scale
Specific Gravity
2.58 - 2.64 g/cm³
Crystal System
Trigonal (due to its quartz composition, though cryptocrystalline)
Color
Dark gray, black, brown, tan, reddish-brown
Luster
Waxy, dull, sometimes vitreous on fresh fracture
Transparency
Opaque to translucent on thin edges
Fracture
Conchoidal (shell-like), producing very sharp edges
Cleavage
None
Composition
Silicon dioxide (SiO2), with minor impurities

Physical characteristics

  • Crystal Habit: Cryptocrystalline aggregates, forming nodules, concretions, or massive beds. Individual crystals are microscopic.
  • Cleavage Type: Absent
  • Fracture Type: Conchoidal, producing extremely sharp, curved surfaces.
  • Tenacity: Brittle, but very tough due to its interlocking microcrystalline structure.
  • Luster Type: Waxy to dull, occasionally sub-vitreous.

Explore Flint

Identify rocks anywhere

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

Open in app