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How to identify Fluorite in Quartz

CaF2 in SiO2

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To correctly identify Fluorite in Quartz (CaF2 in SiO2), 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

    Quartz is typically colorless, white, or milky, but can be various colors (e.g., purple amethyst, yellow citrine, smoky gray). Fluorite exhibits a wide range of colors including purple, green, blue, yellow, pink, and colorless. The combination will show these colors together.

  2. 2

    Luster

    How the surface reflects light: metallic, vitreous, dull

    Quartz has a vitreous (glassy) luster. Fluorite also has a vitreous luster.

  3. 3

    Texture

    Grain size and surface feel: coarse, fine, glassy

    Crystalline, often with distinct crystal faces for both minerals. Can be massive or granular.

  4. 4

    Crystal Form

    Shape of visible crystals or crystal faces

    Quartz typically forms hexagonal prisms with pyramidal terminations. Fluorite commonly forms cubic, octahedral, or dodecahedral crystals. The combination will show these forms either intergrown or as inclusions.

  5. 5

    Cleavage

    How it breaks: flat cleavage planes vs irregular fracture

    Quartz has no cleavage (conchoidal fracture). Fluorite exhibits perfect octahedral cleavage in four directions, which can be observed as flat, shiny surfaces when broken.

  6. 6

    Geological Environment

    The rock formation and setting where it occurs

    Hydrothermal veins, pegmatites, greisens, and as gangue minerals in various metallic ore deposits (e.g., lead-zinc, tin, silver). Often found in granitic and metamorphic terrains.

Key Facts

Hardness
Quartz: 7 on Mohs scale; Fluorite: 4 on Mohs scale. This difference is crucial for identification.
Specific Gravity
Quartz: 2.65 g/cm³; Fluorite: 3.18 g/cm³ (can vary slightly with impurities).
Crystal System
Quartz: Trigonal; Fluorite: Isometric (Cubic).
Color
Variable, as described above, depending on the specific colors of the fluorite and quartz present.
Luster
Vitreous (glassy).
Transparency
Transparent to translucent for both minerals.
Fracture
Quartz: Conchoidal; Fluorite: Subconchoidal to uneven.
Cleavage
Quartz: None; Fluorite: Perfect octahedral (4 directions).
Composition
Quartz: Silicon dioxide (SiO2); Fluorite: Calcium fluoride (CaF2).

Physical characteristics

  • Crystal Habit: Quartz: Prismatic, massive, granular; Fluorite: Cubic, octahedral, massive, granular. Often intergrown or as inclusions.
  • Cleavage Type: Quartz: None; Fluorite: Perfect octahedral {111}.
  • Fracture Type: Quartz: Conchoidal; Fluorite: Subconchoidal to uneven.
  • Tenacity: Quartz: Brittle; Fluorite: Brittle.
  • Luster Type: Vitreous.

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