How to identify Fluorite
Fluorite
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Open the appTo correctly identify Fluorite (Fluorite), 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
Extremely variable: purple, blue, green, yellow, colorless, pink, red, brown, black. Often color-zoned or banded.
- 2
Luster
How the surface reflects light: metallic, vitreous, dull
Vitreous (glassy).
- 3
Texture
Grain size and surface feel: coarse, fine, glassy
Smooth to slightly rough on crystal faces; conchoidal fracture surfaces are smooth.
- 4
Crystal Form
Shape of visible crystals or crystal faces
Typically cubic, octahedral, or dodecahedral crystals. Also massive, granular, or botryoidal habits.
- 5
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
Perfect octahedral cleavage in four directions, producing characteristic triangular or diamond-shaped fragments.
- 6
Geological Environment
The rock formation and setting where it occurs
Hydrothermal veins, often associated with metallic ore deposits (e.g., lead, zinc, silver). Also found in pegmatites, carbonatites, and as an accessory mineral in some igneous and metamorphic rocks. Can occur in sedimentary rocks as a diagenetic or evaporite mineral.
Key Facts
- Hardness
- 4 (Mohs scale)
- Specific Gravity
- 3.17-3.18 g/cm
- Crystal System
- Isometric (Cubic)
- Color
- Variable: purple, blue, green, yellow, colorless, pink, red, brown, black; often color-zoned.
- Luster
- Vitreous
- Transparency
- Transparent to translucent
- Fracture
- Conchoidal to uneven
- Cleavage
- Perfect octahedral in four directions {111}
- Composition
- Calcium Fluoride (CaF₂)
Physical characteristics
- Crystal Habit: Cubic, octahedral, dodecahedral; also massive, granular, botryoidal.
- Cleavage Type: Perfect octahedral {111}
- Fracture Type: Conchoidal to uneven
- Tenacity: Brittle
- Luster Type: Vitreous
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