
mineral
Quartz (Smoky/Clear variety)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Translucent grey to clear; Luster: Vitreous (glassy); Crystal Structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Translucent grey to clear
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: Translucent grey to clear; Luster: Vitreous (glassy); Crystal Structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
Formation & geological history
Formed via hydrothermal activity or cooling of silica-rich magma (igneous/pegmatitic). The coordinates (South of France/Provence) contain the Esterel Massif and Maures Massif, which are rich in metamorphic and igneous rocks where quartz is abundant.
Uses & applications
Used in electronics (piezoelectric properties), glassmaking, abrasives, and as a semi-precious gemstone in jewelry or for metaphysical collecting.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Smoky quartz gets its color from natural irradiation of aluminum impurities within the crystal lattice.
Field identification & locations
Identify in the field by its hardness (will scratch glass and steel) and lack of cleavage (breaks like glass in curved shells). It is widely found in the crystalline massifs of the Var region in France.
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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous
Septarian Pebble
Septarian nodule / Concretion
sedimentary