
mineral
Quartz (Smoky/Rock Crystal)
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: transparent to translucent with tan/brownish iron staining; Luster: Vitreous (glassy); Crystal Structure: Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- transparent to translucent with tan/brownish iron staining
- Luster
- Vitreous (glassy)
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Physical properties
Hardness: 7 on Mohs scale; Color: transparent to translucent with tan/brownish iron staining; Luster: Vitreous (glassy); Crystal Structure: Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
Formation & geological history
Forms in igneous, metamorphic, and sedimentary environments. Typically crystallizes from hydrothermal veins or cooling magmatic bodies. Found globally in a variety of geological ages.
Uses & applications
Used widely in manufacturing glass, electronics (piezoelectric properties), construction aggregates, as well as jewelry and decorative mineral collections.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Its name comes from the German word 'Quarz', which has Slavic origins meaning 'hard'.
Field identification & locations
Identify in the field by its ability to scratch glass, its lack of cleavage, and its vitreous luster. Commonly found in riverbeds, mountains, and as vein-filling material in host rocks.
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Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Sandstone with Mineral Veining or Crust
Sedimentary Sandstone (mostly SiO2 with Fe2O3 tinting)
sedimentary
Schist
Schist
Metamorphic
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Gypsum (variety Selenite or Alabaster)
Calcium sulfate dihydrate (CaSO4·2H2O)
Mineral
Nephrite Jade
Nephrite
Mineral/Rock