
mineral
Quartz (Gray/Smoky Variety)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale), Color: Translucent gray to smoky brown, Luster: Vitreous (glassy), Crystal Structure: Trigonal/Hexagonal, Cleavage: None (conchoidal fracture), Specific Gravity: 2.65
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Physical properties
Hardness: 7 (Mohs scale), Color: Translucent gray to smoky brown, Luster: Vitreous (glassy), Crystal Structure: Trigonal/Hexagonal, Cleavage: None (conchoidal fracture), Specific Gravity: 2.65
Formation & geological history
Forms in igneous rocks like granite, metamorphic rocks, and hydrothermal veins through the crystallization of silica-rich fluids. The gray color can be caused by natural irradiation of aluminum impurities.
Uses & applications
Used in electronics for its piezoelectric properties, glass manufacturing, abrasives, and as semi-precious gemstones in jewelry or for metaphysical collecting.
Geological facts
Quartz is one of the most abundant minerals on Earth's crust. It is highly resistant to both chemical and physical weathering, which is why it is the primary component of most river and beach sands.
Field identification & locations
Identify by its hardness (will scratch glass), lack of cleavage, and glassy appearance. Commonly found in stream beds, gravel pits, and mountainous regions worldwide.
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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