
mineral
Quartz (possibly Citrine or Smoky Quartz variety)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: yellowish-transparent; Luster: Vitreous/glassy; Crystal structure: Trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- yellowish-transparent
- Luster
- Vitreous/glassy
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Physical properties
Hardness: 7 on Mohs scale; Color: yellowish-transparent; Luster: Vitreous/glassy; Crystal structure: Trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
Formation & geological history
Formed through the cooling of silica-rich magma or from hydrothermal veins. This specimen can be found in igneous rocks like granite or metamorphic rocks like quartzite.
Uses & applications
Used extensively in the electronics industry (piezoelectric properties), glassmaking, jewelry (gemstone quality), and as architectural stone.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. It is highly resistant to both chemical and physical weathering.
Field identification & locations
Identify by its 7 hardness (it can scratch glass and steel), lack of cleavage, and glassy appearance. Commonly found in riverbeds, mountains, and desert sands.
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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