
mineral
Quartz Pebble
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale); Color: White, translucent, or light tan; Luster: Vitreous to waxy (especially when water-worn); Crystal Structure: Hexagonal; Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Color
- White, translucent, or light tan
- Luster
- Vitreous to waxy (especially when water-worn)
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Physical properties
Hardness: 7 (Mohs scale); Color: White, translucent, or light tan; Luster: Vitreous to waxy (especially when water-worn); Crystal Structure: Hexagonal; Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65
Formation & geological history
Formed through the cooling of silica-rich magma or from hydrothermal veins. This specific specimen appears to be water-worn, likely tumbled in a river or stream bed over thousands of years.
Uses & applications
Quartz is used extensively in glassmaking, electronics (piezoelectric properties), abrasives, and as construction aggregate.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Pure quartz is known as rock crystal, but impurities create various colors like amethyst, rose quartz, and citrine.
Field identification & locations
Identify in the field by its hardness (it will scratch glass) and lack of cleavage. Common in riverbeds, glacial deposits, and mountain terrain 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
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
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