
mineral
Quartz (Water-worn Pebble)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Translucent grey to white; Luster: Vitreous to waxy (when worn); Crystal Structure: Hexagonal; Cleavage: None (conchoidal fracture).
- Hardness
- 7 on Mohs scale
- Color
- Translucent grey to white
- Luster
- Vitreous to waxy (when worn)
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Physical properties
Hardness: 7 on Mohs scale; Color: Translucent grey to white; Luster: Vitreous to waxy (when worn); Crystal Structure: Hexagonal; Cleavage: None (conchoidal fracture).
Formation & geological history
Formed from silica-rich hydrothermal fluids or within igneous and metamorphic rocks. This specific specimen has been rounded and smoothed by water erosion in a river or beach environment.
Uses & applications
Quartz is used in glassmaking, electronics (piezoelectric properties), abrasives, and as a gemstone or decorative stone.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Its name comes from the German word 'quarz', which had its origin in Slavic languages.
Field identification & locations
Identify by its hardness (can scratch glass) and lack of cleavage. Common in riverbeds, beaches, and gravel pits worldwide. Collectors look for clarity and internal inclusions.
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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