
mineral
Quartz Pebble
Silicon Dioxide (SiO2)
Hardness: 7 (Mohs scale); Color: White, translucent to milky; Luster: Vitreous/waxy; Crystal structure: Hexagonal/Trigonal; Cleavage: None/Conchoidal fracture; Specific gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Color
- White, translucent to milky
- Luster
- Vitreous/waxy
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Physical properties
Hardness: 7 (Mohs scale); Color: White, translucent to milky; Luster: Vitreous/waxy; Crystal structure: Hexagonal/Trigonal; Cleavage: None/Conchoidal fracture; Specific gravity: 2.65
Formation & geological history
Formed from silica-rich hydrothermal fluids or within igneous and metamorphic rocks. These specific specimens are water-worn river pebbles shaped by erosion over thousands of years.
Uses & applications
Used in glass manufacturing, electronics, jewelry (as semi-precious stones), and as decorative landscaping gravel.
Geological facts
Quartz is one of the most abundant minerals on Earth's crust. It is piezoelectric, meaning it can generate an electric charge when mechanical pressure is applied.
Field identification & locations
Identify by its hardness (scratches glass), translucent appearance, and lack of cleavage. Common in riverbeds, beaches, and glaciated plains worldwide.
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Other mineral specimens
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
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
Granite
Granite (Phaneritic intrusive igneous rock)
igneous