
mineral
Quartz Pebble
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Creamy white to pale yellow, translucent; Luster: Waxy to vitreous; Crystal Structure: Trigonal (microcrystalline in this beach-worn form); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Creamy white to pale yellow, translucent
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 7 on Mohs scale; Color: Creamy white to pale yellow, translucent; Luster: Waxy to vitreous; Crystal Structure: Trigonal (microcrystalline in this beach-worn form); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed through hydrothermal processes or as a primary mineral in igneous rocks. This specific specimen is a water-worn river or beach pebble, smoothed over centuries by hydraulic action and abrasion.
Uses & applications
Primarily used for decorative landscaping, gravel, or as a pocket stone. High-purity quartz is used in glassmaking, electronics, and abrasives.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. These rounded shapes are 'nature's tumblers,' where waves or river currents smooth jagged edges into ovoid shapes.
Field identification & locations
Identify by its hardness (it will scratch glass and metal) and lack of visible grains. Found globally on beaches and in riverbeds. Collectors look for high clarity or unique internal inclusions.
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Metamorphic
Epidote
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metamorphic
Gypsum (variety Selenite or Alabaster)
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Mineral
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Mineral/Rock
Granite
Granite (Phaneritic intrusive igneous rock)
igneous