
mineral
Milky Quartz Pebbles
Silicon Dioxide (SiO2)
Hardness: 7 (Mohs scale); Color: Translucent white to pale yellow; Luster: Vitreous to waxy (especially when water-worn); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture).
- Hardness
- 7 (Mohs scale)
- Color
- Translucent white to pale yellow
- Luster
- Vitreous to waxy (especially when water-worn)
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Physical properties
Hardness: 7 (Mohs scale); Color: Translucent white to pale yellow; Luster: Vitreous to waxy (especially when water-worn); Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture).
Formation & geological history
Forms in igneous, metamorphic, and sedimentary environments. These specific specimens are alluvial or river-worn pebbles, shaped by hydraulic erosion over hundreds to thousands of years.
Uses & applications
Used in construction as decorative aggregate, in landscaping, and as a source of silica for glass manufacturing and electronics. Common in beginner rock tumbling and lapidary workshops.
Geological facts
Milky quartz gets its cloudy appearance from microscopic inclusions of fluids or gas trapped during the crystal's growth. It is the most common variety of crystalline quartz.
Field identification & locations
Identify in the field by its hardness (scratches glass), waxy luster when wet, and lack of cleavage. Found globally in riverbeds, beaches, and glacial deposits.
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sedimentary
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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)
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