
mineral
Milky Quartz Pebble
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale; Color: Opaque white to yellowish-cream; Luster: Vitreous to greasy; Crystal Structure: Trigonal (hexagonal system); Cleavage: None; Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Opaque white to yellowish-cream
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on Mohs scale; Color: Opaque white to yellowish-cream; Luster: Vitreous to greasy; Crystal Structure: Trigonal (hexagonal system); Cleavage: None; Specific Gravity: 2.65.
Formation & geological history
Formed through the cooling of silica-rich magma or from hydrothermal veins. The milky appearance is caused by tiny inclusions of liquid or gas trapped during the crystal's growth. This specimen has been rounded by fluvial or glacial transport.
Uses & applications
Used in glassmaking, abrasives, gemstone carving, and as decorative landscaping stone. High-purity quartz is also essential in electronics.
Geological facts
Milky quartz is the most common variety of crystalline quartz. Historically, it was used by many cultures for tools and weapons before the widespread use of metal.
Field identification & locations
Identify in the field by its hardness (it can scratch glass), lack of cleavage, and translucent to opaque white appearance. It is commonly found in stream beds, gravel pits, and beach deposits.
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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
Banded Gneiss (River Rock/Pebble)
Gneiss (specifically a banded variety often found as a river rock)
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