
Mineral
White Quartz Pebbles
Quartz (Silicon Dioxide, SiO2)
Hardness: 7.0 on Mohs scale; Color: Milky white to translucent; Luster: Vitreous to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7
- Color
- Milky white to translucent
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7.0 on Mohs scale; Color: Milky white to translucent; Luster: Vitreous to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed through hydrothermal processes or during the final stages of cooling in igneous intrusions (pegmatites). These specimens appear to be water-worn or mechanically tumbled pebbles from river deposits or sedimentary conglomerate break-ups.
Uses & applications
Used widely in landscaping, filtration systems, glass manufacturing, electronics (piezoelectric properties), and as decorative gravel. Lower grade pieces are used in construction aggregate.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. These specific 'milky' varieties get their color from tiny inclusions of gas or liquid trapped during crystal growth.
Field identification & locations
Identify in the field by its ability to scratch glass and lack of cleavage. It is extremely common in riverbeds, beaches, and mountain trails. Collectors look for high clarity or unique inclusions.
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Mineral/Rock
Banded Gneiss (River Rock/Pebble)
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mineral