
mineral
Milky Quartz (Water-Worn Pebble)
Quartz (Silicon Dioxide, SiO2)
Hardness: 7 on Mohs scale. Color: Milky white to translucent. Luster: Vitreous to waxy. Crystal Structure: Hexagonal/Trigonal (though often cryptocrystalline in common pebbles). Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Milky white to translucent
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 7 on Mohs scale. Color: Milky white to translucent. Luster: Vitreous to waxy. Crystal Structure: Hexagonal/Trigonal (though often cryptocrystalline in common pebbles). Cleavage: None (conchoidal fracture). 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 microscopic inclusions of fluids or gases trapped during crystal growth. This specific specimen has been significantly weathered and rounded by water action in a river or beach environment.
Uses & applications
Industrial uses include glass making, abrasives, and electronics (due to piezoelectric properties). In jewelry, it is often used for beads or cabochons. Large specimens are popular for home decor and garden landscaping.
Geological facts
Quartz is the second most abundant mineral in Earth's continental crust. Historically, the 'milky' look was sometimes believed to represent frozen ice that would never melt. It is highly resistant to chemical and physical weathering, which is why quartz pebbles are so common in riverbeds.
Field identification & locations
Identify by its hardness (it will easily scratch glass) and lack of cleavage planes. To identify in the field, look for the 'greasy' luster on freshly broken surfaces. Common worldwide in gravel pits, beaches, and stream beds.
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