
mineral
Milky Quartz Pebble
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale); Color: Tanslucent to milky white; Luster: Vitreous to waxy (smooth surfaces); Crystal Structure: Hexagonal (Trigonal); Cleavage: None (Conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Color
- Tanslucent to milky white
- Luster
- Vitreous to waxy (smooth surfaces)
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Physical properties
Hardness: 7 (Mohs scale); Color: Tanslucent to milky white; Luster: Vitreous to waxy (smooth surfaces); Crystal Structure: Hexagonal (Trigonal); Cleavage: None (Conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed through the cooling of silica-rich hydrothermal fluids or magma. This specific specimen shows significant rounding and smoothing caused by water erosion in a river, stream, or coastal environment over thousands of years.
Uses & applications
Quartz is used in glassmaking, electronics (piezoelectric properties), abrasives, and as a semi-precious gemstone in jewelry when high quality. Common pebbles are used in landscaping and aggregate.
Geological facts
Milky quartz gets its cloudy appearance from tiny microscopic fluid inclusions of gas or liquid trapped during the crystal's growth. It is the most common variety of crystalline quartz found on Earth.
Field identification & locations
Identify by its hardness (will scratch glass), lack of cleavage, and translucent nature. Look for it in river beds, beaches, and eroded gravel deposits worldwide.
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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous