
mineral
Milky Quartz Pebble
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale); Color: Opaque white to creamy; Luster: Vitreous to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Color
- Opaque white to creamy
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 (Mohs scale); Color: Opaque white to creamy; Luster: Vitreous to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Forms from cooling silica-rich hydrothermal fluids in veins or crystallizing from magma. This specimen is a water-worn pebble likely from a river or beach environment.
Uses & applications
Industrial source of silicon, decorative landscaping, source of glass and high-quality silica, and often used in crystal healing or as a mineral collection starter.
Geological facts
Milky quartz gets its white color from millions of tiny fluid and gas bubbles trapped during crystal growth. It is the most common variety of crystalline quartz found on Earth.
Field identification & locations
Identify by its ability to scratch glass and its lack of cleavage. Often found near granite outcrops or in alluvial deposits like riverbeds and shorelines.
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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
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
Septarian Pebble
Septarian nodule / Concretion
sedimentary