
mineral
Milky Quartz Pebble
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Milky white to translucent; Luster: Vitreous to greasy; Crystal structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Milky white to translucent
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on Mohs scale; Color: Milky white to translucent; Luster: Vitreous to greasy; Crystal structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65.
Formation & geological history
Forms in hydrothermal veins or as a primary constituent in igneous rocks like granite. This specific specimen has been rounded and smoothed by water erosion through transport in a river or beach environment.
Uses & applications
Used in glass making, abrasive manufacturing, electronics (due to piezoelectric properties), and as decorative landscaping stone or tumbled pocket stones.
Geological facts
The milky appearance is caused by millions of tiny fluid inclusions of gas and/or liquid trapped during the crystal's growth. It is one of the most abundant minerals on Earth's crust.
Field identification & locations
Identify by its hardness (it will scratch glass), its white 'milky' color, and lack of cleavage. Often found in riverbeds, glacial deposits, and beaches globally.
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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