
mineral
Milky Quartz Pebble
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale; Color: Opaque white to translucent; Luster: Vitreous to waxy (when water-worn); Crystal Structure: Hexagonal (Trigonal); Cleavage: None (Conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 on Mohs scale
- Color
- Opaque white to translucent
- Luster
- Vitreous to waxy (when water-worn)
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Physical properties
Hardness: 7 on Mohs scale; Color: Opaque white to translucent; Luster: Vitreous to waxy (when water-worn); Crystal Structure: Hexagonal (Trigonal); Cleavage: None (Conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed from silica-rich hydrothermal solutions or as a primary constituent in igneous rocks like granite. This specific specimen has been rounded and smoothed by water erosion (fluvial or beach action).
Uses & applications
Commonly used as decorative landscaping stones, aquarium gravel, in the manufacture of glass and ceramics, and as a minor gemstone for tumbling or lapidary work.
Geological facts
The 'milky' appearance is caused by tiny fluid inclusions of gas or liquid trapped during crystal growth. It is one of the most abundant minerals on Earth's crust.
Field identification & locations
Identify in the field by its hardness (will scratch glass), lack of cleavage, and translucent white appearance. It is found globally in riverbeds, beaches, and mountain outcrops.
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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