
mineral
Milky Quartz Pebble
Quartz (Silicon Dioxide, SiO2)
AI-generated identification · may be incorrectHardness: 7 on Mohs scale. Color: Opaque white to translucent gray with hints of yellow iron staining. Luster: Vitreous to greasy when polished. Crystal Structure: Hexagonal (trigonal). Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Luster
- Vitreous to greasy when polished
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Physical properties
Hardness: 7 on Mohs scale. Color: Opaque white to translucent gray with hints of yellow iron staining. Luster: Vitreous to greasy when polished. 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 water-worn and smoothed by alluvial or glacial transport, then likely mechanically polished.
Uses & applications
Used widely as abrasive material, in glassmaking, construction gravel, landscaping, and commonly sold as 'worry stones' or decorative vase filler.
Geological facts
Milky quartz gets its cloudy appearance from tiny microscopic inclusions of gas or liquid trapped during the crystal's growth. It is the most common variety of crystalline quartz on Earth.
Field identification & locations
Identify in the field by its hardness (it can scratch glass), lack of cleavage, and white sub-vitreous appearance. Found in almost any riverbed or beach globally where granite or quartz veins are eroded.
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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
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Granite
Granite (Phaneritic intrusive igneous rock)
igneous
Septarian Pebble
Septarian nodule / Concretion
sedimentary