
mineral
Milky Quartz Pebble
Silicon Dioxide (SiO2)
Hardness: 7 on Mohs scale. Color: Off-white to light yellowish-tan, opaque to translucent. Luster: Vitreous to greasy. Fracture: Conchoidal. Crystal Structure: Hexagonal (trigonal).
- Hardness
- 7 on Mohs scale
- Color
- Off-white to light yellowish-tan, opaque to translucent
- Luster
- Vitreous to greasy
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Physical properties
Hardness: 7 on Mohs scale. Color: Off-white to light yellowish-tan, opaque to translucent. Luster: Vitreous to greasy. Fracture: Conchoidal. Crystal Structure: Hexagonal (trigonal).
Formation & geological history
Formed in hydrothermal veins and pegmatites through the slow crystallization of silica-rich solutions. This pebble has been rounded and smoothed through erosion in riverbeds or coastal environments.
Uses & applications
Used widely in landscape decoration, glass manufacturing, electronics, and as abrasive material. Small river pebbles are commonly collected by rockhounding enthusiasts.
Geological facts
Milky quartz gets its cloudy white appearance from tiny gas or liquid bubbles trapped within the crystal structure during its formation millions of years ago.
Field identification & locations
Identified by its hardness (scratches glass easily), lack of cleavage, and light color. Found abundantly in gravel beds, streams, and beaches worldwide.
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