Rock Identifier
Milky Quartz Pebble (Silicon Dioxide (SiO2)) — mineral
mineral

Milky Quartz Pebble

Silicon Dioxide (SiO2)

Hardness: 7 (Mohs), Color: Milky white to translucent, Luster: Vitreous to greasy, Crystal Structure: Trigonal/Hexagonal, Cleavage: None/Conchoidal fracture, Specific Gravity: 2.65

Identified More mineral
Explore Milky Quartz Pebble in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Hardness: 7 (Mohs), Color: Milky white to translucent, Luster: Vitreous to greasy, Crystal Structure: Trigonal/Hexagonal, Cleavage: None/Conchoidal fracture, Specific Gravity: 2.65

Formation & geological history

Formed from silica-rich hydrothermal fluids or within magma cooling at depth. This specific piece is a river-worn or water-eroded pebble, likely thousands to millions of years old, weathered out of a quartz vein.

Uses & applications

Source of silicon for electronics, used as an abrasive, in decorative grit/landscaping, and for lapidary tumbling.

Geological facts

Milky quartz gets its white color from tiny bubbles of gas or liquid trapped during the crystal's formation. It is the most common variety of crystalline quartz on Earth.

Field identification & locations

Identify in the field by its hardness (will scratch glass), white color, and lack of cleavage. Commonly found in riverbeds, glacial till, and mountainous regions worldwide.