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

Milky Quartz Pebble

Silicon Dioxide (SiO2)

Hardness: 7 on Mohs scale; Color: Opaque white to cream; Luster: Vitreous to waxy; Crystal structure: Hexagonal (trigonal); Specific gravity: 2.65

Hardness
7 on Mohs scale
Color
Opaque white to cream
Luster
Vitreous to waxy
Identified More mineral
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Physical properties

Hardness: 7 on Mohs scale; Color: Opaque white to cream; Luster: Vitreous to waxy; Crystal structure: Hexagonal (trigonal); Specific gravity: 2.65

Formation & geological history

Formed through the cooling of silica-rich hydrothermal fluids or magma. This specimen is a water-worn river pebble, shaped by erosion over thousands of years.

Uses & applications

Quartz is used in glassmaking, abrasives, and electronics. Small pebbles like this are often used in landscaping or as decorative aggregate.

Geological facts

The milky white color is caused by tiny inclusions of gas or liquid trapped during the crystal's growth. It is the most common variety of crystalline quartz found on Earth's surface.

Field identification & locations

Identify by its hardness (it will scratch glass) and lack of cleavage. Commonly found in riverbeds, beaches, and glacial deposits worldwide.