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

Milky Quartz Pebble

Silicon Dioxide (SiO2)

Hardness: 7 Mohs; Color: White to creamy tan; Luster: Vitreous to waxy (especially when water-worn); Crystal structure: Trigonal/Hexagonal; Cleavage: None/Conchoidal fracture; Specific gravity: 2.65

Hardness
7 Mohs
Color
White to creamy tan
Luster
Vitreous to waxy (especially when water-worn)
Identified More mineral
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Physical properties

Hardness: 7 Mohs; Color: White to creamy tan; Luster: Vitreous to waxy (especially when water-worn); Crystal structure: Trigonal/Hexagonal; Cleavage: None/Conchoidal fracture; Specific gravity: 2.65

Formation & geological history

Formed from molten magma or hydrothermal veins, later eroded and smoothed by water transport in riverbeds or coastal environments. Quartz is found in rocks of all geological ages.

Uses & applications

Used as decorative gravel, in landscaping, and as a source of silica for glass and electronics. High-quality quartz is used in jewelry and timekeeping.

Geological facts

Milky quartz gets its white color from tiny fluid inclusions of gas or liquid trapped during crystal growth. It is the most common variety of crystalline quartz.

Field identification & locations

Identify by its hardness (it will scratch glass) and lack of cleavage. Commonly found in stream beds, beaches, and glacial till globally.