Quartz (Milky Quartz Pebbles)

Physical Properties

Hardness: 7 (Mohs scale); Color: White to translucent; Luster: Vitreous to waxy; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65

Formation & Geological History

Formed from the crystallization of silica-rich magma or precipitation from hydrothermal veins. This specific specimen appears to be a river-worn or tumbled pebble, shaped by water erosion over geological time.

Uses & Applications

Used in glass manufacturing, electronics (due to piezoelectric properties), construction aggregates, and as decorative landscaping stones or metaphysical crystals.

Geological Facts

Quartz is the second most abundant mineral in Earth's continental crust. Milky quartz gets its characteristic white color from microscopic inclusions of gas or liquid trapped during crystal growth.

Field Identification & Locations

Identify in the field by its ability to scratch glass, its lack of cleavage, and its resistance to weathering. Commonly found in riverbeds, beaches, and mountain veins worldwide.

Identified on: 4/19/2026

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