Quartz (Milky Quartz)
Silicon Dioxide (SiO2)
Rock Type: mineral

Physical Properties
Hardness: 7 on Mohs scale; Color: White to creamy/milky; Luster: Vitreous to greasy; Crystal Structure: Hexagonal (Trigonal); Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65.
Formation & Geological History
Formed from the cooling of silica-rich magma or through hydrothermal veins where mineral-saturated hot water deposits crystals in rock fractures. Common in almost all geological ages and environments.
Uses & Applications
Used in glass manufacturing, electronics (due to piezoelectric properties), abrasives, jewelry (as semi-precious gemstones), and as a decorative landscaping stone.
Geological Facts
Quartz is the second most abundant mineral in Earth's continental crust. 'Milky' quartz gets its white color from tiny fluid inclusions of gas or liquid trapped during crystal growth.
Field Identification & Locations
Identify in the field by its ability to scratch glass and steel, its white/waxy appearance, and lack of cleavage. Often found on beaches and in riverbeds as rounded 'water-worn' pebbles.
Identified on: 5/4/2026
Mode: Standard