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

Physical Properties
Hardness: 7 (Mohs scale); Color: White to translucent; Luster: Vitreous (glass-like); Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
Formation & Geological History
Commonly forms from the cooling of silica-rich magma or through hydrothermal activity in veins. It is found in igneous, metamorphic, and sedimentary environments globally.
Uses & Applications
Used in electronics (piezoelectric properties), glassmaking, abrasives, timekeeping components, and as a semi-precious gemstone in jewelry.
Geological Facts
Quartz is the second most abundant mineral in Earth's continental crust. Milky quartz gets its opaque appearance from tiny fluid inclusions trapped during crystal growth.
Field Identification & Locations
Identify by its hardness (scratches glass), lack of cleavage, and vitreous luster. Found in most mountain ranges and riverbeds. It is a target for amateur collectors due to its ubiquity.
Identified on: 5/10/2026
Mode: Standard