Milky Quartz
Silicon Dioxide (SiO2)
Rock Type: mineral

Physical Properties
Hardness: 7 on Mohs scale; Color: Milky white to translucent; Luster: Vitreous to greasy; Crystal Structure: Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & Geological History
Formed through the cooling of silica-rich magma or from hydrothermal veins. The milky appearance is caused by tiny inclusions of gas or liquid trapped during crystal growth. They can be found in a wide variety of geological ages.
Uses & Applications
Used in glass manufacturing, electronics (due to piezoelectric properties), construction aggregates, and as decorative landscaping stone. High-purity quartz is used in solar panels.
Geological Facts
Quartz is the second most abundant mineral in Earth's continental crust. Milky quartz is often found alongside gold in hydrothermal vein deposits, leading many prospectors to use it as an indicator stone.
Field Identification & Locations
Identify in the field by its hardness (it can scratch glass), lack of cleavage, and common occurrence as rounded river pebbles or jagged vein fragments. Found globally in riverbeds, mountains, and beaches.
Identified on: 4/22/2026
Mode: Standard