Milky Quartz
Silicon dioxide (SiO2)
Rock Type: mineral

Physical Properties
Hardness: 7 on Mohs scale; Color: White to opaque white; Luster: Vitreous to greasy; Crystal structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
Formation & Geological History
Formed through the crystallization of magma or from hydrothermal veins. The milky color is caused by microscopic fluid inclusions of gas and/or liquid trapped during crystal growth. They can be found in rocks from all geological eras.
Uses & Applications
Used in the glass and ceramic industries, as an abrasive, in landscaping/decoration, and occasionally for healing crystals or low-cost jewelry.
Geological Facts
Milky quartz is one of the most common minerals on Earth's crust. It is often referred to as 'Snow Quartz' in the gem market. Historical artifacts like arrowheads were sometimes carved from this material because of its hardness and predictability when fracturing.
Field Identification & Locations
Identify in the field by its hardness (will scratch glass and steel), white color, and lack of cleavage. It is commonly found in riverbeds, mountains, and as garden gravel worldwide.
Identified on: 4/15/2026
Mode: Standard