Rock Identifier
Milky Quartz (or Iron-Stained Quartz) (Quartz (Silicon Dioxide, SiO2)) — mineral
mineral

Milky Quartz (or Iron-Stained Quartz)

Quartz (Silicon Dioxide, SiO2)

Hardness: 7 on Mohs scale; Color: Milky white with yellowish-brown iron oxidation staining; Luster: Vitreous to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.

Hardness
7 on Mohs scale
Color
Milky white with yellowish-brown iron oxidation staining
Luster
Vitreous to greasy
Identified More mineral

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Hardness: 7 on Mohs scale; Color: Milky white with yellowish-brown iron oxidation staining; Luster: Vitreous to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.

Formation & geological history

Formed through hydrothermal processes where silica-rich fluids cool in veins, or as a primary mineral in igneous and metamorphic rocks. This specimen likely formed in a hydrothermal vein and has been weathered at the surface, leading to the iron-oxide staining (rust colors).

Uses & applications

Used in glass manufacturing, as an abrasive, in electronics (piezoelectric properties), in construction as aggregate, and as a semi-precious gemstone or metaphysical specimen.

Geological facts

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

Field identification & locations

Identify in the field by its hardness (it will scratch glass and steel), lack of cleavage, and waxy/vitreous luster. Common in mountainous regions, riverbeds, and as veins in surrounding rock. Tips for collectors: check for crystal faces in cavities (vugs).