Rock Identifier
Quartz Druzy (Silicon Dioxide (SiO2)) — mineral
mineral

Quartz Druzy

Silicon Dioxide (SiO2)

Hardness: 7 (Mohs scale), Color: Clear to white/off-white, Luster: Vitreous to Adamantine, Crystal Structure: Trigonal (hexagonal prisms), Cleavage: None (conchoidal fracture), Specific Gravity: 2.65

Identified More mineral
Explore Quartz Druzy in the encyclopedia →

Identify your own rocks.

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

Physical properties

Hardness: 7 (Mohs scale), Color: Clear to white/off-white, Luster: Vitreous to Adamantine, Crystal Structure: Trigonal (hexagonal prisms), Cleavage: None (conchoidal fracture), Specific Gravity: 2.65

Formation & geological history

Formed via hydrothermal precipitation where silica-rich fluids deposit tiny crystals in rock cavities or fractures. Common in vugs of sedimentary rocks like limestone or volcanic geodes.

Uses & applications

Primarily used in jewelry (as pendants or earrings), metaphysical collections, and as decorative mineral specimens.

Geological facts

The term 'druzy' refers to a coating of fine crystals on a rock surface. Quartz is the most common mineral to form druzy, creating a 'sugar-coated' or 'glitter' effect due to the many tiny crystal facets reflecting light.

Field identification & locations

Identified by its signature sparkling 'sugary' appearance and high hardness (it can scratch glass). Commonly found in geodes or lining the walls of veins in various geological environments.