mineral

Quartz Geode (Smoky Quartz)

Silicon Dioxide (SiO2)

Hardness: 7 on Mohs scale; Color: Dark grey to black interior crystals with a light grey or white chalcedony rim and tan/brown host rock; Luster: Vitreous (glassy) on crystal faces; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture).

Hardness: 7 on Mohs scale
Luster: Vitreous (glassy) on crystal faces

Identified May 2, 2026More mineral →

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Physical properties

Formation & geological history

Formed in cavities (vesicles) within volcanic rocks or sedimentary rocks where mineral-rich groundwater precipitates crystals over long periods. As the outer shell hardens, the interior crystals grow inward.

Uses & applications

Primarily used for geological collection, home decor, and crystal healing practices. Large, high-quality geodes are sometimes used as museum showpieces.

Geological facts

Geodes are often called 'thunder eggs' when they are completely filled with minerals. The dark color in smoky quartz is caused by natural irradiation of the aluminum impurities within the silicon dioxide.

Field identification & locations

Identified by its cauliflower-like exterior and hollow interior lined with inward-pointing crystals. Common in volcanic regions and desert environments like Morocco, Brazil, and the Southwestern US.