Rock Identifier
Quartz Geode (Silicon Dioxide (SiO2)) — sedimentary
sedimentary

Quartz Geode

Silicon Dioxide (SiO2)

Mohs hardness of 7, white or clear crystalline appearance, vitreous to sugary luster, trigonal crystal system, conchoidal fracture with no true cleavage, specific gravity of 2.65

Identified More sedimentary
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Physical properties

Mohs hardness of 7, white or clear crystalline appearance, vitreous to sugary luster, trigonal crystal system, conchoidal fracture with no true cleavage, specific gravity of 2.65

Formation & geological history

Formed in cavities of sedimentary or volcanic rocks where silica-rich groundwater percolates and slowly precipitates quartz crystals over millions of years.

Uses & applications

Used in decorative display, crystal collecting, mineral specimens, and occasionally lapidary work.

Geological facts

Geodes appear as ordinary, unassuming spherical rocks on the outside, but cracking them open reveals a sparkling hollow interior lined with crystal formations.

Field identification & locations

Found worldwide, notably in regions with limestone deposits or volcanic ash beds such as Mexico, Brazil, and the Midwestern United States (e.g., Keokuk, Iowa).