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

Quartz Geode

Silicon Dioxide (SiO2)

Hardness: 7 on Mohs scale; Color: Clear to white crystals within a gray or brown rind; Luster: Vitreous/glassy; Crystal Structure: Hexagonal; Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65

Hardness
7 on Mohs scale
Color
Clear to white crystals within a gray or brown rind
Luster
Vitreous/glassy
Identified More mineral

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Physical properties

Hardness: 7 on Mohs scale; Color: Clear to white crystals within a gray or brown rind; Luster: Vitreous/glassy; Crystal Structure: Hexagonal; Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65

Formation & geological history

Formed as hollow cavities in volcanic or sedimentary rocks. Over millions of years, mineral-rich groundwater seeps into these cavities, depositing silica that slowly crystallizes into quartz points growing inward.

Uses & applications

Primarily used as decorative display pieces, for geological education, metaphysics/holistic healing, and as entry-level collector specimens.

Geological facts

Geodes are often nicknamed 'Nature's Surprise' because they appear as plain, round rocks on the outside, only revealing their sparkling interior when cracked open. The word geode comes from the Greek 'geoides', meaning earth-like.

Field identification & locations

Identify by finding round or egg-shaped nodules that feel lighter than they look (indicating a hollow center). Commonly found in desert regions of Morocco, Brazil, and the Midwestern United States like Iowa (the state rock).