Rock Identifier
Quartz Geode with Iron Oxide (Silicon Dioxide (SiO2) with Hematite/Goethite coatings) — mineral
mineral

Quartz Geode with Iron Oxide

Silicon Dioxide (SiO2) with Hematite/Goethite coatings

Hardness: 7 on Mohs scale; Color: Clear to white quartz with brownish-orange to rusty iron oxide staining; Luster: Vitreous to dull; Crystal structure: Trigonal/Hexagonal quartz druse lining a cavity; Cleavage: None (conchoidal fracture).

Hardness
7 on Mohs scale
Luster
Vitreous to dull
Identified More mineral
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Physical properties

Hardness: 7 on Mohs scale; Color: Clear to white quartz with brownish-orange to rusty iron oxide staining; Luster: Vitreous to dull; Crystal structure: Trigonal/Hexagonal quartz druse lining a cavity; Cleavage: None (conchoidal fracture).

Formation & geological history

Forms in hydrothermal veins or cavity pockets within sedimentary or volcanic host rocks where silica-rich fluids precipitate quartz crystals, often stained by secondary iron minerals during weathering.

Uses & applications

Popular among mineral collectors, used in lapidary arts, education, decor, and metaphysical display pieces.

Geological facts

Small cavities lined with tiny crystals like this are called vugs or mini-geodes. The brown-orange rim and accents are caused by limonite, hematite, or goethite precipitation.

Field identification & locations

Identified by tiny hexagonal crystal terminations lining an interior cavity within a massive milky quartz or chalcedonic matrix, alongside rusty iron oxide staining. Common worldwide in volcanic and limestone terrains.