Rock Identifier
Limonite-stained Quartz (Silicon Dioxide with Iron Oxide Hydroxide, SiO2 + FeO(OH)*nH2O) — mineral
mineral

Limonite-stained Quartz

Silicon Dioxide with Iron Oxide Hydroxide, SiO2 + FeO(OH)*nH2O

AI-generated identification · may be incorrect

Hardness of 7 for quartz and 4-5.5 for limonite; yellowish-brown to orange-brown color; vitreous to earthy luster; hexagonal crystal system.

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Physical properties

Hardness of 7 for quartz and 4-5.5 for limonite; yellowish-brown to orange-brown color; vitreous to earthy luster; hexagonal crystal system.

Formation & geological history

Formed through hydrothermal veins or secondary weathering of iron-bearing sulfide minerals, often over millions of years.

Uses & applications

Used as mineral specimens for collectors, decorative stones, and historically as an iron ore and pigment.

Geological facts

Limonite staining is a common surface alteration caused by groundwater interacting with iron minerals, giving rocks a characteristic rusty appearance.

Field identification & locations

Easily identified by its rusty brown coating and hard, glassy quartz core. Found worldwide in weathered quartz veins and gossan caps.