Rock Identifier
Ferruginous Quartz (Silicon Dioxide (SiO2) with Iron Oxide (Hematite/Limonite) inclusions) — mineral
mineral

Ferruginous Quartz

Silicon Dioxide (SiO2) with Iron Oxide (Hematite/Limonite) inclusions

Hardness: 7 on Mohs scale; Color: Reddish-orange, peach, or rusty brown; Luster: Vitreous to greasy; Crystal structure: Trigonal; Cleavage: None/Conchoidal fracture; Specific gravity: 2.65

Hardness
7 on Mohs scale
Color
Reddish-orange, peach, or rusty brown
Luster
Vitreous to greasy
Identified More mineral

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Physical properties

Hardness: 7 on Mohs scale; Color: Reddish-orange, peach, or rusty brown; Luster: Vitreous to greasy; Crystal structure: Trigonal; Cleavage: None/Conchoidal fracture; Specific gravity: 2.65

Formation & geological history

Formed through hydrothermal processes or secondary staining of quartz crystals by iron-rich groundwater. Often found in sedimentary deposits or as weathered vein quartz, dating from any geological period where silica and iron were present.

Uses & applications

Primary use is in aesthetic jewelry (beads, cabochons), lapidary art, and rock collecting. Historically used for carving and as a decorative stone.

Geological facts

Also known as 'Eisenkiesel' in German (meaning iron-pebble). The red color is caused by microscopic hematite or goethite crystals trapped inside the quartz matrix or coating the exterior surfaces.

Field identification & locations

Identify in the field by its superior hardness (cannot be scratched by a steel knife) and the characteristic sparkle of quartz underlying the rusty hue. Found globally in iron-rich soils, riverbeds, and quartz veins.