Rock Identifier
Quartz (Iron-stained or Orange Quartz) (Silicon Dioxide (SiO2)) — mineral
mineral

Quartz (Iron-stained or Orange Quartz)

Silicon Dioxide (SiO2)

Hardness: 7 on Mohs scale; Color: Translucent orange to tan; Luster: Vitreous/waxy; Crystal Structure: Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65

Hardness
7 on Mohs scale
Color
Translucent orange to tan
Luster
Vitreous/waxy
Identified More mineral
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Physical properties

Hardness: 7 on Mohs scale; Color: Translucent orange to tan; Luster: Vitreous/waxy; Crystal Structure: Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65

Formation & geological history

Formed from silica-rich hydrothermal fluids cooling in veins or as massive deposits. The orange color is typically caused by inclusions or surface staining of iron oxides (hematite or limonite).

Uses & applications

Used primarily in lapidary work, jewelry, and as a decorative landscaping stone. Industrial quartz is used in glassmaking and electronics.

Geological facts

Quartz is the second most abundant mineral in Earth's continental crust. Iron-stained varieties like this are often found in riverbeds where water has eroded and polished the specimen over time.

Field identification & locations

Identify by its hardness (will scratch glass) and lack of cleavage planes. Commonly found in riverbeds, mountains, and desert washes globally.