Rock Identifier
Iron-stained quartz (Quartz (SiO₂), likely stained by iron oxides) — mineral
mineral

Iron-stained quartz

Quartz (SiO₂), likely stained by iron oxides

AI-generated identification · may be incorrect

Hardness 7 Mohs; white to translucent with rusty yellow-brown patches and vitreous luster. Hexagonal crystal structure; no cleavage, with uneven to conchoidal fracture. The image does not show enough detail to confirm the identification.

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Physical properties

Hardness 7 Mohs; white to translucent with rusty yellow-brown patches and vitreous luster. Hexagonal crystal structure; no cleavage, with uneven to conchoidal fracture. The image does not show enough detail to confirm the identification.

Formation & geological history

Quartz commonly crystallizes from silica-rich fluids in veins and cavities, or forms as grains in many rock types. The iron staining formed when iron-bearing minerals oxidized; no age can be determined from the image.

Uses & applications

Quartz is widely used in glassmaking, electronics, and construction; attractive pieces may be collected or used decoratively.

Geological facts

Quartz is one of Earth’s most abundant minerals and is a major component of many sands and rocks.

Field identification & locations

Look for glassy luster, hardness sufficient to scratch glass, and absence of cleavage; rusty coloration can result from iron-oxide coatings. Quartz is common worldwide, especially in veins and pegmatites.