Rock Identifier
Quartz-rich iron-stained rock, likely quartzite or quartz vein material (Quartz (SiO₂), with iron oxides/hydroxides such as hematite and goethite) — metamorphic
metamorphic

Quartz-rich iron-stained rock, likely quartzite or quartz vein material

Quartz (SiO₂), with iron oxides/hydroxides such as hematite and goethite

AI-generated identification · may be incorrect

Hardness about 7 Mohs; white to translucent gray quartz with rusty orange-brown staining, vitreous to dull luster, granular or massive texture, and no obvious cleavage. The surface appears weathered and may include minor feldspar or host-rock fragments.

Identified More metamorphic
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Physical properties

Hardness about 7 Mohs; white to translucent gray quartz with rusty orange-brown staining, vitreous to dull luster, granular or massive texture, and no obvious cleavage. The surface appears weathered and may include minor feldspar or host-rock fragments.

Formation & geological history

Likely formed from quartz-rich sediment metamorphosed into quartzite, or precipitated as a hydrothermal quartz vein and later iron-stained by weathering. Its precise geological age cannot be determined from the photograph.

Uses & applications

Commonly used as aggregate, road stone, decorative stone, and occasionally as a lapidary material; generally not gem quality. Attractive polished pieces may have modest collecting value.

Geological facts

Iron oxides create the orange, brown, and reddish colors by filling fractures and coating quartz grains. Quartz should scratch ordinary glass, while a steel knife typically does not scratch it.

Field identification & locations

Common in quartz veins, metamorphic terrains, and gravel deposits worldwide; look for sugary granular texture, glassy translucent areas, and very high hardness. A field test, streak test, and acid test on associated material would improve identification.