Rock Identifier
Iron-stained quartz-rich rock (Likely ferruginous quartzite (quartz, SiO₂, with iron oxides/hydroxides)) — metamorphic
metamorphic

Iron-stained quartz-rich rock

Likely ferruginous quartzite (quartz, SiO₂, with iron oxides/hydroxides)

AI-generated identification · may be incorrect

Rough, granular texture; pale tan-gray with orange-brown iron staining and a dull to slightly glassy luster. Quartz has Mohs hardness 7 and trigonal crystal structure; the specimen’s overall hardness and texture depend on its cementation and other minerals.

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Physical properties

Rough, granular texture; pale tan-gray with orange-brown iron staining and a dull to slightly glassy luster. Quartz has Mohs hardness 7 and trigonal crystal structure; the specimen’s overall hardness and texture depend on its cementation and other minerals.

Formation & geological history

Quartz-rich sandstone can be recrystallized into quartzite during metamorphism; iron-bearing fluids or weathering produce the rusty staining. Precise age and origin cannot be determined from the image.

Uses & applications

Quartzite is used as building and paving stone, aggregate, and sometimes as a decorative stone; this rough specimen is mainly suitable for collecting.

Geological facts

The orange color commonly comes from iron oxides such as hematite or goethite coating or cementing quartz grains.

Field identification & locations

Look for abundant hard quartz grains and a granular or fused texture; quartzite resists scratching by a steel knife. Similar iron-stained material occurs worldwide, but a photo cannot confirm the rock type or locality.