Rock Identifier
Weathered quartz-rich metamorphic rock, likely quartzite (Quartzite; predominantly quartz (SiO₂), with iron-oxide staining and possible feldspar/mica impurities) — metamorphic
metamorphic

Weathered quartz-rich metamorphic rock, likely quartzite

Quartzite; predominantly quartz (SiO₂), with iron-oxide staining and possible feldspar/mica impurities

AI-generated identification · may be incorrect

Hardness about 7 Mohs; coarse, granular texture with gray, cream, and rusty orange-brown colors. Vitreous to dull luster, interlocking quartz grains, and no obvious cleavage; orange areas are likely limonite/hematite staining.

Identified More metamorphic
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Physical properties

Hardness about 7 Mohs; coarse, granular texture with gray, cream, and rusty orange-brown colors. Vitreous to dull luster, interlocking quartz grains, and no obvious cleavage; orange areas are likely limonite/hematite staining.

Formation & geological history

Formed when quartz-rich sandstone was deeply buried and recrystallized under heat and pressure, commonly during mountain building. Its exact geological age cannot be determined from the photograph and depends on the source formation.

Uses & applications

Used as crushed aggregate, road stone, building stone, landscaping rock, and occasionally as decorative slabs. Attractive banded or iron-stained pieces may be collected, but this specimen appears common and uncut.

Geological facts

Quartzite commonly breaks across grains rather than around them and can scratch ordinary glass. Iron-bearing groundwater often produces the characteristic orange, yellow, and red weathering colors.

Field identification & locations

Look for a very hard, sugary texture and quartz grains fused into a massive rock; a steel nail usually will not scratch it. Common occurrences include metamorphic mountain belts worldwide, especially India, Brazil, the United States, and Scandinavia.