Rock Identifier
Weathered sandstone or quartzite fragment (Quartz-rich sandstone; possibly weakly metamorphosed quartzite) — sedimentary
sedimentary

Weathered sandstone or quartzite fragment

Quartz-rich sandstone; possibly weakly metamorphosed quartzite

AI-generated identification · may be incorrect

Tan to brown, fine- to medium-grained, dull to sugary texture with scattered white quartz-rich patches; quartz has Mohs hardness 7, while sandstone commonly has hardness around 6–7. The specimen appears massive, with no obvious cleavage and low to moderate specific gravity (~2.6).

Identified More sedimentary
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Physical properties

Tan to brown, fine- to medium-grained, dull to sugary texture with scattered white quartz-rich patches; quartz has Mohs hardness 7, while sandstone commonly has hardness around 6–7. The specimen appears massive, with no obvious cleavage and low to moderate specific gravity (~2.6).

Formation & geological history

Likely formed from compacted and cemented quartz sand, probably during the Paleozoic or Mesozoic; if quartzite, later burial and metamorphism recrystallized the grains. Exact age and origin cannot be determined from the image alone.

Uses & applications

Used as building stone, paving, aggregate, landscaping material, and occasionally as a decorative slab; ordinary fragments have little jewelry value.

Geological facts

The granular, sand-textured surface and tan coloration are consistent with iron-oxide-stained quartz sandstone. A strong vinegar reaction would suggest carbonate cement, whereas no reaction supports silica cement.

Field identification & locations

Look for visible sand grains, bedding, iron staining, and resistance to scratching; it should not be confused with limestone, which is softer and reacts with dilute acid. Common worldwide, especially in sedimentary basins and former beach or desert environments.