Rock Identifier
Tumbled reddish-brown pebble, likely sandstone or iron-rich quartzite (Probable ferruginous sandstone (quartz-rich; SiO₂ with iron oxides), possibly quartzite) — sedimentary or metamorphic
sedimentary or metamorphic

Tumbled reddish-brown pebble, likely sandstone or iron-rich quartzite

Probable ferruginous sandstone (quartz-rich; SiO₂ with iron oxides), possibly quartzite

AI-generated identification · may be incorrect

Hardness approximately 6–7 Mohs; reddish-brown, fine-grained, dull to silky luster, rounded by abrasion, with no visible crystals or cleavage. The smooth surface and subtle layering suggest a sedimentary sandstone, while a very hard, compact texture would indicate quartzite.

Identified More sedimentary or metamorphic
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Physical properties

Hardness approximately 6–7 Mohs; reddish-brown, fine-grained, dull to silky luster, rounded by abrasion, with no visible crystals or cleavage. The smooth surface and subtle layering suggest a sedimentary sandstone, while a very hard, compact texture would indicate quartzite.

Formation & geological history

Sandstone formed from lithified quartz sand, commonly tens to hundreds of millions of years old; iron oxides produced the red-brown color. If quartzite, it formed when sandstone was metamorphosed under heat and pressure.

Uses & applications

Commonly collected as a polished or naturally rounded specimen and used decoratively; sandstone is also used as building stone and aggregate, while quartzite is used for countertops, paving, and construction.

Geological facts

The image alone cannot reliably distinguish sandstone from quartzite; a streak, hardness, and magnified grain test would help.

Field identification & locations

Likely found in streambeds, gravel deposits, beaches, or weathered sandstone/quartzite outcrops. It should scratch glass if quartz-rich; sandstone may show granular texture and crumble slightly at edges.