Rock Identifier
Rounded brown-gray pebble, likely weathered basalt or iron-stained chert (Indeterminate from image; possible basalt (plagioclase–pyroxene) or chert (microcrystalline SiO₂)) — igneous
igneous

Rounded brown-gray pebble, likely weathered basalt or iron-stained chert

Indeterminate from image; possible basalt (plagioclase–pyroxene) or chert (microcrystalline SiO₂)

AI-generated identification · may be incorrect

Small, smooth, subrounded specimen with mottled brown-gray coloration and dull to slightly earthy luster. Basalt typically has Mohs hardness 5–6 and dense fine-grained texture; chert is harder, about 6.5–7, and may show a waxy luster.

Identified More igneous
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Physical properties

Small, smooth, subrounded specimen with mottled brown-gray coloration and dull to slightly earthy luster. Basalt typically has Mohs hardness 5–6 and dense fine-grained texture; chert is harder, about 6.5–7, and may show a waxy luster.

Formation & geological history

Likely naturally weathered from a stream, beach, or glacial deposit; its geological age and formation cannot be determined from the photograph. Brown areas may reflect oxidation of iron-bearing minerals.

Uses & applications

Common specimens have little commercial value and are mainly used for teaching or casual collecting; basalt is used as aggregate and building stone, while chert can be used for tools and decorative stone.

Geological facts

The rounded shape indicates abrasion during transport. A steel nail or knife may scratch softer basalt but should not scratch chert; streak and acid tests can further assist identification.

Field identification & locations

Commonly found in river gravels, beaches, and glacial tills worldwide. A fresh broken surface, magnetism, visible grains, and hardness testing would improve identification.