Rock Identifier
Possible weathered basalt or iron-rich volcanic stone (Fine-grained mafic rock, possibly basalt; exact identification requires testing) — igneous
igneous

Possible weathered basalt or iron-rich volcanic stone

Fine-grained mafic rock, possibly basalt; exact identification requires testing

AI-generated identification · may be incorrect

Small rounded gray-brown specimen with dull to weakly earthy luster and probable fine texture; basalt typically has Mohs hardness 5–6, no cleavage, and specific gravity about 2.8–3.1.

Identified More igneous
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Physical properties

Small rounded gray-brown specimen with dull to weakly earthy luster and probable fine texture; basalt typically has Mohs hardness 5–6, no cleavage, and specific gravity about 2.8–3.1.

Formation & geological history

Likely formed when mafic lava cooled rapidly at or near Earth’s surface, then became rounded and weathered; basalt commonly ranges from Precambrian to recent age.

Uses & applications

Common basalt is used as crushed aggregate, road material, building stone, and occasionally as a lapidary material; this small specimen has mainly educational or collectible value.

Geological facts

The brown surface may reflect oxidation of iron-bearing minerals, while the dark interior suggests a mafic composition.

Field identification & locations

Look for a dense, fine-grained, dark interior, weak magnetism, and possible tiny feldspar crystals; a streak, hardness, magnet, and fresh broken surface would distinguish basalt from slag, chert, or ironstone. Common worldwide in volcanic regions.