Rock Identifier
Dark gray rounded cobble, likely basalt or fine-grained metamorphic rock (Likely basalt (plagioclase–pyroxene rock); exact identification requires testing) — igneous
igneous

Dark gray rounded cobble, likely basalt or fine-grained metamorphic rock

Likely basalt (plagioclase–pyroxene rock); exact identification requires testing

AI-generated identification · may be incorrect

Fine-grained, massive, dark gray with mottled weathering and subvitreous-to-dull luster; hardness about 5–6 Mohs, no obvious cleavage, and typically specific gravity 2.8–3.1. The rounded shape indicates natural stream/beach abrasion or tumbling.

Identified More igneous
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Physical properties

Fine-grained, massive, dark gray with mottled weathering and subvitreous-to-dull luster; hardness about 5–6 Mohs, no obvious cleavage, and typically specific gravity 2.8–3.1. The rounded shape indicates natural stream/beach abrasion or tumbling.

Formation & geological history

If basalt, it formed from rapidly cooled mafic lava, commonly in volcanic fields or oceanic crust, from any age. Its present rounded form likely developed through prolonged transport and abrasion in a river, shore, or glacial deposit.

Uses & applications

Used as crushed aggregate, road stone, riprap, and occasionally dimension stone; generally low jewelry value, though attractive polished pieces may be collected.

Geological facts

Basalt commonly contains microscopic plagioclase and pyroxene crystals, making it appear uniformly fine-grained. Brown patches are likely iron-oxide weathering rather than metallic mineralization.

Field identification & locations

Look for a dense, dark, nonfoliated rock that may attract a magnet weakly if iron-rich; a streak, acid test, and fresh surface help distinguish it from slate, gabbro, or amphibolite. Common in volcanic and glacial regions worldwide.