Rock Identifier
Tumbled dark stone, likely basalt (Basalt; fine-grained mafic rock composed mainly of plagioclase feldspar and pyroxene, commonly with olivine) — igneous
igneous

Tumbled dark stone, likely basalt

Basalt; fine-grained mafic rock composed mainly of plagioclase feldspar and pyroxene, commonly with olivine

AI-generated identification · may be incorrect

Very dark gray-green to black, rounded and polished, with a dull to faintly waxy luster; hardness about 5–6 Mohs, fine-grained massive texture, no visible cleavage, and specific gravity roughly 2.8–3.0.

Identified More igneous
Explore Tumbled dark stone, likely basalt in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Very dark gray-green to black, rounded and polished, with a dull to faintly waxy luster; hardness about 5–6 Mohs, fine-grained massive texture, no visible cleavage, and specific gravity roughly 2.8–3.0.

Formation & geological history

Basalt forms when iron- and magnesium-rich lava cools rapidly at or near Earth’s surface, commonly in volcanic fields and oceanic crust; its age may range from recent eruptions to billions of years.

Uses & applications

Used as aggregate, roadstone, building stone, ballast, and landscaping material; attractive tumbled pieces are inexpensive decorative or educational specimens.

Geological facts

The image shows a small, uniformly rounded, human-tumbled pebble; exact identification is limited because its texture and minerals are obscured by polishing and low resolution.

Field identification & locations

Commonly found in volcanic regions, river gravels, beaches, and commercial tumbling mixes. Test for a dark streak, lack of fizz in dilute acid, and hardness sufficient to scratch glass; examine a fresh edge for tiny feldspar crystals.