Rock Identifier
Weathered volcanic rock, likely vesicular basalt (Basalt; primarily plagioclase feldspar, pyroxene, and iron oxides) — igneous
igneous

Weathered volcanic rock, likely vesicular basalt

Basalt; primarily plagioclase feldspar, pyroxene, and iron oxides

AI-generated identification · may be incorrect

Gray, fine-grained, matte surface with small weathering pits or vesicles; hardness about 5–6 Mohs, typically massive with no visible cleavage, and specific gravity roughly 2.8–3.0.

Identified More igneous
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Physical properties

Gray, fine-grained, matte surface with small weathering pits or vesicles; hardness about 5–6 Mohs, typically massive with no visible cleavage, and specific gravity roughly 2.8–3.0.

Formation & geological history

Basalt forms when basaltic lava cools rapidly at or near Earth’s surface, commonly in volcanic flows; the specimen’s age cannot be determined from the image and may range from recent to billions of years.

Uses & applications

Used as aggregate, road stone, building material, and ballast; attractive polished pieces may be collected, though this example appears ordinary and unpolished.

Geological facts

Its rounded shape and pitted surface indicate prolonged water or abrasion weathering rather than a fresh angular fracture.

Field identification & locations

Common in volcanic regions, riverbeds, beaches, and glacial deposits. Confirm with a dark streak, lack of strong acid reaction, and microscopic crystals; a magnet may show weak attraction if iron-rich.