Rock Identifier
Dark basalt cobble (Basalt; fine-grained mafic volcanic rock composed chiefly of plagioclase, pyroxene, and commonly olivine) — igneous
igneous

Dark basalt cobble

Basalt; fine-grained mafic volcanic rock composed chiefly of plagioclase, pyroxene, and commonly olivine

AI-generated identification · may be incorrect

Black to dark gray, fine-grained, massive, and weakly vitreous to dull; Mohs hardness about 6, with no visible cleavage and specific gravity roughly 2.8–3.0. The smooth rounded shape indicates water or beach abrasion, possibly with minor surface weathering.

Identified More igneous
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Physical properties

Black to dark gray, fine-grained, massive, and weakly vitreous to dull; Mohs hardness about 6, with no visible cleavage and specific gravity roughly 2.8–3.0. The smooth rounded shape indicates water or beach abrasion, possibly with minor surface weathering.

Formation & geological history

Basalt forms when iron- and magnesium-rich lava rapidly cools at or near Earth’s surface, commonly at oceanic ridges, hotspots, and continental volcanic fields. The specimen’s exact age and locality cannot be determined from the image.

Uses & applications

Used as crushed aggregate, road base, railway ballast, riprap, paving stone, and occasionally architectural facing; rounded examples are mainly educational or decorative.

Geological facts

Basalt is the most abundant volcanic rock on Earth and makes up much of the oceanic crust. It commonly attracts a magnet weakly to moderately because of iron-bearing minerals.

Field identification & locations

Identify it by its uniformly dark color, fine texture, high density, and lack of large crystals; a streak, magnet, and fresh broken surface would help distinguish it from andesite or slag. Common worldwide, especially in volcanic regions and stream or beach gravels.