Rock Identifier
Likely basalt fragment (Basalt, a fine-grained mafic volcanic rock composed mainly of plagioclase feldspar and pyroxene, commonly with olivine) — igneous
igneous

Likely basalt fragment

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

AI-generated identification · may be incorrect

Dark gray to black, fine-grained, dull to mildly vitreous, with no visible crystals or cleavage; typically Mohs 6, specific gravity about 2.8–3.0. The straight sides suggest it may be cut or shaped rather than naturally broken.

Identified More igneous
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Physical properties

Dark gray to black, fine-grained, dull to mildly vitreous, with no visible crystals or cleavage; typically Mohs 6, specific gravity about 2.8–3.0. The straight sides suggest it may be cut or shaped rather than naturally broken.

Formation & geological history

Basalt forms when low-silica lava rapidly cools at or near Earth’s surface, commonly in oceanic crust, lava flows, and volcanic islands. Most examples range from Precambrian to modern, depending on locality.

Uses & applications

Used extensively as crushed aggregate, road stone, riprap, railway ballast, paving, and building stone; attractive polished pieces may be sold as decorative material. This small fragment has minimal commercial value.

Geological facts

Basalt is the most abundant volcanic rock and makes up much of the ocean floor. It is commonly confused with dark fine-grained rocks such as andesite, diabase, slag, or artificial stone.

Field identification & locations

Look for a uniformly dark, compact, fine texture and greater density than many sedimentary rocks; a streak is usually gray, and dilute acid produces no fizz. Confirming identification requires a fresh surface, hand lens, magnetism test, and locality information.