Rock Identifier
Polished black stone, likely basalt (Basalt; predominantly plagioclase feldspar and pyroxene, commonly with minor magnetite or olivine) — igneous
igneous

Polished black stone, likely basalt

Basalt; predominantly plagioclase feldspar and pyroxene, commonly with minor magnetite or olivine

AI-generated identification · may be incorrect

Typically dark gray to black, fine-grained, opaque, and dull to subtly waxy; hardness about 5–6 Mohs, with no visible cleavage and irregular fracture. The smooth surface appears polished or naturally water-worn, so exact identification from the image alone is limited.

Identified More igneous
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Physical properties

Typically dark gray to black, fine-grained, opaque, and dull to subtly waxy; hardness about 5–6 Mohs, with no visible cleavage and irregular fracture. The smooth surface appears polished or naturally water-worn, so exact identification from the image alone is limited.

Formation & geological history

Basalt forms when low-viscosity mafic lava cools rapidly at or near Earth’s surface, commonly in volcanic fields and oceanic crust; specimens range from recent to Precambrian in age.

Uses & applications

Used as crushed aggregate, road base, concrete, riprap, paving, and decorative stone; polished pieces are sold as ornaments or worry stones.

Geological facts

Its dark color reflects abundant iron- and magnesium-rich minerals. A magnet may show weak attraction if magnetite is present.

Field identification & locations

Look for a uniformly fine texture, high density, dark streakless appearance, and possible tiny feldspar crystals; test hardness against glass and inspect for vesicles. Common worldwide, especially volcanic regions and river gravels.