Rock Identifier
Polished black stone, likely gabbro or black basalt (Gabbro/basalt; chiefly plagioclase feldspar and pyroxene, possibly minor magnetite) — igneous
igneous

Polished black stone, likely gabbro or black basalt

Gabbro/basalt; chiefly plagioclase feldspar and pyroxene, possibly minor magnetite

AI-generated identification · may be incorrect

Dark gray-black, polished, opaque, with faint granular mottling and submetallic reflections; typical hardness about 6–7 Mohs, no visible cleavage, fine- to medium-grained crystalline texture, and specific gravity roughly 2.8–3.1.

Identified More igneous
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Physical properties

Dark gray-black, polished, opaque, with faint granular mottling and submetallic reflections; typical hardness about 6–7 Mohs, no visible cleavage, fine- to medium-grained crystalline texture, and specific gravity roughly 2.8–3.1.

Formation & geological history

An igneous rock formed when mafic magma cooled slowly underground (gabbro) or rapidly at the surface (basalt), generally from Precambrian to Cenozoic settings. The rounded shape and sheen indicate human tumbling and polishing.

Uses & applications

Used for decorative stone, cabochons, worry stones, aggregates, countertops, and landscaping; ordinary pieces have little gem value.

Geological facts

The specimen may contain magnetite and show weak attraction to a magnet. Its mottled texture distinguishes it from uniformly black glass or dyed agate.

Field identification & locations

Look for tiny interlocking gray crystals, high density, and a non-vitreous granular interior; a streak test is usually gray-black. Common worldwide in oceanic crust, volcanic fields, and mafic intrusions.