Rock Identifier
Tumbled black basalt (Basalt; fine-grained plagioclase–pyroxene volcanic rock, commonly with olivine and iron oxides) — igneous
igneous

Tumbled black basalt

Basalt; fine-grained plagioclase–pyroxene volcanic rock, commonly with olivine and iron oxides

AI-generated identification · may be incorrect

Typically Mohs 5–6, opaque black to dark gray, with dull to weakly glassy luster and very fine interlocking crystals. The rounded, polished form and bluish reflective patches may indicate weathering, vesicle filling, or surface coating; exact identification cannot be confirmed visually.

Identified More igneous
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Physical properties

Typically Mohs 5–6, opaque black to dark gray, with dull to weakly glassy luster and very fine interlocking crystals. The rounded, polished form and bluish reflective patches may indicate weathering, vesicle filling, or surface coating; exact identification cannot be confirmed visually.

Formation & geological history

Forms when mafic lava rapidly cools at or near Earth’s surface, commonly in oceanic crust, volcanic plateaus, and lava flows. Basalt ranges from Precambrian to modern and is actively forming today.

Uses & applications

Used as crushed aggregate, roadstone, building stone, and landscaping material; polished pieces are sold as decorative stones and occasionally marketed as grounding or healing stones.

Geological facts

Basalt is the most widespread volcanic rock and makes up much of the ocean floor. Its dark color reflects abundant iron- and magnesium-rich minerals.

Field identification & locations

Look for high density, fine grain, dark color, and weak attraction to a magnet if magnetite-rich; a glassy streak or coating can complicate testing. Common sources include Hawaii, Iceland, India, the Pacific Northwest, and oceanic islands.