Rock Identifier
Tumbled dark stone, likely basalt or slate (Basalt (fine-grained plagioclase–pyroxene rock), possibly slate/phyllite) — igneous
igneous

Tumbled dark stone, likely basalt or slate

Basalt (fine-grained plagioclase–pyroxene rock), possibly slate/phyllite

AI-generated identification · may be incorrect

Smooth, rounded, dark blue-gray to black, matte-to-waxy luster, very fine-grained and lacking visible crystals; apparent Mohs hardness about 5–7. The straight pale line may be a natural vein, fracture, or surface scratch.

Identified More igneous
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Physical properties

Smooth, rounded, dark blue-gray to black, matte-to-waxy luster, very fine-grained and lacking visible crystals; apparent Mohs hardness about 5–7. The straight pale line may be a natural vein, fracture, or surface scratch.

Formation & geological history

If basalt, it formed from rapidly cooled mafic lava, commonly in oceanic crust and volcanic regions; if slate/phyllite, it formed by low-grade metamorphism of shale. Exact age and identification require fresh surface, hardness, and streak tests.

Uses & applications

Commonly sold as a worry stone, tumbled landscaping stone, or decorative specimen; basalt is used for aggregate and construction, while slate is used for roofing and architectural finishes.

Geological facts

The shape and polish indicate human tumbling, but processing does not exclude geological origin. Color alone cannot reliably distinguish basalt from dark metamorphic rocks.

Field identification & locations

Test an inconspicuous area: basalt commonly scratches glass weakly or not at all and has a gray streak; slate tends to show planar cleavage. Common sources include volcanic regions worldwide and slate belts.