Rock Identifier
Tumbled gray pebble, likely basalt or dark chert (Most consistent with fine-grained basalt (plagioclase–pyroxene), though gray chert (microcrystalline SiO₂) is possible) — igneous
igneous

Tumbled gray pebble, likely basalt or dark chert

Most consistent with fine-grained basalt (plagioclase–pyroxene), though gray chert (microcrystalline SiO₂) is possible

AI-generated identification · may be incorrect

Smooth, rounded, dark gray, dull to faintly waxy luster, with no visible crystals or cleavage; estimated hardness 5.5–6.5 (basalt) or about 7 (chert), and specific gravity roughly 2.6–3.0.

Identified More igneous
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Physical properties

Smooth, rounded, dark gray, dull to faintly waxy luster, with no visible crystals or cleavage; estimated hardness 5.5–6.5 (basalt) or about 7 (chert), and specific gravity roughly 2.6–3.0.

Formation & geological history

Likely naturally water-worn or mechanically tumbled from volcanic or siliceous rock; basalt commonly formed from rapidly cooled lava, generally ranging from Precambrian to modern in age.

Uses & applications

Commonly used as a decorative pebble, craft/tumbled stone, or landscaping material; ordinary specimens have little jewelry value.

Geological facts

The uniformly fine texture indicates rapid cooling or microcrystalline silica. A steel nail may scratch softer basalt but should not scratch chert; glass can help test higher hardness.

Field identification & locations

Common in streambeds, beaches, gravel deposits, and volcanic regions worldwide. A strong vinegar reaction would indicate carbonate rock instead, while a streak plate and hardness test can distinguish basalt from chert.