
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 incorrectSmooth, 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.
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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.