Rock Identifier
Rounded gray pebble, likely basalt or andesite (Fine-grained mafic to intermediate volcanic rock; commonly plagioclase with pyroxene and/or olivine) — igneous
igneous

Rounded gray pebble, likely basalt or andesite

Fine-grained mafic to intermediate volcanic rock; commonly plagioclase with pyroxene and/or olivine

AI-generated identification · may be incorrect

Hardness about 5.5–6.5 Mohs; gray, dull to faintly granular luster, compact texture, and no visible cleavage or crystals at this scale. Its smooth, flattened shape indicates water or beach abrasion; exact identification requires a fresh surface or testing.

Identified More igneous →
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Physical properties

Hardness about 5.5–6.5 Mohs; gray, dull to faintly granular luster, compact texture, and no visible cleavage or crystals at this scale. Its smooth, flattened shape indicates water or beach abrasion; exact identification requires a fresh surface or testing.

Formation & geological history

Likely formed from rapidly cooled lava, then rounded by erosion in a stream, lake, or shoreline environment. The rock may be millions to hundreds of millions of years old, depending on its source.

Uses & applications

Suitable mainly as a decorative pebble, paperweight, landscaping stone, or lapidary material; ordinary specimens have little industrial or jewelry value.

Geological facts

Basalt is the most abundant volcanic rock on Earth and commonly forms oceanic crust and extensive lava flows.

Field identification & locations

Look for a dark gray fine-grained interior, high density, lack of layering, and possible tiny feldspar crystals; a streak, magnetism, acid, and thin-section test can distinguish basalt from andesite or other pebbles. Common worldwide, especially volcanic regions and riverbeds.