Rock Identifier
Rounded volcanic pebble, likely basalt (Basalt; fine-grained mafic rock composed mainly of plagioclase and pyroxene, commonly with olivine) — igneous
igneous

Rounded volcanic pebble, likely basalt

Basalt; fine-grained mafic rock composed mainly of plagioclase and pyroxene, commonly with olivine

AI-generated identification · may be incorrect

Gray-green, dull to slightly earthy luster, fine-grained and vesicular with small pores; hardness about 5–6 Mohs, no visible cleavage, and typical specific gravity around 2.8–3.0.

Identified More igneous
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Physical properties

Gray-green, dull to slightly earthy luster, fine-grained and vesicular with small pores; hardness about 5–6 Mohs, no visible cleavage, and typical specific gravity around 2.8–3.0.

Formation & geological history

Formed when basaltic lava cooled rapidly at or near Earth’s surface, likely within the Cenozoic or older volcanic history, then rounded by stream or wave transport. Exact age and provenance cannot be determined from the photograph.

Uses & applications

Commonly used as aggregate, roadstone, riprap, and landscaping material; attractive polished pieces may be sold as inexpensive décor or curiosities.

Geological facts

The rounded shape indicates abrasion during transport, while the tiny holes are gas vesicles preserved in the lava. Green coloration may reflect olivine, chlorite, or weathering.

Field identification & locations

Look for a heavy, dark, fine-grained pebble with scattered vesicles and no obvious mineral grains; it commonly occurs near volcanic terrains, beaches, and river gravel beds. A simple streak, magnet, and acid test can help distinguish it from slag or other dark rocks.