Rock Identifier
Weathered basalt pebble (Basalt, a fine-grained mafic volcanic rock composed mainly of plagioclase feldspar, pyroxene, and commonly olivine) — igneous
igneous

Weathered basalt pebble

Basalt, a fine-grained mafic volcanic rock composed mainly of plagioclase feldspar, pyroxene, and commonly olivine

AI-generated identification · may be incorrect

Dark gray-brown, rounded, and weakly granular with a dull to faintly subvitreous luster; typically massive with no cleavage. Hardness about 5–6 Mohs and specific gravity roughly 2.8–3.0.

Identified More igneous
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Physical properties

Dark gray-brown, rounded, and weakly granular with a dull to faintly subvitreous luster; typically massive with no cleavage. Hardness about 5–6 Mohs and specific gravity roughly 2.8–3.0.

Formation & geological history

Formed when mafic lava rapidly cooled at or near Earth’s surface, commonly during the Cenozoic or older volcanic episodes; its rounded shape and surface alteration indicate stream or beach transport and weathering.

Uses & applications

Used as crushed aggregate, road base, riprap, railway ballast, and occasionally ornamental stone; this small weathered pebble has minimal commercial or jewelry value.

Geological facts

Basalt is the most abundant volcanic rock on oceanic crust and commonly forms lava flows, pillow lavas, and volcanic plateaus.

Field identification & locations

Identify it by its dark color, heavy feel, fine texture, and lack of visible large crystals; a streak test is usually gray, and a magnet may show weak attraction if iron-bearing minerals are abundant. Common worldwide in volcanic and alluvial settings.