Rock Identifier
Weathered basalt (likely) (Basalt; fine-grained mafic volcanic rock, mainly plagioclase and pyroxene with possible olivine) — igneous
igneous

Weathered basalt (likely)

Basalt; fine-grained mafic volcanic rock, mainly plagioclase and pyroxene with possible olivine

AI-generated identification · may be incorrect

Dark gray-green, dull to faintly matte, fine-grained and rounded by weathering; typically Mohs 5–6, with no visible cleavage and an interlocking crystalline texture. The green tint may reflect chlorite or other alteration minerals.

Identified More igneous
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Physical properties

Dark gray-green, dull to faintly matte, fine-grained and rounded by weathering; typically Mohs 5–6, with no visible cleavage and an interlocking crystalline texture. The green tint may reflect chlorite or other alteration minerals.

Formation & geological history

Formed when basaltic lava cooled rapidly at or near Earth’s surface, commonly during the Cenozoic or older volcanic episodes; the specimen’s rounded shape indicates erosion or stream/beach transport.

Uses & applications

Used as crushed aggregate, road base, riprap, concrete material, and occasionally decorative stone; ordinary hand specimens have minimal commercial value.

Geological facts

Basalt is the most widespread volcanic rock on Earth and forms much of the oceanic crust, including seafloor pillow lavas.

Field identification & locations

Identify by its dense, fine texture, dark color, and lack of obvious quartz or large crystals; common in volcanic regions, river gravels, and glacial deposits. Exact identification would benefit from a fresh surface, streak, magnetism, and density tests.