Rock Identifier
Weathered basaltic rock (Fine-grained mafic volcanic rock, likely basalt (composition dominated by plagioclase and pyroxene)) — igneous
igneous

Weathered basaltic rock

Fine-grained mafic volcanic rock, likely basalt (composition dominated by plagioclase and pyroxene)

AI-generated identification · may be incorrect

Dark gray-brown, fine-grained, dull to weakly vitreous luster, with weathering stains and possible vesicles or fractures. Typical hardness is about 6 on the Mohs scale; cleavage is not visible and specific gravity is commonly 2.8–3.0.

Identified More igneous
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Physical properties

Dark gray-brown, fine-grained, dull to weakly vitreous luster, with weathering stains and possible vesicles or fractures. Typical hardness is about 6 on the Mohs scale; cleavage is not visible and specific gravity is commonly 2.8–3.0.

Formation & geological history

Likely formed when mafic lava cooled rapidly at or near Earth’s surface; its precise geological age cannot be determined from the image. Brown coloration reflects surface oxidation and weathering.

Uses & applications

Used as crushed aggregate, road base, riprap, railroad ballast, and dimension stone; unexceptional pieces have little jewelry value.

Geological facts

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

Field identification & locations

Identify by its dense, fine texture, dark mafic color, lack of visible large crystals, and relatively high density; common worldwide, especially volcanic regions and oceanic settings.