Rock Identifier
Likely basalt or weathered mafic rock (Basalt; predominantly plagioclase feldspar and pyroxene, possibly olivine) — igneous
igneous

Likely basalt or weathered mafic rock

Basalt; predominantly plagioclase feldspar and pyroxene, possibly olivine

AI-generated identification · may be incorrect

Dark gray to black, fine- to medium-grained, dull to weakly vitreous luster, with rounded weathered surfaces. Hardness about 5–6 Mohs; typically massive with no obvious cleavage and specific gravity around 2.8–3.1.

Identified More igneous
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Physical properties

Dark gray to black, fine- to medium-grained, dull to weakly vitreous luster, with rounded weathered surfaces. Hardness about 5–6 Mohs; typically massive with no obvious cleavage and specific gravity around 2.8–3.1.

Formation & geological history

Formed when iron- and magnesium-rich lava cooled at or near Earth’s surface, commonly in volcanic flows; age cannot be determined from the photograph and may range from recent to billions of years.

Uses & applications

Used widely as crushed aggregate, road base, riprap, building stone, and occasionally ornamental material. Small ordinary specimens generally have little commercial value.

Geological facts

The lumpy surface may reflect vesicles or weathering, but the image is too blurred to confirm texture or mineral grains. It could also be another dark volcanic rock, such as andesite or gabbro.

Field identification & locations

Common in volcanic regions and oceanic crust, including Iceland, Hawaii, the Pacific Northwest, India, and ocean-floor environments. A fresh broken surface, streak, magnetism, and visible crystals would improve identification; avoid relying on color alone.