Rock Identifier
Likely basaltic rock fragment (Fine-grained mafic igneous rock, probably basalt (plagioclase–pyroxene ± olivine)) — igneous
igneous

Likely basaltic rock fragment

Fine-grained mafic igneous rock, probably basalt (plagioclase–pyroxene ± olivine)

AI-generated identification · may be incorrect

Dark gray to black, fine-grained, dull to subvitreous luster, massive texture, and no visible cleavage; estimated Mohs hardness 5–6 and specific gravity about 2.8–3.1. The irregular angular form may be a broken or weathered fragment.

Identified More igneous
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Physical properties

Dark gray to black, fine-grained, dull to subvitreous luster, massive texture, and no visible cleavage; estimated Mohs hardness 5–6 and specific gravity about 2.8–3.1. The irregular angular form may be a broken or weathered fragment.

Formation & geological history

Basalt forms when iron- and magnesium-rich lava rapidly cools at or near Earth’s surface, commonly in volcanic fields and oceanic crust. Its exact age cannot be determined from the photograph; basalt ranges from ancient to recent.

Uses & applications

Used as crushed aggregate, road base, riprap, railroad ballast, and occasionally dimension stone; attractive polished pieces may be collected but this fragment has little commercial value.

Geological facts

Basalt is the most abundant volcanic rock and makes up much of the ocean floor. A small metallic-looking fleck could be pyrite, magnetite, or mica, but it is not diagnostic visually.

Field identification & locations

Look for a uniformly fine texture, dark color, heavy feel, and possible tiny vesicles; test with a steel nail and inspect a fresh surface. Common worldwide, especially volcanic regions and river gravels.