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

Likely weathered mafic rock (basalt or gabbro)

Basalt–gabbroic rock; chiefly plagioclase feldspar, pyroxene, and possibly olivine

AI-generated identification · may be incorrect

Dark gray to black, coarse-to-fine crystalline texture, dull to locally vitreous luster, irregular fractures, and apparent vesicles or weathering cavities; hardness about 5–6 and specific gravity roughly 2.8–3.1.

Identified More igneous
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Physical properties

Dark gray to black, coarse-to-fine crystalline texture, dull to locally vitreous luster, irregular fractures, and apparent vesicles or weathering cavities; hardness about 5–6 and specific gravity roughly 2.8–3.1.

Formation & geological history

Formed from mafic magma cooling at or near Earth’s surface (basalt) or underground (gabbro), generally in volcanic or oceanic-crust settings; the specimen’s exact age and origin cannot be determined from the image.

Uses & applications

Common basalt is used as crushed aggregate, roadstone, riprap, and building stone; attractive polished pieces may be sold as decorative specimens, but this example appears low-grade.

Geological facts

Its dark color reflects iron- and magnesium-rich minerals. Metallic-looking highlights may be fresh pyroxene, mica, or weathered surfaces rather than metal ore.

Field identification & locations

Test for a glassy versus granular texture, check for magnetic response, and use a streak, hardness, and thin-section test for confirmation; common worldwide, especially volcanic regions and oceanic terrains.