Rock Identifier
Black granite (likely polished gabbro or diabase) (Granitoid rock dominated by feldspar, quartz, and dark mafic minerals; exact identification requires testing) — igneous
igneous

Black granite (likely polished gabbro or diabase)

Granitoid rock dominated by feldspar, quartz, and dark mafic minerals; exact identification requires testing

AI-generated identification · may be incorrect

Coarse-grained, dark gray to black with reflective interlocking crystals and polished luster; typical hardness about 6–7 Mohs, no strong cleavage as a rock, and specific gravity roughly 2.7–3.1.

Identified More igneous
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Physical properties

Coarse-grained, dark gray to black with reflective interlocking crystals and polished luster; typical hardness about 6–7 Mohs, no strong cleavage as a rock, and specific gravity roughly 2.7–3.1.

Formation & geological history

Slow cooling of silica-rich to mafic magma produced visible crystals, generally during Precambrian to Phanerozoic intrusive activity. The glossy surface indicates cutting and polishing.

Uses & applications

Widely used for countertops, flooring, monuments, tiles, and architectural stone; attractive slabs have moderate decorative value rather than gemstone value.

Geological facts

Commercially labeled “black granite” may technically be gabbro, norite, diabase, or anorthosite rather than true granite. The image shows reflective platy minerals, possibly biotite or amphibole, mixed with feldspar.

Field identification & locations

Identify by visible interlocking crystals, great durability, and lack of fizz in dilute acid; a streak, hardness, and thin-section test can separate gabbro from granite. Common sources include India, Brazil, Scandinavia, South Africa, and Zimbabwe.