Rock Identifier
Polished black-and-white stone, likely gabbro or diorite (Gabbro/diorite; chiefly plagioclase feldspar, pyroxene, and possibly amphibole or biotite) — igneous
igneous

Polished black-and-white stone, likely gabbro or diorite

Gabbro/diorite; chiefly plagioclase feldspar, pyroxene, and possibly amphibole or biotite

AI-generated identification · may be incorrect

Dark greenish-black, polished, medium- to coarse-grained with irregular pale mineral patches; likely Mohs 6–7, vitreous to dull luster, no obvious cleavage on the rounded surface, and specific gravity about 2.8–3.1.

Identified More igneous
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Physical properties

Dark greenish-black, polished, medium- to coarse-grained with irregular pale mineral patches; likely Mohs 6–7, vitreous to dull luster, no obvious cleavage on the rounded surface, and specific gravity about 2.8–3.1.

Formation & geological history

A slowly cooled intrusive igneous rock formed when magma crystallized deep within Earth, generally during Precambrian to younger continental crust formation; the specimen has been tumbled or polished.

Uses & applications

Used as decorative stone, countertops, architectural aggregate, landscaping material, and an inexpensive lapidary or worry stone.

Geological facts

Gabbro is the coarse-grained intrusive equivalent of basalt; diorite is compositionally intermediate and commonly has contrasting black-and-white “salt-and-pepper” coloration.

Field identification & locations

Identify it by its dense black-and-white crystalline texture, lack of layering, and inability to scratch it with a steel knife easily; common sources include India, Brazil, Scandinavia, and North America. Exact identification requires a fresh surface or thin-section analysis.