Rock Identifier
Black-and-white veined stone, likely marble or calcite-veined metamorphic rock (Probable calcite marble: predominantly recrystallized calcite (CaCO₃) with dark graphite-, mica-, or amphibole-rich minerals) — metamorphic
metamorphic

Black-and-white veined stone, likely marble or calcite-veined metamorphic rock

Probable calcite marble: predominantly recrystallized calcite (CaCO₃) with dark graphite-, mica-, or amphibole-rich minerals

AI-generated identification · may be incorrect

Dark gray to black, fine- to medium-grained, with white calcite veins and a glassy-to-dull luster on fractured surfaces; calcite has Mohs hardness 3 and effervesces in dilute hydrochloric acid. The specimen appears massive rather than visibly crystalline, and its exact identification cannot be certain from an image alo…

Identified More metamorphic
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Physical properties

Dark gray to black, fine- to medium-grained, with white calcite veins and a glassy-to-dull luster on fractured surfaces; calcite has Mohs hardness 3 and effervesces in dilute hydrochloric acid. The specimen appears massive rather than visibly crystalline, and its exact identification cannot be certain from an image alone.

Formation & geological history

Likely formed when carbonate-rich sedimentary rock was metamorphosed, recrystallizing into marble; white veins formed when hot, carbonate-bearing fluids filled fractures. Age depends on locality and cannot be determined visually.

Uses & applications

Used as ornamental or dimension stone, aggregate, carvings, and lapidary material; attractive polished pieces may be used in décor or jewelry.

Geological facts

The strong contrast between dark host rock and white carbonate veining is characteristic of decorative marble and related calcite-rich rocks.

Field identification & locations

Test a fresh surface with dilute HCl, check for calcite softness, and inspect a thin section or streak; common sources include Italy, Greece, Turkey, India, and many metamorphic belts worldwide.