Rock Identifier
Translucent calcite-rich rock, possibly calcite vein or marble (Calcite (CaCO₃), likely in a calcite-rich aggregate; exact rock identification is uncertain from the photo) — metamorphic
metamorphic

Translucent calcite-rich rock, possibly calcite vein or marble

Calcite (CaCO₃), likely in a calcite-rich aggregate; exact rock identification is uncertain from the photo

AI-generated identification · may be incorrect

Cream to tan, translucent where illuminated, with a dull-to-vitreous luster and irregular fracture. Calcite has Mohs hardness 3, trigonal crystal structure, and three-direction rhombohedral cleavage; the image does not show diagnostic crystal faces or a reliable cleavage surface.

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Physical properties

Cream to tan, translucent where illuminated, with a dull-to-vitreous luster and irregular fracture. Calcite has Mohs hardness 3, trigonal crystal structure, and three-direction rhombohedral cleavage; the image does not show diagnostic crystal faces or a reliable cleavage surface.

Formation & geological history

Calcite commonly precipitates from groundwater or hydrothermal fluids in fractures, and also forms marble when limestone recrystallizes during metamorphism. The specimen’s age and precise formation setting cannot be determined visually.

Uses & applications

Calcite is used in cement and lime, construction stone, and as a mineral specimen; clear, well-formed crystals may be collected or cut, though this rough piece does not show gem-quality features.

Geological facts

Calcite effervesces vigorously in dilute hydrochloric acid and can be scratched with a copper coin. The bright center appears to be transmitted or reflected light, so it does not establish that the whole piece is transparent.

Field identification & locations

A scratch test and a drop of dilute acid on a hidden spot can help distinguish calcite from harder quartz; avoid acid if preserving the specimen. The reported Oman-region location is compatible with carbonate rocks, but does not identify this specimen conclusively.