Rock Identifier
Banded calcite (likely cave-flowstone or marble fragment) (Calcite, CaCO₃; the visible bands are growth or compositional layers) — mineral
mineral

Banded calcite (likely cave-flowstone or marble fragment)

Calcite, CaCO₃; the visible bands are growth or compositional layers

AI-generated identification · may be incorrect

Pale gray and white with curved bands and a vitreous-to-satin luster; calcite has Mohs hardness 3, trigonal crystal structure, and perfect rhombohedral cleavage. The specimen’s banding and shape are consistent with calcite, though the photo alone cannot confirm its exact origin.

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Physical properties

Pale gray and white with curved bands and a vitreous-to-satin luster; calcite has Mohs hardness 3, trigonal crystal structure, and perfect rhombohedral cleavage. The specimen’s banding and shape are consistent with calcite, though the photo alone cannot confirm its exact origin.

Formation & geological history

Calcite precipitates from mineral-rich water in caves, springs, and veins; marble forms when limestone recrystallizes during metamorphism. The specimen’s age and formation setting cannot be determined from the image.

Uses & applications

Calcite is used in cement, lime, fillers, and optical instruments; attractive banded pieces are collected or used decoratively.

Geological facts

Calcite reacts with dilute acid, producing visible fizzing; this is a useful field test, but avoid testing valuable specimens.

Field identification & locations

Look for hardness near 3, rhombohedral cleavage, and acid reaction. Banded calcite occurs worldwide, including in caves and hydrothermal veins.