
metamorphic
Banded calcite (banded limestone/marble fragment)
Calcite, CaCO₃; likely banded calcitic marble or recrystallized limestone
AI-generated identification · may be incorrectCream, tan, and brown flowing bands; waxy to dull luster; hardness about 3 Mohs, with strong effervescence in dilute hydrochloric acid. Calcite is trigonal and has excellent rhombohedral cleavage; the specimen appears polished or naturally smoothed.
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Physical properties
Cream, tan, and brown flowing bands; waxy to dull luster; hardness about 3 Mohs, with strong effervescence in dilute hydrochloric acid. Calcite is trigonal and has excellent rhombohedral cleavage; the specimen appears polished or naturally smoothed.
Formation & geological history
Formed from carbonate sediment that was lithified and variably recrystallized during metamorphism, producing the banding; age cannot be determined from the photograph. Similar material occurs in marbles and travertine-related deposits.
Uses & applications
Used as decorative stone, carvings, countertops, aggregate, and cement feedstock; attractive pieces are sold as lapidary specimens.
Geological facts
The layered appearance may reflect original sedimentary bedding, impurities, or mineral-rich fluids rather than true crystal banding.
Field identification & locations
Identify it by its low hardness, pale color, rhombohedral cleavage, and acid fizz; a steel knife can scratch it. Common sources include Italy, Turkey, Mexico, Pakistan, and the United States.
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