Rock Identifier
Tumbled tan stone, likely calcite or limestone (Calcite (CaCO₃), possibly microcrystalline limestone) — mineral
mineral

Tumbled tan stone, likely calcite or limestone

Calcite (CaCO₃), possibly microcrystalline limestone

AI-generated identification · may be incorrect

Pale tan, opaque, dull to weakly waxy luster, and rounded from tumbling; calcite has Mohs hardness 3, rhombohedral cleavage, and specific gravity about 2.71. The image alone cannot confirm composition or distinguish it from similar soft carbonate rocks.

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Physical properties

Pale tan, opaque, dull to weakly waxy luster, and rounded from tumbling; calcite has Mohs hardness 3, rhombohedral cleavage, and specific gravity about 2.71. The image alone cannot confirm composition or distinguish it from similar soft carbonate rocks.

Formation & geological history

Carbonate minerals form by precipitation from groundwater or seawater, biological accumulation, or alteration of limestone; ages may range from modern to hundreds of millions of years. The specimen has been human-shaped or tumbled.

Uses & applications

Common calcite and limestone are used for cement, aggregate, soil conditioning, and building stone; attractive pieces may be sold as inexpensive decorative specimens.

Geological facts

Calcite effervesces visibly with dilute hydrochloric acid, while dolomite reacts weakly unless powdered. A steel nail can scratch it, helping distinguish it from harder quartz.

Field identification & locations

Likely sources include sedimentary carbonate regions worldwide, especially Mexico, the United States, Europe, and North Africa. Test an inconspicuous spot with vinegar or acid, observe cleavage, and compare hardness; identification remains provisional without testing.