
sedimentary
Travertine (likely polished limestone)
Calcite-rich carbonate rock; predominantly CaCO₃
AI-generated identification · may be incorrectTypically cream to tan, porous or subtly banded, with a dull to satin polish; calcite has Mohs hardness 3, rhombohedral cleavage, and specific gravity around 2.7. The visible coin provides scale; the surface appears to be a polished slab or tile.
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Physical properties
Typically cream to tan, porous or subtly banded, with a dull to satin polish; calcite has Mohs hardness 3, rhombohedral cleavage, and specific gravity around 2.7. The visible coin provides scale; the surface appears to be a polished slab or tile.
Formation & geological history
Forms by precipitation of calcium carbonate from mineral springs, caves, or groundwater, commonly during the Quaternary and older Cenozoic. It may contain fossil traces, voids, and secondary calcite veins.
Uses & applications
Widely used for flooring, countertops, wall cladding, monuments, and decorative stone; lower-grade pieces are common architectural materials rather than collector specimens.
Geological facts
Travertine is a chemically deposited limestone and differs from dense marble by its frequent pores and earthy banding. Acid, including vinegar, causes visible fizzing on exposed calcite.
Field identification & locations
Identify by its tan color, calcite reaction to dilute hydrochloric acid, softness, and pores or layered texture; common sources include Italy, Turkey, Mexico, and the United States. This image alone cannot distinguish travertine confidently from other polished limestone.
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