
sedimentary
Travertine
Travertine (form of massive calcium carbonate, CaCO3)
AI-generated identification · may be incorrectHardness: 3-4 (Mohs scale); Color: Tan, cream, beige, or yellowish; Luster: Dull to pearly; Crystal structure: Trigonal (microcrystalline); Cleavage: Perfect in three directions (in calcite crystals); Specific gravity: 2.71
- Hardness
- 3-4 (Mohs scale)
- Color
- Tan, cream, beige, or yellowish
- Luster
- Dull to pearly
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Physical properties
Hardness: 3-4 (Mohs scale); Color: Tan, cream, beige, or yellowish; Luster: Dull to pearly; Crystal structure: Trigonal (microcrystalline); Cleavage: Perfect in three directions (in calcite crystals); Specific gravity: 2.71
Formation & geological history
Formed by the rapid precipitation of calcium carbonate, often at the mouth of a hot spring or in a limestone cave. Over geological time, pressure and mineral-rich waters create these banded or mottled terrestrial sedimentary deposits.
Uses & applications
Extensively used as a building material for flooring, wall cladding, and bathroom surfaces. It is also used for garden paths, decorative furniture, and statuary.
Geological facts
Travertine is one of the most frequently used stones in modern architecture. The Colosseum in Rome is the largest building in the world constructed largely of travertine.
Field identification & locations
Identify by its characteristic porous texture (often filled with resin in tiles), light earth-toned colors, and susceptibility to acid (it will fizz with dilute HCl). Commonly found in Italy, Turkey, and Yellowstone National Park.
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