
sedimentary
Travertine / Tufa
Calcium Carbonate (CaCO3)
Hardness: 3 on Mohs scale; Color: Tan, brownish-red, cream, beige; Luster: Vitreous to dull/earthy; Structure: Trigonal (microcrystalline calcite); Cleavage: Perfect rhombohedral in calcite grains, but usually porous and irregular bulk structure.
- Hardness
- 3 on Mohs scale
- Color
- Tan, brownish-red, cream, beige
- Luster
- Vitreous to dull/earthy
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Physical properties
Hardness: 3 on Mohs scale; Color: Tan, brownish-red, cream, beige; Luster: Vitreous to dull/earthy; Structure: Trigonal (microcrystalline calcite); Cleavage: Perfect rhombohedral in calcite grains, but usually porous and irregular bulk structure.
Formation & geological history
Forms through the rapid precipitation of calcium carbonate from solution, often around geothermal hot springs, limestone caves, or alkaline lake beds. It frequently encrusts organic matter, leaving porous, spongy textures.
Uses & applications
Widely used as a decorative building stone, floor tiling, wall cladding, landscape rock, and as educational geological samples.
Geological facts
Famous structures like the Colosseum in Rome were built largely from travertine. Tufa deposits often preserve delicate plant fossils and leaf imprints coated in calcite precipitation.
Field identification & locations
Recognized by its porous, pitted texture and effervescent reaction to dilute hydrochloric acid. It can be found in limestone-rich areas and near historic or active hydrothermal vents.
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