Travertine Stone Detail
Travertine is a form of limestone deposited by mineral springs, especially hot springs. Travertine often has a fibrous or concentric appearance and exists in white, tan, and cream-colored varieties. It is formed by a process of rapid precipitation of calcium carbonate, often at the mouth of a hot spring or in a limestone cave. In the latter, it can form stalactites, stalagmites, and other speleothems. It is frequently used in Italy and elsewhere as a building material.
Travertine is a terrestrial sedimentary rock, formed by the precipitation of carbonate minerals from solution in ground and surface waters, and/or geothermally heated hot-springs.Similar (but softer and extremely porous) deposits formed from ambient-temperature water are known as tufa.
In North East Sulawesi, Indonesia is the Wawolesea Karst. A notable feature of this area is a pond several meters from the beach which is formed by a salty, hot water fountain extant since the Neogene period.
Travertine Stone
Travertine Stone
Travertine Stone
Travertine Stone
Travertine Stone
Travertine Stone
Travertine Stone
Travertine Stone
Travertine Stone
Travertine Stone
Travertine Stone
Travertine Stone
Travertine Stone
Travertine Stone
Travertine Stone
Travertine Stone
Travertine Stone
Travertine Stone
Travertine Stone
Travertine is a form of limestone deposited by mineral springs, especially hot springs. Travertine often has a fibrous or concentric appearance and exists in white, tan, and cream-colored varieties. It is formed by a process of rapid precipitation of calcium carbonate, often at the mouth of a hot spring or in a limestone cave. In the latter, it can form stalactites, stalagmites, and other speleothems. It is frequently used in Italy and elsewhere as a building material.
Travertine is a terrestrial sedimentary rock, formed by the precipitation of carbonate minerals from solution in ground and surface waters, and/or geothermally heated hot-springs.Similar (but softer and extremely porous) deposits formed from ambient-temperature water are known as tufa.
In North East Sulawesi, Indonesia is the Wawolesea Karst. A notable feature of this area is a pond several meters from the beach which is formed by a salty, hot water fountain extant since the Neogene period.
Travertine Stone
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