Travertine and limestone are both sedimentary rocks composed of grains; however, most grains in limestone are skeletal fragments of marine organisms such as coral. Travertine is a banded, compact variety of limestone formed along streams, particularly where there are waterfalls, and around hot or cold springs.
There are far more geological similarities than differences between travertine and limestone. Both are formed by the settling of plants, animals, sea shells, sand, and mud on the sea beds. As millions of years pass, this sediment continues to settle and the weight of additional settlement causes the limestone and travertine to compress and harden. This process creates the fossils frequently found in both of these stones. If, at this stage, hot water rich in carbon dioxide from hot springs percolates through the limestone and dissolves some of the stone leaving behind inclusions, holes or voids, travertine is formed. As the water resurfaces, the sudden drop in pressure and change in temperature causes the water to release carbon dioxide gas. The calcium carbonate or limestone then re-crystallizes as travertine.
Limestone is a good building material, especially for cathedrals, since you can carve it easily. It does get eroded by being dissolved slowly by rain, especially acid rain. Limestone, like all natural stone should be sealed and can be maintain by a neutral pH cleaner, you never want to use anything acidic on natural stone surfaces as they can ruin the surface of natural stone.
Stop by Carpets Plus and test your skills at distinguishing these two products, and check out our inexpensive cleaners.
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