Travertine | Geology | Britannica

Ask the Chatbot Games & Quizzes History & Society Science & Tech Biographies Animals & Nature Geography & Travel Arts & Culture ProCon Money Videos travertine Introduction References & Edit History Related Topics Images travertine Showing the presence of travertine, a CaCO3 precipitate of calcite or aragonite, speleothem (cave formation), in southwestern Virginia, U.S. Travertine terraces Quizzes Basalt sample returned by Apollo 15, from near a long sinous lunar valley called Hadley Rille.  Measured at 3.3 years old. (Bed) Rocks and (Flint) Stones Britannica AI Icon Contents Science Earth Science, Geologic Time & Fossils Earth Sciences CITE verifiedCite While every effort has been made to follow citation style rules, there may be some discrepancies. Please refer to the appropriate style manual or other sources if you have any questions. Select Citation Style MLA APA Chicago Manual of Style Copy Citation Share Share Share to social media Facebook X URL https://www.britannica.com/science/travertine Feedback External Websites Feedback Corrections? Updates? Omissions? Let us know if you have suggestions to improve this article (requires login). Feedback Type Select a type (Required) Factual Correction Spelling/Grammar Correction Link Correction Additional Information Other Your Feedback Submit Feedback Thank you for your feedback

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travertine, dense, banded rock composed of calcite (calcium carbonate, CaCO3). Formed by the evaporation of river and spring waters, it is a variety of limestone that has a light colour and takes a good polish; it is often used for walls and interior decorations in public buildings. Travertine deposits along the Aniene River, near Rome, are several metres thick. In the United States the Mammoth Hot Springs in Yellowstone National Park, Wyoming, are actively depositing travertine. It also occurs in limestone caves in the form of stalactites and stalagmites, as, for example, in Carlsbad Caverns, New Mexico.

This article was most recently revised and updated by Amy Tikkanen.

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