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Travertine is a sedimentary rock formed by the chemical precipitation of calcium carbonate minerals from fresh water, [4] typically in springs, rivers, and lakes; [5] [6] that is, from surface and ground waters. [7]
Tufa columns at Mono Lake, California. Tufa is a variety of limestone formed when carbonate minerals precipitate out of water in unheated rivers or lakes. Geothermally heated hot springs sometimes produce similar (but less porous) carbonate deposits, which are known as travertine or thermogene travertine.
Phosphorite – Sedimentary rock containing large amounts of phosphate minerals – A non-detrital sedimentary rock that contains high amounts of phosphate minerals; Sandstone – Type of sedimentary rock; Shale – Fine-grained, clastic sedimentary rock; Siltstone – Sedimentary rock which has a grain size in the silt range
Coquina – Sedimentary rock that is composed mostly of fragments of shells; Coral rag – Limestone composed of ancient coral reef material; Chalk – Soft carbonate rock; Fossiliferous limestone – Limestone containing fossils; Lithographic limestone – Type of limestone with hard fine grain; Marble – Metamorphic limestone
Travertine terrace formations. Pamukkale's terraces are made of travertine, a sedimentary rock deposited by mineral water from the hot springs. [1] In this area, there are 17 hot springs with temperatures ranging from 35 °C (95 °F) to 100 °C (212 °F).
This rock was part of the Roman aqueduct of Mons/Montauroux–Fréjus and was most probably derived from the karst area in the vicinity. In geology, lamination (from Latin lāmina 'thin layer') is a small-scale sequence of fine layers (pl.: laminae; sg.: lamina) that occurs in sedimentary rocks.
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