The genesis of this type of carbonate rock begins by accumulations of shells, corals and calcareous algae and in marine and tropical. resort best known are present in the valleys of the Dolomites Cortina d’Ampezzo in the Basin Ampezzo, Auronzo-Misurina in Val d’Ansiei Rocca Pietore Marmolada in the Val-Harness, Selva and Ortisei in Val Gardena, in Dobbiaco, Sesto Pusteria, Castelrotto at the foot of the Dolomites, Canazei and Moena in Val di Fassa, in Falcade Biois Valley, San Martino di Castrozza in Primiero, Arabba in the Valley of Livinallongo, Corvara, La Villa, San Cassiano, Badia Val Badia, Madonna di Campiglio Val Rendena and Forni di Sopra in Friuli Venezia Giulia.
Numerous natural parks protect this special nature and various ad hoc committees were involved in proposing the Dolomites as a World Heritage Site by UNESCO.Marmolada is the highest peak in the Dolomites, with its 3,343 m above sea level, but it should be noted that this training is by no means consists of dolomite, but predominantly white very compact limestones derived from coral reefs, with inserts of volcanic material: therefore, strictly speaking, not part of the Marmolada group.




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