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The Dolomites (Italian: Dolomiti [doloˈmiːti]), [1] also known as the Dolomite Mountains, Dolomite Alps or Dolomitic Alps, are a mountain range in northeastern Italy. They form part of the Southern Limestone Alps and extend from the River Adige in the west to the Piave Valley ( Pieve di Cadore ) in the east.
The Friulian Dolomites (Italian: Dolomiti Friulane), also known as Dolomiti d'Oltre Piave ("Dolomites beyond the Piave") are a mountain range in the Carnic and Gailtal Alps. They are located in northeastern Veneto and Friuli-Venezia Giulia, in northeastern Italy. They are the easternmost dolomitic group.
The dissolution of the Western Roman Empire brings in Italy the creation of many barbarian kingdoms, as, for example, Kingdom of the Lombards, that evolved over the centuries in feudal lordships. During this period were built the medieval villages with fortified walls and towers.
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The Marmolada is an ultra-prominent peak (Ultra), known as the "Queen of the Dolomites". In 2009, as part of the Dolomites, the Marmolada massif was named a UNESCO World Heritage site. [2] [3] The largest glacier in the Dolomites, the Marmolada Glacier, is located on the northern face of the mountain. [4]
It is located in the western part of the Dolomites and has an elevation between 1,680 meters (5,510 ft) and 2,350 meters (7,710 ft); it extends for 52 square kilometers (20 sq mi) between Val Gardena to the north, the Sassolungo Group to the northeast, and the Sciliar massif to the southeast, which with its unmistakable profile is one of the best-known symbols of all the Dolomites.
The Ampezzo Dolomites Natural Park (Italian: Parco naturale delle Dolomiti d'Ampezzo) is a nature reserve in Veneto, Italy.Established in 1990, it is entirely located in the territory of Cortina d’Ampezzo, in the Province of Belluno, and encompasses some of the most famous Dolomitic groups, such as the Tofane, Monte Cristallo, the Croda Rossa d'Ampezzo, Lagazuoi, Pomagagnon and Col Bechei.
The region was formed in the early Triassic period (about 230 million years ago) as a coral reef in a shallow tropical sea. Hard limestone was able to form on the outside of the reef, whilst the rock in the interior remained brittle and was quickly eroded away following the uplifting of the range.