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The Dolomites (Italy) are a UNESCO World Heritage Site.. The Alps (/ æ l p s /) [a] are one of the highest and most extensive mountain ranges in Europe, [b] [2] stretching approximately 1,200 km (750 mi) across eight Alpine countries (from west to east): Monaco, France, Switzerland, Italy, Liechtenstein, Germany, Austria and Slovenia.
the Penninic system: mainly Central Alps (Engadine and "Tauern window") and Flysch Alps, the Austroalpine system: Northern Limestone Alps, Graywacke-Schist zone, Central Crystalline, the Southern Alps (Southern Limestone Alps and other chains south of the Periadriatic Seam) south of a huge geologic fault ("alpine-dinaric seam") parts of the ...
Main chain of the Alps. The main chain of the Alps, also called the Alpine divide is the central line of mountains that forms the drainage divide of the range. Main chains of mountain ranges are traditionally designated in this way, and generally include the highest peaks of a range.
The Alps form part of a Cenozoic orogenic belt of mountain chains, called the Alpide belt, that stretches through southern Europe and Asia from the Atlantic all the way to the Himalayas. This belt of mountain chains was formed during the Alpine orogeny. A gap in these mountain chains in central Europe separates the Alps from the Carpathians to
The Alpine biogeographic region of Europe includes the Alps in France, Italy, Germany, Austria, Slovenia, Switzerland and Monaco, the Apennines in Italy, the Pyrenees between Spain and France, the Scandes in Sweden, Finland and Norway and the Carpathians in Slovakia, Poland, Romania and Ukraine. [1]
This page tabulates only the most prominent mountains of the Alps, selected for having a topographic prominence of at least 300 metres (980 ft), all exceeding 3,000 metres (9,800 ft) in height. Although the list contains 537 summits, some significant alpine mountains are necessarily excluded for failing to meet the stringent prominence criterion.
For a list by height, see the list of mountains of the Alps. By descending to 1,500 m of prominence, this list includes all the Ultras of the Alps. Some famous peaks, such as the Matterhorn and Eiger, are not Ultras because they are connected to higher mountains by high cols and therefore do not achieve enough topographic prominence.
Tectonic map of southern Europe and the Middle East, showing tectonic structures of the western Alpide mountain belt. The Alpine orogeny or Alpide orogeny [dubious – discuss] is an orogenic phase in the Late Mesozoic [1] (Eoalpine) and the current Cenozoic that has formed the mountain ranges of the Alpide belt.