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Satellite image of the Alps, March 2007 Folded rock layers exposed in the Swiss Alps. 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 ...
Pohorje is a young mountain massif and is the southeasternmost part of the Central Alps. [4] It is the only mountain chain in Slovenia made of silicate rock. Its peripheral parts consist of Paleozoic metamorphic rock, and its central parts of igneous rock, particularly granodiorite (known also as the Pohorje tonalite) and dacite. [5]
While smaller groups within the Alps may be easily defined by the passes on either side, defining larger units can be problematic. A traditional divide exists between the Western Alps and the Eastern Alps, which uses the Splügen Pass (Italian: Passo dello Spluga) on the Swiss-Italian border, together with the Rhine to the north and Lake Como in the south as the defining features.
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.
Significant volcanic activity took place in the Lower Paleozoic in the Malé Karpaty Mts., where the relicts are seen in the rock of the Pernek Group with typical basic volcanism. [14] Large volumes of volcanic rock, considered a product of stratovolcanos, significantly changed by metamorphism, are present in the Gemeric. Basic volcanism is ...
Tilted layers of sedimentary rock in the Rolle Pass in the Dolomites, Trentino. The geology of Italy includes mountain ranges such as the Alps and the Apennines formed from the uplift of igneous and primarily marine sedimentary rocks all formed since the Paleozoic. [1] Some active volcanoes are located in Insular Italy.
The mountain's current shape is the result of cirque erosion due to multiple glaciers diverging from the peak, such as the Matterhorn Glacier at the base of the north face. Sometimes referred to as the Mountain of Mountains (German: Berg der Berge), [5] it has become an indelible emblem of the Alps in general. Since the end of the 19th century ...
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.