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The Transhimalaya was described by the Columbia Lippincott Gazetteer in 1952 as an "ill-defined mountain area" with "no marked crest line or central alignment and no division by rivers." On more-modern maps the Kailas Range (Gangdise or Kang-to-sé Shan) in the west is shown as distinct from the Nyenchen Tanglha range in the east. [4]
Accordingly K2 is only in the table below for reference and not shown on the map on this page. The interactive map on this page ranks Himalayan peaks above 7,500 m (24,600 ft) and is more inclusive. A peak has a different definition to a mountain and different authorities may use different definitions of either.
The Alpide belt or Alpine-Himalayan orogenic belt, [1] or more recently and rarely the Tethyan orogenic belt, is a seismic and orogenic belt that includes an array of mountain ranges extending for more than 15,000 kilometres (9,300 mi) along the southern margin of Eurasia, stretching from Java and Sumatra, through the Indochinese Peninsula, the Himalayas and Transhimalayas, the mountains of ...
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.
Some couples such as Denmark , Netherlands , Spain (Canary Islands) and Portugal (Azores Islands) have part of their territory and their high points outside of Europe; their non-European high points are mentioned in the Notes. For more details about Serbian and Kosovan highest points and ranks, see list of mountains in Kosovo.
Physiographic world map with mountain ranges and highland areas in brown, pink, and gray. This is a list of mountain ranges on Earth and a few other astronomical bodies.First, the highest and longest mountain ranges on Earth are listed, followed by more comprehensive alphabetical lists organized by continent.
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.
The Himalayas consists of four parallel mountain ranges: the Sivalik Hills on the south; the Lower Himalayas; the Great Himalayas, which is the highest and central range; and the Tibetan Himalayas on the north. The range varies in width from 350 km (220 mi) in the north-west to 150 km (93 mi) in the south-east.