Mountain range facts for kids
A mountain range (mountain chain, mountain belt) is a geographic area with many mountains. A 'mountain system' or 'system of mountain ranges' includes geological features that are in the same region as a mountain range.
Mountain ranges usually include highlands or mountain passes and valleys. Individual mountains in the same range do not always have the same geology or petrology. They may be a mix of different orogenic expressions and terrains, for example thrust sheets, uplifted blocks, fold mountains, and volcanic landforms. This results in a variety of rock types.
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Major ranges
Most geologically young mountain ranges on the Earth's land surface are associated with either in the Pacific Ring of Fire or the Alpide Belt. The Pacific Ring of Fire includes the Andes of South America, extends through the North American Cordillera along the Pacific Coast, the Aleutian Range, on through Kamchatka, Japan, Taiwan, the Philippines, Papua New Guinea, to New Zealand. The Andes is 7,000 kilometres (4,350 mi) long and is often described as the world's longest mountain system.
The Alpide belt includes Indonesia and southeast Asia, through the Himalayas, and ends in the Alps. The belt also includes other European and Asian mountain ranges. The Himalayas contain the highest mountains in the world, including Mount Everest, at 8,848 metres (29,029 ft) of elevation.
Mountain ranges outside of these two systems include the Arctic Cordillera, the world's northernmost mountain system. If the definition of a mountain range includes underwater mountains, then the ocean ridges form the longest continuous mountain system on Earth, with a length of 65,000 kilometres (40,400 mi).
Divisions and categories
Many mountain ranges have sub-ranges within them. It can be thought of as a parent-child relationship. For example, the Appalachian Mountains range is the parent of its own ranges, two of which are the White Mountains and the Blue Ridge Mountains. The White Mountains are a child of the Appalachians, and there are also children of the Whites, like the Sandwich Range and the Presidential Range.
Climate
The position of mountains influences climate, such as rain or snow. When air masses move up and over mountains, the air cools producing precipitation (rain or snow). As the air descends on the leeward side, it warms again and is drier, having been stripped of much of its moisture. Often, a rain shadow will occur on the leeward side of a range.
Erosion
Mountain ranges are always being eroded. Erosion is at work while the mountains are being uplifted and long after until the mountains are reduced to low hills and plains. The basins next to an eroding mountain range are filled with sediments which are buried and turned into sedimentary rock.
The early Cenozoic uplift of the Rocky Mountains of Colorado are an example. As the uplift was occurring some 10,000 feet (3,000 m) of mostly Mesozoic sedimentary strata were removed by erosion and spread as sand and clays across the Great Plains to the east. This mass of rock was removed as the range was actively undergoing uplift.
Mountain ranges by height
Name | Continent(s) | Country/ies | Highest point | Altitude (metres above sea level) |
---|---|---|---|---|
Himalayas | Asia | India, Nepal, Bhutan, China, Pakistan | Everest | 8848.86 |
Karakoram (Note 2) | Asia | Pakistan, China, India | K2 | 8611 |
Hindu Kush (Note 2) | Asia | Afghanistan, Pakistan | Tirich Mir | 7708 |
Pamirs (Note 2) | Asia | Tajikistan, Kyrgyzstan, China, Afghanistan, Pakistan | Kongur Tagh (Note 1) | 7649 |
Hengduan Mountains (Note 2) | Asia | China, Myanmar | Mount Gongga | 7556 |
Tian Shan | Asia | China, Kyrgyzstan, Kazakhstan, Uzbekistan; | Jengish Chokusu | 7439 |
Kunlun | Asia | China | Liushi Shan | 7167 |
Transhimalaya (Note 2) | Asia | China | Mount Nyenchen Tanglha | 7162 |
Andes | South America | Argentina, Chile, Peru, Bolivia, Ecuador, Colombia, Venezuela | Aconcagua | 6961 |
Hindu Raj | Asia | Pakistan | Koyo Zom | 6873 |
Alaska Range | North America | United States | Denali | 6194 |
Saint Elias Mountains | North America | United States, Canada | Mount Logan | 5959 |
Caucasus Mountains | Europe and Asia | Georgia, Russia, Azerbaijan | Mount Elbrus | 5642 |
Note 1: A peak included in the "Eastern Pamirs" more often than in the Kunlun Mountains, as Kongur Tagh and the Kunlun range are separated by the large Yarkand River valley; no valley of such significance separates the Pamirs and Kongur Tagh, just political boundaries.
Note 2: Part of Hindu Kush-Himalayas region
All of the Asian ranges above have been formed in part over the past 35 to 55 million years by the collision between the Indian Plate and Eurasian Plate. The Indian Plate is still particularly mobile and these mountain ranges continue to rise in elevation every year and this page may need to be updated in a few years; of these the Himalayas are rising most quickly; the Kashmir and Pamirs region to the north of the Indian subcontinent is the point of confluence of these mountains which encircle the Tibetan Plateau.
Related pages
Images for kids
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The Andes, the world's longest mountain range on the surface of the Earth, have a dramatic impact on the climate of South America
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Montes Apenninus on the Moon was formed by an impact event.
See also
In Spanish: Cordillera para niños
- Cordillera
- Drainage divide
- List of mountain types
- Lists of mountains
- Massif
- Mountain chain
- Mountain formation
- Ridge – an elongated mountain or hill, or chain of them