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Mountain range facts for kids

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Himalayas
The Himalayas, the highest mountain range on Earth, seen from space

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.

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.

World Distribution of Mid-Oceanic Ridges
The mid-ocean ridges, the world's longest mountain range (chain)

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

Aerial photo of the Andes
The Andes, the world's longest mountain range on the surface of a continent, seen from the air.

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.

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Kids robot.svg In Spanish: Cordillera para niños

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