Mountain range

Geographic area containing several geologically related mountains

For financial options, see Mountain range (options).

File:Himalayas.jpg

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

A mountain range or hill range is a series of mountains or hills ranged in a line and connected by high ground. A mountain system or mountain belt is a group of mountain ranges with similarity in form, structure, and alignment that have arisen from the same cause, usually an orogeny.[1] Mountain ranges are formed by a variety of geological processes, but most of the significant ones on Earth are the result of plate tectonics. Mountain ranges are also found on many planetary mass objects in the Solar System and are likely a feature of most terrestrial planets.

Mountain ranges are usually segmented by highlands or mountain passes and valleys. Individual mountains within the same mountain range do not necessarily have the same geologic structure or petrology. They may be a mix of different orogenic expressions and terranes, for example thrust sheets, uplifted blocks, fold mountains, and volcanic landforms resulting in a variety of rock types.

## Contents

* 1 Major ranges
* 2 Climate
* 3 Erosion
* 4 Extraterrestrial "Montes"
* 5 See also
* 6 References
* 7 External links

## Major ranges[edit | edit source]

File:World Distribution of Mid-Oceanic Ridges.gif

The Ocean Ridge, the world's longest mountain range (chain)

Most geologically young mountain ranges on the Earth's land surface are associated with either 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.[2] The Andes is 7,000 kilometres (4,350 mi) long and is often considered the world's longest mountain system.[3]

The Alpide belt includes Indonesia and Southeast Asia, through the Himalaya, Caucasus Mountains, Balkan Mountains fold mountain range, the Alps, and ends in the Spanish mountains and the Atlas Mountains.[4] The belt also includes other European and Asian mountain ranges. The Himalayas contain the highest mountains in the world, including Mount Everest, which is 8,848 metres (29,029 ft) high and traverses the border between China and Nepal.[5]

Mountain ranges outside these two systems include the Arctic Cordillera, the Urals, the Appalachians, the Scandinavian Mountains, the Great Dividing Range, the Altai Mountains and the Hijaz Mountains. If the definition of a mountain range is stretched to include underwater mountains, then the Ocean Ridges form the longest continuous mountain system on Earth, with a length of 65,000 kilometres (40,400 mi).[6]

## Climate[edit | edit source]

The Andes, the world's longest mountain range on the surface of the Earth, have a dramatic impact on the climate of South America

The position of mountain ranges influences climate, such as rain or snow. When air masses move up and over mountains, the air cools producing orographic precipitation (rain or snow). As the air descends on the leeward side, it warms again (following the adiabatic lapse rate) and is drier, having been stripped of much of its moisture. Often, a rain shadow will affect the leeward side of a range.[7] As a consequence, large mountain ranges, such as the Andes, compartmentalize continents into distinct climate regions.

## Erosion[edit | edit source]

Mountain ranges are constantly subjected to erosional forces which work to tear them down. The basins adjacent to an eroding mountain range are then filled with sediments that are buried and turned into sedimentary rock. Erosion is at work while the mountains are being uplifted until the mountains are reduced to low hills and plains.

The early Cenozoic uplift of the Rocky Mountains of Colorado provides an example. As the uplift was occurring some 10,000 feet (3,000 m) of mostly Mesozoic sedimentary strata were removed by erosion over the core of the mountain range and spread as sand and clays across the Great Plains to the east.[8] This mass of rock was removed as the range was actively undergoing uplift. The removal of such a mass from the core of the range most likely caused further uplift as the region adjusted isostatically in response to the removed weight.

Rivers are traditionally believed to be the principal cause of mountain range erosion, by cutting into bedrock and transporting sediment. Computer simulation has shown that as mountain belts change from tectonically active to inactive, the rate of erosion drops because there are fewer abrasive particles in the water and fewer landslides.[9]

## Extraterrestrial "Montes"[edit | edit source]

Further information: List of tallest mountains in the Solar System

Montes Apenninus on the Moon was formed by an impact event.

Mountains on other planets and natural satellites of the Solar System, including the Moon, are often isolated and formed mainly by processes such as impacts, though there are examples of mountain ranges (or "Montes") somewhat similar to those on Earth. Saturn's moon Titan[10] and Pluto,[11] in particular exhibit large mountain ranges in chains composed mainly of ices rather than rock. Examples include the Mithrim Montes and Doom Mons on Titan, and Tenzing Montes and Hillary Montes on Pluto. Some terrestrial planets other than Earth also exhibit rocky mountain ranges, such as Maxwell Montes on Venus taller than any on Earth[12] and Tartarus Montes on Mars.[13] Jupiter's moon Io has mountain ranges formed from tectonic processes including Boösaule Montes, Dorian Montes, Hi'iaka Montes and Euboea Montes.[14]

## See also[edit | edit source]

* Cordillera
* Drainage divide
* List of mountain ranges
* Category:Lists of mountain ranges
* List of mountain types
* Lists of mountains
* Massif
* Mountain chain
* Mountain formation
* Ridge – an elongated mountain or hill, or chain of them

## References[edit | edit source]

1. ^ "Definition of mountain system". Mindat.org. Hudson Institute of Mineralogy. Retrieved 26 August 2017.
2. ^ Rosenberg, Matt (22 December 2018). "Ring of Fire". ThoughtCo.
3. ^ Thorpe, Edgar (2012). The Pearson General Knowledge Manual. Pearson Education India. p. A-36.
4. ^ Chester, Roy (2008). Furnace of Creation, Cradle of Destruction. AMACOM Div American Mgmt Assn. p. 77. ISBN 9780814409206.
5. ^ "Nepal and China agree on Mount Everest's height". BBC. 8 April 2010.
6. ^ "The mid-ocean ridge is the longest mountain range on Earth". US National Oceanic and Atmospheric Service. 11 Jan 2013.
7. ^ "Orographic precipitation". Encyclopedia Britannica. Retrieved 23 January 2020.
8. ^ "A Guide to the Geology of Rocky Mountain National Park, Colorado". USGS. Archived from the original on 2012-10-24.
9. ^ Egholm, David L.; Knudsen, Mads F.; Sandiford, Mike (2013). "Lifespan of mountain ranges scaled by feedbacks between landslide and erosion by rivers". Nature. 498 (7455): 475–478. Bibcode:2013Natur.498..475E. doi:10.1038/nature12218. PMID 23803847. S2CID 4304803.
10. ^ Mitri, Giuseppe; Bland, Michael T.; Showman, Adam P.; Radebaugh, Jani; Stiles, Bryan; Lopes, Rosaly M. C.; Lunine, Jonathan I.; Pappalardo, Robert T. (2010). "Mountains on Titan: Modeling and observations". Journal of Geophysical Research. 115 (E10): E10002. Bibcode:2010JGRE..11510002M. doi:10.1029/2010JE003592. ISSN 0148-0227. S2CID 12655950.
11. ^ Gipson, Lillian (24 July 2015). "New Horizons Discovers Flowing Ices on Pluto". NASA. Retrieved 25 July 2015.
12. ^ Keep, Myra; Hansen, Vicki L. (1994). "Structural history of Maxwell Montes, Venus: Implications for Venusian mountain belt formation". Journal of Geophysical Research. 99 (E12): 26015. Bibcode:1994JGR....9926015K. doi:10.1029/94JE02636. ISSN 0148-0227. S2CID 53311663.
13. ^ Plescia, J.B. (2003). "Cerberus Fossae, Elysium, Mars: a source for lava and water". Icarus. 164 (1): 79–95. Bibcode:2003Icar..164...79P. doi:10.1016/S0019-1035(03)00139-8. ISSN 0019-1035.
14. ^ Jaeger, W. L. (2003). "Orogenic tectonism on Io". Journal of Geophysical Research. 108 (E8): 12–1–12–18. Bibcode:2003JGRE..108.5093J. doi:10.1029/2002JE001946. ISSN 0148-0227.

## External links[edit | edit source]

* Peakbagger Ranges Home Page
* Bivouac.com

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Earth's landforms

List of landforms

Mountainous|

* Butte
* Hill
* Flat
* Mountain
* Mountain range
* Plateau
* Ridge
* Table
* Valley

Continental plain|

* Ice sheet
* Plain
* Steppe
* Tundra

Fluvial|

* Alluvial fan
* Beach
* Canyon
* Cave
* Channel
* Cliff
* Lake
* Levee
* Floodplain
* Meander
* Oasis
* Pond
* Rapids
* River
* River delta
* River mouth
* Strait
* Swamp
* Valley
* Waterfall

Glacial|

* Arête
* Cirque
* Esker
* Glacier
* Ice field
* Fjord
* Tunnel valley

Oceanic and
coastal landforms|

* Atoll
* Bay
* Cape
* Channel
* Coast
* Continental shelf
* Coral reef
* Estuary
* High island
* Island
* Isthmus
* Lagoon
* Mid-ocean ridge
* Oceanic trench
* Peninsula
* Seamount

Volcanic|

* Caldera
* Geyser
* Guyot
* High island
* Lava dome
* Lava field
* Mid-ocean ridge
* Submarine volcano
* Volcanic crater
* Volcanic crater lake
* Volcanic plateau
* Volcanic plug
* Volcano
* Wall rock

Aeolian|

* Desert
* Dry lake
* Dune
* Sandhill
* Tundra

Artificial|

* Artificial island
* Artificial reef
* Bridge
* Building
* Canal
* Dam
* Ditch
* Land reclamation
* Levee
* Polder
* Quarry
* Reservoir
* Road
* Tunnel

* See also: Geographical feature

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