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Mountain

From Halbeeg, the open encyclopedia · Af-Soomaali

221 languages
Gunong ace
Berg af
Berg als
Beorg ang
جبل arz
Monte ast
Dağ az
داغ azb
Gunung ban
Beag bar
Kalns bat-smg
Bukid bcl
Belud bdr
Гара be-x-old
Gunung bew
Gunung bjn
Săng cdo
Bukid ceb
کێو ckb
Dağ crh
Hora cs
Ту cv
Zoli dag
Berg de
Taŋa dga
Ko diq
Mägi fiu-vro
Berag frr
gan
Dongor gom
Hu'idu gor
Sân hak
הר he
Hora hsb
Mòn ht
Hegy hu
Սար hyw
ii
Bantay ilo
Gora isv
ja
Mountn jam
cmana jbo
Taw kaa
A̱fan kcg
ko
Zuor kus
Mons la
Сув lez
Monte lfn
Crëp lld
گَر mzn
Tepetl nah
Barg nds
Barg nds-nl
Thaba nso
Seru pap
غر ps
Urqu qu
Paxro rmy
Munti roa-rup
Mundagne roa-tara
Adrar shi
Mountain simple
Gora sl
Gomo sn
Buur so
Berg sv
Gōra szl
buyu' szy
Dag tk
Dağ tr
Phiri tum
Mägi vep
Núi vi
Berg vls
Bel vo
Bukid war
wuu
Bya za
zh
zh-classical
Soaⁿ zh-min-nan
zh-yue
Buur
Ama Dablam Peak ("Mother's Necklace", आमा दब्लम, 6,812 metres (22,349 ft)) as seen from Chola Valley. Khumbu Everest Zone. Nepal, Himalayas.Vyacheslav Argenberg · CC BY 4.0 · Commons

A mountain is a portion of land that rises significantly above the surrounding terrain and typically has a steep slope (flank) and a distinct summit. Most mountains (plural form) are found in ranges or chains, which are connected by valleys and passes.

There is no universally agreed international threshold that distinguishes a mountain from a hill. Some countries apply specific elevation criteria to define the height of a summit or the difference between a peak and the surrounding land.

How mountains form

Most large mountains result from historical tectonic activity: when two continental plates collide, rock layers fold and rise upward. There are also volcanic mountains built from lava rock that emerged from the earth, and those formed when hard rock resists erosion while the surrounding land wears away.

Climate and life

As elevation increases, temperature drops and air humidity decreases. For this reason, a single mountain can have multiple distinct ecological zones stacked one above another: dense forest at the base, then sparse trees and woodland, followed by rock and ice at high altitudes. Very high mountains hold permanent snow and glaciers, which feed the rivers of the lowlands below.

People and mountains

People living on mountains typically rely on pastoralism, terraced farming, and trade along mountain passes. Mountains also hold religious and cultural significance, with certain peaks regarded as sacred sites. Mountain climbing has developed as both a sport and a recreational activity.

UncertaintyElevation measurements and specific mountain names are not included here, as they require verified sources.
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