Mountain


A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. A mountain differs from a plateau in having a limited summit area, and is larger than a hill, typically rising at least 300 metres (1000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges.[1]

Mountains are formed through tectonic forces, erosion, or volcanism,[1] which act on time scales of up to tens of millions of years.[2] Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers.

High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and climate, mountains tend to be used less for agriculture and more for resource extraction, such as mining and logging, along with recreation, such as mountain climbing and skiing.

The highest mountain on Earth is Mount Everest in the Himalayas of Asia, whose summit is 8,850 m (29,035 ft) above mean sea level. The highest known mountain on any planet in the Solar System is Olympus Mons on Mars at 21,171 m (69,459 ft).

There is no universally accepted definition of a mountain. Elevation, volume, relief, steepness, spacing and continuity have been used as criteria for defining a mountain.[3] In the Oxford English Dictionary a mountain is defined as "a natural elevation of the earth surface rising more or less abruptly from the surrounding level and attaining an altitude which, relatively to the adjacent elevation, is impressive or notable."[3]

Whether a landform is called a mountain may depend on local usage. Mount Scott outside Lawton, Oklahoma, USA, is only 251 m (823 ft) from its base to its highest point. Whittow's Dictionary of Physical Geography[4] states "Some authorities regard eminences above 600 metres (1,969 ft) as mountains, those below being referred to as hills."


Mount Everest, Earth's highest mountain
Mount Fuji, Japan's highest mountain
Mount Kilimanjaro in Tanzania, Africa's highest mountain
Peaks of Mount Kenya
Mount Elbrus, the highest mountain in Russia and Europe
Mount Wilhelm in Papua New Guinea
Geological cross-section of Fuji volcano
Illustration of mountains that developed on a fold that has been thrusted
Pirin Mountain, Bulgaria, part of the fault-block Rila-Rhodope massif
The Catskills in Upstate New York represent an eroded plateau.
A combination of high latitude and high altitude makes the northern Urals in picture to have climatic conditions that make the ground barren.
An alpine mire in the Swiss Alps
Mount Ararat in Turkey, as seen from Khor Virap, Armenia
The city of La Paz reaches up to 4,000 metres (13,000 ft) in elevation.
Climbers ascending Mount Rainier
Chimborazo, Ecuador. The point on Earth's surface farthest from its centre.[49]