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Introduction

Appalachian Mountains
Mount Everest, Earth's highest mountain

A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (980 ft) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges.

Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. 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). (Full article...)

Selected mountain-related landform

Skeiðarársandur in Iceland, viewed from its eastern margin at the terminus of Svínafellsjökull glacier

An outwash plain, also called a sandur (plural: sandurs), sandr or sandar, is a plain formed of glaciofluvial deposits due to meltwater outwash at the terminus of a glacier. As it flows, the glacier grinds the underlying rock surface and carries the debris along. The meltwater at the snout of the glacier deposits its load of sediment over the outwash plain, with larger boulders being deposited near the terminal moraine, and smaller particles travelling further before being deposited. Sandurs are common in Iceland where geothermal activity accelerates the melting of ice flows and the deposition of sediment by meltwater. (Full article...)

Selected mountain range

The Sierra de San Borja, also known as Sierra La Libertad is a mountain range on the Baja California Peninsula of Mexico. It is one of the Peninsular Ranges which form the backbone of Baja California. The Sierra de San Borja is located between 28° North latitude (the border of the states of Baja California and Baja California Sur) and 29° North latitude (Highway 12). The highest point of the Sierra is Cerro La Sandia, 1,775 metres (5,823 ft) in elevation located at .

The Sierra de San Borja is nearly uninhabited. Desert vegetation prevails with only a few water sources. Tourists visit the San Francisco Borja Mission (founded 1762) and the extensive prehistoric rock art scattered throughout the mountains. (Full article...)

Selected mountain type

Sarmatian Kurgan, 4th century BC, Fillipovka, South Urals, Russia. A dig led by Russian Academy of Sciences Archeology Institute Prof. L. Yablonsky excavated this kurgan in 2006. It is the first kurgan known to have been completely destroyed and then rebuilt to its original appearance.
A kurgan is a type of tumulus constructed over a grave, often characterized by containing a single human body along with grave vessels, weapons and horses. Originally in use on the Pontic–Caspian steppe, kurgans spread into much of Central Asia and Eastern, Southeast, Western and Northern Europe during the 3rd millennium BC.

The earliest kurgans date to the 4th millennium BC in the Caucasus, and some researchers associate these with the Indo-Europeans. Kurgans were built in the Eneolithic, Bronze, Iron, Antiquity and Middle Ages, with ancient traditions still active in Southern Siberia and Central Asia. (Full article...)

Selected climbing article

Site of the Fort de Buoux

Buoux [bju̟ːks] is a commune in the Vaucluse department in the Provence-Alpes-Côte d'Azur region in southeastern France.

Located on the north side of the Luberon, the town is known for the high cliffs that surround it, making it a popular venue for rock-climbing enthusiasts, as well as the ruins of a medieval fort that was built in the 13th century and destroyed in 1660. The town's population peaked in the mid 19th century with 244 inhabitants in 1836 before falling to only 44 people in 1961. The population has since rebounded some to 122 in 2006. (Full article...)

Related portals

General images

The following are images from various mountain-related articles on Wikipedia.

Selected skiing article

Biathletes in the shooting area of a competition

The biathlon is a winter sport that combines cross-country skiing and rifle shooting. It is treated as a race, with contestants skiing through a cross-country trail whose distance is divided into shooting rounds. The shooting rounds are not timed per se, but depending on the competition, missed shots result in extra distance or time being added to the contestant's total. (Full article...)

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Topics

NASA Landsat-7 imagery of Himalayas
NASA Landsat-7 imagery of Himalayas
Shivling
Shivling
Eruption of Pinatubo 1991

Flora and fauna

Climbing in Greece
Climbing in Greece

Lists of mountains

Recognized content

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