Portal:Mountains

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Introduction

Silvretta panorama from the Ochsenkopf
Silvretta panorama from the Ochsenkopf
Mount Everest, Earth's highest mountain

A mountain is an elevated portion of the surface of a planet, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain is usually considered higher than a hill, typically rising 300 metres (980 ft) above the surrounding land. It may either have a limited summit area or be a smaller plateau with high elevation and steep sides. A few mountains are isolated summits, but most occur in mountain ranges.[page needed]

Mountains are formed through tectonic forces, erosion, or volcanism,[page needed] 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). The highest mountain from base to peak Mauna Kea in Hawaii at 9,330 m (30,610 ft) from its base at the bottom of the ocean; some scientists consider it to be the tallest on earth. (Full article...)

African Rift Valley. From left to right: Lake Upemba, Lake Mweru, Lake Tanganyika (largest), and Lake Rukwa.

A rift valley is a linear shaped lowland between several highlands or mountain ranges produced by the action of a geologic rift. Rifts are formed as a result of the pulling apart of the lithosphere due to extensional tectonics. The linear depression may subsequently be further deepened by the forces of erosion. More generally the valley is likely to be filled with sedimentary deposits derived from the rift flanks and the surrounding areas. In many cases rift lakes are formed. One of the best known examples of this process is the East African Rift. On Earth, rifts can occur at all elevations, from the sea floor to plateaus and mountain ranges in continental crust or in oceanic crust. They are often associated with a number of adjoining subsidiary or co-extensive valleys, which are typically considered part of the principal rift valley geologically. (Full article...)

Selected mountain range

The Brabazon Range ( Brabazon Mountains ) is a mountain range located in the U.S. state of Alaska in Saint Elias Mountains in Tongass National Forest. The Brabazon Range stretches for about 28 miles from Alsek River at Gateway Knob to Harlequin Lake, located 44 miles southeast of Yakutat in south central Alaska. It is situated to the southeast of Mount Reaburn (1684 m) and northeast of Square Lake Cabin and north of Bear Island.

The name for the mountain ranger was first proposed by then University of Wisconsin geologist, Eliot Blackwelder. It is named after A. J. Brabazon, who created the first topographic map of the ranger in 1895. (Full article...)

Selected mountain type

Fell (from Old Norse: fell, "mountain → landscape over the tree line"; cf. Icelandic: fell, Norwegian: fjell, Swedish: fjäll) is a high and barren landscape feature, such as a mountain or moor-covered hill, often mountain landscape over the tree line, etc. The term is most often employed in Fennoscandia, Iceland, the Isle of Man, parts of northern England, and Scotland. (Full article...)

Selected climbing article

Ice axe
1  pick
2  head
3  adze
4  leash
5  leash stop
6  shaft with rubber grip
7  spike

An ice axe is a multi-purpose hiking and climbing tool used by mountaineers in both the ascent and descent of routes that involve snow or ice covered (e.g. ice climbing or mixed climbing) conditions. Its use depends on the terrain: in its simplest role it is used like a walking stick, with the mountaineer holding the head in the center of their uphill hand. On steep terrain it is swung by its handle and embedded in snow or ice for security and an aid to traction. It can also be buried pick down, the rope tied around the shaft to form a secure anchor on which to bring up a second climber, or buried vertically to form a stomp belay. The adze is used to cut footholds, as well as scoop out compacted snow to bury the axe as a belay anchor. (Full article...)

General images

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

Selected skiing article

This glossary of skiing and snowboarding terms is a list of definitions of terms and jargon used in skiing, snowboarding, and related winter sports. (Full article...)

Subcategories

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Topics

NASA Landsat-7 imagery of Himalayas
NASA Landsat-7 imagery of Himalayas

Flora and fauna

Lists of mountains

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