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Portal:Mountains

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Introduction

View of the south side of the Santa Catalina Mountains as seen from Tucson, Arizona.
View of the south side of the Santa Catalina Mountains as seen from Tucson, Arizona.
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). The tallest mountain including submarine terrain is Mauna Kea in Hawaii from its underwater base at 9,330 m (30,610 ft); some scientists consider it to be the tallest on earth. (Full article...)

Argentinian proglacial lakes: Lago Viedma (middle), Lago Argentino (left) and Lago San Martin (right). Retreating glaciers are visible at the top.

In geology, a proglacial lake is a lake formed either by the damming action of a moraine during the retreat of a melting glacier, a glacial ice dam, or by meltwater trapped against an ice sheet due to isostatic depression of the crust around the ice. At the end of the last ice age about 10,000 years ago, large proglacial lakes were a widespread feature in the northern hemisphere. (Full article...)

Selected mountain range

Looking south with Mount Lewis centered and Bens Peak to the left

The Shoshone Range is a mountain range in Lander County, Nevada. The northeast end of the range extends into Eureka County at Shoshone Point on the Humboldt River.

The range was named from the Shoshoni language meaning "grass". (Full article...)

Selected mountain type

Tower karst at Li River, Guilin, China

Tower karst are tall rock structures made up of soluble rock such as limestone. Tower karst forms as near-vertical joints and fractures are eroded downward by solution, leaving parts of a previously coherent rock mass isolated from each other. Tower karst is most common in tropical regions, although it may form in other climates as well.

Examples include Khao Phing Kan, also known as James Bond Island, in Thailand, and Cat Ba Island in Vietnam. (Full article...)

Selected climbing article

In climbing, a Tyrolean traverse is a technique that enables climbers to cross a void between two fixed points, such as between a headland and a detached rock pillar (e.g. a sea stack), or between two points that enable the climbers to cross over an obstacle such as chasm or ravine, or over a fast moving river. Originally developed by Tyrolean mountaineers in the Dolomites in the late 19th to early 20th century, Tyrolean traverses are used in other areas including in caving and in mountain rescue situations.

With a traverse-rope fixed between two anchor points — ideally under some tension — the climber attaches to the rope using a short quickdraw (or equivalent alternative) that is attached to their harness. A backup attachment loop using carabiners and slings is also recommended. Any backpacks are separately clipped to the rope and also clipped to the climber, so they can be dragged across. The climber lies horizontal to the rope with their head facing the direction of travel and moves by pulling hand-over-hand on the rope. Devices such as ascenders can help pull along the rope, pulleys can help reduce friction, and progress capture devices (PCDs) can prevent slippage back along the rope. (Full article...)

General images

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

Selected skiing article

Lebanon at the 2010 Winter Olympics

Skiing in Lebanon has been a sport since an engineering student returning from studying in Switzerland brought back with him the sport of skiing to Lebanon in the early twentieth century. Lebanon is home to six developed ski resorts. Cedars Ski Resort Bsharri is the oldest and received its first ski lift. Mzaar Ski Resort, Kfardebian, is Lebanon's largest ski resort. (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

Recognized content

Associated Wikimedia

The following Wikimedia Foundation sister projects provide more on this subject: