Portal:Mountains

Wikipedia portal for content related to Mountains From Wikipedia, the free encyclopedia

  Portal   WikiProject   Discussion

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 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 610 metres (2,000 ft) or more 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 on Earth from base to peak is Mauna Kea in Hawaii, which rises 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...)

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 610 metres (2,000 ft) or more 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. (Full article...)

Selected mountain range

View of Cross Mountain, the highest summit of the Cumberland Mountains in Tennessee

The Cumberland Mountains are a mountain range in the southeastern section of the Appalachian Mountains. They are located in western Virginia, southwestern West Virginia, the eastern edges of Kentucky, and eastern middle Tennessee, including the Crab Orchard Mountains. Their highest peak, with an elevation of 4,223 feet (1,287 m) above mean sea level, is High Knob, which is located near Norton, Virginia.

According to the USGS, the Cumberland Mountain range is 131 miles (211 km) long and 20 miles (32 km) wide, bounded by the Russell Fork on the northeast, the Pound River and Powell River on the southeast, Cove Creek on the southwest, and Tackett Creek, the Cumberland River, Poor Fork Cumberland River, and Elkhorn Creek on the northwest. The crest of the range forms the Kentucky and Virginia boundary from the Tennessee border to the Russell Fork River. (Full article...)

Selected mountain type

Uluru in Australia

An inselberg or monadnock (/məˈnædnɒk/ mə-NAD-nok) is an isolated rock hill, knob, ridge, or small mountain that rises abruptly from a gently sloping or virtually level surrounding plain. If the inselberg is dome-shaped and formed from granite or gneiss, it can also be called a bornhardt, though not all bornhardts are inselbergs. An inselberg results when a body of rock resistant to erosion, such as granite, occurring within a body of softer rocks, is exposed by differential erosion and lowering of the surrounding landscape. (Full article...)

Selected climbing article

A 'lead climber' on the bolted sport climbing route Gezurren Erresuma 8c (5.14b), in Spain. Her rope has been clipped into several protection points.

Lead climbing (or leading) is a technique in rock climbing where two climbers work together to ascend a climbing route. The 'lead climber' — who climbs — clips the rope to pieces of protection as they ascend. The 'second' (or 'belayer') stands at the base of the route controlling the other end of the rope, which is called belaying (e.g. if the 'lead climber' falls, the 'second' locks the rope). The term distinguishes between the two roles and the greater effort and increased risk of the role of the 'lead climber'.

Leading a route is in contrast with the alternative rock climbing technique of top roping, where even though there is still a 'second' belaying the rope, the 'lead climber' faces no risk in the event of a fall and does not need to clip into any protection as the rope is already anchored to the top of the route (e.g. if they fall they will just hang from the static rope). Leading a climbing route is a core activity in rock climbing, and first ascents (FA) and first free ascents (FFA) of new routes must be done via lead climbing. (Full article...)

General images

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

Selected skiing article

The "Panorama Bahn" hybrid lift in Turracher Höhe, Austria. Chairs load from the station on the left of this image, gondolas along the carpeted area to the right.

A hybrid lift is a type of ski lift that combines the elements of a chairlift and a gondola lift. First introduced by Poma, who refers to them as Telemix, they have since been built by most lift manufacturers who refer to them by a variety of names; Doppelmayr refers to them as a combined lift, Bartholet refers to them with the French name, téléporté mixte, while the more generic terms chondola and telecombi are common in North America.

Both chairs and gondolas have advantages for lift operations. Gondolas offer protection from the elements and are particularly useful in rain or very cold conditions. They can also be used during the summer for walk-on guests, cyclists or wheelchairs, and in the winter for snowshoers. In the winter, gondolas require skiers and snowboarders to remove their equipment and walk into the cabin. Chairs are generally more convenient and easier to board for skiers. Some lifts have so-called 'bubble' chairs, which add a retractable acrylic glass dome to protect passengers from weather. (Full article...)

Subcategories

Need help?

Do you have a question about Mountains that you can't find the answer to? Consider asking it at the Wikipedia reference desk.

Get involved

For editor resources and to collaborate with other editors on improving Wikipedia's Mountains-related articles, see WikiProject Mountains.

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:


Related Articles

Wikiwand AI