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 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...)

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. (Full article...)

Selected mountain range

The Little Snowy Mountains are a small mountain range in central Montana about 25 miles (40 km) southeast of Lewistown. The range lies mostly in Fergus County, but the southern part of the range extends into Golden Valley and Musselshell counties.

The range is a lower continuation of the Big Snowy Mountains which lie immediately to the west. The small Pike Creek Hills are 12 miles (19 km) to the east. (Full article...)

Selected mountain type

Pietra di Bismantova in the Apennines, Italy

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. In Southern Africa a similar formation of granite is known as a koppie, an Afrikaans word ("little head") from the Dutch diminutive word kopje. 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

Lead climber on the bolted sport climbing route Gezurren Erresuma 8c (5.14b), in Spain.

Lead climbing (or leading) is a technique in rock climbing where the lead climber clips their rope to the climbing protection as they ascend a pitch of the climbing route, while their second (or belayer) remains at the base of the route belaying the rope to protect the lead climber in the event that they fall. The term is used to distinguish between the two roles, and the greater effort and increased risk, of the role of the lead climber.

Leading a climb is in contrast with top roping a climb, where even though there is still a second belaying the rope, the lead climber faces little or 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 (i.e. if they fall off, they just hang from the rope). (Full article...)

General images

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

Selected skiing article

Three smiling women stand side by side with one arm over each other's back. Each holds high a flower bouquet and wears a medal around the neck. On the left, a long-haired blond wears a shiny light-gray jacket and winter cap with a badge bearing the Norwegian flag and Olympic rings. On the center, another long-haired blond wears a red jacket and red-and-white winter cap. On the right, a long-haired brunette wears a white jacket with blue and red stripes on the back.
The medalists of the inaugural women's ski cross event at the 2010 Winter Olympics. From left to right: Hedda Berntsen of Norway (silver), Ashleigh McIvor of Canada (gold), and Marion Josserand of France (bronze).

Freestyle skiing is one of the six skiing disciplines contested at the Winter Olympic Games, and one of the youngest. In 1924, the first Winter Olympics featured Nordic skiing disciplines (cross-country skiing, ski jumping, and Nordic combined), while alpine skiing was first contested in 1936. Only at the 1992 Winter Olympics, in Albertville, France, were freestyle skiing events first held as official medal events. Before that, freestyle skiing was contested at the 1988 Winter Olympics as a demonstration sport, consisting of events for both men and women in three variants: moguls, aerials and ski ballet. In Albertville, moguls was the first-ever official freestyle skiing medal event; aerials and ski ballet were also held but still as demonstration events. The growing popularity of aerials convinced the International Olympic Committee (IOC) to add this freestyle discipline to the 1994 Winter Olympics official program. Moguls and aerials have thus been contested at every Winter Games since. Ski cross inclusion in the Winter Olympics program was approved at an IOC Executive Board meeting in November 2006, and the first events were held at the 2010 Winter Olympics.

At the 2002 Winter Olympics, two days after Steve Bradbury gave Australia its first-ever Winter Olympic gold medal, Alisa Camplin won the freestyle aerials event, becoming the first Australian woman to win gold at the Winter Games; four years later, she collected a second consecutive medal, a bronze. In 2010, the third Olympics hosted by Canada finally consecrated a Canadian athlete as Olympic champion: Alexandre Bilodeau took the gold medal in the men's moguls, overcoming defending champion Dale Begg-Smith of Australia. Kari Traa of Norway has won three medals (one gold, one silver, one bronze) in three successive Games, more than any other freestyle skier at the Winter Olympics. Alexandre Bilodeau and David Wise are the most successful male freestyle skiers, with two gold medals. Alexandre Bilodeau was also the first freestyle skier to win back to back gold medals when he won gold in the 2010 and 2014 moguls. The youngest freestyle skier to win an Olympic medal is Swiss Mathilde Gremaud, who secured a silver in 2018 with 18 years old, while Tatjana Mittermayer of Germany is the oldest medalist, following her silver in the 1998 moguls event, aged 33. (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

Associated Wikimedia

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