ⓘ Mountain

List of highest mountains on Earth

There are at least 109 mountains on Earth with elevations greater than 7.200 metres above sea level. The vast majority of these mountains are located on the edge of the Indian and Eurasian continental plates. Only those summits are included that, by an objective measure, may be considered individual mountains as opposed to subsidiary peaks.


A summit is a point on a surface that is higher in elevation than all points immediately adjacent to it. The topographic terms acme, apex, peak, and zenith are synonymous. The term top mountain top is generally used only for a mountain peak that is located at some distance from the nearest point of higher elevation. For example, a big massive rock then to the main summit of a mountain is not considered a summit. Summits near a higher peak, with some prominence or isolation, but not reaching a certain cutoff value for the quantities, are often considered subsummits or subpeaks of the higher ...


In mathematics, the slope or gradient of a line is a number that describes both the direction and the steepness of the line. Slope is often denoted by the letter m ; there is no clear answer to the question why the letter m is used for slope, but its earliest use in English appears in OBrien who wrote the equation of a straight line as y = mx + b and it can also be found in Todhunter who wrote it as y = mx + c ". Slope is calculated by finding the ratio of the "vertical change" to the "horizontal change" between any two distinct points on a line. Sometimes the ratio is expressed as a quoti ...

Mountain pass

A mountain pass is a navigable route through a mountain range or over a ridge. Since many of the worlds mountain ranges have presented formidable barriers to travel, passes have played a key role in trade, war, and both human and animal migration throughout Earths history. At lower elevations it may be called a hill pass. The highest vehicle-accessible pass in the world appears to be Mana Pass, located in the Himalayas on the border between India and Tibet, China.


A valley is a low area between hills or mountains typically with a river running through it. In geology, a valley or dale is a depression that is longer than it is wide. The terms U-shaped and V-shaped are descriptive terms of geography to characterize the form of valleys. Most valleys belong to one of these two main types or a mixture of them, at least with respect to the cross section of the slopes or hillsides.


A glacier is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. Glaciers slowly deform and flow due to stresses induced by their weight, creating crevasses, seracs, and other distinguishing features. They also abrade rock and debris from their substrate to create landforms such as cirques and moraines. Glaciers form only on land and are distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice i ...


A moraine is any glacially formed accumulation of unconsolidated glacial debris that occurs in both currently and formerly glaciated regions on Earth, through geomorphological processes. Moraines are formed from debris previously carried along by a glacier, and normally consist of somewhat rounded particles ranging in size from large boulders to minute glacial flour. Lateral moraines are formed at the side of the ice flow and terminal moraines at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines and medial moraines.


ⓘ Mountain

A mountain is a large landform that rises above the surrounding land in a limited area, usually in the form of a peak. A mountain is generally steeper than a hill. Mountains are formed through tectonic forces or volcanism. These forces can locally raise the surface of the earth. Mountains erode slowly through the action of rivers, weather conditions, and glaciers. A few mountains are isolated summits, but most occur in huge mountain ranges.

High elevations on mountains produce colder climates than at sea level. 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 and 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.


1. Definition

There is no universally accepted definition of a mountain. Elevation, volume, relief, steepness, spacing and continuity have been used as criteria for defining a mountain. In the Oxford English Dictionary a mountain is defined as "a natural elevation of the earth surface rising more or less abruptly from the surrounding level and attaining an altitude which, relatively to the adjacent elevation, is impressive or notable."

Whether a landform is called a mountain may depend on local usage. Mount Scott outside Lawton, Oklahoma, USA, is only 251 m 823 ft from its base to its highest point. Whittows Dictionary of Physical Geography states "Some authorities regard eminences above 600 metres 2.000 ft as mountains, those below being referred to as hills."

In the United Kingdom and the Republic of Ireland, a mountain is usually defined as any summit at least 2.000 feet 610 m high, which accords with the official UK governments definition that a mountain, for the purposes of access, is a summit of 2.000 feet 610 m or higher. In addition, some definitions also include a topographical prominence requirement, typically 100 or 500 feet 30 or 152 m. At one time the U.S. Board on Geographic Names defined a mountain as being 1.000 feet 300 m or taller, but has abandoned the definition since the 1970s. Any similar landform lower than this height was considered a hill. However, today, the United States Geological Survey USGS concludes that these terms do not have technical definitions in the US.

The UN Environmental Programmes definition of "mountainous environment" includes any of the following:

  • Elevation of at least 2.500 m 8.200 ft;
  • Elevation of at least 1.500 m 4.900 ft, with a slope greater than 2 degrees;
  • Elevation of at least 1.000 m 3.300 ft, with a slope greater than 5 degrees;
  • Elevation of at least 300 m 980 ft, with a 300 m 980 ft elevation range within 7 km 4.3 mi.

Using these definitions, mountains cover 33% of Eurasia, 19% of South America, 24% of North America, and 14% of Africa. As a whole, 24% of the Earths land mass is mountainous.


2. Geology

There are three main types of mountains: volcanic, fold, and block. All three types are formed from plate tectonics: when portions of the Earths crust move, crumple, and dive. Compressional forces, isostatic uplift and intrusion of igneous matter forces surface rock upward, creating a landform higher than the surrounding features. The height of the feature makes it either a hill or, if higher and steeper, a mountain. Major mountains tend to occur in long linear arcs, indicating tectonic plate boundaries and activity.


2.1. Geology Volcanoes

Volcanoes are formed when a plate is pushed below another plate, or at a mid-ocean ridge or hotspot. At a depth of around 100 km, melting occurs in rock above the slab due to the addition of water, and forms magma that reaches the surface. When the magma reaches the surface, it often builds a volcanic mountain, such as a shield volcano or a stratovolcano. Examples of volcanoes include Mount Fuji in Japan and Mount Pinatubo in the Philippines. The magma does not have to reach the surface in order to create a mountain: magma that solidifies below ground can still form dome mountains, such as Navajo Mountain in the US.


2.2. Geology Fold mountains

Fold mountains occur when two plates collide: shortening occurs along thrust faults and the crust is overthickened. Since the less dense continental crust "floats" on the denser mantle rocks beneath, the weight of any crustal material forced upward to form hills, plateaus or mountains must be balanced by the buoyancy force of a much greater volume forced downward into the mantle. Thus the continental crust is normally much thicker under mountains, compared to lower lying areas. Rock can fold either symmetrically or asymmetrically. The upfolds are anticlines and the downfolds are synclines: in asymmetric folding there may also be recumbent and overturned folds. The Balkan Mountains and the Jura Mountains are examples of fold mountains.


2.3. Geology Block mountains

Block mountains are caused by faults in the crust: a plane where rocks have moved past each other. When rocks on one side of a fault rise relative to the other, it can form a mountain. The uplifted blocks are block mountains or horsts. The intervening dropped blocks are termed graben: these can be small or form extensive rift valley systems. This form of landscape can be seen in East Africa, the Vosges, the Basin and Range Province of Western North America and the Rhine valley. These areas often occur when the regional stress is extensional and the crust is thinned.


2.4. Geology Erosion

During and following uplift, mountains are subjected to the agents of erosion which gradually wear the uplifted area down. Erosion causes the surface of mountains to be younger than the rocks that form the mountains themselves. Glacial processes produce characteristic landforms, such as pyramidal peaks, knife-edge arêtes, and bowl-shaped cirques that can contain lakes. Plateau mountains, such as the Catskills, are formed from the erosion of an uplifted plateau.

In Earth science, erosion is the action of surface processes such as water flow or wind that removes soil, rock, or dissolved material from one location on the Earths crust, and then transport it away to another location not to be confused with weathering which involves no movement. The particulate breakdown of rock or soil into clastic sediment is referred to as physical or mechanical erosion; this contrasts with chemical erosion, where soil or rock material is removed from an area by its dissolving into a solvent typically water, followed by the flow away of that solution. Eroded sediment or solutes may be transported just a few millimetres, for thousands of kilometres.


3. Climate

Climate in the mountains becomes colder at high elevations, due to an interaction between radiation and convection. Sunlight in the visible spectrum hits the ground and heats it. The ground then heats the air at the surface. If radiation were the only way to transfer heat from the ground to space, the greenhouse effect of gases in the atmosphere would keep the ground at roughly 333 K 60 °C; 140 °F, and the temperature would decay exponentially with height.

However, when air is hot, it tends to expand, which lowers its density. Thus, hot air tends to rise and transfer heat upward. This is the process of convection. Convection comes to equilibrium when a parcel of air at a given altitude has the same density as its surroundings. Air is a poor conductor of heat, so a parcel of air will rise and fall without exchanging heat. This is known as an adiabatic process, which has a characteristic pressure-temperature dependence. As the pressure gets lower, the temperature decreases. The rate of decrease of temperature with elevation is known as the adiabatic lapse rate, which is approximately 9.8 °C per kilometre or 5.4 °F 3.0 °C per 1000 feet) of altitude.

Note that the presence of water in the atmosphere complicates the process of convection. Water vapor contains latent heat of vaporization. As air rises and cools, it eventually becomes saturated and cannot hold its quantity of water vapor. The water vapor condenses forming clouds, and releases heat, which changes the lapse rate from the dry adiabatic lapse rate to the moist adiabatic lapse rate 5.5 °C per kilometre or 3 °F 1.7 °C per 1000 feet) The actual lapse rate can vary by altitude and by location.

Therefore, moving up 100 metres on a mountain is roughly equivalent to moving 80 kilometres 45 miles or 0.75° of latitude towards the nearest pole. This relationship is only approximate, however, since local factors such as proximity to oceans such as the Arctic Ocean can drastically modify the climate. As the altitude increases, the main form of precipitation becomes snow and the winds increase.

The effect of the climate on the ecology at an elevation can be largely captured through a combination of amount of precipitation, and the biotemperature, as described by Leslie Holdridge in 1947. Biotemperature is the mean temperature; all temperatures below 0 °C 32 °F are considered to be 0 °C. When the temperature is below 0 °C, plants are dormant, so the exact temperature is unimportant. The peaks of mountains with permanent snow can have a biotemperature below 1.5 °C 34.7 °F.


4. Ecology

The colder climate on mountains affects the plants and animals residing on mountains. A particular set of plants and animals tend to be adapted to a relatively narrow range of climate. Thus, ecosystems tend to lie along elevation bands of roughly constant climate. This is called altitudinal zonation. In regions with dry climates, the tendency of mountains to have higher precipitation as well as lower temperatures also provides for varying conditions, which enhances zonation.

Some plants and animals found in altitudinal zones tend to become isolated since the conditions above and below a particular zone will be inhospitable and thus constrain their movements or dispersal. These isolated ecological systems are known as sky islands.

Altitudinal zones tend to follow a typical pattern. At the highest elevations, trees cannot grow, and whatever life may be present will be of the alpine type, resembling tundra. Just below the tree line, one may find subalpine forests of needleleaf trees, which can withstand cold, dry conditions. Below that, montane forests grow. In the temperate portions of the earth, those forests tend to be needleleaf trees, while in the tropics, they can be broadleaf trees growing in a rain forest.


5. Mountains and humans

The highest known permanently tolerable altitude is at 5.950 metres 19.520 ft. At very high altitudes, the decreasing atmospheric pressure means that less oxygen is available for breathing, and there is less protection against solar radiation UV. Above 8.000 metres 26.000 ft elevation, there is not enough oxygen to support human life. This is known as the "death zone". The summits of Mount Everest and K2 are in the death zone.


5.1. Mountains and humans Mountain societies and economies

Mountains are generally less preferable for human habitation than lowlands, because of harsh weather and little level ground suitable for agriculture. While 7% of the land area of Earth is above 2.500 metres 8.200 ft, only 140 million people live above that altitude and only 20-30 million people above 3.000 metres 9.800 ft elevation. About half of mountain dwellers live in the Andes, Central Asia, and Africa.

With limited access to infrastructure, only a handful of human communities exist above 4.000 metres 13.000 ft of elevation. Many are small and have heavily specialized economies, often relying on industries such as agriculture, mining, and tourism. An example of such a specialized town is La Rinconada, Peru, a gold-mining town and the highest elevation human habitation at 5.100 metres 16.700 ft. A counterexample is El Alto, Bolivia, at 4.150 metres 13.620 ft, which has a highly diverse service and manufacturing economy and a population of nearly 1 million.

Traditional mountain societies rely on agriculture, with higher risk of crop failure than at lower elevations. Minerals often occur in mountains, with mining being an important component of the economics of some montane societies. More recently, tourism supports mountain communities, with some intensive development around attractions such as national parks or ski resorts. About 80% of mountain people live below the poverty line.

Most of the worlds rivers are fed from mountain sources, with snow acting as a storage mechanism for downstream users. More than half of humanity depends on mountains for water.

In geopolitics mountains are often seen as preferable "natural boundaries" between polities.


5.2. Mountains and humans Mountaineering

Mountaineering, mountain climbing, or alpinism is the sport, hobby or profession of hiking, skiing, and climbing mountains. While mountaineering began as attempts to reach the highest point of unclimbed big mountains it has branched into specializations that address different aspects of the mountain and consists of three areas: rock-craft, snow-craft and skiing, depending on whether the route chosen is over rock, snow or ice. All require experience, athletic ability, and technical knowledge to maintain safety.


5.3. Mountains and humans Mountains as sacred places

Mountains often play a significant role in religions and philosophical beliefs. There are for example a number of sacred mountains within Greece such as Mount Olympos which was held to be the home of the gods. In Japanese culture, the 3.776.24 m 12.389 ft volcano of Mount Fuji is also held to be sacred with tens of thousands of Japanese ascending it each year. In Ireland, pilgrimages are made up the 952 metres 3.123 ft Mount Brandon by Irish Catholics. The Himalayan peak of Nanda Devi is associated with the Hindu goddesses Nanda and Sunanda; it has been off-limits to climbers since 1983.


6. Superlatives

Heights of mountains are typically measured above sea level. Using this metric, Mount Everest is the highest mountain on Earth, at 8.848 metres 29.029 ft. There are at least 100 mountains with heights of over 7.200 metres 23.622 ft above sea level, all of which are located in central and southern Asia. The highest mountains above sea level are generally not the highest above the surrounding terrain. There is no precise definition of surrounding base, but Denali, Mount Kilimanjaro and Nanga Parbat are possible candidates for the tallest mountain on land by this measure. The bases of mountain islands are below sea level, and given this consideration Mauna Kea 4.207 m 13.802 ft above sea level) is the worlds tallest mountain and volcano, rising about 10.203 m 33.474 ft from the Pacific Ocean floor.

The highest mountains are not generally the most voluminous. Mauna Loa 4.169 m or 13.678 ft is the largest mountain on Earth in terms of base area about 2.000 sq mi or 5.200 km 2 and volume about 18.000 cu mi or 75.000 km 3. Mount Kilimanjaro is the largest non-shield volcano in terms of both base area 245 sq mi or 635 km 2 and volume 1.150 cu mi or 4.793 km 3. Mount Logan is the largest non-volcanic mountain in base area 120 sq mi or 311 km 2.

The highest mountains above sea level are also not those with peaks farthest from the centre of the Earth, because the figure of the Earth is not spherical. Sea level closer to the equator is several miles farther from the centre of the Earth. The summit of Chimborazo, Ecuadors tallest mountain, is usually considered to be the farthest point from the Earths centre, although the southern summit of Perus tallest mountain, Huascaran, is another contender. Both have elevations above sea level more than 2 kilometres 6.600 ft less than that of Everest.