Chimborazo, Ecuador, the point farthest from the center of the Earth, the closest point to outer space[1]
The view of Jeff Davis Peak from the glacier-carved summit of Wheeler Peak, Nevada. Because Boundary Peak, Nevada is partially in California, and is actually a sub-peak of Montgomery Peak, the shorter Wheeler Peak can be considered the tallest mountain in Nevada.
Mountain in Carbon County, Utah
Mount Olympus in Greece
Chomo Lonzo Makalu Mount Everest Tibetan Plateau Rong River Changtse Rongbuk Glacier North Face East Rongbuk Glacier North Col north ridge route Lhotse Nuptse South Col route Gyachung Kang Cho Oyu Press hyperlinks (or button to enlarge image)
The Himalayan mountain range with Mount Everest

A mountain is a large landform that stretches above the surrounding land in a limited area usually in the form of a peak. A mountain is generally steeper than a hill. The adjective montane is used to describe mountainous areas and things associated with them. The study of mountains is called Orography. Exogeology deals with planetary mountains, which in that branch of science are usually called montes (singular—mons). The highest mountain on Earth based from sea level is Mount Everest (8,848 m (29,029 ft)) in the Himalayas of Asia. The highest known mountain in the Solar System is Olympus Mons on the planet Mars at 21,171 m (69,459 ft). Mountains and mountain ranges on Earth are typically formed by the movement and/or interaction of lithospheric plates.



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.[2] 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."[2]

Whether a landform is called a mountain may depend on usage among the local people. The highest point in San Francisco, California, is called Mount Davidson, notwithstanding its height of 300 m (980 ft), which makes it ten feet short of the minimum for a mountain by American designations.[citation needed] Similarly, Mount Scott outside Lawton, Oklahoma is only 251 m (823 ft) from its base to its highest point.

Definitions of "mountain" include:[3]

  • Height over base of at least 2,500 m (8,202 ft);
  • Height over base of 1,500 m (4,921 ft).–2,500 m (8,202 ft). with a slope greater than 2 degrees
  • Height over base of 1,000 m (3,281 ft).–1,500 m (4,921 ft). with a slope greater than 5 degrees
  • Local (radius 7,000 m (22,966 ft). elevation greater than 300 m (984 ft)., or 300 m (984 ft)–1,000 m (3,281 ft). if local (radius 7,000 m (22,966 ft). elevation is greater than 300 m (984 ft).

By this definition,[which?] mountains cover 64% of Asia, 25% of Europe, 22% of South America, 17% of Australia, and 3% of Africa. As a whole, 24% of the Earth's land mass is mountainous and 10% of people live in mountainous regions.[4] Most of the world's rivers are fed from mountain sources, and more than half of humanity depends on mountains for water.[5][6]


Tall mountains reach into the colder layers of the atmosphere. They are consequently subject to glaciation, and erosion through frost action. Such processes produce the peak shape. Some mountains have glacial lakes, created by melting glaciers; for example, there are an estimated 3,000 glacial lakes in Bhutan. Mountains can be eroded and weathered, altering their characteristics over time.

Tall mountains have different climatic conditions at the top than at the base, and will thus have altitudinal zonation of ecosystems. At the highest elevations, trees cannot grow, and whatever life may be present will be of the alpine type, resembling tundra.[7] Just below the tree line, one may find subalpine forests of needleleaf trees, which can withstand cold, dry conditions.[8] In regions with dry climates, the tendency of mountains to have higher precipitation as well as lower temperatures also provides for varying conditions, which in turn leads to differing flora and fauna.[7][9] Some plants and animals found in these zones tend to become isolated since the conditions above and below a particular zone will be inhospitable and thus constrain their movements or dispersal. On the other hand, birds, being capable of flight, may take advantage of montane habitats and migrate into a region that would otherwise not provide appropriate habitat.[10] These isolated ecological systems, or microclimates, are known as sky islands.[11]

Mountains are generally colder than their surrounding lowlands due to the way that the sun heats the surface of the Earth. Practically all the heat at the surface of the Earth comes from the sun, in the form of solar energy. The sun's radiation is absorbed by land and sea, whence the heat is transferred into the air. Static air is a poor conductor of heat, so conduction of heat from the ground to the atmosphere is negligible. Heat is mainly transferred into the atmosphere through convection and radiation. The air immediately adjacent to the warmed surface will rise due to its buoyancy, leading to convective circulation, in the form of thermals, within the lowest layer of the atmosphere, the troposphere. When heat radiates from the surface of the earth, it is released as long-wave radiation, which can move freely through gases composed of diatomic molecules (such as the atmosphere's oxygen and nitrogen), but is readily absorbed by triatomic molecules, such as carbon dioxide and water vapor. Since most of the atmosphere's quantity of such triatomic gases is contained within the troposphere, this portion of the atmosphere is readily heated by the earth's radiation. The tropopause forms a blanket of air keeping the surface warm. This is the Greenhouse Effect. The higher the altitude, the less of this blanket there is to keep in the heat. Thus, higher elevations, such as mountains, are colder than surrounding lowlands.[12] Air temperature in the lowest layer of the atmosphere, the troposphere, decreases with gains in altitude. The rate at which the temperature drops with elevation, called the environmental lapse rate, is not constant (it can fluctuate throughout the day or seasonally and also regionally), but a normal lapse rate is 5.5°C per 1,000 m (3.57°F per 1,000 ft).[13][14][15] The temperature continues to drop with increasing altitude, until the tropopause (11,000m or 36,089 ft in the U.S. Standard Atmosphere, where it does not decrease further. However, this is higher than the highest mountaintop.

Mountains are generally less preferable for human habitation than lowlands; the weather is often harsher, and there is little level ground suitable for agriculture. The decreasing atmospheric pressure means that less oxygen is available for breathing, and there is less protection against solar radiation (UV). Acute mountain sickness (caused by hypoxia—a lack of oxygen in the blood) affects over half of lowlanders who spend more than a few hours above 3,500 metres (11,480 ft).

Many mountains and mountain ranges throughout the world have been left in their natural state, and are today primarily used for recreation, while others are used for logging, mining, grazing, or see little use. Some mountains offer spectacular views from their summits, while others are densely wooded. Summit accessibility is affected by height, steepness, latitude, terrain, weather. Roads, ski lifts, or aerial tramways allow access. Hiking, backpacking, mountaineering, rock climbing, ice climbing, downhill skiing, and snowboarding are recreational activities enjoyed on mountains. Mountains that support heavy recreational use (especially downhill skiing) are often the locations of mountain resorts.

Mountains are made up of earth and rock materials. The outermost layer of the Earth or the Earth's crust is composed of seven primary plates. When two plates move or collide each other, vast land areas are uplifted, forming mountains.


Classified by the geological processes that shape them, there are five major types of mountains:

Left to right: Mount Everest, Lhotse and Ama Dablam in the Himalayas
Mount Kinabalu, 4,101 metres (13,455 ft), Malaysia
The Adirondack Mountains of New York are remnants of an eroded plateau.
Fold mountains
Fold mountains are the most common type of mountains. They are formed due to collision of two plates, causing folding of the Earth's crust. Examples of fold mountains are the Himalayas of Asia and the Alps in Europe.[citation needed]
Fault-Block mountains
As the name suggests, fault-block mountains or fault mountains are formed when blocks of rock materials slide along faults in the Earth's crust. There are two types of block mountains, namely the lifted and tilted. Lifted mountains have two steep sides; whereas, the tilted type has one steep side and a gentle sloping side. Examples of fault-block mountains are found in the Sierra Nevada mountain range of the western United States.
Volcanic mountains
Volcanic mountains are formed due to volcanic eruptions where magma piles up on the surface of the Earth. Examples of volcanoes include Mount Fuji in Japan and Mount Pinatubo in the Philippines. Inactive or extinct volcanic mountain include Mount Elbrus in Russia, Mount Kinabalu in Malaysia, Cotopaxi in Ecuador and Aconcagua in Argentina/
Dome mountains
Dome mountains are formed when the hot magma rises from the mantle and uplifts the overlying sedimentary layer of the Earth's crust. In the process, the magma is not erupted, but it cools down and forms the core of the mountain. They are called dome mountains due to their appearance that resembles a dome shape. An example of a dome mountain is Navajo Mountain in the U.S. state of Utah.
Plateau mountains
Plateau mountains are formed erosion of an uplifted plateau. Examples of plateau mountains are in the Adirondack Mountains in the U.S. state of New York.


A mountain is usually produced by the movement of lithospheric plates, either orogenic movement or epeirogenic movement. 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. The absolute heights of features termed mountains and hills vary greatly according to an area's terrain. The major mountains tend to occur in long linear arcs, indicating tectonic plate boundaries and activity. Two types of mountain are formed in this way depending on how the rock reacts to the tectonic forces, — fold mountains or fault-block mountains. Other mountain building processes include volcanoes and sea floor spreading.

Fold mountains

Compressional forces in continental collisions may cause the compressed region to thicken and fold, with material forced both upwards and downwards. Since the less dense continental crust "floats" (cf iceberg) 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 (see isostasy) of a much greater volume forced downward into the mantle. Thus the continental crust is normally much thicker under mountains ( sometimes called "mountain roots"),[16] compared to lower lying areas. However, in many continental collisions (e.g. the Himalayas) part of one continent may simply override the other, crumpling in the process with the overridden crust forming much of the support. Mountains may similarly be partly supported by oceanic crust subducted beneath the continental crust (e.g. the Andes as the Nazca plate flows beneath the South American Plate).

Fault-block mountain

Block mountains are created when large areas are widely broken up by faults creating large vertical displacements. This occurrence is fairly common. 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.

Rock that does not fault may 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 Jura Mountains are an example of folding. Over time, erosion can bring about an inversion of relief: the soft upthrust rock is worn away so the anticlines are actually lower than the tougher, more compressed rock of the synclines.


Some isolated mountains are produced by volcanoes, including many apparently small islands or seamounts that reach a great height above the ocean floor.

Mid-ocean ridges

The mid-ocean ridges formed during sea-floor spreading are often referred to as undersea mountain ranges due to their bathymetric prominence.

See also

The Zugspitze, the highest mountain in Germany


  1. ^ "The 'Highest' Spot on Earth". 
  2. ^ a b Gerrard, A. J. 1990. Mountain Environments
  3. ^ Blyth, S., Groombridge, B., Lysenko, I., Miles, L. & Newton, A. (2002). "Mountain Watch". UNEP World Conservation Monitoring Centre, Cambridge, UK. Retrieved 2009-02-17. 
  4. ^ Panos (2002). "High Stakes". Retrieved 2009-02-17. 
  5. ^ "International Year of Freshwater 2003". Retrieved 2006-12-07. 
  6. ^ "The Mountain Institute". Retrieved 2006-12-07. 
  7. ^ a b "Biotic Communities of the Colorado Plateau: C. Hart Merriam and the Life Zones Concept". Retrieved 30 January 2010. 
  8. ^ "Tree". Microsoft Encarta Reference Library 2003. Microsoft Corporation. 1993-2002. 60210-442-1635445-74407. 
  9. ^ "Mountain Environments". United Nations Environment Programme World Conservation Monitoring Centre. Retrieved 30 January 2010. 
  10. ^ Taylor, Richard Cachor (2005). A Birder's Guide to Southeastern Arizona. American Birding Association. pp. 2–4. ISBN 1-878788-22-1. 
  11. ^ Tweit, Susan J. (1992). The Great Southwest Nature Factbook. Alaska Northwest Books. pp. 209–210. ISBN 0-88240-434-2. 
  12. ^ Lutgens, Frederick K.; Tarbuck, Edward J. (1998). The Atmosphere: An Introduction to Meteorology. Prentice Hall. pp. 15–17, 30–35, 38–40. ISBN 0-13-742974-6. 
  13. ^ "Temperature". Microsoft Encarta Reference Library 2003. 
  14. ^ "Atmosphere". Microsoft Encarta Reference Library 2003. 
  15. ^ Dommasch, Daniel O. (1961). Airplane Aerodynamics (3rd ed.). Pitman Publishing Co.. p. 22. 
  16. ^ Press, Frank and Siever, Raymond, Earth, W. H. Freeman, 4th ed., 1985, p. 413 ISBN 978-0716717430

Further reading

  • Fraknoi, A., Morrison, D., & Wolff, S. (2004). Voyages to the Planets. 3rd Ed. Belmont: Thomson Books/Cole.

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