Mountain

For other uses, see Mountain (disambiguation).
Mount Everest, the highest peak on Earth
Chimborazo, Ecuador. The point on Earth's surface farthest from its center.[1]
Aiguille du Dru in the French Alps

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. 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.

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).

Definition

The Matterhorn, Swiss Alps
Peaks of Mount Kenya

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 local usage. The highest point in San Francisco, California, is called Mount Davidson, notwithstanding its height of 300 m (980 ft), which makes it twenty feet short of the minimum for a mountain by American designations. Similarly, Mount Scott outside Lawton, Oklahoma is only 251 m (823 ft) from its base to its highest point. Whittow's Dictionary of Physical Geography[3] states "Some authorities regard eminences above 600 m (2,000 ft) as mountains, those below being referred to as hills."

In the United Kingdom and the Irish Republic, a mountain is usually defined as any summit at least 2,000 feet (or 610 metres) high,[4][5][6][7][8] whilst the official United Kingdom government's definition of a mountain, for the purposes of access, is a summit of 600 metres or higher.[9] In addition, some definitions also include a topographical prominence requirement, typically 100 or 500 feet (30 or 152 m).[10] For a while, the US defined a mountain as being 1,000 feet (300 m) or taller. 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.[11]

The UN Environmental Programme's definition of "mountainous environment" includes any of the following:[12]

Using these definitions, mountains cover 33% of Eurasia, 19% of South America, 24% of North America, and 14% of Africa.[13] As a whole, 24% of the Earth's land mass is mountainous.[14]

Geology

Jeff Davis Peak seen from the glacier-carved summit of Wheeler Peak, Nevada

There are three main types of mountains: volcanic, fold, and block.[15] All three types are formed from plate tectonics: when portions of the Earth's 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.

Volcanoes

Main article: Volcano
Geological cross-section of Fuji volcano

Volcanoes are formed when a plate is pushed below another plate, or at a mid-ocean ridge or hotspot.[16] 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.[17] 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 United States.

Fold mountains

Main article: Fold mountains

Fold mountains occur when two plates collide: shortening occurs along thrust faults and the crust is overthickened.[18] 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.[19] 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 Jura Mountains are an example of fold mountains.

Block mountains

Main article: Block mountains
The Catskills in Upstate New York represent an eroded plateau.

Block mountains are caused by faults in the crust: a seam where rocks can move past each other. When rocks on one side of a fault rise relative to the other, it can form a mountain.[20] 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.

Erosion

Main article: Erosion

During and following uplift, mountains are subjected to the agents of erosion (water, wind, ice, and gravity) which gradually wear the uplifted area down. Erosion causes the surface of mountains to be younger than the rocks that form the mountains themselves.[21] 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.

Climate

Main article: Alpine climate
A mountain in Carbon County, Utah
Valley of the Ten Peaks, Canadian Rockies

Climate on mountains become colder at high elevations, due 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 (140 °F), and the temperature would decay exponentially with height.[22]

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 at 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 curve. 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 kilometer (or 5.4 °F per 1000 feet) of altitude.[22]

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 kilometer or 3&nbsp°F per 1000 feet)[23] The actual lapse rate can vary by altitude and by location.

Therefore, moving up 100 meters on a mountain is roughly equivalent to moving 80 kilometers (45 miles or 0.75° of latitude) towards the nearest pole.[24] This relationship is only approximate, however, since local factors such as proximity to oceans (such as the Arctic Ocean) can drastically modify the climate.[25] As the altitude increases, the main form of precipitation becomes snow and the winds increase.[26]

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.[27] 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).

Ecology

Main article: Montane ecology
An alpine mire in the Swiss Alps

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.[28] 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.[29][30]

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.[31]

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.[30] Just below the tree line, one may find subalpine forests of needleleaf trees, which can withstand cold, dry conditions.[32] 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.

In society

Mountain climbers ascending Mount Rainier
The summit of Ben Nevis, the British Isles' highest, has a memorial

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),[13] only 140 million people live above that altitude[33] and only 20-30 million people above 3,000 metres (9,800 ft) elevation.[34] The decreasing atmospheric pressure with increasing elevation means that less oxygen is available for breathing, and there is less protection against solar radiation (UV).[29] Due to decreasing oxygen, the highest known permanent habitation in the world is at 5,100 metres (16,700 ft), while the highest known permanently tolerable altitude is at 5,950 metres (19,520 ft).[35] Above 8,000 metres (26,000 ft) elevation, there is not enough oxygen to support human life. This is known as the "death zone".[36] The summits of Mount Everest and K2 are in the death zone.

About half of mountain dwellers live in the Andes, Central Asia, and Africa.[14] 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.[37] About 80% of mountain people live below the poverty line.[14]

Most of the world's rivers are fed from mountain sources, with snow acting as a storage mechanism for downstream users.[38] More than half of humanity depends on mountains for water.[39][40]

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.[41]

Superlatives

The Zugspitze, the highest mountain in Germany
Maat Mons of Venus (22.5x exaggeration)

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).[42] 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,[43] 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 world's tallest mountain and volcano, rising about 10,203 m (33,474 ft) from the Pacific Ocean floor.[44]

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 km2) and volume (about 18,000 cu mi or 75,000 km3).[45] Mount Kilimanjaro is the largest non-shield volcano in terms of both base area (245 sq mi or 635 km2) and volume (1,150 cu mi or 4,793 km3). Mount Logan is the largest non-volcanic mountain in base area (120 sq mi or 311 km2).

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, Ecuador's tallest mountain, is usually considered to be the farthest point from the Earth's centre, although the southern summit of Peru's tallest mountain, Huascarán, is another contender.[46] Both have elevations above sea level more than 2 kilometres (6,600 ft) less than that of Everest.

See also

Notes

  1. ↑ "The 'Highest' Spot on Earth". Npr.org. 7 April 2007. Retrieved 31 July 2012.
  2. 1 2 Gerrard 1990.
  3. ↑ Whittow, John (1984). Dictionary of Physical Geography. London: Penguin. p. 352. ISBN 0-14-051094-X.
  4. ↑ Nuttall, John & Anne (2008). England. The Mountains of England & Wales 2 (3rd ed.) (Milnthorpe, Cumbria: Cicerone). ISBN 1-85284-037-4.
  5. ↑ "Survey turns hill into a mountain". BBC. Retrieved 3 February 2013.
  6. ↑ "A Mountain is a Mountain – isn't it?". www.go4awalk.com. Retrieved 3 February 2013.
  7. ↑ "mountain". dictionary.reference.com. Retrieved 3 February 2013.
  8. ↑ Wilson, Peter (2001). "Listing the Irish hills and mountains". Irish Geography (Coleraine: University of Ulster) 34 (1): 89. doi:10.1080/00750770109555778. Archived from the original (PDF) on 2013-06-27.
  9. ↑ "What is a "Mountain"? Mynydd Graig Goch and all that...". Metric Views. Retrieved 3 February 2013.
  10. ↑ Helman, Adam (2005). The Finest Peaks - Prominence and Other Mountain Measures. Trafford Publishing. ISBN 978-1412059954.
  11. ↑ "What is the difference between lake and pond; mountain and hill; or river and creek?". USGS. Archived from the original on 2013-02-12. Retrieved 11 February 2013.
  12. ↑ Blyth 2002, p. 74.
  13. 1 2 Blyth 2002, p. 14.
  14. 1 2 3 Panos (2002). "High Stakes" (PDF). Retrieved 17 February 2009.
  15. ↑ "Chapter 6: Mountain building". Science matters: earth and beyond; module 4. Pearson South Africa. 2002. p. 75. ISBN 0-7986-6059-7.
  16. ↑ Butz, Stephen D (2004). "Chapter 8: Plate tectonics". Science of Earth Systems. Thompson/Delmar Learning. p. 136. ISBN 0-7668-3391-7.
  17. ↑ Gerrard 1990, p. 194.
  18. ↑ Searle, Michael P (2007). "Diagnostic features and processes in the construction and evolution of Oman-, Zagros-, Himalayan-, Karakoram-, and Tibetan type orogenic belts". In Robert D. Hatcher Jr., MP Carlson, JH McBride & JR Martinez Catalán. 4-D framework of continental crust. Geological Society of America. p. 41 ff. ISBN 0-8137-1200-9.
  19. ↑ Press, Frank; Siever, Raymond (1985). Earth (4th ed.). W. H. Freeman. p. 413. ISBN 978-0-7167-1743-0.
  20. ↑ Ryan, Scott (2006). "Figure 13-1". CliffsQuickReview Earth Science. Wiley. ISBN 0-471-78937-2.
  21. ↑ Fraknoi, Morrison & Wolff 2004, p. 160.
  22. 1 2 Goody, Richard M.; Walker, James C.G. (1972). "Atmospheric Temperatures" (PDF). Atmospheres. Prentice-Hall.
  23. ↑ "Dry Adibatic Lapse Rate". tpub.com. Retrieved 2016-05-02.
  24. ↑ Blyth 2002, p. 15.
  25. ↑ "Factors affecting climate". The United Kingdom Environmental Change Network. Archived from the original on 16 July 2011.
  26. ↑ Blyth 2002, p. 12.
  27. ↑ Lugo, Ariel E.; Brown, Sandra L.; Dodson, Rusty; Smith, Tom S.; Shugart, Hank H. (1999). "The Holdridge Life Zones of the conterminous United States in relation to ecosystem mapping". Journal of Biogeography 26 (5): 1025–1038. doi:10.1046/j.1365-2699.1999.00329.x. Archived from the original on 2013-02-12.
  28. ↑ Daubenmire, R.F. (June 1943). "Vegetational Zonation in the Rocky Mountains". Botanical Review 9 (6): 325–393. doi:10.1007/BF02872481.
  29. 1 2 Blyth 2002.
  30. 1 2 "Biotic Communities of the Colorado Plateau: C. Hart Merriam and the Life Zones Concept". Archived from the original on 2013-02-04. Retrieved 30 January 2010.
  31. ↑ Tweit, Susan J. (1992). The Great Southwest Nature Factbook. Alaska Northwest Books. pp. 209–210. ISBN 0-88240-434-2.
  32. ↑ "Tree". Microsoft Encarta Reference Library 2003. Microsoft Corporation. 2002 [1993]. 60210-442-1635445-74407.
  33. ↑ Moore, Lorna G. (2001). "Human Genetic Adaptation to High Altitude". High Alt Med Biol 2 (2): 257–279. doi:10.1089/152702901750265341. PMID 11443005.
  34. ↑ Cook, James D.; Boy, Erick; Flowers, Carol; del Carmen Daroca, Maria (2005). "The influence of high-altitude living on body iron". Blood 106 (4): 1441–1446. doi:10.1182/blood-2004-12-4782. PMID 15870179.
  35. ↑ West, JB (2002). "Highest permanent human habitation". High Altitude Medical Biology 3 (4): 401–7. doi:10.1089/15270290260512882. PMID 12631426.
  36. ↑ "Everest:The Death Zone". Nova. PBS. 24 February 1998.
  37. ↑ Blyth 2002, p. 17.
  38. ↑ Blyth 2002, p. 22.
  39. ↑ "International Year of Freshwater 2003". Archived from the original on 7 October 2006. Retrieved 7 December 2006.
  40. ↑ "The Mountain Institute". Archived from the original on 9 July 2006. Retrieved 7 December 2006.
  41. ↑ Cox, Steven M.; Fulsaas, Kris, eds. (2009) [2003]. Mountaineering: The Freedom of the Hills (7 ed.). Seattle: The Mountaineers. ISBN 0-89886-828-9.
  42. ↑ "Nepal and China agree on Mount Everest's height". BBC News. 8 April 2010. Retrieved 22 August 2010.
  43. ↑ Helman, Adam (2005). The Finest Peaks: Prominence and Other Mountain Measures. Trafford. p. 9. ISBN 1412236649. the base to peak rise of Denali is the largest of any mountain that lies entirely above sea level, some 18,000 feet.
  44. ↑ "Mountains: Highest Points on Earth". National Geographic Society. Retrieved 19 September 2010.
  45. ↑ Kaye, G.D. (2002). "Using GIS to estimate the total volume of Mauna Loa Volcano, Hawaii". 98th Annual Meeting. Geological Society of America.
  46. ↑ Krulwich, Robert (7 April 2007). "The 'Highest' Spot on Earth?". Retrieved 21 March 2009.

References

External links

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