Learn more about Continent
A continent is one of several large areas of land on Earth, which are identified by convention rather than any strict criteria. The specific areas of land vary, but seven areas are commonly reckoned as continents - they are, in order of size, Asia, Africa, North America, South America, Antarctica, Europe and Australia.
 Definitions and application
"Continents are understood to be large, continuous, discrete masses of land, ideally separated by expanses of water."<ref>Lewis, Martin W., Kären E. Wigen (1997). The Myth of Continents: a Critique of Metageography. Berkeley: University of California Press, p. 21. ISBN 0520207424, ISBN 0520207432.</ref> However many of the seven most commonly recognized continents are identified by convention rather than adherence to the ideal criterion that each be a discrete landmass, separated by water from others. Likewise the criterion that each be a continuous landmass is often disregarded by the inclusion of the continental shelf and oceanic islands.
 Extent of continents
The narrowest meaning of continent is that of a continuous<ref>"continent n. 5. a." (1989) Oxford English Dictionary, 2nd edition. Oxford University Press ; "continent1 n." (2006) The Concise Oxford English Dictionary, 11th edition revised. (Ed.) Catherine Soanes and Angus Stevenson. Oxford University Press ; "continent1 n." (2005) The New Oxford American Dictionary, 2nd edition. (Ed.) Erin McKean. Oxford University Press ; "continent [2, n] 4 a" (1996) Webster's Third New International Dictionary, Unabridged. ProQuest Information and Learning.</ref> area of land or mainland, with the coastline and any land boundaries forming the edge of the continent. In this sense the term continental Europe is used to refer to mainland Europe, excluding islands such as the British Isles, and the term continent of Australia may refer to the mainland of Australia, excluding Tasmania.
From the perspective of geology or physical geography, continent may be extended beyond the confines of continuous dry land to include the shallow, submerged adjacent area (the continental shelf)<ref>"continent [2, n] 6" (1996) Webster's Third New International Dictionary, Unabridged. ProQuest Information and Learning. "a large segment of the earth's outer shell including a terrestrial continent and the adjacent continental shelf"</ref> and the islands on the shelf (continental islands), as they are structurally part of the continent.<ref>Monkhouse, F. J., John Small (1978). A Dictionary of the Natural Environment. London: Edward Arnold, pp. 67-68. “structurally it includes shallowly submerged adjacent areas (continental shelf) and neighbouring islands”</ref> From this perspective the edge of the continental shelf is the true edge of the continent, as shorelines vary with changes in sea level.<ref name=Ollier>Ollier, Cliff D. (1996). Planet Earth. In Ian Douglas (Ed.), Companion Encyclopedia of Geography : The Environment and Humankind. London: Routledge, p. 30. "Ocean waters extend onto continental rocks at continental shelves, and the true edges of the continents are the steeper continental slopes. The actual shorelines are rather accidental, depending on the height of sea-level on the sloping shelves."</ref> In this sense the British Isles are part of Europe, and Australia and the island of New Guinea together form a continent (Australia-New Guinea).
As a cultural construct, the concept of a continent may go beyond the continental shelf to include oceanic islands and continental fragments. In this way, Iceland may be considered part of Europe and Madagascar part of Africa. Extrapolating the concept to its extreme, some geographers take Australia and all the islands of Oceania (or sometimes Australasia) to be equivalent to a continent, allowing the entire land surface of the Earth to be divided into continents or quasi continents.<ref>Lewis, Martin W., Kären E. Wigen (1997). The Myth of Continents: a Critique of Metageography. Berkeley: University of California Press, p. 40. ISBN 0520207424, ISBN 0520207432. “The joining of Australia with various Pacific islands to form the quasi continent of Oceania ....”</ref>
 Separation of continents
The ideal criterion that each continent be a discrete landmass is commonly disregarded in favor of more arbitrary, historical conventions. Of the seven most commonly recognized continents, only Antarctica and Australia are separated from other continents.
Several continents are defined not as absolutely distinct bodies but as "more or less discrete masses of land."<ref>Lewis, Martin W., Kären E. Wigen (1997). The Myth of Continents: a Critique of Metageography. Berkeley: University of California Press, p. 35. ISBN 0520207424, ISBN 0520207432.</ref> Asia and Africa are joined by the Isthmus of Suez, and North America and South America by the Isthmus of Panama. Both these isthmuses are very narrow in comparison with the bulk of the landmasses they join.
The division of the landmass of Eurasia into the separate continents of Asia and Europe is an anomaly with no basis in physical geography. The separation is maintained for historical and cultural reasons. An alternative view is that Eurasia is a single continent, one of six continents in total. This view is held by some geographers and is preferred in Russia (which spans Asia and Europe) and Eastern Europe.
North America and South America are now treated as separate continents in much of Western Europe, China, and most native English-speaking countries. However in earlier times they were viewed as a single continent known as America or, to avoid ambiguity with the United States of America, as the Americas. They are still viewed as a single continent, one of six in total, in Latin America, Iberia, Italy and some other parts of Europe.
When continents are defined as discrete landmasses, embracing all the contiguous land of a body, then Asia, Europe and Africa form a single continent known by various names such as Africa-Eurasia. This produces a four-continent model consisting of Africa-Eurasia, the Americas, Antarctica and Australia.
When sea levels were lower during the Pleistocene ice age, greater areas of continental shelf were exposed as dry land, forming land bridges. At this time Australia-New Guinea was a single, continuous continent. Likewise North America and Asia were joined by the Bering land bridge. Other islands such as Great Britain were joined to the mainlands of their continents. At this time there were just three discrete continents: Africa-Eurasia-America, Antarctica and Australia-New Guinea.
 Number of continents
There are several ways of distinguishing the continents.
|7 continents<ref name=AoCA>The World - Continents, Atlas of Canada</ref><ref name=EB>"Continent". Encyclopædia Britannica. 2006. Chicago: Encyclopædia Britannica, Inc.</ref><ref name=NatlGeo>World, National Geographic - Xpeditions Atlas. 2006. Washington, DC: National Geographic Society.</ref><ref name=Oxford1>The New Oxford Dictionary of English. 2001. New York: Oxford University Press.</ref><ref name=Encarta>"Continent". MSN Encarta Online Encyclopedia 2006.</ref><ref name=Oxford2>"Continent". McArthur, Tom, ed. 1992. The Oxford Companion to the English Language. New York: Oxford University Press; p. 260.</ref>||Antarctica||<center>North America||Europe||Asia||Africa||Australia|
|6 continents<ref name=Columbia>"Continent". The Columbia Encyclopedia. 2001. New York: Columbia University Press - Bartleby.</ref><ref name=EB /><ref name=McGrawHill>"Continent". McGraw-Hill Concise Encyclopedia of Earth Science (extracted from online McGraw-Hill Encyclopedia of Science and Technology). 2005. New York: McGraw-Hill Professional; pp. 136-7.</ref>||Antarctica||<center>South America||<center>North America||<center>Eurasia||Africa||Australia|
|4 continents||Antarctica||<center>America <center>||<center>Africa-Eurasia||Australia|
The 7-continent model is usually taught in Western Europe, China, and most native English-speaking countries. The 6-continent combined-Eurasia model is preferred by the geographic community, Russia, Eastern Europe, and Japan. The 6-continent combined-America model is taught in Latin America, Iberia, Italy, Iran and some other parts of Europe.
 Size and population
Continents ranked by size and population
 Other "continents"
Certain parts of continents are recognized as subcontinents, particularly those on different tectonic plates to the rest of the continent. The most notable examples are the Indian subcontinent and the Arabian Peninsula. The large island of Greenland, though on the North American Plate, is sometimes referred to as a subcontinent.
Some islands lie on sections of continental crust that have rifted and drifted apart from a main continental landmass. While not considered continents because of their relatively small size, they may be considered minicontinents. Madagascar, the largest example, is usually considered part of Africa but has been referred to as "the eighth continent". New Zealand and New Caledonia are island groups on continental crust separate from the Australia-New Guinea continental shelf.
 History of the concept
 Early concepts of the Old World continents
The first distinction between continents was made by ancient Greek mariners who gave the names Europe and Asia to the lands on either side of the waterways of the Aegean Sea, the Dardanelles strait, the Sea of Marmara, the Bosphorus strait and the Black Sea. <ref name=Toynbee> Toynbee, Arnold J. (1954). A Study of History. London: Oxford University Press, v. 8, pp. 711-12.</ref> The names were first applied just to lands near the coast and only later extended to include the hinterlands.<ref>Tozer, H. F. (1897). A History of Ancient Geography. Cambridge: University Press, p. 69.</ref> But the division was only carried through to the end of navigable waterways. "... beyond that point the Hellenic geographers never succeeded in laying their finger on any inland feature in the physical landscape that could offer any convincing line for partitioning an indivisible Eurasia ...".<ref name=Toynbee/>
Ancient Greek thinkers subsequently debated whether Africa (then called Libya) should be considered part of Asia or a third part of the world. Division into three parts eventually came to predominate.<ref>Tozer, H. F. (1897). A History of Ancient Geography. Cambridge: University Press, p. 67.</ref> From the Greek viewpoint, the Aegean Sea was the center of the world; Asia lay to the east, Europe to the west and north and Africa to the south.<ref>Lewis, Martin W., Kären E. Wigen (1997). The Myth of Continents: a Critique of Metageography. Berkeley: University of California Press, pp. 21-22. ISBN 0520207424, ISBN 0520207432.</ref> The boundaries between the continents were not fixed. Early on, the Europe-Asia boundary was taken to run from the Black Sea along the Rioni River (known then as the Phasis) in Georgia. Later it was viewed as running from the Black Sea through Kerch Strait, the Sea of Azov and along the Don River (known then as the Tanais) in Russia.<ref>Tozer, H. F. (1897). A History of Ancient Geography. Cambridge: University Press, p. 68.</ref> The boundary between Asia and Africa was generally taken to be the Nile River. Herodotus<ref>Herodotus. Translated by George Rawlinson (2000). The Histories of Herodotus of Halicarnassus . Ames, Iowa: Omphaloskepsis, book 2, p. 18.</ref> in the fifth century BC, however, objected to the unity of Egypt being split into Asia and Africa ("Libya") and took the boundary to lie along the western border of Egypt, regarding Egypt as part of Asia. He also queried the division into three of what is really a single landmass,<ref>Herodotus. Translated by George Rawlinson (2000). The Histories of Herodotus of Halicarnassus . Ames, Iowa: Omphaloskepsis, book 4, p. 38. "I cannot conceive why three names ... should ever have been given to a tract which is in reality one"</ref> a debate that continues nearly two and a half millennia later.
Eratosthenes, in the third century BC, noted that some geographers divided the continents by rivers (the Nile and the Don), thus considering them "islands". Others divided the continents by isthmuses, calling the continents "peninsulas". These latter geographers set the border between Europe and Asia at the isthmus between the Black Sea and the Caspian Sea, and the border between Asia and Africa at the isthmus between the Red Sea and the mouth of Lake Bardawil on the Mediterranean Sea.<ref>Strabo. Translated by Horace Leonard Jones (1917). Geography. Harvard University Press, book 1, ch. 4.</ref>
Through the Roman period and the Middle Ages, a few writers took the Isthmus of Suez as the boundary between Asia and Africa, but most writers continued to take it to be the Nile or the western border of Egypt (Gibbon). In the Middle Ages the world was portrayed on T and O maps, with the T representing the waters dividing the three continents. By the middle of the eighteenth century, "the fashion of dividing Asia and Africa at the Nile, or at the Great Catabathmus [the boundary between Egypt and Libya] farther west, had even then scarcely passed away". <ref>Goddard, Farley Brewer (1884). "Researches in the Cyrenaica". The American Journal of Philology, 5 (1) p. 38.</ref>
 European discovery of the Americas
Christopher Columbus sailed across the Atlantic Ocean to the West Indies in 1492, sparking a period of European exploration of the Americas. But despite four voyages to the Americas, Columbus never believed he had reached a new continent – he always thought it was part of Asia.
In 1501, Amerigo Vespucci and Gonçalo Coelho attempted to sail around the southern end of the Asian mainland into the Indian Ocean. On reaching the coast of Brazil, they sailed a long way south along the coast of South America, confirming that this was a land of continental proportions and that it extended much further south than Asia was known to.<ref name=OGorman>O'Gorman, Edmundo (1961). The Invention of America. Indiana University Press, pp. 106-112.</ref> On return to Europe, an account of the voyage, called Mundus Novus ("New World"), was published under Vespucci’s name in 1502 or 1503,<ref name=formisano1>Formisano, Luciano (Ed.) (1992). Letters from a New World: Amerigo Vespucci's Discovery of America. New York: Marsilio, pp. xx-xxi. ISBN 0941419622.</ref> although it seems that it had additions or alterations by another writer.<ref name=Zerubavel1>Zerubavel, Eviatar (2003). Terra Cognita: The Mental Discovery of America. New Brunswick: Transaction Publishers, pp. 77–79. ISBN 0765809877.</ref> Regardless of who penned the words, Mundus Novus attributed Vespucci with saying, "I have discovered a continent in those southern regions that is inhabited by more numerous people and animals than our Europe, or Asia or Africa",<ref name=formisano2>Formisano, Luciano (Ed.) (1992). Letters from a New World: Amerigo Vespucci's Discovery of America. New York: Marsilio, p. 45. ISBN 0941419622.</ref> the first known explicit identification of part of the Americas as a continent like the other three.
Within a few years the name "New World" began appearing as a name for South America on world maps, such as the Oliveriana (Pesaro) map of around 1504–1505. Maps of this time though still showed North America connected to Asia and showed South America as a separate land.<ref name=Zerubavel1/>
In 1507 Martin Waldseemüller published a world map, Universalis Cosmographia, which was the first to show North and South America as separate from Asia and surrounded by water. A small inset map above the main map explicitly showed for the first time the Americas being east of Asia and separated from Asia by an ocean, as opposed to just placing the Americas on the left end of the map and Asia on the right end. In the accompanying book Cosmographiae Introductio, Waldseemüller noted that the earth is divided into four parts, Europe, Asia, Africa and the fourth part which he named "America" after Amerigo Vespucci's first name.<ref name=Zerubavel2>Zerubavel, Eviatar (2003). Terra Cognita: The Mental Discovery of America. New Brunswick: Transaction Publishers, pp. 80–82. ISBN 0765809877.</ref> On the map, the word "America" was placed on part of South America.
 The word continent
From the 1500s the English noun continent was derived from the term continent land, meaning continuous or connected land<ref name=oed>"continent n." (1989) Oxford English Dictionary, 2nd edition. Oxford University Press.</ref> and translated from the Latin terra continens.<ref>"continent1 n." (2006) The Concise Oxford English Dictionary, 11th edition revised. (Ed.) Catherine Soanes and Angus Stevenson. Oxford University Press.</ref> The noun was used to mean "a connected or continuous tract of land" or mainland.<ref name=oed/> It was not applied only to very large areas of land — in the 1600s, references were made to the continents (or mainlands) of Kent, Ireland and Wales and in 1745 to Sumatra.<ref name=oed/> The word continent was used in translating Greek and Latin writings about the three "parts" of the world, although in the original languages no word of exactly the same meaning as continent was used.<ref> Lewis, Martin W., Kären E. Wigen (1997). The Myth of Continents: a Critique of Metageography. Berkeley: University of California Press, p. 29. ISBN 0520207424, ISBN 0520207432.</ref>
While continent was used on the one hand for relatively small areas of continuous land, on the other hand geographers again raised Herodotus’s query about why a single large landmass should be divided into separate continents. In the mid 1600s Peter Heylin wrote in his Cosmographie that "A Continent is a great quantity of Land, not separated by any Sea from the rest of the World, as the whole Continent of Europe, Asia, Africa." In 1727 Ephraim Chambers wrote in his Cyclopædia, "The world is ordinarily divided into two grand continents: the old and the new." And in his 1752 atlas, Emanuel Bowen defined a continent as "a large space of dry land comprehending many countries all joined together, without any separation by water. Thus Europe, Asia, and Africa is one great continent, as America is another."<ref>Bowen, Emanuel. (1752). A Complete Atlas, or Distinct View of the Known World. London, p. 3.</ref> However, the old idea of Europe, Asia and Africa as "parts" of the world ultimately persisted with these being regarded as separate continents.
 Beyond four continents
From the late 18th century some geographers started to regard North America and South America as two parts of the world, making five parts in total. Overall though the fourfold division prevailed well into the 19th century.<ref name=lewis30> Lewis, Martin W., Kären E. Wigen (1997). The Myth of Continents: a Critique of Metageography. Berkeley: University of California Press, p. 30. ISBN 0520207424, ISBN 0520207432.</ref>
Europeans discovered Australia in 1606 but for some time it was taken as part of Asia. By the late 18th century some geographers considered it a continent in its own right, making it the sixth (or fifth for those still taking America as a single continent).<ref name=lewis30/> In 1813 Samuel Butler wrote of Australia as "New Holland, an immense island, which some geographers dignify with the appellation of another continent" and the Oxford English Dictionary was just as equivocal some decades later.<ref>"continent n. 5. a." (1989) Oxford English Dictionary, 2nd edition. Oxford University Press. "the great island of Australia is sometimes reckoned as another [continent]"</ref>
Antarctica was sighted in 1820 and described as a continent by Charles Wilkes on the United States Exploring Expedition in 1838, the last continent to be identified, although a great "antarctic" (antipodean) landmass had been anticipated for millennia. An 1849 atlas labelled Antarctica as a continent but few atlases did so until after World War II.<ref> Lewis, Martin W., Kären E. Wigen (1997). The Myth of Continents: a Critique of Metageography. Berkeley: University of California Press, pp. 32, 220. ISBN 0520207424, ISBN 0520207432.</ref>
From the mid-19th century, United States atlases more commonly treated North and South America as separate continents, while atlases published in Europe usually considered them one continent. However it was still not uncommon for United States atlases to treat them as one continent up till World War II.<ref name=lewis32> Lewis, Martin W., Kären E. Wigen (1997). The Myth of Continents: a Critique of Metageography. Berkeley: University of California Press, p. 32. ISBN 0520207424, ISBN 0520207432.</ref> The Olympic symbol, devised in 1913, has five rings representing the five inhabited, participating continents, with America being treated as one continent and Antarctica not included.
From the 1950s, most United States geographers divided America in two and, with the addition of Antarctica, this made the seven-continent model.<ref name=lewis32/> However, this division of America never appealed to Latin America, which saw itself spanning an America that was a single landmass, and there the conception of six continents remains, as it does in scattered other countries such as Japan.
Geologists use the term continent in a different manner than geographers. Rather than simply identifying large land masses, geologists have distinct criteria for identifying continents. Continents are portions of the Earth's crust characterized by a stable platform of Precambrian metamorphic and igneous rock (typically 1.5 to 3.8 billion years old) largely of granitic composition, called the craton, and a central "shield" where the craton is exposed at the surface. The craton itself is an accretionary complex of ancient mobile belts (mountain belts) from earlier cycles of subduction, continental collision and break up from plate tectonic activity. An outward-thickening veneer of younger, minimally deformed sedimentary rock covers much of the rest of the craton. The margins of the continents are characterized by currently-active or relatively recently active mobile belts and/or deep troughs of accumulated marine or deltaic sediments. Beyond the margin, there is either a continental shelf and drop off to the basaltic-rock ocean basin or the margin of another continent, depending on the current plate-tectonic setting of the continent. A continental boundary does not have to be a body of water. Over geologic time, continents are periodically submerged under large epicontinental seas, and continental collisions result in a continent becoming attached to another continent. The current geologic era is relatively anomalous in that so much of the continental areas are "high and dry" compared to much of geologic history.
It is believed that continents are accretionary crustal "rafts" which, unlike the denser basaltic crust of the ocean basins, are not subjected to destruction through the plate tectonic process of subduction. This accounts for the great age of the rocks comprising the continental cratons.
By the geologists' definition, Europe and Asia are separate continents since they have separate, distinct ancient shield areas and a distinct newer mobile belt (the Ural Mountains) forming the mutual margin. Also, India is a geological continent, as it contains a central shield, and the geologically recent Himalaya mobile belt forms its northern margin. North America and South America are separate continents, the connecting isthmus being largely the result of volcanism from relatively recent subduction tectonics. But the North American continent also includes Greenland, which is a portion of Canadian Shield, and the mobile belt forming its western margin includes the easternmost portion of the Asian land mass.
 See also
|Wikimedia Commons has media related to:|
 References and notes
ar:قارة an:Continén ast:Continente bn:মহাদেশ zh-min-nan:Tāi-lio̍k be:Кантынэнт bs:Kontinent br:Kevandir bg:Континент ca:Continent cv:Континент cs:Kontinent cy:Cyfandir da:Verdensdel de:Kontinent arc:ܝܒܝܫܬܐ el:Ήπειροι es:Continente eo:Kontinento eu:Kontinente fa:قاره fr:Continent fy:Wrâlddiel ga:Mór-roinn gl:Continente ko:대륙 hi:महाद्वीप hr:Kontinent io:Kontinento id:Benua ia:Continente is:Heimsálfa it:Continente he:יבשת kn:ಖಂಡ ka:კონტინენტი ks:Bhūgōla kw:Brastir ky:Материк sw:Bara ku:Kîşwer la:Continens lv:Kontinents lb:Kontinent lt:Žemynai jbo:braplu hu:Kontinens mk:Континент mg:Kontinenta ms:Benua mo:Континент nl:Continent ja:大陸 no:Kontinent nn:Kontinent nrm:Continnent ug:ئۆزىنى تۇتۇالغان nds:Eerddeel pl:Kontynent pt:Continente ro:Continent rmy:Kontinento qu:Allpa pacha ru:Континент sm:Konitineta sq:Kontinenti scn:Cuntinenti simple:Continent sk:Svetadiel sl:Celina sr:Континент sh:Kontinent su:Buana fi:Maanosa sv:Världsdel ta:கண்டம் th:ทวีป tg:Қитъа tpi:Kontinen tr:Kıta uk:Материк wa:Continint yi:קאנטינענטzh:洲