Boundary Between Europe And Asia

Determining the boundaries between the continents is generally a matter of geographical convention. Several slightly different conventions are in use. The number of continents is most commonly considered seven (in English-speaking countries) but may range as low as four when Afro-Eurasia and the Americas are both considered as single continents. An island can be considered to be associated with a given continent by either lying on the continent's adjacent continental shelf (e.g. Singapore, the British Isles) or being a part of a microcontinent on the same principal tectonic plate (e.g. Madagascar and Seychelles). An island can also be entirely oceanic while still being associated with a continent by geology (e.g. Bermuda, the Australian Indian Ocean Territories) or by common geopolitical convention (e.g. Ascension Island, the South Sandwich Islands). Another example is the grouping into Oceania of the Pacific Islands with Australia and Zealandia.

There are three overland boundaries subject to definition:
* between Africa and Asia (dividing Afro-Eurasia into Africa and Eurasia): at the Isthmus of Suez;
* between Asia and Europe (dividing Eurasia): along the Turkish straits, the Caucasus, and the Urals and the Ural River (historically also north of the Caucasus, along the Kuma–Manych Depression or along the Don River);
* between North America and South America (dividing the Americas): at some point on the Isthmus of Panama, with the most common demarcation in atlases and other sources following the Darién Mountains watershed along the Colombia–Panama border where the isthmus meets the South American continent (see Darién Gap).

While today the isthmus between Asia and Africa is navigable via the Suez Canal, and that between North and South America via the Panama Canal, these artificial channels are not generally accepted as continent-defining boundaries in themselves. The Suez Canal happens to traverse the Isthmus of Suez between the Mediterranean Sea and the Red Sea, dividing Africa and Asia. The continental boundaries are considered to be within the very narrow land connections joining the continents.

The remaining boundaries concern the association of islands and archipelagos with specific continents, notably:
* the delineation between Africa, Asia, and Europe in the Mediterranean Sea;
* the delineation between Asia and Europe in the Arctic Ocean;
* the delineation between Europe and North America in the North Atlantic Ocean;
* the delineation between North and South America in the Caribbean Sea;
* the delineation of Antarctica from Africa, Australia, and South America in the Indian, South Pacific, and South Atlantic oceans, respectively (referred to collectively by some geographers as the Southern Ocean or the Antarctic Ocean);
* the delineation of Asia from Australia in the Ceram Sea, Arafura Sea, Timor Sea, Halmahera Sea, and the Wallacean region of the Indonesian Archipelago
* the delineation of Asia from North America in the North Pacific Ocean.

Africa and Asia

Historically in Greco-Roman geography, "Africa" meant Ancient Libya, and its eastern extent was taken to be around Marmarica, at the '' Catabathmus Magnus.'' This was not considered to be a continent. As wider knowledge of geography developed, the shape of the African landmass (and Egypt's "natural" inclusion in that landmass) became apparent. In 1806, William George Browne still titled his travelogue ''Travels in Africa, Egypt, and Syria''. Similarly, James Bruce in 1835 published ''Travels through part of Africa, Syria, Egypt, and Arabia''. On the other hand, as early as 1670 John Ogilby under the title ''Africa'' published ''"an accurate Description of the Regions of Egypt, Barbary, Libya, and Billedulgerid, the Land of Negroes, Guinea, Æthiopia, and the Abyssines, with all the adjacent Islands, either in the Mediterranean, Atlantic, Southern, or Oriental Seas, belonging thereunto"''.

The usual line taken to divide Africa from Asia today is at the Isthmus of Suez, the narrowest gap between the Mediterranean Sea and the Gulf of Suez, the route today followed by the Suez Canal. This makes the Sinai Peninsula geographically Asian, and Egypt a transcontinental country. Less than 2% of the Egyptian population live on the Sinai Peninsula, and hence Egypt, even though technically transcontinental, is usually considered an African country entirely and not partly Asian. But when discussing the geopolitical region of the Middle East and North Africa, Egypt is usually grouped with the Western Asian countries as part of the Middle East, while Egypt's western neighbor Libya is grouped with the remaining North African countries as the Maghreb. Both are members of the African Union. However, the geological boundary is located further to the east, along the Gulf of Aqaba and the Dead Sea Transform, with the Sinai Peninsula, Israel, Palestine, much of Lebanon and the coastal governorates of Syria being located on the African Plate.

The Comoros, Madagascar, Mauritius, and Seychelles are island countries in the Indian Ocean which are nominally associated with Africa. The Socotra Archipelago may be considered African as it lies on its continental shelf; however, it is politically a part of Yemen, an Asian country.

Africa and Europe

The African and European mainlands are non-contiguous, and the delineation between these continents is thus merely a question of which islands are to be associated with which continent.

The Portuguese Atlantic island possession of the Azores is from Europe and from Africa, and is sometimes grouped with Europe. By contrast, the Canary Islands and the Madeira islands (the latter of which also include the Desertas Islands and the Savage Islands) off the Atlantic coast of Morocco are much closer to, and usually grouped with, Africa; the Canary Islands are only from the African mainland at their closest point but from the European mainland, while Madeira is from the African mainland and from the European mainland. In his 1895 book ''Africa: Volume 2'', author Augustus Henry Keane remarked, "In the North Atlantic there are four insular groups — Madeira, the Canaries, Cape Verde and Azores — which are usually assigned to Africa, although the Canaries and Cape Verde alone belong geographically to that continent, the Azores are lost, so to say, in mid-Atlantic."

The Mediterranean island country of Malta is about from the coast of Sicily — much closer than the distance to the African mainland. The nearby Italian island of Lampedusa (principal island of the Pelagie Islands) is from Sicily while just from the African mainland; similarly, Pantelleria is from Sicily and just from the African mainland. All of these Mediterranean islands, including Malta and Sicily, are actually located on the African Plate, and could be considered part of the African continent geologically. However, for political and cultural reasons, maps generally display them as part of Europe instead.

A single Spanish islet, known as Alboran Island, is also debatably located on either the African Plate or the Eurasian Plate. This island is located in the Alboran Sea, 50 km (31 mi) north of the Moroccan coast and 90 km (56 mi) south of Spain.

European-governed territories in Africa

There are six definitive occurrences of territories unequivocally being a part of the African continent, but legally being administered by a European state. Three of these are administered by France, and the other three by Spain. The existence of these territories further blurs the line between the borders of Africa and Europe, in particular with regard to the Spanish territories which lie immediately adjacent to and/or connected to the African mainland. The French territories lie within the Indian Ocean, and, consequently, are more dislocated from the principal boundary between the two continents.

The uninhabited Spanish unincorporated overseas minor territories, known as the plazas de soberanía ("Localities of Sovereignty"), are small islands that lie immediately adjacent to the North African coastline, with the exception of Peñón de Vélez de la Gomera, which was originally an island like the other 'localities' but has subsequently become directly connected to the Moroccan (African) mainland. The two other Spanish territories are the exclaves of Ceuta and Melilla, which are two populated coastal cities located directly on the African mainland, both bordering only Morocco.

Two of the French territories are the inhabited overseas departments and regions of Mayotte and Réunion. Mayotte is an island territory located west of the island country of Madagascar within the Mozambique Channel. Réunion is an island territory located near the island country of Mauritius and to the east of Madagascar (both nominally considered part of the African continent). The final territory is the Scattered Islands in the Indian Ocean, administratively a part of the French Southern and Antarctic Lands. This French territory consists of a range of minor uninhabited atolls in the Indian Ocean, located in the deep sea surrounding Madagascar.

Antarctica

Antarctica along with its outlying islands have no permanent population. All land claims south of 60°S latitude are held in abeyance by the Antarctic Treaty System.

Australia's Heard Island and McDonald Islands (an external territory) and the French Kerguelen Islands are located on the Kerguelen Plateau, on the Antarctic continental plate. Both are still within the bounds of the Indian Ocean. The United Nations categorizes Heard Island and McDonald Islands, which are politically affiliated with Australia, as being part of Oceania. The islands are 4,000 km from Perth in Australia, and have never been inhabited by indigenous peoples of Oceania or any other humans. Heard Island has only been visited 240 times throughout its entire history, and the McDonald Islands have only ever been visited twice, in 1971 and 1980. The World Factbook categorizes these islands as part of Antarctica rather than Oceania.

The French Crozet Islands, Île Amsterdam, Île Saint-Paul, and the Norwegian Bouvet Island are also located on the Antarctic continental plate, and are not often associated with other continents. The United Nations categorize Bouvet Island as part of South America, while the World Factbook categorizes it as part of Antarctica.

South Georgia and the South Sandwich Islands are closer to Antarctica than to any other continent. However, they are politically associated with the Falkland Islands, which are less geographically isolated from South America. Furthermore, Argentina, a South American country, maintains its irredentist claims on all of these islands, which are administered by the United Kingdom. The United Nations consider them to be part of South America. Definitions of South America that exclude the Galápagos Islands and Juan Fernández Islands (both oceanic in nature) still generally include the Falklands, which share biographical affinities to Patagonia and Tierra del Fuego, and which are located on the South American continental shelf. The Falkland Islands and South Georgia and the South Sandwich Islands were uninhabited when discovered by Europeans, with some theorizing that the Falklands were visited by Indigenous peoples of the Americas during prehistoric times. These theories are usually considered dubious, as there is no archaeological evidence indicating prehistoric human inhabitation on the Falklands. South Georgia and the South Sandwich Islands do not have any permanent residents. The Falkland Islands have historically had a British population, with a culture distinct from that of mainland South America. There was a violent war between Argentina and the United Kingdom regarding ownership of the islands in 1982, and the residents of the Falklands do not currently wish to be associated with South America, despite their geographical proximity.

The Prince Edward Islands are located between Africa and Antarctica, and are the territory of South Africa, an African country.

Macquarie Island and the Antipodes Islands, Auckland Islands, and Campbell Islands are all uninhabited, and are located between Australia and New Zealand and Antarctica. The Antipodes Islands, Auckland Islands and Campbell Islands are politically part of New Zealand, while Macquarie Island has been integrated into the Australian state of Tasmania. None are discrete political entities like Heard Island and McDonald Islands. As such, they are likely considered by the United Nations also to be part of Oceania. The Auckland Islands could be considered part of Oceania on cultural grounds rather than mere political grounds, as they are believed to be the southernmost island group to have been settled by Polynesians during prehistoric times. The islands were uninhabited when discovered by Europeans, but archaeological traces have since been found to indicate Polynesian settlement, dating to the 13th century, on Enderby Island. Macquarie Island is theorized to have possibly had contact with Polynesians, although there is no archaeological evidence to support this.

Asia and Australia

The continental boundary between Asia and Australia is somewhere in the Wallacean region of the Malay Archipelago. The boundary is frequently divided along the anthropologic Melanesian Line or the biogeographic Weber's Line. Geologically, the Aru Islands in Maluku Province and western New Guinea, which contain six provinces of Indonesia, are part of the Australian continent. The eastern half of New Guinea is a part of Papua New Guinea which is considered to be a part of Oceania. Indonesia is commonly referred to as one of the Southeast Asian countries. Indonesia's eastern region of Western New Guinea and nearby islands, makes it a transcontinental country; Western New Guinea is often considered part of Oceania because of its Indigenous Melanesian inhabitants and geological association with the Australian continental landmass. East Timor, an independent state that was formerly a part of Indonesia, is classified by the United Nations as a part of the South-eastern Asia subregion. It is expected to join the Association of Southeast Asian Nations, having been involved as an ASEAN Regional Forum member since independence, and has participated in the Southeast Asian Games since 2003.

Occasionally, all of the Malay Archipelago is included in Oceania, although this is extremely rare, especially as most of the archipelago lies on the Asian continental shelf. The Malay Archipelago was more frequently associated with Oceania during the 19th century, when the term was first coined. Many inhabitants in the Malay Archipelago are Austronesians, sharing genetic and linguistic affinities to the Melanesian, Micronesian and Polynesian inhabitants of Oceania, who also fall under the Austronesian umbrella. However, the Austronesians of the Malay Archipelago had significant contact with mainland Asia during prehistoric times, unlike with the Austronesians and Indigenous Australians of Oceania, who were isolated from the culture of Asia and the eastern world. Epeli Hauʻofa, a scholar of Tongan and Fijian descent, considered the Malay Archipelago separate from Oceania for this very reason. He wrote, "Before the advent of Europeans into the Pacific, our cultures were truly oceanic, in the sense that the sea barrier shielded us for millennia from the great cultural influences that raged through continental land masses and adjacent islands. This prolonged period of isolation allowed for the emergence of distinctive oceanic cultures with the only non-oceanic influences being the original cultures that the earliest settlers brought with them when they entered the vast, uninhabited region. Scholars of antiquity may raise the issue of continental cultural influences on the western and northwestern border islands of Oceania, but these are exceptions, and the Asian mainland influences were largely absent until the modern era. On the eastern extremity of the region there were some influences from the Americas, but these were minimal. It is for these reasons that Pacific Ocean islands from Japan, through the Philippines and Indonesia, which are adjacent to the Asian mainland, do not have oceanic cultures, and are therefore not part of Oceania. This definition of our region delineates us clearly from Asia and the pre-Columbian Americas and is based on our own historical developments, rather than on other people's perceptions of us."

The United Nations and The World Factbook categorize the Australian Indian Ocean external territories of Christmas Island and Cocos (Keeling) Islands (both geographically adjacent to Java) as being part of Oceania, rather than Asia. The islands lie within the bounds of the Australian Plate, and were uninhabited prior to European discovery in the 17th century. They have oceanic geology, making them distinct from both mainland Asia and mainland Australia.

Japan possesses the Bonin Islands (also known as the Ogasawara Islands), the Volcano Islands, and three remote islets ( Nishinoshima, Minami-Tori-shima and Okinotorishima), all governed collectively as Ogasawara Village, which is an administrative division consisting of scattered island atolls located in the Pacific Ocean. These mostly uninhabited islands are located at some distance southeast of the Japanese archipelago. Owing to the location and oceanic nature of these islands, they are sometimes considered to be a part of Oceania as well. The islands are within the Oceanian biogeographical realm, unlike the rest of Japan, and may have been inhabited by Micronesians around 2,000 years ago. Their official discovery came much later in the 16th century, through Europeans. The most remote island within this group, Minami-Tori-shima (also known as Marcus Island) is nearly 2,000 km removed from Tokyo, and is geographically closer to the Micronesian territories of Guam and Northern Mariana Islands. Inhabitants of the Ryukyu Islands, on the periphery of the main Japanese archipelago, are sometimes associated with Austronesians. The islands are geologically and historically linked with Asia, and are excluded from most definitions of Oceania, along with the similarly non-oceanic Japanese archipelago, which is not associated with Austronesians. To the north of Japan is the disputed Kuril Islands, currently administered by Russia. Usually, these islands are associated with the Russian Far East. This is primarily as a result of their non-tropical biogeography, and their inhabitants, who are mostly ethnically Russian mainlanders.

Australia has a more developed economy than neighboring Pacific Island nations, and is occasionally associated with mainland Asia as a result of this, despite being geologically distinct and having no cultural links to it prior to European discovery. It has historically been included in definitions of Oceania, ever since the term was first coined in the early 1810s. In the 19th century, many geographers divided up Oceania into mostly racially-based subdivisions; ''Australasia'', ''Malaysia'' (encompassing the Malay Archipelago), ''Melanesia'', ''Micronesia'' and ''Polynesia''. Australia, Guam and Northern Mariana Islands currently compete in the Asian Football Confederation (AFC), with Australia and Northern Mariana Islands having originally been part of the Oceania Football Confederation (OFC). Guam was never an official OFC member, although they exclusively played against teams from Oceania prior to joining the AFC. The presence of these teams in the AFC is not necessarily related to geography or politics, but rather because the Asian Football Confederation have far more resources than the Oceania Football Confederation. All three are members of the Pacific Islands Forum, the major governing body for the Oceania region, with Australia being a founding member in 1971. Guam and Northern Mariana Islands have had similar histories to the rest of Micronesia, and are biogeographically and geologically distinct from mainland Asia. Palau made an unsuccessful attempt to join the Asian Football Confederation in 2009. They too share much of the same history as the rest of Micronesia, and are a member of the Pacific Islands Forum.

Taiwan has at times been associated with Oceania, not only because of their loose status as a Pacific Island, but also because of their indigenous population, who are related to the natives of Oceania. In 2010, Australian historian Bronwen Douglas claimed in ''The Journal of Pacific History'' that "a strong case could be made for extending Oceania to at least Taiwan, the homeland of the Austronesian language family whose speakers colonized significant parts of the region about 6,000 years ago." Definitions of Oceania which include Taiwan are extremely rare because Taiwan has historical ties to mainland Asia, Taiwan is close to China (being 180 km away), and Taiwan lies on the continental shelf of Asia. Taiwan was formerly a member of the Oceania Football Confederation; this was for political reasons: It was forced to compete against teams from Oceania because China, its political administrator, did not recognize its sovereignty and would not compete against them. It was a member from 1975 to 1989, but now competes as part of the Asian Football Confederation. Taiwan, Japan and most of the nations in the Malay Archipelago are dialogue partners of the Pacific Islands Forum, but none have full membership, only Australia, New Zealand and the island states in Polynesia, Melanesia and Micronesia do.

Asia and Europe

The boundary between Asia and Europe is unusual among continental boundaries because of its largely mountain-and-river-based characteristics north and east of the Black Sea. Asia and Europe are considered separate continents for historical reasons; the division between the two goes back to the early Greek geographers.

In the modern sense of the term "continent", Eurasia is more readily identifiable as a "continent", and Europe has occasionally been described as a subcontinent of Eurasia.

Mainland

History

The threefold division of the Old World into Africa, Asia, and Europe has been in use since the 6th century BC by early Greek geographers such as Anaximander and Hecataeus.

Anaximander placed the boundary between Asia and Europe along the Phasis River (the modern Rioni in Georgia in the Caucasus Mountains), from Rioni mouth in Poti on the Black Sea coast, through the Surami Pass and along the Kura River to the Caspian Sea, a convention still followed by Herodotus in the 5th century BC.

As geographic knowledge of the Greeks increased during the Hellenistic period, this archaic convention was revised, and the boundary between Asia and Europe was now considered to be the Tanais (the modern Don River). This is the convention used by Roman era authors such as Posidonius, Strabo and Ptolemy.

Throughout the Middle Ages and into the 18th century, the traditional division of the landmass of Eurasia into two continents, Asia and Europe, followed Ptolemy, with the boundary following the Turkish Straits, the Black Sea, the Kerch Strait, the Sea of Azov and the Don (known in antiquity as the Tanais). But maps produced during the 16th to 18th centuries tended to differ in how to continue the boundary beyond the Don bend at Kalach-na-Donu (where it is closest to the Volga, now joined with it by the Volga–Don Canal), into territory not described in any detail by the ancient geographers.

Philip Johan von Strahlenberg in 1725 was the first to depart from the classical Don boundary by drawing the line along the Volga, following the Volga north until the Samara Bend, along Obshchy Syrt (the drainage divide between the Ural and Volga rivers) and then north along the Ural Mountains. The mapmakers continued to differ on the boundary between the lower Don and Samara well into the 19th century. The 1745 atlas published by the Russian Academy of Sciences has the boundary follow the Don beyond Kalach as far as Serafimovich before cutting north towards Arkhangelsk, while other 18th- to 19th-century mapmakers such as John Cary followed Strahlenberg's prescription. To the south, the Kuma–Manych Depression was identified circa 1773 by a German naturalist, Peter Simon Pallas, as a valley that, once upon a time, connected the Black Sea and the Caspian Sea, and subsequently was proposed as a natural boundary between continents.

By the mid-19th century, there were three main conventions, one following the Don, the Volga–Don Canal and the Volga, the other following the Kuma–Manych Depression to the Caspian and then the Ural River, and the third abandoning the Don altogether, following the Greater Caucasus watershed to the Caspian. The question was still treated as a controversy in geographical literature of the 1860s, with Douglas Freshfield advocating the Caucasus crest boundary as the best possible, citing support from various modern geographers.

In Russia and the Soviet Union, the boundary along the Kuma–Manych Depression was the most commonly used as early as 1906. In 1958, the Soviet Geographical Society formally recommended that the boundary between Asia and Europe be drawn in textbooks from Baydaratskaya Bay, on the Kara Sea, along the eastern foot of the Ural Mountains, then following the Ural River until the Mugodzhar Hills, and then the Emba River

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