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Continental Europe

Continental Europe

Continental Europe, also referred to as mainland Europe or simply the continent, refers to the continent of Europe, explicitly excluding European islands and peninsulae. Notably, in British English and Hiberno-English usage, the term means Europe excluding the British Isles.

The English concept

In the English mind Continental Europe is foremost represented by the Benelux, Germany, and especially France.

The Nordic concept

In Nordic usage, the British Isles, Scandinavia, Iceland and Finland are excluded.

Continent

shows land mass with minimal distortion as only one continuous continent]] A continent (Latin continere, "to hold together") is a large continuous land mass. There are several conceptions of what a continent is, geographic, geologic, and tectonic.

Geographic continents

Because geography is defined by local convention, there are several conceptions as to which landmasses qualify as continents. There are names for six, but America is often divided, and Europe is often united with Asia. Ignoring cases where Antarctica is omitted, there are half a dozen lists. tectonic The 7-continent model is usually taught in Western Europe, the United States, Australia, and much of Asia. In Canada, the government-approved [http://atlas.gc.ca/site/english/maps/reference/international/world/referencemap_image_view Atlas of Canada] names 7 continents and teaches Oceania instead of Australia. The 6-continent combined-America model is taught in Iran, and Latin America. The 6-continent Eurasia model is preferred by the scientific community, and as such is commonly found in all parts of the world, but is especially used in Russia and other countries of Eastern Europe, and in Japan. Historians may use the 5-continent model in which North Africa is separated from Sub-Saharan Africa and attached to Eurasia (Jared Diamond) or the 4-continent Afro-Eurasian model (Andre Gunder Frank). In its original sense, "continent" meant (and still means) mainland. In the Greco-Roman world, there was but one known, the Continent, which we today call the Old World. 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." As late as 1727 Ephraim Chambers wrote in his Cyclopædia, "The world is ordinarily divided into two grand continents: the old and the new." However, since Classical times this Continent was divided into "peninsulas" which also came to be called continents, since they were great land masses themselves. Through the Middle Ages, there were three such continents in the Western conception: Europe, Africa, and Asia. The European discovery of America in 1492 made four; and Australia in 1606 would make five, though not right away: as late as 1813 geographers wrote of Australia as "New Holland, an immense Island, which some geographers dignify with the appellation of another continent". However, dividing America in two was commonplace by this time, and would also produce a fifth continent. The idea of the Five Continents is still strong in Europe and Asia, and is represented by the five rings on the Olympic flag. Antarctica was sighted in 1820, for the sixth and last continent to be given a separate name, though a great "antarctic" (antipodean) landmass had been anticipated for millennia. Dividing the Americas now made seven continents, nicely symmetrical with the magical number of the Seven Seas, Seven Heavens, and the seven heavenly bodies that gave their names to the seven days of the week. However, this division never appealed to Latin America, which saw itself spanning America as a single landmass, and there the conception of six continents remains, as it does in scattered other countries such as Japan. From a modern perspective, the continent with the least reason for separate recognition is Europe, and in scientific circles people generally prefer to subsume Europe and Asia into Eurasia. This appealed to Russia, which spans Eurasia, and in Russia and (at least formerly) in Eastern Europe, Eurasia is or was taught as being one of six continents. Geographers and historians often find it useful to define larger land masses connected by land bridges: # Africa-Eurasia (also called Eurafrasia): the combined land mass of Africa and Eurasia; # America (or the Americas): the combined land mass of North America and South America; # Laurasia: the combined land mass of Eurasia and North America, which were connected by Beringia during the Ice Age; # Sahul: the combined land mass of Australia, New Guinea, and Tasmania during the Ice Age. That is, during the last Ice Age, there were three large landmasses: Africa-Eurasia + America (which has no name), Sahul, and Antarctica. These larger land masses are usually considered supercontinents rather than continents, however. In the last century it has also become conventional to subdivide Eurasia into the regions of Europe, Asia, and the Middle East. America is often divided into the regions of North America, Central America, and South America. Continents are also sometimes subdivided into subcontinents that are isolated by geological features. The prototype of this is the Indian subcontinent. Islands are usually considered to belong geographically to the continent they are closest to. The Coral Sea and South Pacific islands may be associated with Australia/Australasia to form the "continent" of Oceania (though the Pacific islands without Australia are also called Oceania). The British Isles have always been considered part of Europe, and Greenland is considered part of North America. When the Continent is referred to without clarification by a speaker of British English, it is usually presumed to mean Continental Europe, that is Europe, explicitly excluding Great Britain and Ireland. The Continental United States excludes Hawaii. Contiguous or Co(n)terminous United States means the United States without Alaska or Hawaii (the "Lower 48"), but it is very common for people to say continental for contiguous. See also List of countries by continent, Satellite Images of Continents.

Geologic continents

Geologically, the surface of Earth consists of many tectonic plates, consisting of rigid lithospheric mantle and crust moving together over the much less viscous asthenosphere. Continental crust is primarily granitic in composition, overlain by sedimentary and metamorphic rocks. Much of the continental crust extends above sea level as dry land. Oceanic crust is basaltic in composition, and much thinner than continental crust, thus generally lying below sea level. Although from a human perspective shallow inland seas such as the Bering Sea appear to divide up land masses into continents, such ephemeral features do not define continents geologically. For instance, many times over the past few million years, the continents of Eurasia and America were connected by dry land. A geologic continent, therefore, is a continuous piece of continental crust, whether wet or dry at a particular time. As such, Laurasia and Africa-Arabia are one continent, which for the past three million years has also been linked to South America. This world-spanning land mass has no name except for the Classical meaning of "The Continent". The other large geologic continents are Sahul and Antarctica, but there are many so-called microcontinents as well: Madagascar, the Seychelles (the northern Mascarene Plateau), New Zealand, New Caledonia, etc., which are splinters of the ancient supercontinent of Gondwana. Note that volcanic Iceland is an exposed bit of oceanic crust at the mid-ocean ridge, and therefore not a microcontinent. Likewise, the British Isles, Sri Lanka, Borneo, and Newfoundland are integral parts of the Laurasian continent which happen to be separated by shallow (and temporary) inland seas flooding its margins.

Tectonic plates

During the 20th century, it became accepted by geologists that continents move location on the face of the planet over the geologic timescale, a process known as continental drift, explained by the theory of plate tectonics. It is the tectonic plates that have drifted, broken apart and joined together over time to give rise to the continents we now recognize. Consequently, in the geological past and prior to the present continents, other continents existed - see :Category:Historical continents. Occasionally there are calls for the continents to be defined by the tectonic plates that carry them. However, not only would this make Arabia on the Arabian plate and India on the Indian plate continents, but also Central America on the Caribbean plate and California on the Pacific plate, and this definition has never been widely accepted.

Europe

:This article is about the continent. For other meanings, see Europe (disambiguation). Europe is geologically and geographically a peninsula or subcontinent, forming the westernmost part of Eurasia. It is conventionally considered a continent, which, in this case, is more of a cultural distinction than a geographic one. It is bounded to the north by the Arctic Ocean, to the west by the Atlantic Ocean and to the south by the Mediterranean and Black Seas and the Caucasus. Europe's boundary to the east is vague, but has traditionally been given as the Ural Mountains and Caspian Sea to the southeast: the Urals are considered by most to be a geographical and tectonic landmark separating Asia from Europe. :See also Continent, Bicontinental country, and Table of European territories and regions. Table of European territories and regions Table of European territories and regions Europe is the world's second-smallest continent in terms of area, covering around 10,790,000 km² (4,170,000 sq mi) or 2.1% of the Earth's surface, and is only larger than Australia. In terms of population, it is the third-largest continent (Asia and Africa are larger) with a population of more than 700,000,000, or about 11% of the world's population.

Etymology

Africa.]] In Greek mythology, Europa was a Phoenician princess who was abducted by Zeus in bull form and taken to the island of Crete, where she gave birth to Minos. For Homer, Europé (Greek: Ευρωπη; see also List of traditional Greek place names) was a mythological queen of Crete, not a geographical designation. Later Europa stood for mainland Greece, and by 500 BC its meaning had been extended to lands to the north. The Greek term Europe has been derived from Greek words meaning broad (eurys) and face (ops) -- broad having been an epitheton of Earth herself in the reconstructed Proto-Indo-European religion; see Prithvi (Plataia). A minority, however, suggest this Greek popular etymology is really based on a Semitic word such as the Akkadian erebu meaning "sunset" (see also Erebus). From the Middle Eastern vantagepoint, the sun does set over Europe, the lands to the west. Likewise, Asia is sometimes thought to have derived from the Akkadian word asu, meaning "sunrise", and is the land to the east from a Mesopotamian perspective.

History

Europe has a long history of cultural and economic achievement, starting as far back as the Palaeolithic, although this is true for the rest of the Old World as well. The recent discovery at Monte Poggiolo, Italy, of thousands of hand-shaped stones, tentatively carbon-dated to 800,000 years ago, may prove to be of particular importance. The origins of Western democratic and individualistic culture are often attributed to Ancient Greece, though numerous other distinct influences, in particular Christianity, can also be credited with the spread of concepts like egalitarianism and universality of law. The Roman Empire divided the continent along the Rhine and Danube for several centuries. Following the decline of the Roman Empire, Europe entered a long period of changes arising from what is known as the Age of Migrations. That period has been known as the "Dark Ages" to Renaissance thinkers. During this time, isolated monastic communities in Ireland and elsewhere carefully safeguarded and compiled written knowledge accumulated previously. The Renaissance and the New Monarchs marked the start of a period of discovery, exploration, and increase in scientific knowledge. In the 15th century Portugal opened the age of discoveries, soon followed by Spain. They were later joined by France, the Netherlands and the United Kingdom in building large colonial empires with vast holdings in Africa, the Americas, and Asia. After the age of discovery, the ideas of democracy took hold in Europe. Struggles for independence arose, most notably in France during the period known as the French Revolution. This led to vast upheaval in Europe as these revolutionary ideas propagated across the continent. The rise of democracy led to increased tensions within Europe on top of the tensions already existing due to competition within the New World. The most famous of these conflicts was when Napoleon Bonaparte rose to power and set out on a conquest, forming a new French empire that soon collapsed. After these conquests Europe stabilised, but the old foundations were already beginning to crumble. The Industrial Revolution started in the United Kingdom in the late 18th century, leading to a move away from agriculture, much greater general prosperity and a corresponding increase in population. Many of the states in Europe took their present form in the aftermath of World War I. From the end of World War II through the end of the Cold War, Europe was divided into two major political and economic blocks: Communist nations in Eastern Europe and capitalist countries in Western Europe. Around 1990, with the fall of the Berlin Wall, the Eastern bloc disintegrated.

Geography and extent

Eastern bloc Geographically Europe is a part of the larger landmass known as Eurasia. The continent begins at the Ural Mountains in Russia, which define Europe's eastern boundary with Asia. The southeast boundary with Asia isn't universally defined. Most commonly the Ural or, alternatively, the Emba river can serve as possible boundaries. The boundary continues with the Caspian Sea, and then the Araxes river in the Caucasus, and on to the Black Sea; the Bosporus, the Sea of Marmara, and the Dardanelles conclude the Asian boundary. The Mediterranean Sea to the south separates Europe from Africa. The western boundary is the Atlantic Ocean, but Iceland, much farther away than the nearest points of Africa and Asia, is also often included in Europe. There is ongoing debate on where the geographical centre of Europe is. At times "Europe" is defined with greater regard to political, economic, and other cultural considerations. This has led to there being several different Europes that are not always identical in size, including or excluding countries according to the definition of Europe used. Almost all European countries are members of the Council of Europe, the exceptions being Belarus, and the Holy See (Vatican City). The idea of the European continent is not held across all cultures. Some non-European geographical texts refer to the continent of Eurasia, or to the European peninsula, given that Europe is not surrounded by sea. In the past concepts such as Christendom were deemed more important. In another usage, Europe is increasingly being used as a short-form for the European Union (EU) and its members, currently consisting of 25 member states. A number of other European countries are negotiating for membership, and several more are expected to begin negotiations in the future (see Enlargement of the European Union).

Physical features

In terms of shape, Europe is a collection of connected peninsulas. The two largest of these are "mainland" Europe and Scandinavia to the north, divided from each other by the Baltic Sea. Three smaller peninsulas (Iberia, Italy and the Balkans) emerge from the southern margin of the mainland into the Mediterranean Sea, which separates Europe from Africa. Eastward, mainland Europe widens much like the mouth of a funnel, until the boundary with Asia is reached at the Ural Mountains. Land relief in Europe shows great variation within relatively small areas. The southern regions, however, are more mountainous, while moving north the terrain descends from the high Alps, Pyrenees and Carpathians, through hilly uplands, into broad, low northern plains, which are vast in the east. This extended lowland is known as the Great European Plain, and at its heart lies the North German Plain. An arc of uplands also exists along the northwestern seaboard, beginning in the western British Isles and continuing along the mountainous, fjord-cut spine of Norway. This description is simplified. Sub-regions such as Iberia and Italy contain their own complex features, as does mainland Europe itself, where the relief contains many plateaus, river valleys and basins that complicate the general trend. Iceland and the British Isles are special cases. The former is a land unto itself in the northern ocean which is counted as part of Europe, while the latter are upland areas that were once joined to the mainland until rising sea levels cut them off. Due to the few generalisations that can be made about the relief of Europe, it is less than surprising that its many separate regions provided homes for many separate nations throughout history.

Biodiversity

Having lived side-by-side with agricultural peoples for millennia, Europe's animals and plants have been profoundly affected by the presence and activities of man. With the exception of Scandinavia and northern Russia, few areas of untouched wilderness are today to be found in Europe, except for different natural parks. The main natural vegetation cover in Europe is forest. The conditions for growth are very favourable. In the north, the Gulf Stream and North Atlantic Drift warm the continent. Southern Europe could be described as having a warm, but mild climate. There are frequent summer droughts in this region. Mountain ridges also affect the conditions. Some of these (Alps, Pyrenees) are oriented east-west and allow the wind to carry large masses of water from the ocean in the interior. Others are oriented south-north (Scandinavian Mountains, Dinarides, Carpathians, Apennines) and because the rain falls primarily on the side of mountains that is oriented towards sea, forests grow well on this side, while on the other side, the conditions are much less favourable. Few corners of mainland Europe have not been grazed by livestock at some point in time, and the cutting down of the pre-agricultural forest habitat caused disruption to the original plant and animal ecosystems. Eighty to ninety per cent of Europe was once covered by forest. It stretched from the Mediterranean Sea to the Arctic Ocean. Though over half of Europe's original forests disappeared through the centuries of colonisation, Europe still has over one quarter of the world's forests - spruce forests of Scandinavia, vast pine forests in Russia, chestnut rainforests of the Caucasus and the cork oak forests in the Mediterranean. During recent times, deforestation has been stopped and many trees were planted. However, in many cases conifers have been preferred over original deciduous trees, because these grow quicker. The plantations and monocultures now cover vast areas of land and this offers very poor habitats for European forest dwelling species. The amount of original forests in Western Europe is just two to three per cent (in the European part of Russia five to ten per cent). The country with the smallest forest-covered area is Ireland (eight per cent), while the most forested country is Finland (72 per cent). In "mainland" Europe, deciduous forest prevails. The most important species are beech, birch and oak. In the north, where taiga grows, a very common tree species is the birch tree. In the Mediterranean, many olive trees have been planted, which are very well adapted to its arid climate. Another common species in Southern Europe is the cypress. Coniferous forests prevail at higher altitudes up to the forest boundary and as one moves north within Russia and Scandinavia, giving way to tundra as the Arctic is approached. The semi-arid Mediterranean region hosts much scrub forest. A narrow east-west tongue of Eurasian grassland—the steppe—extends eastwards from Ukraine and southern Russia and ends in Hungary and traverses into taiga to the north. Glaciation during the most recent ice age and the presence of man affected the distribution of European fauna. As for the animals, in many parts of Europe most large animals and top predator species have been hunted to extinction. The woolly mammoth and aurochs were extinct before the end of the Neolithic period. Today wolves (carnivores) and bears (omnivores) are endangered. Once they were found in most parts of Europe. However, deforestation caused these animals to withdraw further and further. By the Middle Ages the bears' habitats were limited to more or less inaccessible mountains with sufficient forest cover. Today, the brown bear lives primarily in the Balkan peninsula, in the North and in Russia; a small number also persist in other countries across Europe (Austria, Pyrenees etc.), but in these areas brown bear populations are fragmented and marginalised because of the destruction of their habitat. In the far North of Europe, polar bears can also be found. The wolf, the second largest predator in Europe after the brown bear, can be found primarily in Eastern Europe and in the Balkans. Other important European carnivores are Eurasian lynx, European wild cat, foxes (especially the red fox), jackal and different species of martens, hedgehogs, different species of snakes (vipers, grass snake...), different birds (owls, hawks and other birds of prey) Important European herbivores are snails, amphibians, fish, different birds, and mammals, like rodents, deers and roe deers, boars, and living in the mountains, marmots, steinbocks, chamoises among others. Sea creatures are also an important part of European flora and fauna. The sea flora is mainly phytoplankton. Important animals that live in European seas are zooplankton, molluscs, echinoderms, different crayfish, squids and octopuses, fish, dolphins, and whales. Some animals live in caves, for example proteus and bats.

Demographics

Almost all of Europe was possibly settled before or during the last ice age ca. 10,000 years ago. Neanderthal man and modern man coexisted during at least some of this time. Roman road building helped with the interbreeding of the native Europeans' genetics. In contemporary times Europe has one of the lowest inbreeding rates in the world because of an extensive transport network paired with open borders. Europe passed well over 600 million people before the turn of the 20th century, but now is entering a period of population decline, for a variety of social factors.

Territories and divisions

Political divisions

Independent states

interbreeding on this map.]] :See also: Table of European territories and regions The following independent states have territory in Europe: ² Azerbaijan and Georgia lie partly in Europe according to the usual definition which consider the crest of the Caucasus as the boundary with Asia.
³ Kazakhstan's European territory consists of a portion west of the Ural and Emba Rivers.
⁴ The name of this state is a matter of international dispute. See Republic of Macedonia for details.
⁵ Those territories of Russia lying west of the Ural Mountains are considered as part of Europe.
⁶ State union of Republic of Serbia and the Republic of Montenegro.
⁷ European Turkey comprises territory to the west and north of the Bosporus and the Dardanelles straits.
^{2, 3, 5, 7} See Countries in both Europe and Asia for details.

Dependent territories

The European territories listed below are recognised as being culturally and geographically defined. Most have a degree of autonomy. In the list below, each territory is followed by its legal status.
- Faroe Islands (autonomous region of Denmark)
- Gibraltar (UK overseas territory)
- Guernsey (British crown dependency)
- Jersey (British crown dependency)
- Man, Isle of (British crown dependency)
- Svalbard (autonomous region of Norway) Note that this is not a list of all dependencies of all European countries. Dependencies located on other continents are not listed.

Unilaterally seceded territories

Following are breakaway regions of independent states. These regions have declared and de facto achieved independence, but this is not recognised de jure by their home state or by the other independent states.
- Abkhazia (from Georgia)
- Nagorno-Karabakh (disputed by Armenia and Azerbaijan)
- South Ossetia (from Georgia)
- Transnistria (from Moldova)

Territories under United Nations administration

- Kosovo and Metohia (province of Serbia)

Table of European territories and regions

Notes:
¹ Continental regions as per UN categorisations/map. Depending on definitions, various territories cited below (notes 2-6, 8, 9) may be in one or both of Europe and Asia.
² Armenia is sometimes considered a transcontinental country in Eastern Europe and Western Asia (as per UN categorisations/map).
³ Azerbaijan is often considered a transcontinental country in Western Asia (UN region) and Eastern Europe; population and area figures are for European portion only.
⁴Cyprus is often considered a transcontinental country in Western Asia (UN region) and Southern Europe; population and area figures are for de jure Greek-administered portion only.
⁵Georgia is often considered a transcontinental country in Western Asia (UN region) and Eastern Europe; population and area figures are for European portion only.
⁶Kazakhstan is sometimes considered a transcontinental country in Central Asia (UN region) and Eastern Europe.
⁷Netherlands population for July 2004; Amsterdam is the de facto capital, while The Hague is the country's administrative seat.
⁸Russia is generally considered a transcontinental country in Eastern Europe (UN region) and Asia; population and area figures are for European portion only.
⁹Turkey is generally considered a transcontinental country in Western Asia (UN region) and Southern Europe; population and area figures are for European portion only, including all of Istanbul.

Linguistic and cultural regions

The sub-division in several linguistic and cultural regions is much less subjective than the geographical sub-division, since they correspond to people's cultural connections. There are three main groups:

Germanic Europe

Germanic Europe, where Germanic languages are spoken. This area corresponds more or less to north-western Europe and some parts of central Europe. The main religion of the region is Protestantism, even if there are also some countries with Catholic majority (particularly Austria). This region consists of: United Kingdom, Ireland, Iceland, Germany, Austria, Netherlands, Denmark, Sweden, Norway, Luxembourg, Liechtenstein, the Faroe Islands, German-speaking Switzerland, the Flemish part of Belgium, the Swedish-speaking municipalities of Finland, and the South Tyrol part of Italy.

Latin Europe

Latin Europe, where the Romance languages are spoken. This area corresponds more or less to south-western Europe, with the exception of Romania and Moldova which are situated in Eastern Europe. The major religion is Catholicism, except in Romania and Moldova. This area consists of: Italy, Spain, Portugal, France, Romania, Moldova, French-speaking Belgium and French speaking Switzerland, and Italian and Romansh speaking Switzerland as well.

Slavic Europe

Slavic Europe, where Slavic languages are spoken. This area corresponds, more or less, to Central and Eastern Europe. The main religions are Orthodox Christianity and Catholicism, with large Muslim populations in some parts formerly ruled by the Ottoman Empire. This area consists of: Belarus, Bosnia and Herzegovina, Bulgaria, Croatia, the Czech Republic, the Republic of Macedonia, Poland, Russia, Serbia and Montenegro, Slovakia, Slovenia and Ukraine.

Others

Outside of these three main groups we can find:
- The Celtic nations: Scotland, Wales, Northern Ireland, Cornwall (within the United Kingdom); the Isle of Man (a British Crown dependency); the Republic of Ireland; Brittany (within France). These are all nations where a Celtic language is spoken, or was spoken into modern times, and there is a degree of shared culture (see Pan Celticism). Also considered Celtic nations, by some, are both Galicia (Spain) and Asturias, (within Spain), whose own Celtic language died out several hundred years ago.
- Greece, the only country of "Hellenic Europe".In Hellenic Europe we can consider also the Greek Cypriot community It is sometimes associated with the Latin countries, due to the geographical and cultural ties to the Mediterranean Sea, and sometimes to the Slavic-Orthodox part of Europe due to the importance or Orthodoxy in Greece.
- Armenia has a language that constitutes a separate branch of Indo-European family of languages. The Armenian language is spoken in Armenia and other European countries with Armenian communities (such as France, Greece, Belgium, Russia, Germany etc.).
- Ibero-Caucasian, a group that includes ethnic groups throughout the Caucasus region (both North and South). Ibero-Caucasian languages are not linked to the Indo-European languages. This group includes Georgians, Abkhaz, Chechens, Balkars, and a number of other smaller ethnic groups that reside in the Caucasus.
- Turkey, having an Altaic language not of Indo-European origin, and mainly a Muslim country, unlike the main regions' different versions of Christianity.
- Hungary, having a language related to Finnish and Estonian. Due to its location Hungary is normally grouped with Central or Eastern European countries.
- Finland and Estonia, whose languages are related to Hungarian. Despite this connection (not a close one), Finland and Estonia are normally associated with northern European countries (of an even farther connection).

External links

-
- [http://www.democracyineurope.com Democracy in Europe]
- [http://www.holidayhomeseuro.com European holiday homes]
- [http://phoenicia.org/europa.html Europa, the Phoenician Princess] - overwhelmed Zeus with love
- [http://www.europestartpage.com EUROPEstartpage.com, travel and city guide to Europe]
- [http://www.limitlesseurope.com LimitlessEurope.com : information guide to Europe]
- [http://earthobservatory.nasa.gov/Newsroom/NewImages/images.php3?img_id=13266 Europe at Night] at NASA Earth Observatory
- [http://www.geog.tamu.edu/~prout/GVmidtermTwo.html Regions of Europe]
- [http://p086.ezboard.com/balbanau Evropa / Europa / Europe]
- [http://www.eufpc.org EUFPC European Foreign Policy Council]
- [http://www.itmaps.com/?modul=map Map of Europe]
- [http://www.freeworldmaps.net/europe/index.html Physical Map of Europe]
- [http://www.parks.it/europa/Eindex.html Parks in Europe] - National parks, nature parks, reserves and other protected areas. Category:Continents als:Europa roa-rup:Evropa zh-min-nan:Europa ko:유럽 ms:Eropah ja:ヨーロッパ simple:Europe th:ทวีปยุโรป

Island

in New York, USA]] An island or isle is any piece of land that is completely surrounded by water. Very small islands are called islets. Although seldom adhered to, it is also proper to call an emergent land feature on an atoll an islet, since an atoll is a type of island. A key or cay is also another name for a relatively small island. Groups of related islands are called archipelagos. There are three main types of islands: continental islands, river islands, and volcanic islands. There are also some artificial islands. The word island derives ultimately from the Old English word igland. It was originally spelled phonetically: iland. The letter "s" was added out of the mistaken belief that it derived from isle (< Old French < Latin insula) + land, where no such etymological relationship existed.

Continental islands

Continental islands are bodies of land that are connected by the continental shelf to a continent. That is, these islands are part of an adjacent continent and are located on the continental shelf of that continent. Examples include Greenland and Sable Island off North America, Barbados and Trinidad off South America, Sicily off Europe, Sumatra and Java off Asia, New Guinea and Tasmania off Australia. A special type of continental island is the microcontinental island, which results when a continent is rifted. The best example is Madagascar off Africa. The Kerguelen Islands and some of the Seychelles are also examples. Another subtype is the barrier island: accumulations of sand on the continental shelf.

River islands

River islands occur in river deltas and in large rivers. They are caused by deposition of sediment at points in the flow where the current loses some of its carrying capacity. In essence, they are river bars, isolated in the stream. While some are ephemeral, and may disappear if the river's water volume or speed changes, others are stable and long-lived.

Volcanic islands

Volcanic islands are built by volcanoes. Mid-ocean examples are not geologically part of any continent. One type of volcanic island is found in a volcanic island arc. These islands arise from volcanoes where the subduction of one plate under another is occurring. Examples include the Mariana Islands, the Aleutian Islands, and most of Tonga in the Pacific Ocean. Some of the Lesser Antilles and the South Sandwich Islands are the only Atlantic Ocean examples. Another type of volcanic island occurs where an oceanic rift reaches the surface. There are two examples: Iceland, which is the world's largest volcanic island, and Jan Mayen—both are in the Atlantic. The last type of volcanic island are those formed over volcanic hotspots. A hot spot is more or less stationary relative to the moving tectonic plate above it, so a chain of islands results as the plate drifts. Over long periods of time, this type of island is eventually eroded down and "drowned" by isostatic adjustment, becoming a seamount. Plate movement across a hot-spot produces a line of islands oriented in the direction of the plate movement. An example is the Hawaiian Islands, from Hawaii to Kure, which then extends beneath the sea surface in a more northerly direction as the Emperor Seamounts. Another chain with similar orientation is the Tuamotu Archipelago; its older, northerly trend is the Line Islands. The southernmost chain is the Austral Islands, with its northerly trending part the atolls in the nation of Tuvalu. Tristan da Cunha is an example of a hotspot volcano in the Atlantic Ocean. An atoll is an island formed from a coral reef that has grown on an eroded and submerged volcanic island. The reef rises above the surface of the water and forms a new island. Atolls are typically ring-shaped with a central, shallow lagoon. Examples include the Maldives in the Indian Ocean and Bora Bora in the Pacific.

External links

- [http://www.un.org/Depts/los/convention_agreements/texts/unclos/part8.htm Definition of island] from United Nations Convention on the Law of the Sea Category:Islands Category:Landforms zh-min-nan:Tó-sū ko:섬 ms:Pulau ja:島 simple:Island th:เกาะ

Peninsula

A peninsula (Latin, literally meaning almost island) is a geographical formation consisting of an extension of land from a larger body, surrounded by water on three sides. A peninsula can also be a headland, cape, promontory, bill, or spit.

Peninsulas of the World

Eurasia

Continental Europe

- Apsheron, Azerbaijan
- Brittany, France
- Butjadingen, Germany
- Cotentin Peninsula, France
- Crimea, Ukraine
- Gallipoli, Turkey
- Grenen, Denmark
- Hel Peninsula, Poland
- Italian Peninsula, Italy
- Jutland Peninsula, northern Germany and Denmark
- Peniche Peninsula, Portugal
- Piran, Slovenia
- Saint-Tropez, on the French Riviera
- Walcheren, Netherlands
- Zuid-Beveland, Netherlands

Balkan peninsula

- Chalkidiki, Greece
- Pilio, Greece
- Kassandra, Greece
- Mani Peninsula, Greece
- Mount Athos, Greece
- Peloponnesos, Greece
- Sithonia, Greece
- Zadar, Croatia
- Istria, Croatia
- Peljesac peninsula, Croatia

Iberian Peninsula

encompassing the whole of Spain and Portugal
- Cabo Espichel, Portugal
- Cabo de São Vicente, Portugal
- Tróia, Portugal
- Gibraltar (British Territory)

Scandinavian Peninsula

encompassing Sweden and Norway
- Svaerholthalvoya, Norway
- Varangerhalvoya, Norway

Indian subcontinent

- Mumbai city
- Kathiawar Peninsula, Gujarat

East Asia

- Malay Peninsula
- Kowloon Peninsula, Hong Kong (China)
- Leizhou Bandao, China
- Liaodong Bandao, China
- Shandong Bandao, China
- Ca Mau Peninsula, Vietnam

Korean Peninsula

The whole land mass encompassing South and North Korea is a Peninsula

Japan

Kyushu:
- Nishi-sonogi-hanto
- Kunisaki-hato Honshu:
- Shiriya-zaki
- Oshika-hanto
- Noto-hanto
- Oga-hanto
- Miura-hato
- Boso-hanto
- Inubo-zaki
- Izu-hanto

Philippines

- Bataan Peninsula
- Bondoc peninsula, Luzon
- Zamboanga, Mindanao
- San Ildefonso peninsula, Luzon

Indonesia

- Poluostrov Yamau
- Semenanjung Blambangan, Java,
- Semenanjung Minahassa, Sulawesi
- East Peninsula, Sulawesi
- South-east Peninsula, Sulawesi
- South Peninsula, Sulawesi

Madeira Islands

(Portuguese Territory)
- Ponta de São Lourenço

The Americas

United States of America

- Alaska Peninsula, Alaska
- Cape Cod, Massachusetts
- Cleveland peninsula, Alaska
- Delmarva Peninsula, encompassing parts of Delaware, Maryland, and Virginia
- Door Peninsula, Wisconsin, in Lake Michigan
- Florida Peninsula, encompassing most of Florida state
- Kenai Peninsula, Alaska
- Keweenaw Peninsula, Michigan, in Lake Superior
- Key Peninsula, Washington, in Puget Sound
- Leelanau Peninsula, Michigan, in Lake Michigan
- Lower Peninsula, Michigan
- Middle Peninsula, Virginia, on the western shore of Chesapeake Bay
- Mokapu, Hawaii
- Northern Neck, Virginia, on the western shore of Chesapeake Bay
- Old Mission Peninsula, Michigan, in Grand Traverse Bay
- Olympic Peninsula, Washington
- Pinellas Peninsula, Florida
- Sandy Hook, New Jersey
- San Francisco Peninsula, California
- Upper Peninsula, Michigan
- Virginia Peninsula, Virginia, on the western shore of Chesapeake Bay

Canada

Greenland

(Danish Territory)
- Alfred Wegeners Halvo
- Hayes Halvo
- Ingnerit
- Nuussuaq Halvo
- Svartenhuk Halvo

Mexico

- Baja California peninsula, Mexico, containing the state of Baja California and state of Baja California Sur
- Yucatán peninsula, partly separating the Gulf of Mexico from the Caribbean Sea

Central America

- Península de Azuero, Panama

South America

- Paraguana, Venezuela
- Araya Peninsula, Venezuela
- Brunswick Peninsula, Chile
- Guajira Peninsula, Colombia
- Paracas Peninsula, Peru
- Paria Peninsula, Venezuela
- Taitao Peninsula, Chile
- Verde Peninsula, Argentina
- Valdes Peninsula, Argentina

Caribbean

- Barrio Obrero, Puerto Rico, despite its name, it is also a peninsula

Australia & Oceania

Australia

Australia
- Beecroft Peninsula, New South Wales
- Cape York Peninsula, Queensland
- Cobourg Peninsula, Northern Territory
- Eyre Peninsula, South Australia
- Fleurieu Peninsula, South Australia
- Freycinet Peninsula, Tasmania
- Inskip Peninsula, Queensland
- Jervis Bay Territory
- Mornington Peninsula, Victoria
- Tasman Peninsula, Tasmania
- Wilsons Promontory, Victoria
- Yorke Peninsula, South Australia
- Younghusband Peninsula, South Australia

New Zealand

- Banks Peninsula, South Island
- Bluff Peninsula, South Island
- Bream Head, North Island
- Cape Brett, North Island
- Cape Campbell, South Island
- Cape Foulwind, South Island
- Cape Kidnappers, North Island
- Cape Turnagain, North Island
- Coromandel Peninsula, North Island
- Farewell Spit, South Island
- Kaikoura Peninsula, South Island
- Karikari Peninsula, North Island
- Mahia Peninsula, North Island
- Miramar Peninsula, North Island
- Mount Maunganui, North Island
- Mount Nicaragua, North Island
- North Auckland Peninsula, North Island
- Otago Peninsula, South Island
- Tiwai Point, South Island
- Whangaparaoa Peninsula, North Island

Papua New Guinea

- Gazelle Peninsula, New Britain
- Huon

Africa

- Bakassi, Cameroon but disputed with Nigeria
- Buri Peninsula, Eritrea
- Cabo Blanco, Mauritania/Western Sahara
- Cape of Good Hope, South Africa
- Cap-Vert, Senegal
- Ceuta, Spain
- Punta Durnford, Western Sahara
- Raas Xaafuun peninsula/Ras Hafun, Somalia

Antarctica

- Antarctic Peninsula
- Edward VII Peninsula
- Fletcher Peninsula
- Fowler Peninsula
- Martin Peninsula ko:반도 ja:半島 simple:Peninsula zh-min-nan:Poàn-tó

British English

British English (BrE) is a term used to differentiate the form of the written English language in the United Kingdom from other forms of the English language. It is also used by some, particularly Americans, to describe the spoken versions of English used within England. The term is rarely heard within the United Kingdom. British people say that they speak English - but never British - and that others speak English with an accent, such as a 'South African accent'. When speaking, they will often drop the word "accent" and simply say Canadian, American, Jamaican and so on. A less ambiguous term is English English. Although British English can describe the formal written English used in the United Kingdom, the forms of spoken English used in the United Kingdom vary considerably more than in most other areas of the world where English is spoken. Dialects and accents vary not only within regions of the UK, for example in Scotland, Northern Ireland and Wales, but also within England. The written form of the language, as taught in schools, is universally Commonwealth English with a slight emphasis on a few words that might be more common in some areas than in others. For example, although the words "wee" and "small" are interchangeable, one is more likely to see "wee" written by a Scot than by a Londoner. For historical reasons dating back to the rise of London in the 9th century, the variety of language spoken in London and the East Midlands became the standard English within the Court and thus the form of language generally accepted for use in the law, government, literature and education of the British Isles. Like other forms of languages, the English used in Britain changes over time. Although British English is often used in the United States to denote the English spelling and lexicon used outside the US, the term Commonwealth English is more accurate for this purpose. The British spellings were most famously recorded in Samuel Johnson's A Dictionary of the English Language (1755). Historically, the widespread usage of English across the world is attributed to the power once held by the British Empire, and hence the most common form of English used by the British ruling class was the English used in south-east England (in the area around the capital city London, and the main English university towns of Oxford and Cambridge). This form of the language is associated with Received Pronunciation (RP), which is still regarded by many people outside the UK (especially in the United States) as "the British accent". From the second half of the 20th century to the present day, the preeminence of the English language has largely been linked to the economic, military and political dominance of the United States in world affairs, and American English is often regarded as the most prominent form of English in the world today, especially with the large amount of U.S. cultural products (such as films, books, and music) around the world, which is not matched in volume by those from other English-speaking nations. The form of English spoken and particularly written in the United Kingdom still has a major cultural influence on the English used in many Commonwealth countries, including Australia, South Africa, and India, as well as in the European Union. Although British English is taught and used in the former British colonies of Hong Kong, Singapore and Malaysia, American English is often taught in Chinese and Japanese schools, and in other schools throughout Asia.

-ise versus -ize

Words of the sort organize/organise and their derivatives can be spelt with either s or z in British English. The -ize forms are promoted by the Oxford English Dictionary. British English with -ize is sometimes known as OED spelling, and may be marked by the registered IANA language tag 'en-GB-oed'. It is the spelling used by the Encyclopaedia Britannica, by the United Nations, and by many international organizations and academic publications. The -ize forms were used by the London Times until the mid-1980s. The -ise forms are now generally used by the British government, by the European Union and mostly taught in the British school system. They are far more prevalent in common usage. Pam Peters (2004, -ize/-ise) relates that British National Corpus data indicates the ratio of popularity for -ise forms to -ize forms in Britain is 3:2.

British Isles

:For an explanation of often confusing terms like (Great) Britain, United Kingdom and England see also British Isles (terminology). :The "British Isles" is also an old name for the British and Irish Lions rugby team. British and Irish Lions The British Isles is a term traditionally given to the group of islands off the northwest coast of Europe including Great Britain (containing England, Scotland, and Wales), Ireland, and several thousand smaller adjacent islands. The name was extensively used historically, derived from when the island of Great Britain was called Britannias, and Ireland and the other islands near Great Britain were called Britanniae (the Latin genitive case meaning of Britannias.) In 1922 most of the island of Ireland ceased to be in the United Kingdom and became the independent sovereign state of the Republic of Ireland. However, even before this, and especially since, the usage of the term British Isles has been seen by many people, especially in Ireland, as problematic, due to an implied continued British sovereignty over the whole of Ireland, or more generally as referring to Ireland as being British in any sense. This is not a result of anti-British sentiment, but simply a reflection that Irish people do not regard themselves or their country as British. The term is also considered by some to be offensive to people in Wales and Scotland. In terms of geography the term British Isles is understood to refer to the whole archipelago, from Scilly to Shetland, containing more than 6,000 islands and totalling 315,134 km² (121,674 square miles) of land. These islands were originally inhabited by the ancient Britons (hence the name "British Isles"). The historic name British Isles derives from terms used by classical geographers to describe the island group. Pliny the Elder, in his Natural History (iv.xvi.102) records of Great Britain that "it was itself named Albion while all the islands about which we shall soon briefly speak were called the Britanniae".

List of the British Isles

Albion]] :Main article: Complete list of the British Isles
- Great Britain
- Northern Isles (including Orkney, Shetland and Fair Isle)
- Hebrides (including the Inner Hebrides, Outer Hebrides and Small Isles)
- Islands of the lower Firth of Clyde (including the Isle of Arran and Bute)
- Anglesey (in Welsh: Ynys Môn)
- Lundy
- Isles of Scilly
- Isle of Wight
- Lindisfarne
- Ireland
- Ulster: Rathlin Island
- , Arranmore, Tory Island
- Connacht: Achill Island, Clew Bay islands, Inishturk, Inishbofin, Inishark, Aran Islands
- Munster: Blasket Islands, Valentia Island, Cape Clear , Sherkin Island, Great Island
- Leinster: Lambay Island, Ireland's Eye
- Isle of Man
- Channel Islands¹
- Rockall Many other small islands are not listed.
- Rathlin Island is the only Irish island part of Northern Ireland and hence the UK.

Origin of the term British Isles

In classical times, foreign sources used "Brit-" or "Prit-" with various endings and native sources used oceani insulae meaning "islands of the ocean" or insularum meaning "islands". Only in modern times has British Isles entered the English language.

Classical geographers

The inhabitants of the British Isles in classical times were the Celtic Bruthin or Priteni, later known as the "Brythons", who were in Great Britain and Ireland some time before the 5th century BC, whether as a result of cultural changes in the native population or of immigration, possibly through conquest. The classical writers of geographies named the group of islands after these inhabitants, using a transliteration into their own language such as Latin (e.g. Bretannae) or Greek (e.g. Βρηττανων). Throughout Book 4 of his Geography, Strabo is consistent in spelling the island Britain (transliterated) as Prettanikee; he uses the terms Prettans or Brettans for the islands as a group. For example, in Geography 2.1.18, "...οι νοτιωτατοι των Βρηττανων βορηιοτηροι τουτον ηισιν". (...the most southern of the Brettans are further north than this)². He was writing around AD 10, although the earliest surviving copy of his work dates from the 6th century. Pliny the Elder writing around AD 70 uses a Latin version of the same terminology in section 4.102 of his Naturalis Historia. He writes of Great Britain: Albion ipsi nomen fuit, cum Britanniae vocarentur omnes de quibus mox paulo dicemus. (Albion was its own name, when all [the islands] were called the Britannias; I will speak of them in a moment). In the following section, 4.103, Pliny enumerates the islands he considers to make up the Britannias, listing Great Britain, Ireland, and many smaller islands. Ptolemy is quite clear that Ireland – h

Continental Europe

The English concept

The Nordic concept

See also

Continent

Geographic continents

Geologic continents

Tectonic plates

See also

Europe

Etymology

History

Geography and extent

Physical features

Biodiversity

Demographics

Territories and divisions

Political divisions

Independent states

Dependent territories

Unilaterally seceded territories

Territories under United Nations administration

Table of European territories and regions

Linguistic and cultural regions

Germanic Europe

Latin Europe

Slavic Europe

Others

See also

Lists and tables

External links

Island

Continental islands

River islands

Volcanic islands

See also

External links

Peninsula

Peninsulas of the World

Eurasia

Continental Europe

The Americas

Australia & Oceania

British English

-ise versus -ize

See also

British Isles

List of the British Isles

Origin of the term British Isles

Classical geographers