Europe

Europe is a continent forming the westermost part of the Eurasian supercontinent. Europe is bounded to the north by the Arctic Ocean, to the west by the Atlantic Ocean, to the south by the Mediterranean Sea and the Black Sea, and to the east by the Ural Mountains.

In terms of area, Europe is the world's second smallest continent, with an area of 10,400,000 km² (4,000,000 square miles), making it slightly larger than Australia.

In terms of population it is the third largest continent after Asia and Africa. The population of Europe in 2001 was estimated to be 666,498,000: roughly one seventh of the world's population.

Etymology

According to Homer the name Europe was originally given to central Greece. Later it stood for mainland Greece and by 500 BC its meaning was extended to all the lands of the north.

The term Europe is often said to derive from Greek words meaning broad (eurys) and face (ops). Many, however, see a Semitic origin, pointing to the Semitic word ereb which means "sunset". From a Middle Eastern viewpoint, the sun sets over Europe: the lands to the west.

In ancient mythology, Europa was a Phoenician princess who was abducted by a bull-shaped Zeus.

 

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Geography and Extent

Political and geographic boundaries in Europe do not always match. This physical and political map shows Europe at its furthest extent. Geographically Europe is a part of the larger landmass known as Eurasia. The continent begins at the Ural Mountains in Russia, which defines Europe's eastern boundary with Asia. The southeast boundary with Asia isn't universally defined, with either the Ural or Emba rivers serving as possible boundaries, continuing with the Caspian Sea, and either the Kuma and Manych rivers or the Caucasus mountains as possibilities, and onto 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 included in Europe. There is ongoing debate on where the geographical centre of Europe is.

In practice the borders of Europe are often drawn 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, the Holy See (Vatican City), Kazakhstan, and Monaco.

The idea of a European "continent" is not universally held. Some non-European geographical texts refer to a Eurasian Continent, or to a European "sub-continent", given that "Europe" is not surrounded by sea and is, in any case, much more a cultural than a geographically definable area. In the past concepts such as "Christendom" were deemed more important.

Confusingly, the word "Europe" is increasingly being used as a short-form for the European Union (EU) and its members. 25 European sovereign countries currently belong to the EU. A number of other European countries are negotiating for membership and several more are expected to begin negotiations in the future.

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 peninuslas—Iberia, Italy and Greece—emerge from the southern margin of the mainland into the Medeterranean 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. 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.

The few generalizations that can be made about the relief of Europe make it less than suprising that the continent's many separate regions provided homes for many separate nations throughout history.