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Isthmus

Isthmus

An isthmus (from Greek ισθμός, isthmos; plural isthmuses or isthmi; pronounced ) is a narrow strip of land that is bordered on two sides by water and connects two larger land masses. It is the inverse of a strait (which lies between two land masses and connects two larger bodies of water). Isthmuses are a naturally good place to build canals. The Panama Canal, which connects the Atlantic and Pacific Oceans, drastically reduces the naval travel time between the east and west coasts of the Americas. The Suez Canal is another example - it allows ship transportation between Europe and Asia without the circumnavigation of Africa.

List of isthmuses

- the Isthmus of Panama - the most famous isthmus. Connects North America and South America.
- the Isthmus of Corinth in Greece - the first isthmus to bear that name
- the Isthmus of Dubrovnik - today's Stradun, (main center street), which connected Laus and Dub into a single city unit
- the Isthmus of Suez - the isthmus between North Africa and Southwest Asia, in Egypt where the Suez Canal is located
- the Isthmus of Kra, which joins the Malay Peninsula with mainland Asia
- the Isthmus of Avalon in Canada - separates the main island of Newfoundland from the Avalon Peninsula (where the capital, St. John's, is located)
- the Isthmus of Chignecto - connects the mainland portion of Nova Scotia with North America
- the Isthmus of Tehuantepec - connects Yucatan and Central America with the rest of Mexico
- the Isthmus of Perekop between Crimea and Ukraine proper
- the Karelian Isthmus between Gulf of Finland and Lake Ladoga
- the Madison Isthmus, between Lake Mendota and Lake Monona in Madison, Wisconsin

Greek language

Greek (Greek Ελληνικά, IPA – "Hellenic") is an Indo-European language with a documented history of 3,500 years. Today, it is spoken by 15 million people in Greece, Cyprus, the former Yugoslavia, particularly The Former Yugoslav Republic of Macedonia, Bulgaria, Albania and Turkey. There are also many Greek emigrant communities around the world, such as those in Melbourne, Australia which is the third-largest Greek-populated city in the world, after Athens and Thessaloniki. Greek has been written in the Greek alphabet, the first true alphabet, since the 9th century B.C. and before that, in Linear B and the Cypriot syllabaries. Greek literature has a long and rich tradition.

History

This article does not cover the reconstructed history of Greek prior to the use of writing. For more information, see main article on Proto-Greek language. Greek has been spoken in the Balkan Peninsula since the 2nd millennium BC. The earliest evidence of this is found in the Linear B tablets dating from 1500 BC. The later Greek alphabet (q.v.) is unrelated to Linear B, and was derived from the Phoenician alphabet (abjad); with minor modifications, it is still used today. Greek is conventionally divided into the following periods:
- Mycenean Greek: the language of the Mycenean civilisation. It is recorded in the Linear B script on tablets dating from the 16th century BC onwards.
- Classical Greek (also known as Ancient Greek): In its various dialects was the language of the Archaic and Classical periods of Greek civilisation. It was widely known throughout the Roman empire. Classical Greek fell into disuse in western Europe in the Middle Ages, but remained known in the Byzantine world, and was reintroduced to the rest of Europe with the Fall of Constantinople and Greek migration to Italy.
- Hellenistic Greek (also known as Koine Greek): The fusion of various ancient Greek dialects with Attic (the dialect of Athens) resulted in the creation of the first common Greek dialect, which gradually turned into one of the world's first international languages. Koine Greek can be initially traced within the armies and conquered territories of Alexander the Great, but after the Hellenistic colonisation of the known world, it was spoken from Egypt to the fringes of India. After the Roman conquest of Greece, an unofficial diglossy of Greek and Latin was established in the city of Rome and Koine Greek became a first or second language in the Roman Empire. Through Koine Greek it is also traced the origin of Christianity, as the Apostles used it to preach in Greece and the Greek-speaking world. It is also known as the Alexandrian dialect, Post-Classical Greek or even New Testament Greek (after its most famous work of literature).
- Medieval Greek: The continuation of Hellenistic Greek during medieval Greek history as the official and vernacular (if not the literary nor the ecclesiastic) language of the Byzantine Empire, and continued to be used until, and after the fall of that Empire in the 15th century. Also known as Byzantine Greek.
- Modern Greek: Stemming independently from Koine Greek, Modern Greek usages can be traced in the late Byzantine period (as early as 11th century). Two main forms of the language have been in use since the end of the medieval Greek period: Dhimotikí (Δημοτική), the Demotic (vernacular) language, and Katharévousa (Καθαρεύουσα), an imitation of classical Greek, which was used for literary, juridic, and scientific purposes during the 19th and early 20th centuries. Demotic Greek is now the official language of the modern Greek state, and the most widely spoken by Greeks today. It has been claimed that an "educated" speaker of the modern language can understand an ancient text, but this is surely as much a function of education as of the similarity of the languages. Still, Koinē , the version of Greek used to write the New Testament and the Septuagint, is relatively easy to understand for modern speakers. Greek words have been widely borrowed into the European languages: astronomy, democracy, philosophy, thespian, etc. Moreover, Greek words and word elements continue to be productive as a basis for coinages: anthropology, photography, isomer, biomechanics etc. and form, with Latin words, the foundation of international scientific and technical vocabulary. See English words of Greek origin, and List of Greek words with English derivatives.

Classification

Greek is an independent branch of the Indo-European language family. The ancient languages which were probably most closely related to it, Ancient Macedonian language (which may be regarded as a dialect of Greek) and Phrygian, are not well enough documented to permit detailed comparison. Among living languages, Armenian seems to be the most closely related to it.

Geographic distribution

Modern Greek is spoken by about 15 million people mainly in Greece and Cyprus. There are also Greek-speaking populations in Georgia, Ukraine, Egypt, Turkey, Albania, Former Yugoslav Republic of Macedonia and Southern Italy. The language is spoken also in many other countries where Greeks have settled, including Armenia, Australia, Austria, Belgium, Bulgaria, Canada, Denmark, France, Germany, Netherlands, Sweden, United Kingdom, and the United States.

Official status

Greek is the official language of Greece where it is spoken by about 99.5% of the population. It is also, alongside Turkish, the official language of Cyprus. Due to the membership of Greece and Cyprus, Greek is one of the 20 official languages of the European Union.

Phonology

This section generally describes the post-Classic phonology of the Greek language. :All phonetic transcriptions in this section use the International Phonetic Alphabet

Vowel sounds

Greek has 5 vowel sounds, all phonemic:

Strait

A strait is a narrow channel of water that connects two larger bodies of water, and thus lies between two land masses. The terms strait, channel, and passage can be synonymous and interchangeable, although channel has other meanings. Many straits are economically important. Straits can lie on important shipping routes, and wars have been fought for control of these straits. Numerous artificial channels, called canals, have been constructed to connect two bodies of water over land. Well-known straits in the world include the English Channel, between England and France, which connects the North Sea with the Atlantic Ocean off France; the Strait of Gibraltar, which is the only natural passage between the Atlantic Ocean and the Mediterranean Sea; the Bosporus and the Dardanelles, which connects the Mediterranean and the Black Sea; and the Straits of Malacca, which lie between Malaysia and Sumatra and connect the Indian Ocean with the South China Sea. Although rivers and canals often form a bridge between two large lakes or a lake and a sea, and these seem to suit the formal definition of straits, they are not usually referred to as straits. Straits are typically much larger, wider structures that do not have water running in a single direction, and normally connect two seas. Straits are the duals of isthmuses. That is, while straits lie between two land masses and connect two larger bodies of water, isthmuses lie between two bodies of water and connect two larger land masses.

Canal

, France]] France] Canals are man-made waterways, usually connecting existing lakes, rivers, or oceans. Irrigation canals are man-made waterways for the delivery of water and preceded the use of transportation canals used by barges or narrowboats on smaller canals, and by ships on ship canals that connect to the ocean. The oldest-known canals were built in Mesopotamia, c. 4000 BC. Ancient canals in the West were dwarfed by the Grand Canal of China, the longest canal built in ancient times. In Europe and then in the young United States, inland canals preceded the development of railroads during the earliest phase of the Industrial Revolution; some canals were later drained and used as railroad rights-of-way. Navigable canals reached into previously isolated areas and brought them in touch with the world economy. The Erie Canal, for instance, opened up a connection from the populated Northeast to the fertile Great Plains. Erie Canal] The pace of draining of fenland and polder in the Low Countries quickened in the 14th century and canalization made the village of Amsterdam a port. Canals are so deeply identified with Venice that many cities that have canals used as waterways have been called "the Venice of..." Some rivers have also been 'canalised' to make them navigable. Competition from the railroad network made many canals obsolete for commercial transportation, and many fell into decay. A movement that began in Britain and France to use the picturesque early industrial canals for pleasure boats has spurred rehabilitation of stretches of historic canals. Canals have found another use in the 21st century, as wayleaves for fibre optic telecommunications networks.

Miscellaneous

For a time in the early 20th century, it was believed that there were canals on Mars. canals on Mars

Famous canals and lists

- List of waterways
- Canals of Ireland
- List of canals in the United States
- Canals of the United Kingdom
- Suez Canal
- Panama Canal
- Corinth Canal
- Venice
- Amsterdam
- Welland Canal - Central Canada
- Saint Lawrence Seaway - Quebec, Ontario, Canada
- Rideau Canal - Ottawa, Ontario, Canada
- Shubie Canal - Nova Scotia, Canada

Atlantic Ocean

The Atlantic Ocean is Earth's second-largest ocean, covering approximately one-fifth of its surface. The ocean's name, derived from Greek mythology, means the "Sea of Atlas". This ocean occupies an elongated, S-shaped basin extending in a north-south direction and is divided into the North Atlantic and South Atlantic by equatorial counter currents at about 8° north latitude. Bounded by the Americas on the west and Europe and Africa on the east, the Atlantic is linked to the Pacific Ocean by the Arctic Ocean on the north and the Drake Passage on the south. An artificial connection between the Atlantic and Pacific is also provided by the Panama Canal. On the east, the dividing line between the Atlantic and the Indian Ocean is the 20° east meridian. The Atlantic is separated from the Arctic Ocean by a line from Greenland to northwestern Iceland and then from northeastern Iceland to southernmost tip of Spitsbergen and then to North Cape in northern Norway. Norway on a fair day.]] Covering approximately 20% of Earth's surface, the Atlantic Ocean is second only to the Pacific in size. With its adjacent seas it occupies an area of about 106,400,000 km² (41,100,000 square miles); without them, it has an area of 82,400,000 km² (31,800,000 mi²). The land area that drains into the Atlantic is four times that of either the Pacific or Indian oceans. The volume of the Atlantic Ocean with its adjacent seas is 354,700,000 km³ (85,100,000 mi³) and without them 323,600,000 km³ (77,640,000 mi³). The average depth of the Atlantic, with its adjacent seas, is 3,332 m (10,932 ft); without them it is 3,926 m (12,881 ft). The greatest depth, 8,605 m (28,232 ft), is in the Puerto Rico Trench. The width of the Atlantic varies from 2,848 km (1,770 miles) between Brazil and Liberia to about 4,830 km (3,000 miles) between the United States and northern Africa. The Atlantic Ocean has irregular coasts indented by numerous bays, gulfs, and seas. These include the Caribbean Sea, Gulf of Mexico, Gulf of St. Lawrence, Mediterranean Sea, Black Sea, North Sea, Labrador Sea, Baltic Sea, and Norwegian-Greenland Sea. Islands in the Atlantic Ocean include Faroe Islands, Greenland, Iceland, Rockall, Great Britain, Ireland, Fernando de Noronha, the Azores, the Madeira Islands, the Canaries, the Cape Verde Islands,Sao Tome e Principe, Newfoundland, Bermuda, the West Indies, Ascension, St. Helena, Trindade, Martin Vaz, Tristan da Cunha, the Falkland Islands, and South Georgia Island. South Georgia Island

Ocean bottom

The principal feature of the bottom topography of the Atlantic Ocean is a great submarine mountain range called the Mid-Atlantic Ridge. It extends from Iceland in the north to approximately 58° south latitude, reaching a maximum width of about 1,600 km (1,000 miles). A great rift valley also extends along the ridge over most of its length. The depth of water over the ridge is less than 2,700 m (8,900 ft) in most places, and several mountain peaks rise above the water, forming islands. The South Atlantic Ocean has an additional submarine ridge, the Walvis Ridge. The Mid-Atlantic Ridge separates the Atlantic Ocean into two large troughs with depths averaging between 3,700 and 5,500 m (12,000 and 18,000 ft). Transverse ridges running between the continents and the Mid-Atlantic Ridge divide the ocean floor into numerous basins. Some of the larger basins are the Guiana, North American, Cape Verde, and Canaries basins in the North Atlantic. The largest South Atlantic basins are the Angola, Cape, Argentina, and Brazil basins. The deep ocean floor is thought to be fairly flat, although numerous seamounts and some guyots exist. Several deeps or trenches are also found on the ocean floor. The Puerto Rico Trench, in the North Atlantic, is the deepest. The Laurentian Abyss is found off the eastern coast of Canada. In the south Atlantic, the South Sandwich Trench reaches a depth of 8,428 m (27,651 ft). A third major trench, the Romanche Trench, is located near the equator and reaches a depth of about 7,454 m (24,455 ft). The shelves along the margins of the continents constitute about 11% of the bottom topography. In addition, a number of deep channels cut across the continental rise. Ocean sediments are composed of terrigenous, pelagic, and authigenic material. Terrigenous deposits consist of sand, mud, and rock particles formed by erosion, weathering, and volcanic activity on land and then washed to sea. These materials are largely found on the continental shelves and are thickest off the mouths of large rivers or off desert coasts. Pelagic deposits, which contain the remains of organisms that sink to the ocean floor, include red clays and Globigerina, pteropod, and siliceous oozes. Covering most of the ocean floor and ranging in thickness from 60 m to 3,300 m (200 ft to 11,000 ft), they are thickest in the convergence belts and in the zones of upwelling. Authigenic deposits consist of such materials as manganese nodules. They occur where sedimentation proceeds slowly or where currents sort the deposits.

Water characteristics

sediment The salinity of the surface waters in the open ocean ranges from 33 to 37 parts per thousand by mass and varies with latitude and season. Although the minimum salinity values are found just north of the equator, in general the lowest values are in the high latitudes and along coasts where large rivers flow into the ocean. Maximum salinity values occur at about 25° north latitude. Surface salinity values are influenced by evaporation, precipitation, river inflow, and melting of sea ice. Surface water temperatures, which vary with latitude, current systems, and season and reflect the latitudinal distribution of solar energy, range from less than −2 °C to 29 °C (28 °F to 84 °F). Maximum temperatures occur north of the equator, and minimum values are found in the polar regions. In the middle latitudes, the area of maximum temperature variations, values may vary by 7 °C to 8 °C (13 °F to 15 °F). The Atlantic Ocean consists of four major water masses. The North and South Atlantic central waters constitute the surface waters. The sub-Antarctic intermediate water extends to depths of 1,000 m (3,300 ft). The North Atlantic deep water reaches depths of as much as 4,000 m (13,200 ft). The Antarctic bottom water occupies ocean basins at depths greater than 4,000 m (13,200 ft). Within the North Atlantic, ocean currents isolate a large elongated body of water known as the Sargasso Sea, in which the salinity is noticeably higher than average. The Sargasso Sea contains large amounts of seaweed, and is also the spawning ground for the European eel. Due to the Coriolis effect, water in the North Atlantic circulates in a clockwise direction, whereas water circulation in the South Atlantic is counter clockwise. The South tides in the Atlantic Ocean are semi-diurnal; that is, two high tides occur during each 24 lunar hours. The tides are a general wave that moves from south to north. In latitudes above 40° north some east-west oscillation occurs.

Climate

diurnal The climate of the Atlantic Ocean and adjacent land areas is influenced by the temperatures of the surface waters and water currents as well as the winds blowing across the waters. Because of the oceans' great capacity for retaining heat, maritime climates are moderate and free of extreme seasonal variations. Precipitation can be approximated from coastal weather data and air temperature from the water temperatures. The oceans are the major source of the atmospheric moisture that is obtained through evaporation. Climatic zones vary with latitude; the warmest climatic zones stretch across the Atlantic north of the equator. The coldest zones are in the high latitudes, with the coldest regions corresponding to the areas covered by sea ice. Ocean currents contribute to climatic control by transporting warm and cold waters to other regions. Adjacent land areas are affected by the winds that are cooled or warmed when blowing over these currents. The Gulf Stream, for example, warms the atmosphere of the British Isles and northwestern Europe, and the cold water currents contribute to heavy fog off the coast of northeastern Canada (the Grand Banks area) and the northwestern coast of Africa. In general, winds tend to transport moisture and warm or cool air over land areas. Hurricanes develop in the southern part of the North Atlantic Ocean.

History and economy

The Atlantic Ocean appears to be the second youngest of the world's oceans, after the Southern Ocean. Evidence indicates that it did not exist prior to 180 million years ago, when the continents that formed from the breakup of the ancestral supercontinent, Pangaea, were being rafted apart by the process of seafloor spreading. The Atlantic has been extensively explored since the earliest settlements were established along its shores. The Vikings, Portuguese, and Christopher Columbus were the most famous among its early explorers. After Columbus, European exploration rapidly accelerated, and many new trade routes were established. As a result, the Atlantic became and remains the major artery between Europe and the Americas (known as transatlantic trade). Numerous scientific explorations have been undertaken, including those by the German Meteor expedition, Columbia University's Lamont Geological Observatory, and the U.S. Navy Hydrographic Office. The ocean has also contributed significantly to the development and economy of the countries around it. Besides its major "transatlantic" transportation and communication routes, the Atlantic offers abundant petroleum deposits in the sedimentary rocks of the continental shelves and the world's richest fishing resources, especially in the waters covering the shelves. The major species of fish caught are cod, haddock, hake, herring, and mackerel. The most productive areas include the Grand Banks of Newfoundland, the shelf area off Nova Scotia, Georges Bank off Cape Cod, the Bahama Banks, the waters around Iceland, the Irish Sea, the Dogger Bank of the North Sea, and the Falkland Banks. Eel, lobster, and whales have also been taken in great quantities. All these factors, taken together, tremendously enhance the Atlantic's great commercial value. Because of the threats to the ocean environment presented by oil spills, marine debris, and the incineration of toxic wastes at sea, various international treaties exist to reduce some forms of pollution.
- In 1858, the first Transatlantic telegraph cable was laid by Cyrus Field.
- In 1919, the American NC-4 became the first airplane to cross the Atlantic (though it made a couple of landings on islands along the way).
- Later in 1919, a British airplane piloted by Alcock and Brown made the first non-stop transatlantic flight from Newfoundland to Ireland.
- In 1921, the British were the first to cross the North Atlantic in an airship.
- In 1922, the Portuguese were the first to cross the South Atlantic in an airship.
- The first transatlantic telephone call was made on January 7, 1927.
- In 1927, Charles Lindbergh made the first solo non-stop transatlantic flight in an airplane (between New York City and Paris).
- After rowing for 81 days and 2,962 miles, on December 3, 1999 Tori Murden became the first woman to cross the Atlantic Ocean by rowboat alone when she reached Guadeloupe from the Canary Islands. Location: body of water between Africa, Europe, the Southern Ocean, and the Americas Geographic coordinates: Map references: World Area:
- total: 76.762 million km²
- note: includes the Baltic Sea, Black Sea, Caribbean Sea, Davis Strait, Denmark Strait, part of the Drake Passage, Gulf of Mexico, Labrador Sea, Mediterranean Sea, North Sea, Norwegian Sea, almost all of the Scotia Sea, and other tributary water bodies Area - comparative: slightly less than 6.5 times the size of the US Coastline: 111,866 km Climate: Tropical cyclones (hurricanes) develop anywhere from off the coast of Africa near Cape Verde to the Windward Islands and move westward into the Caribbean Sea or up the east coast of North America; hurricanes can occur from May to December, but are most frequent from late July to early November. Storms are common in the North Atlantic during northern winters, making ocean crossings more difficult and dangerous.

Terrain

The surface is usually covered with sea ice in the Labrador Sea, Denmark Strait, and Baltic Sea from October to June. There is a clockwise warm-water gyre (broad, circular system of currents) in the northern Atlantic, and a counter-clockwise warm-water gyre in the southern Atlantic. The ocean floor is dominated by the Mid-Atlantic Ridge, a rugged north-south centerline for the entire Atlantic basin, first discovered by the Challenger Expedition.

Elevation extremes

- lowest point: Milwaukee Deep in the Puerto Rico Trench -8,605 m
- highest point: sea level 0 m

Natural resources

Petroleum and gas fields, fish, marine mammals (seals and whales), sand and gravel aggregates, placer deposits, polymetallic nodules, precious stones

Natural hazards

Icebergs are common in the Davis Strait, Denmark Strait, and the northwestern Atlantic Ocean from February to August and have been spotted as far south as Bermuda and the Madeira Islands. Ships are subject to superstructure icing in extreme northern Atlantic from October to May. Persistent fog can be a maritime hazard from May to September. So can hurricanes north of the equator (May to December). The Bermuda Triangle is popularly believed to be the site of numerous aviation and shipping incidents, due to unexplained and supposedly mysterious causes, but coastguard records do not support this belief.

Current environmental issues

Endangered marine species include the manatee, seals, sea lions, turtles, and whales. Drift net fishing is killing dolphins, albatrosses and other seabirds (petrels, auks), hastening the decline of fish stocks and contributing to international disputes. There is municipal sludge pollution off eastern US, southern Brazil, and eastern Argentina, oil pollution in the Caribbean Sea, Gulf of Mexico, Lake Maracaibo, Mediterranean Sea, and North Sea, and industrial waste and municipal sewage pollution in the Baltic Sea, North Sea, and Mediterranean Sea.

Notes on geography

Major chokepoints include the Strait of Gibraltar and the Panama Canal; strategic straits include the Strait of Dover, Straits of Florida, Mona Passage, The Sound (Oresund), and Windward Passage; the Equator divides the Atlantic Ocean into the North Atlantic Ocean and South Atlantic Ocean (previously known as the Ethiopic Ocean). During the Cold War the so called Greenland-Iceland-UK (GIUK) Gap was a major strategic concern, the seabed in that area was laid with extensive hydrophone systems to track Soviet submarines.

Ports and harbours

- A Coruña (Spain)
- Abidjan (Côte d'Ivoire)
- Accra (Ghana)
- Amsterdam (Netherlands)
- Antwerp (Belgium)
- Bahia Blanca (Argentina)
- Baltimore (US)
- Banjul (The Gambia)
- Belfast (Northern Ireland)
- Bergen (Norway)
- Bissau (Guinea-Bissau)
- Bodø (Norway)
- Bordeaux (France)
- Boston (US)
- Bremen (Germany)
- Brest (France)
- Bristol (England)
- Cadiz (Spain)
- Cape Town (South Africa)
- Casablanca (Morocco)
- Cayenne (French Guiana)
- Charleston (US)
- Cherbourg (France)
- Conakry (Guinea)
- Cork (Republic of Ireland)
- Cotonou (Benin)
- Dakar (Senegal)
- Douala (Cameroon)
- Dublin (Republic of Ireland)
- Dunkirk (France)
- Edinburgh (Scotland)
- Fortaleza (Brazil)
- Georgetown (Guyana)
- Glasgow (Scotland)
- Gothenburg(Sweden)
- Hamburg (Germany)
- Halifax (Canada)
- Jacksonville (US)
- Lagos (Nigeria)
- Las Palmas (Spain)
- Le Havre (France)
- Libreville (Gabon)
- Lisbon (Portugal)
- Liverpool (England)
- Lomé (Togo)
- London (England)
- Luanda (Angola)
- Maceió (Brazil)
- Malabo (Equatorial Guinea)
- Miami (US)
- Monrovia (Liberia)
- Montréal (Canada)
- Morehead City (US)
- Nantes (France)
- Nantucket (US)
- Narvik (Norway)
- New Haven (US)
- New London (US)
- New York (US)
- Newcastle upon Tyne (England)
- Newport News (US)
- Norfolk (US)
- Nouakchott (Mauritania)
- Oslo (Norway)
- Ostend (Belgium)
- Paramaribo (Suriname)
- Philadelphia (US)
- Port Harcourt (Nigeria)
- Portland (US)
- Porto (Portugal)
- Porto-Novo (Benin)
- Portsmouth (England)
- Portsmouth (US)
- Providence (US)
- Puerto Cortes (Honduras)
- Québec (Canada)
- Rabat (Morocco)
- Recife (Brazil)
- Reykjavík (Iceland)
- Rio de Janeiro (Brazil)
- Rotterdam (Netherlands)
- Salvador (Brazil)
- Saint-Nazaire (France)
- Santa Cruz de Tenerife (Spain)
- Santander (Spain)
- Santos (Brazil)
- Savannah (US)
- Seville (Spain)
- Saint John (Canada)
- St. John's (Canada)
- Southampton (England)
- Stavanger (Norway)
- Tangier (Morocco)
- Tromsø (Norway)
- Trondheim (Norway)
- Vigo (Spain)
- Vitória (Brazil)
- Walvis Bay (Namibia)
- Wilmington (US)
- Yarmouth (Canada)
- Ålesund (Norway)

Note on transportation

The Saint Lawrence Seaway is an important waterway.

References

- Much of this article comes from the public domain site http://oceanographer.navy.mil/atlantic.html (dead link). It is now accessible from the Internet Archive at http://web.archive.org/web/20020221215514/http%3a//oceanographer.navy.mil/atlantic.html.
- Disclaimers for this website, including its status as a public domain resource, are recorded on the Internet Archive at http://web.archive.org/web/20020212021049/http%3a//oceanographer.navy.mil/warning.html.

External links

- [http://dapper.pmel.noaa.gov/dchart/ NOAA In-situ Ocean Data Viewer] Plot and download ocean observations
- [http://www.cia.gov/cia/publications/factbook/geos/zh.html CIA – The World Factbook – Atlantic Ocean] Category:Atlantic Ocean Category:Oceans als:Atlantik zh-min-nan:Tāi-se-iûⁿ ko:대서양 ja:大西洋 simple:Atlantic Ocean th:มหาสมุทรแอตแลนติก

Suez Canal

The Suez Canal (Arabic, Qanā al-Suways), west of the Sinai Peninsula, is a 163 km maritime canal in Egypt between Port Said (Būr Sa'īd) on the Mediterranean Sea and Suez (al-Suways) on the Red Sea. The canal allows two-way north to south water transport between Europe and Asia without circumnavigating Africa. Before the opening of the canal, some transport was conducted by offloading ships and carrying the goods overland between the Mediterranean and the Red Sea. The canal comprises two parts, north and south of the Great Bitter Lake, linking the Mediterranean Sea to the Gulf of Suez on the Red Sea.

History

Antiquity

Perhaps as early as the 12th Dynasty, Pharaoh Senusret III (1878 BC - 1839 BC) may have had a west-east canal dug through the Wadi Tumilat, joining the Nile with the Red Sea, for direct trade with Punt. Evidence indicates its existence at least by the 13th century BC during the time of Ramesses II (see [http://www.1911encyclopedia.org/S/SU/SUEZ_CANAL.htm], [http://www.denverseminary.edu/dj/articles1998/0100/0114.php], [http://lexicorient.com/cgi-bin/eo-direct-frame.pl?http://i-cias.com/e.o/suez_can.htm], [http://www.e-c-h-o.org/khd/location.html], [http://www.realidade.com.br/rih2/egipto.htm]). It later fell into disrepair, and according to the Histories of the Greek historian Herodotus, re-excavation was undertaken about 600 BC by Necho II; though Necho II never completed his project. The canal was finally completed around 500 BC by King Darius I, the Persian conqueror of Egypt. Darius commemorated his achievement with a number of granite stelae that he set up on the Nile bank, including one near Kabret, 130 kilometres from Suez. The Darius Inscriptions read: :Saith King Darius: I am a Persian. Setting out from Persia, I conquered Egypt. I ordered this canal dug from the river called the Nile that flows in Egypt, to the sea that begins in Persia. When the canal had been dug as I ordered, ships went from Egypt through this canal to Persia, even as I intended. [http://www.livius.org/aa-ac/achaemenians/DZ.html] The canal was again restored by Ptolemy II about 250 BC. Over the next 1000 years it was successively modified, destroyed and rebuilt, until finally being put out of commission in the eighth century by the Abbasid Caliph al-Mansur. al-Mansur
The modern Suez Canal
More than a thousand years elapsed before the next attempt was made to dig a canal. At the end of the 18th century, Napoleon Bonaparte, while in Egypt, contemplated the construction of a canal to join the Mediterranean and Red Seas. His project was abandoned, however, after a French survey erroneously concluded that the waters of the Red Sea were higher than those of the Mediterranean, making a lockless canal impossible. In 1854 and 1856 Ferdinand de Lesseps obtained concessions from Said Pasha, the viceroy of Egypt, whom de Lesseps had as a French diplomat come to know in the 1830s. Said Pasha authorized the creation of a company for the purpose of constructing a maritime canal open to ships of all nations according to plans created by Austrian engineer Alois Negrelli. By way of a lease of the relevant land, the company was to operate the canal for 99 years from its opening to navigation. The Suez Canal Company (Compagnie Universelle du Canal Maritime de Suez) came into being on December 15, 1858. The excavation operations through the desert took nearly eleven years by poor Egyptians who forcibly dug the canal. Some of them were actually beaten to continue digging. Numerous technical, political, and financial problems were overcome. The final cost was more than double the original estimate. The canal opened to traffic on November 17, 1869. 1869The canal had an immediate and dramatic effect on world trade. Combined with the completion of the American Transcontinental Railroad six months earlier, the entire world could be circled in record time. It played an important role in increasing European penetration and colonization of Africa. External debts forced Said Pasha's successor, Isma'il Pasha, to sell his country's share in the canal to the United Kingdom in 1875. The Convention of Constantinople in 1888 declared the canal a neutral zone under the protection of the British, after British troops had moved in to protect it in 1882. Under the Anglo-Egyptian Treaty of 1936, the United Kingdom insisted on retaining control over the canal. In 1951, Egypt repudiated the treaty, and by 1954 the United Kingdom had agreed to pull out. After the United Kingdom and the United States withdrew their pledge to support the construction of the Aswan Dam because Egypt had sought weaponry from the Soviet Union (being unable to attain it from the U.S.), President Gamal Abdel Nasser nationalized the canal. This caused Britain, France, and Israel to invade, in the week-long 1956 Suez War. As a result of damage and sunken ships, the canal was closed until April 1957, when it had been cleared with UN assistance. A United Nations force (UNEF) was established to maintain the neutrality of the canal and the Sinai Peninsula. After the Six Day War in 1967, the canal was closed until June 5, 1975. In 1973, during the Yom Kippur War, the canal was the scene of a major crossing by the Egyptian army into Israeli-controlled Sinai; later, the Israeli army crossed the canal westward. A UN peacekeeping force has been stationed in the Sinai Peninsula since 1974. UN peacekeeping
Present day
The canal has no locks because there is no sea-level difference and there are no hills to climb. The canal allows the passage of ships of up to some 150,000 tons displacement, with cargo. It permits ships of up to 16 m (53 ft) draft to pass, and improvements are planned to increase this to 22 m (72 ft) by 2010 to allow supertanker passage. Presently supertankers can offload part of their cargo onto a canal-owned boat and reload at the other end of the canal. There is one shipping lane with several passing areas. Some 25,000 ships can pass through the canal each year, bearing about 14% of world shipping. The passage takes between 11 and 16 hours. Since 1980 there has been a road tunnel under the canal, and since 1999 a powerline has crossed it. A railway on the west bank runs parallel to the canal for its entire length.
Connections between the shores
For north to south:
- In El Qantara there is a high-level fixed road bridge.
- In 2001 the El Ferdan Railway Bridge 20 km north of Ismailia was completed: the longest swing span bridge in the world, with a span of 340 m (1100 ft). The previous bridge was destroyed in 1967 during the Arab-Israeli conflict.
- South of the Great Bitter Lake is the [http://www.nccnet.co.jp/english/introduction/suezcanal.html Ahmed Hamdi tunnel], built in 1983. Because of leakage problems, in the period 1992–1995 a [http://www.kajima.co.jp/topics/perspect/vol_15_3/salt/ new water-tight tunnel] was built inside the old one.
See also

- wikisource:Constantinople Convention of the Suez Canal
- Pharaoh (historical novel by Bolesław Prus, incorporating motifs of an ancient "Suez Canal").
External links

- [http://www.livius.org/aa-ac/achaemenians/DZ.html Darius the Great's Suez Inscriptions]
- [http://www.mfa.gov.eg/MFA_Portal/en-GB/Foreign_Policy/Treaties/CONVENTION+RESPECTING+THE+FREE+NAVIGATION+OF+THE+SUEZ+MARITIME+CANAL.htm Constantinople Convention of the Suez Canal, 1888]
- [http://www.halcrow.com/archivenews_nov01_swingbrid.asp El Ferdan railway bridge]
- [http://lexicorient.com/cgi-bin/eo-direct-frame.pl?http://i-cias.com/e.o/suez_can.htm Encyclopedia of the Orient: Suez Canal]
- [http://www.randomhouse.com/acmart/catalog/display.pperl?037570812X Parting the Desert] by Zachary Karabell
- [http://maps.google.com/maps?q=egypt&ll=30.519681,32.324524&spn=1.721732,2.906708&t=k&hl=en Google Maps Satellite Photo] of the Suez Canal Category:Canals Category:Transportation in Egypt Category:geography of Egypt Category:Economy of Egypt Category:Historic civil engineering landmarks Category:Coastal construction ko:수에즈 운하 ja:スエズ運河 simple:Suez Canal th:คลองสุเอซ

Isthmus of Panama

The Isthmus of Panama is the narrow strip of land that lies between the Caribbean Sea and the Pacific Ocean, linking North and South America. It was formed some 3 million years ago during the Pliocene epoch. It lies in the nation of Panama, and is cut by the Panama Canal. Like many isthmuses, it is a location of great strategic value due to its importance in both land and sea transportation. Category:Geography of Panama Panama ko:파나마 지협 ja:パナマ地峡

South America

South America is a continent, with most of its area in the Southern Hemisphere. South America is situated between the Pacific Ocean and the Atlantic Ocean. Commonly referred to as part of America, like North America, South America is named after Amerigo Vespucci, who was the first European to suggest that the Americas were not the East Indies, but a previously undiscovered New World. South America has an area of 17,821,601 km² (6,880,959 sq mi), or almost 3.5% of the Earth's surface. As of 2005, its population was estimated at more than 371,200,000. South America ranks fourth in area (after Asia, Africa, and North America) and fifth in population (after Asia, Africa, Europe, and North America).Europe __TOC__

Geography

The classification of its geographic location is subject to dispute, as in some non-English speaking regions of the world, the Americas are a continent and North, Central and South America are its subcontinents. In English-speaking and certain other regions of the world, North and South America are considered to be continents and their union is referred to as the supercontinent of the Americas. The classification given to South America, as a subcontinent in a continent or a continent in a supercontinent, depends entirely on regional preferences. It became attached to North America only recently (geologically speaking) with the formation of the Isthmus of Panama some 3 million years ago, which resulted in the Great American Interchange. The Andes, likewise a comparatively young and seismically restless mountain range, run down the western edge of the continent; the land to the east of the Andes is largely tropical rain forest, the vast Amazon River basin. The continent also contains drier regions such as Patagonia and the extremely arid Atacama desert. The region of South America also includes various islands, most of which belong to countries on the continent. The Caribbean territories are grouped with North America. The South American nations that border the Caribbean Sea – including Colombia, Venezuela, Guyana, Suriname, and French Guiana – are also known as Caribbean South America. Major natural resources are copper, iron ore, tin and oil. The many resources in South America have become useful around the world, but they have failed to diversify their economies. This has lead to major highs and lows in their economy causing instability. South America is home to many interesting species of animals including parrots, tarantulas, snakes, and mammals. The largest country in South America by far, in both area and population, is Brazil followed by Argentina. Regions in South America include the Andean States, the Guianas, the Southern Cone, and Eastern South America.

History

South America is thought to have been first inhabited by people crossing the Bering Land Bridge, now the Bering strait, though there are also suggestions of migration from the southern Pacific Ocean.

Chavín

The Chavín established a trade network and developed agriculture by 900 BC, according to some estimates and archeological finds. Artifacts were found at a site called Chavín de Huantar in modern Peru at an elevation of 3,177 meters. Chavín civilization spanned 900 BC to 300 BC.

Inca

Holding their capital at the great city of Cusco, the Inca civilization dominated the Andes region from 1438 to 1533. Known as Tahuantinsuyu, or "the land of the four regions," in Quechua, the Inca culture was highly distinct and developed. Cities were built with precise, unmatched stonework, constructed over many levels of mountain terrain. Terrace farming was a useful form of agriculture. There is evidence of excellent metalwork and even successful brain surgery in Inca civilization.

European colonization

Before arrival of Europeans, an estimated 30 million people lived in South America. brain surgery In 1494, Portugal and Spain, the two great maritime powers of that time, on the expectation of new lands being discovered in the west, signed the Treaty of Tordesillas, by which they agreed that all the land outside Europe should be an exclusive duopoly between the two countries. The Treaty established an imaginary line along a north-south meridian 370 leagues west of Cape Verde Islands, roughly 46° 37' W. In terms of the treaty, all land to the west of the line (which is now known to comprehend most of the South American soil), would belong to Spain, and all land to the east, to Portugal. As accurate measurements of longitude were impossible at that time, the line was not strictly enforced, resulting in a Portuguese expansion of Brazil across the meridian. Beginning in the 1530s, the people and natural resources of South America were repeatedly exploited by foreign conquistadors, first from Spain and later from Portugal. These competing colonial nations claimed the land and resources as their own and divided it into colonies. European diseases (smallpox, influenza, measles and typhus) to which the native populations had no resistance, and cruel systems of forced labor, such as the infamous haciendas and mining industry's mita, decimated the American population under Spanish control. After this, African slaves, who had developed immunities to these diseases, were quickly brought in to replace them. The Spaniards were committed to converting their American subjects to Christianity, and were quick to purge any native cultural practices that hindered this end. However, most initial attempts at this were only partially successful, as American groups simply blended Catholicism with their traditional beliefs. On the other hand, the Spaniards did not impose their language to the degree they did their religion, and the Catholic Church's evangelization in , and actually contributed to the expansion of these American languages, equipping them with writing systems. Eventually the Natives and the Spaniards interbred, forming a Mestizo class. These and the original Americans were often forced to pay unfair taxes to the Spanish government and were punished harshly for disobeying their laws. Many native artworks were considered pagan idols and destroyed by Spanish explorers. This included the many gold and silver sculptures found in the Americas, which were melted down before transport to Europe. Mestizo

Independence

The Spanish colonies won their independence in the first quarter of the 19th century, in the South American Wars of Independence. Simon Bolivar and José de San Martín led their independence struggle. In Brazil, a Portuguese colony, Dom Pedro I (also Pedro IV of Portugal), son of the Portuguese king Dom João VI, proclaimed the country's independence in 1822 and became Brazil's first Emperor. This was peacefully accepted by the crown in Portugal. Although Bolivar attempted to keep the Spanish-speaking parts of the continent politically unified, they rapidly became independent of one another as well, and several further wars were fought, such as the War of the Triple Alliance and the War of the Pacific. A few countries did not gain independence until the 20th century:
- Trinidad and Tobago, from the United Kingdom, in 1962
- Guyana, from the United Kingdom, in 1966.
- Suriname, from the Dutch control, in 1975 French Guiana remains part of France as of 2005, and hosts the European Union's principal spaceport, the Centre Spatial Guyanais.

Recent history

The continent, like many others, became a battlefield of the Cold War in the late 20th century. The government of Chile was overthrown in the early 1970s, as a late (and peculiar) development of the U.S. Monroe Doctrine. Throughout the 1980s and 1990s, Peru suffered from internal conflicts (see Túpac Amaru Revolutionary Movement and Shining Path). Other revolutions and military dictatorships have been common, but starting in the 1980s a wave of democratization came through the continent, and democratic rule is the norm now. Allegations of corruption remain common, and several nations have seen crises which have forced the resignation of their presidents, although normal civilian succession has continued. International indebtedness became a notable problem, as most recently illustrated by Argentina's default in the early 21st century.

Economy

As of 2002, South America's gross domestic product declined by 0.3 percent, and its unemployment rate was 10.8 percent. Due to histories of high inflation in nearly all South American countries, interest rates and thus investment remain high and low, respectively. Interest rates are usually double that of the United States. For example, interest rates are about 22 percent in Venezuela and 23 percent in Suriname. The exception is Chile, which had a head start from 1973 under Augusto Pinochet. The South American Community of Nations is a planned continent-wide free trade zone to unite two existing free-trade organizations—Mercosur and the Andean Community. In South America, the gap between the rich and the poor is tremendous. In Venezuela, Paraguay, Brazil, and many other South American countries, the richest 20 percent may own over 60 percent of the nation's wealth, while the poorest 20 percent may own less than 5 percent. This wide gap can be seen in many large South American cities where makeshift shacks and slums lie next to skyscrapers and upper-class luxury apartments.

Culture

Roman Catholicism is the dominant religion. French Guiana also has a large number of Protestants. Guyana and Suriname are exceptions, with three major religions: Christianity in general, Hinduism, and Islam. Portuguese and Spanish are the primary languages of the continent. The majority of South Americans (51%) speak Portuguese. However, most South American countries are Spanish-speaking, and nearly all of the continent's lusophones reside in Brazil. Among other languages used by many South Americans are:
- Aymará in Bolivia and Peru.
- Quechua in Bolivia, Ecuador, and Peru.
- Guaraní in Paraguay.
- English in Guyana.
- Hindi in Guyana and Suriname.
- Dutch and Indonesian in Suriname.
- Italian and German in certain pockets across southern South America. South American nations have a rich variety of music. Some of the most famous genres include samba from Brazil and cumbia from Colombia. Because of South America's ethnic mix, South American cuisine takes on African, American Indian, and European influences. Bahia, Brazil, is especially well-known for its West African-influenced cuisine.

People

Ethnic groups of South America include:
- Awá
- Banawa
- Caiapos
- Enxet
- European descendants, especially from Spain, Portugal and Italy.
- Ge
- Guarani
- Incas
- Quechuas
- Juris
- Latin peoples
- Mapuche
- Mestizo
- Xucuru
- Zaparos Indigenous peoples make up the majority of the population in Bolivia and Peru, and are a significant element in most other former Spanish colonies. Exceptions to this include Argentina and Uruguay. At least three of the Amerindian languages (Quechua in Peru and Bolivia, Aymara also in Bolivia, and Guarani in Paraguay) are recognized along with Spanish as national languages. Argentina is 10 percent Indian.

Mestizos

"Mestizo" is a term of Spanish origin used to designate the peoples of mixed European and Amerindian racial strain inhabiting the region spanning the Americas. Mestizos officially make up the majority of the populations of Chile (90%), Colombia (58%), Ecuador (65%), Paraguay (95%) and Venezuela (67%). Figures in other countries are Argentina (about 13%), Bolivia (30%), Brazil (about 12%), Uruguay (8%) and Peru (37%).

African ancestry

Africans first arrived with the Spanish and Portuguese in the 16th century. Most were brought as slaves and delivered to Brazil and the Caribbean. Brazil now has about 60 million black people. Venezuela and Colombia also have significant black population. "Mulato" is a term of Spanish origin (Mulatto in English) describing Latin Americans of mixed African and White racial descent. "Zambo" is a term of Spanish origin describing Latin Americans of mixed African and Amerindian racial descent. The feminine form is zamba.

Territories and divisions

Notes:
¹ La Paz is the administrative capital of Bolivia; Sucre is the judicial seat.
² Santiago is the administrative capital of Chile; Valparaíso is the site of legislative meetings.
³ Claimed by Argentina.
⁴ The South Georgia and the South Sandwich Islands have no permanent population, only hosting a periodic contingent of about 100 researchers and visitors.
- Depending on definitions, Panama and Trinidad and Tobago have territory in one or both of South and North America.

External links

News
- [http://www.notisur.com/ NOTISUR -- Political and social news of South America (in Spanish)] Sports
- [http://www.conmebol.com/ CONMEBOL -- Confederación Sudamericana de Fútbol (The South American Footbal Confederation) in Spanish and Portuguese] Geography
- [http://www.freeworldmaps.net/southamerica/index.html Physical map of South America] South American Community of Nations Category:Continents South America zh-min-nan:Lâm Bí-chiu ko:남아메리카 ja:南アメリカ simple:South America th:ทวีปอเมริกาใต้

Greece

Greece, (Greek: Ελλάδα, older form: Ελλάς, Hellas), officially the Hellenic Republic (Greek: Ελληνική Δημοκρατία, Ellinikí Dimokratía; see also List of traditional Greek place names), is a country in southern Europe on the tip of the Balkan peninsula. It has land boundaries with Bulgaria, The Republic of Macedonia, and Albania to the north and with Turkey to the east. The waters of the Aegean Sea border Greece to the east, and those of the Ionian and Mediterranean Sea to the west and south. Regarded by many as the cradle of Western civilization and the birthplace of democracy, Greece has a long and rich history during which its culture has proven especially influential in Europe, North Africa, and the Middle East.

Name

Main article: Names of the Greeks The historical name of Greece in Greek is Ellás . This name is also written Hellas in English, following the ancient Greek pronunciation . In modern Greek it is called more commonly Ελλάδα Elládha . The mythical ancestor of the Greeks is the eponymous Hellen. The name of Greece in European languages (English: Greece, French: Grèce, Portuguese: Grécia, Spanish and Italian: Grecia, Welsh: Groeg, German: Griechenland, Dutch: Griekenland, Russian: Греция, etc.) comes from a different root: Graikós (via Latin Graecus) which according to Aristotle was an ancient name for the Greeks. The Japanese name is ギリシャ (Girisha), lent from European languages. On the other hand, the name of Greece in some Middle Eastern and Eastern languages (Turkish: Yunanistan, Arabic: يونان, Hebrew: יוון, ancient Persian: Yaunâ, Indian Pali: Yona, Malay and Indonesian: Yunani) derives from the Greek toponym Iōnía. Norwegian, Chinese (希腊 Xila) and Vietnamese are three of the few languages apart from Greek in which the name Hellas predominates. An interesting and unique form is kept in Georgian. In ancient times, Georgians (Colchs and Iberians) called Greeks ბერძენი berdzeni. This form derives from the Georgian word ბრძენი brdzeni – wise. According to Georgian historians, the name is connected with the notion that philosophy was born in Greece. Modern Georgians still call Greeks ბერძენი berdzeni and Greece საბერძნეთი saberdznet'i, 'Greeks' land' or literally 'land of the wise'. Some Greeks prefer the name Hellas for the country and Hellenes for the people even in English. See Hellenes for discussion.

History

Hellenes Main Article: History of Greece.

Prehistory and antiquity

The shores of Greece's Aegean Sea saw the emergence of the first civilizations in Europe, namely the Minoan and the Mycenaean. After these, a Dark Age followed until around 800 BC, when a new era of Greek city-states emerged establishing colonies along the Mediterranean. Greek culture would later become the basis of the Hellenistic civilization that followed the empire of Alexander the Great. For a detailed history of Ancient Greece see the relevant articles in: History of Greece.

Roman rule and Middle Ages

Militarily, Greece itself declined to the point that the Romans conquered the land (168 BC onwards), though, in many ways, Greek culture would in turn conquer Roman life. Greece became a province of the Roman Empire, but Greek culture continued to dominate the eastern Mediterranean. When the Roman Empire finally split in two, the Eastern Roman Empire, known as the Byzantine Empire, centered around Constantinople (known in ancient times as Byzantium), remained Greek in nature, encompassing Greece itself. From the 4th century to the 15th century, the Byzantine Empire survived eleven centuries of attacks from the north, west and east until Constantinople fell on May 29 1453 to the Ottoman Empire, when Constantine XI, the last emperor of the Palaeologus dynasty, fell. Greece was gradually conquered by the Ottomans during the 15th century.

Ottoman rule

While the Ottomans completed the conquest of the Greek Mainland, two Greek migrations occurred. The first migration saw the Greek intelligentsia migrate to Western Europe and contribute to the advent of the Renaissance. The second migration of Greeks left the plains of the Greek peninsula and resettled in the mountains. The Ottomans were unable to create a permanent military and administrative presence in these mountainous regions. As a result some Greek mountain clans across the peninsula, as well as some islands, were able to maintain a status of independence. The Sphakiots of Crete, the Souliots from Souli of Epirus, and the Maniots from Mani of Peloponnesus were the most resilient mountain clans throughout the Ottoman Empire. By the end of the 16th century and until the 17th century, Greeks began to migrate back to the plains and cities, adding to the increasing urban population. The millet system contributed to the ethnic cohesion of Orthodox Greeks by segregating the various peoples within the Ottoman Empire based on religion. The Orthodox Church, a religious institution with a strong national character, helped the Greeks from all geographical areas of the peninsula (i.e. mountains, plains, and islands) to preserve their ethnic, cultural and linguistic heritage during the years of the Ottoman rule (although at the time it was not stictly speaking a "Greek" church - the Greek Church was instituted after the liberation). The Greeks who remained on the plains during Ottoman occupation were either Christians, who dealt with the burdens of foreign rule, or to a considerable extent Crypto-Christians (Greeks Muslims who were secret practitioners of the Orthodox faith) in order to avoid heavy taxation. The Greeks who converted to Islam and were not Crypto-Christians became Turks in the eyes of Orthodox Greeks. There were no "Greek Muslims", and no "Christian Turks". As a result, religion played an integral part in the formation of the Modern Greek and other post-Ottoman national identities. Turks

Creation of the modern Greek state

The Ottomans ruled Greece until the early 19th century. In 1821, the Greeks rebelled and declared their independence, but did not succeed in winning it until 1829. The elites of powerful European nations saw the war of Greek independence, with its accounts of Turkish atrocities, in a romantic light (see, for example, the 1824 painting the Massacre of Chios by Eugène Delacroix). Scores of non-Greeks volunteered to fight for the cause — including people like Lord Byron. At times the Ottomans seemed on the verge of entirely suppressing the Greek revolution but were eventually forced to give in by the direct military intervention of France, Great Britain and Russia. This was the prelude of the so called "Eastern Question", the gradual dismemberment of the decaying empire by the western powers. The Russian ex-minister of foreign affairs, Ioannis Kapodistrias, himself a Greek, actually a noble from the Ionian Islands, a British protectorate in the Ionian Sea, was chosen as President of the new Republic following Greek independence. That republic disappeared when a few years later Western powers helped turn Greece into a monarchy, the first king coming from Bavaria and the second from Denmark. During the 19th and especially the early 20th centuries, in a series of wars with the Ottomans, Greece sought to enlarge its boundaries to include the ethnic Greek population of the Ottoman Empire (the Ionian State however was donated by Britain upon the arrival of the new king from Denmark in 1863, and Thessaly was ceded by the Ottomans without a fight). Greece would slowly grow in territory and population until reaching its present configuration in 1947. In World War I, Greece sided with the entente powers against Turkey and the other Central Powers. In the war's aftermath, the Great Powers awarded parts of Asia Minor to Greece, including the city of Smyrna (known as Izmir today) which had a large Greek population. At that time, however, the Turkish nationalists, led by Mustafa Kemal Atatürk, denounced the Sultan's government in Istanbul and organised a new one in Ankara. During the Greco-Turkish War (1919-1922) the Turks eventually defeated the Greek armies and regained control of Asia Minor. Soon afterwards, the Treaty of Lausanne was signed, fixing the borders to this date. A population exchange was included in the agreement and immediately afterwards, hundreds of thousands of Turks then living in mainland Greek territory left for Turkey in exchange for about a million Greeks living in Turkey. The refugees from Asia Minor revived the population, provided cheap labour and hellenized the now depopulated regions, especially in Macedonia. In 1936, General Ioannis Metaxas established an authoritarian conservative dictatorship in Greece, seen as similar to Antonio Salazar's "New State". Greece under Metaxas is also compared to Spain at the time, although it lacked the political violence associated with Francisco Franco's regime. Despite the country's numerically small and ill-equipped armed forces, Greece made an important contribution to the Allied efforts in World War II. At the start of the war Greece sided with the Allies and refused to give in to Italian demands (see Oxi Day). Italy invaded Greece on 28 October 1940, but Greek troops repelled the invaders after a bitter struggle (see Greco-Italian War). This marked the first Allied victory in the war. Hitler then reluctantly stepped in, primarily to secure his strategic southern flank. Troops from Germany, Hungary, Bulgaria, and Italy successfully invaded Greece, overcoming Greek, British, Australian, and New Zealand units within weeks. To reduce the threat of a counter-offensive by Allied forces in Egypt, the Germans attempted to seize Crete in a massive attack by paratroops. Allied forces, along with Cretan civilians, however, offered fierce resistance. Although Crete eventually fell, it is pointed out by historians that this, and the whole Greek campaign, delayed German plans