Australia

Area	8,468,300 km2 (3,269,600 sq mi)
Population	~31,260,000 (estimated population of Australia, Papua New Guinea and the Papua and West Papua provinces of Indonesia for 2009)
Pop. density	~ 3.7 /km2 (9.6 /sq mi)
Demonym	Australian
Countries	3 (Australia, Papua New Guinea and portions of Indonesia)
Languages	English, Indonesian, Tok Pisin, Hiri Motu, 269 indigenous Papuan and Austronesian languages and about 70 Indigenous Australian languages
Time Zones	GMT+10, GMT+9.30, GMT+8
Internet TLD	.au, .pg and .id
Largest cities	List of cities in Australia by population List Sydney Melbourne Brisbane Perth Adelaide Gold Coast-Tweed Newcastle Canberra-Queanbeyan Canberra Wollongong

Australia is a continent comprising the mainland of the country of Australia and proximate islands including Tasmania, New Guinea, the Aru Islands, and the Raja Ampat Islands. These are a single geological landmass, separated by seas overlying the continental shelf — the Arafura Sea and Torres Strait between Australia and New Guinea, and Bass Strait between mainland Australia and Tasmania. When sea levels were lower during the Pleistocene ice age, including the last glacial maximum about 18,000 BC, they were connected by dry land. During the past ten thousand years, rising sea levels overflowed the lowlands and separated the continent into today's low-lying arid to semi-arid mainland and the two mountainous islands of New Guinea and Tasmania. Geologically, a continent extends to the edge of its continental shelf, so the now-separate islands are considered part of the continent.^[1] Due to the spread of flora and fauna across the single Pleistocene landmass the separate lands have a related biota.

New Zealand is not part of the continent of Australia, but of the separate, submerged continent of Zealandia. Zealandia and Australia are both part of the wider regions known as Australasia and Oceania. The continent of Australia is sometimes known in technical contexts by the names Sahul, Australinea or Meganesia, to distinguish it from the Australian mainland. It is the smallest of the seven traditional continents in the English conception.

Geography and nomenclature[link]

Mainland Australia showing the continental Sahul Shelf (light blue) extending to the islands of New Guinea in the north, the island of Timor in the northwest, and Tasmania in the south

Satellite image of the country of Australia

The Australian continent is the smallest and lowest-lying human-inhabited continent on Earth, having a total land area of some 8,560,000 square kilometres (3,305,000 sq. mi.). The continental shelf connecting the islands, half of which is less than 50 metres deep covers some 2,500,000 square kilometres, including the Sahul Shelf^[2][3] and Bass Strait. As the country of Australia is mostly on a single landmass, and comprises most of the continent, it is sometimes informally referred to as an "island" continent, surrounded by oceans.^[4]

Prior to the 1970s, archaeologists called the single Pleistocene landmass by the name Australasia,^[5] derived from the Latin australis, meaning "southern", although this word is most often used for a wider region that includes lands like New Zealand that are not on the same continental shelf.

In the early 1970s, they introduced the term Greater Australia for the Pleistocene continent.^[5] Then at a 1975 conference and consequent publication,^[6] they extended the name Sahul from its previous use for just the Sahul Shelf to cover the continent.^[5]

In 1984, biologists suggested the name Meganesia, meaning "great island" or "great island-group", applying it to both the Pleistocene continent and the present-day lands,^[7] and this name has been taken up by biologists.^[8] Others have used Meganesia with different meanings: travel writer Paul Theroux included New Zealand in his definition^[9] and others have used it for Australia, New Zealand and Hawaii.^[10] Another biologist, Richard Dawkins coined the name Australinea in 2004.^[11] Australia-New Guinea has also been used.^[12]

Geology[link]

The continent primarily sits on the Indo-Australian Plate. The lands were joined with Antarctica as part of the southern supercontinent Gondwana until the plate began to drift north about 96 million years ago. For most of the time since then, Australia–New Guinea has remained a single, continuous landmass. When the last ice age ended in about 10,000 BC, rising sea levels formed Bass Strait, separating Tasmania from the mainland. Then between about 8,000 and 6,500 BC, the lowlands in the north were flooded by the sea, separating New Guinea and Australia.

Biogeography[link]

As the continent drifted north from Antarctica, unique flora and fauna developed. Marsupials and monotremes also existed on other continents, but only in Australia–New Guinea did they out-compete the placental mammals and come to dominate. Bird life also flourished, in particular the ancestors of the great passerine order that would eventually spread to all parts of the globe and account for more than half of all living avian species.

Animal groups such as macropods, monotremes, and cassowaries are endemic to Australia. There were three main reasons for the enormous diversity that developed in both plant and animal life.

• While much of the rest of the world underwent significant cooling and thus loss of species diversity, Australia–New Guinea was drifting north at such a pace that the overall global cooling effect was roughly equalled by its gradual movement toward the equator. Temperatures in Australia–New Guinea, in other words, remained reasonably constant for a very long time, and a vast number of different plant and animal species were able to evolve to fit particular ecological niches.
• Because the continent was more isolated than any other, very few outside species arrived to colonise, and unique native forms developed unimpeded.
• Finally, despite the fact that the continent was already very old and thus relatively infertile, there are dispersed areas of high fertility. Where other continents had volcanic activity and/or massive glaciation events to turn over fresh, unleached rocks rich in minerals, the rocks and soils of Australia–New Guinea were left largely untouched except by gradual erosion and deep weathering. In general, fertile soils produce a profusion of life, and a relatively large number of species/level of biodiversity. This is because where nutrients are plentiful, competition is largely a matter of outcompeting rival species, leaving great scope for innovative co-evolution as is witnessed in tropical, fertile ecosystems. In contrast, infertile soils tend to induce competition on an abiotic basis meaning individuals all face constant environmental pressures, leaving less scope for divergent evolution, a process instrumental in creating new species.

For about 40 million years Australia–New Guinea was almost completely isolated. During this time, the continent experienced numerous changes in climate, but the overall trend was towards greater aridity. When South America eventually separated from Antarctica, the development of the cold Antarctic Circumpolar Current changed weather patterns across the world. For Australia–New Guinea, it brought a marked intensification of the drying trend. The great inland seas and lakes dried out. Much of the long-established broad-leaf deciduous forest began to give way to the distinctive hard-leaved sclerophyllous plants that characterise the modern Australian landscape.

For many species, the primary refuge was the relatively cool and well-watered Great Dividing Range. Even today, pockets of remnant vegetation remain in the cool uplands, some species not much changed from the Gondwanan forms of 60 or 90 million years ago.

Eventually, the Australia–New Guinea tectonic plate collided with the Eurasian plate to the north. The collision caused the northern part of the continent to buckle upwards, forming the high and rugged mountains of New Guinea and, by reverse (downwards) buckling, the Torres Strait that now separates the two main landmasses. The collision also pushed up the islands of Wallacea, which served as island 'stepping-stones' that allowed plants from Southeast Asia's rainforests to colonise New Guinea, and some plants from Australia–New Guinea to move into Southeast Asia. The ocean straits between the islands were narrow enough to allow plant dispersal, but served as an effective barrier to exchange of land mammals between Australia–New Guinea and Asia.

Although New Guinea is the most northerly part of the continent, and could be expected to be the most tropical in climate, the altitude of the New Guinea highlands is such that a great many animals and plants that were once common across Australia–New Guinea now survive only in the tropical highlands where they are severely threatened by overpopulation pressures.

See also[link]

• List of basic Australia topics
• Plate tectonics
• Paleoclimatology
• Australasia
• Oceania

References[link]

v t e Regions of the World Africa Northern Middle East Sub-Saharan Central Southern Western Eastern Oceania Australasia Australia Zealandia Melanesia Micronesia Polynesia America North Northern Middle Central Caribbean South Southern Northern Western Guianan States Anglo Latin (Hispanic) Polar regions Arctic Antarctic Asia Central Eastern Northeastern Northern Southeastern Mainland Maritime Southern Indian subcontinent Western Middle East Oceans World Arctic Atlantic Indian Pacific Southern Europe Central Eastern Northern Southeastern Middle East Southern Western Seas List of seas Related Continents of the world List of seas Physical Earth

v t e Australia History Timeline Prehistory Archaeology Exploration 1606–1787 1788–1850 1851–1900 1901–1945 Since 1945 Constitutional Diplomatic Economic Federation Immigration Indigenous Military Monarchy Railway Geography States and Territories Capitals Cities Cities by population Climate Continent Deserts Environment Flora Fauna Forests Geology Islands Mountains Regions Protected Areas Rivers Governance Government Constitution Monarchy Australian governments Parliament Foreign relations Military Law Law Enforcement Courts Electoral system Public Service Intelligence and Security Federal Budget National debt Politics Political parties Elections Political donations Economy Agriculture Companies Energy Home ownership Homelessness Manufacturing Media Mining Poverty Taxation Telecommunications Tourism Transportation Australian dollar Reserve Bank Stock Exchange Household income Gross state product Welfare system Superannuation Society Crime Demographics Education Health care Human rights Immigration LGBT rights Culture Australians Architecture Arts Australian English Cinema Cuisine Wine Dance Indigenous Literature Music Public holidays Religion Sport Television Theatre Art Symbols Coat of arms Flags Honours States and Territories Other Australian of the Year Award Environmental issues Overviews Index Outline Book Category Portal WikiProject

Coordinates: 26°S 141°E / 26°S 141°E / -26; 141lez:Австралия (континент)vep:Avstralii (kontinent)

Commonwealth of Australia
Flag Coat of arms
Anthem: "Advance Australia Fair" Royal anthem: "God Save the Queen"[N 1]
Capital		Canberra 35°18.48′S 149°7.47′E / 35.308°S 149.1245°E / -35.308; 149.1245
Largest city		Sydney
Official language(s)		None[N 2]
National language		English (de facto)[N 2]
Demonym		Australian, Aussie[3][4]
Government		Federal parliamentary constitutional monarchy
-	Monarch	Elizabeth II
-	Governor-General	Quentin Bryce
-	Prime Minister	Julia Gillard
Legislature		Parliament
-	Upper house	Senate
-	Lower house	House of Representatives
Independence		from the United Kingdom
-	Constitution	1 January 1901
-	Statute of Westminster	11 December 1931
-	Statute of Westminster Adoption Act	9 October 1942 (with effect from 3 September 1939)
-	Australia Act	3 March 1986
Area
-	Total	7,617,930 km2 (6th) 2,941,299 sq mi
Population
-	2012 estimate	22,944,040[5] (52nd)
-	2006 census	19,855,288[6]
-	Density	2.8/km2 (233rd) 7.3/sq mi
GDP (PPP)		2011 estimate
-	Total	$914.482 billion[7] (18th)
-	Per capita	$40,234[7] (12th)
GDP (nominal)		2011 estimate
-	Total	$1.488 trillion[7] (13th)
-	Per capita	$65,477[7] (5th)
Gini (2006)		30.5[8] (medium)
HDI (2011)		0.929[9] (very high) (2nd)
Currency		Australian dollar (AUD)
Time zone		various[N 3] (UTC+8 to +10.5)
-	Summer (DST)	various[N 3] (UTC+8 to +11.5)
Date formats		dd-mm-yyyy
Drives on the		left
ISO 3166 code		AU
Internet TLD		.au
Calling code		+61

Australia ( /əˈstreɪljə/), officially the Commonwealth of Australia,^[10] is a country in the Southern Hemisphere comprising the mainland of the Australian continent as well as the island of Tasmania and numerous smaller islands in the Indian and Pacific Oceans.^{[N 4]} It is the world's sixth-largest country by total area. Neighbouring countries include Indonesia, East Timor and Papua New Guinea to the north; the Solomon Islands, Vanuatu and New Caledonia to the north-east; and New Zealand to the south-east.

For at least 40,000 years^[12] before European settlement in the late 18th century, Australia was inhabited by indigenous Australians,^[13] who belonged to one or more of roughly 250 language groups.^[14][15] After discovery by Dutch explorers in 1606, Australia's eastern half was claimed by Great Britain in 1770 and settled through penal transportation to the colony of New South Wales from 26 January 1788. The population grew steadily in subsequent decades; the continent was explored and an additional five self-governing Crown Colonies were established.

On 1 January 1901, the six colonies federated, forming the Commonwealth of Australia. Since Federation, Australia has maintained a stable liberal democratic political system which functions as a federal parliamentary democracy and constitutional monarchy. The federation comprises six states and several territories. The population of 22.9 million is heavily concentrated in the Eastern states and is highly urbanised.

A highly developed country, Australia is the world's 13th-largest economy and has the world's fifth-highest per capita income. Australia's military expenditure is the world's 13th-largest. With the second-highest human development index globally, Australia ranks highly in many international comparisons of national performance, such as quality of life, health, education, economic freedom, and the protection of civil liberties and political rights.^[16] Australia is a member of the G20, OECD, WTO, APEC, UN, Commonwealth of Nations, ANZUS, and the Pacific Islands Forum.

Etymology[link]

Pronounced [əˈstɹæɪljə, -liə] in Australian English,^[17] the name Australia is derived from the Latin australis, meaning "southern". The country has been referred to colloquially as Oz since the early 20th century.^{[N 5]} Aussie is a common colloquial term for "Australian". In neighbouring New Zealand the term "Aussie" is sometimes applied as a noun to the nation as well as its residents.^[22]

Legends of Terra Australis Incognita—an "unknown land of the South"—date back to Roman times and were commonplace in medieval geography, although not based on any documented knowledge of the continent. Following European discovery, names for the Australian landmass were often references to the famed Terra Australis.

The earliest recorded use of the word Australia in English was in 1625 in "A note of Australia del Espíritu Santo, written by Sir Richard Hakluyt", published by Samuel Purchas in Hakluytus Posthumus, a corruption of the original Spanish name "Tierra Austral del Espíritu Santo" (Southern Land of the Holy Spirit)^[23] for an island in Vanuatu.^[24] The Dutch adjectival form Australische was used in a Dutch book in Batavia (Jakarta) in 1638, to refer to the newly discovered lands to the south.^[25] Australia was later used in a 1693 translation of Les Aventures de Jacques Sadeur dans la Découverte et le Voyage de la Terre Australe, a 1676 French novel by Gabriel de Foigny, under the pen-name Jacques Sadeur.^[26] Referring to the entire South Pacific region, Alexander Dalrymple used it in An Historical Collection of Voyages and Discoveries in the South Pacific Ocean in 1771. By the end of the 18th century, the name was being used to refer specifically to Australia, with the botanists George Shaw and Sir James Smith writing of "the vast island, or rather continent, of Australia, Australasia or New Holland" in their 1793 Zoology and Botany of New Holland,^[27] and James Wilson including it on a 1799 chart.^[28]

The name Australia was popularised by the explorer Matthew Flinders, who pushed for it to be formally adopted as early as 1804. When preparing his manuscript and charts for his 1814 A Voyage to Terra Australis, he was persuaded by his patron, Sir Joseph Banks, to use the term Terra Australis as this was the name most familiar to the public. Flinders did so, but allowed himself the footnote:

"Had I permitted myself any innovation on the original term, it would have been to convert it to Australia; as being more agreeable to the ear, and an assimilation to the names of the other great portions of the earth."^[29]

This is the only occurrence of the word Australia in that text; but in Appendix III, Robert Brown's General remarks, geographical and systematical, on the botany of Terra Australis, Brown makes use of the adjectival form Australian throughout,^[30]—the first known use of that form.^[31] Despite popular conception, the book was not instrumental in the adoption of the name: the name came gradually to be accepted over the following ten years.^[32]

The first time that the name Australia appears to have been officially used was in a despatch to Lord Bathurst of 4 April 1817 in which Governor Lachlan Macquarie acknowledges the receipt of Capt. Flinders' charts of Australia.^[33] On 12 December 1817 Macquarie recommended to the Colonial Office that it be formally adopted.^[34] In 1824, the Admiralty agreed that the continent should be known officially as Australia.^[35]