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The of Australia, sometimes known in technical contexts as Sahul (), Australia-New Guinea, Australinea, or Meganesia to distinguish it from the , is located within the Southern and Eastern hemispheres, near the Maritime Southeast Asia. The continent includes mainland Australia, , the island of (Papua New Guinea and Western New Guinea), the Aru Islands, the Ashmore and Cartier Islands, most of the Coral Sea Islands, and some other nearby islands. Situated in the geographical region of , more specifically in the subregion of , Australia is the smallest of the seven traditional continents.

The continent includes a continental shelf overlain by shallow seas which divide it into several landmasses—the and between mainland Australia and New Guinea, and between mainland Australia and Tasmania. When were lower during the Pleistocene ice age, including the Last Glacial Maximum about 18,000 BC, they were connected by dry land into the combined landmass of . The name "Sahul" derives from the , which is a part of the continental shelf of the Australian continent. During the past 18,000 to 10,000 years, rising sea levels overflowed the lowlands and separated the continent into today's low-lying to semi-arid mainland and the two mountainous islands of New Guinea and Tasmania. With a total land area of , the Australian continent is the smallest, lowest, flattest, and second-driest continent (after ) on . 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.

(1983). 9780091304607, Hutchinson Group.

Papua New Guinea, a country within the continent, is one of the most culturally and linguistically diverse countries in the world. It is also one of the most rural, as only 18 percent of its people live in urban centres. West Papua, a region in Indonesia, is home to an estimated 44 uncontacted tribal groups. Australia, the largest landmass in the continent, is highly , and has the world's 14th-largest economy with the second-highest human development index globally.Data refer mostly to the year 2014. World Economic Outlook Database-April 2015, International Monetary Fund. Accessed on 25 April 2015. Australia also has the world's 9th largest immigrant population.United Nations, Department of Economic and Social Affairs, Population Division, (2019). 'International Migration' in International migrant stock 2019. Accessed from International migrant stock 2015: maps on 24 May 2017.


Terminology
The continent of Australia is sometimes known by the names Sahul, Australinea, or Meganesia to differentiate it from the country of Australia, and consists of the landmasses which sit on Australia's continental plate. This includes mainland Australia, , and the island of , which comprises Papua New Guinea and Western New Guinea (Papua and West Papua, provinces of ).
(2025). 9780759123908, AltaMira Press. .
(2018). 9780199925070, Oxford University Press. .
(2025). 9781921313042, ANU e Press. .
The name "Sahul" takes its name from the , which is part of the continental shelf of the Australian continent. The term , originally a "great division" of the world in the 1810s, was replaced in countries by the concept of Australia as one of the world's continents in the 1950s.

Prior to the 1950s, before the popularization of the theory of , , Australia and were sometimes described as island continents, but none were usually taught as one of the world's continents in English-speaking countries.: "...the 1950s... was also the period when... Oceania as a "great division" was replaced by Australia as a continent along with a series of isolated and continentally attached islands. Footnote" Scottish wrote in 1873 that, "the consists of , and the peninsula of attached to it. These divisions are generally themselves spoken as continents, and to them has been added another, embracing the large island of Australia and numerous others in the Pacific Ocean, under the name of Oceania. There are thus six great divisions of the earth — , , , North America, South America and Oceania."

The American author Samuel Griswold Goodrich wrote in his 1854 book History of All Nations that, "geographers have agreed to consider the island world of the Pacific Ocean as a third continent, under the name Oceania." In this book the other two continents were categorized as being the New World (consisting of North America and South America) and the (consisting of Africa, Asia and Europe). In his 1879 book Australasia, British naturalist Alfred Russel Wallace commented that, "Oceania is the word often used by continental geographers to describe the great world of islands we are now entering upon" and that "Australia forms its central and most important feature." He did not explicitly label Oceania a continent in the book, but did note that it was one of the six major divisions of the world. He considered it to encompass the insular Pacific area between Asia and the Americas, and claimed it extended up to the , which are among the northernmost islands in the Pacific Ocean. However, definitions of Oceania varied during the 19th century. In the 19th century, many geographers divided up Oceania into mostly racially-based subdivisions; , Malaysia (encompassing Malay Archipelago), , and .

Today, the Malay Archipelago is typically considered part of , and the term is often used to denote the region encompassing the Australian continent, , and in the that are not included in the model. It has been recognized by the as one of the world's five major continental divisions since its foundation in 1947, along with , , and the .

(2025). 9781576076941, ABC-CLIO.
The UN's definition of Oceania utilizes four of the five subregions from the 19th century; Australasia, Melanesia, Micronesia, and Polynesia. They include , and their external territories, the , (), the Federated States of Micronesia, , , Galapagos Islands (), , , the , , , , , the Northern Mariana Islands, Ogasawara (), , Papua New Guinea, , , the , , , , , Wallis and Futuna, Western New Guinea, and the United States Minor Outlying Islands (, , , , , and ) as well as (one of 50 states of the United States). The original UN definition of Oceania from 1947 included these same countries and semi-independent territories, which were mostly still at that point.

The island states of , , the , and , all located within the bounds of the Pacific or associated , are excluded from the UN definition. The states of and , located in both mainland Asia and marginal seas of the Pacific, are also excluded, as is the nation of , which shares the island of with Indonesia and Malaysia. Further excluded are and Indonesian (or Western) New Guinea, areas which are biogeographically or geologically associated with the Australian landmass. This definition of Oceania is used in statistical reports, by the International Olympic Committee, and by many atlases.

(1997). 9780520207424, University of California Press. .
The CIA World Factbook also categorize Oceania or the Pacific area as one of the world's major continental divisions, but use the term "Australia and Oceania" to refer to the area. Their definition does not include Australia's subantarctic external territory Heard Island and McDonald Islands, but is otherwise the same as the UN definition, and it is also used for statistical purposes.

In countries such as , , , , , , , , , , the , , , or , Oceania is treated as a continent in the sense that it is "one of the parts of the world", and Australia is only seen as an island nation. In other countries, including , and , Australia and are thought of as continents, while Asia, Europe and Oceania are regarded as "parts of the world". In the Pacific Ocean Handbook (1945), author Eliot Grinnell Mears wrote that he categorized Australia, New Zealand and Pacific islands under the label of Oceania for "scientific reasons; Australia's fauna is largely continental in character, New Zealand's are clearly insular; and neither Commonwealth realm has close ties with Asia." He further added that, "the term Australasia is not relished by and this name is too often confused with Australia." Some 19th century definitions of Oceania grouped Australia, New Zealand and the islands of Melanesia together under the label of Australasia, in other 19th century definitions of Oceania, the term was only used to refer to Australia itself, with New Zealand being categorized with the islands of Polynesia in such definitions.

Archaeological terminology for this region has changed repeatedly. Before the 1970s, the single Pleistocene landmass was called Australasia, derived from the 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, the term Greater Australia was introduced for the Pleistocene continent. Then at a 1975 conference and consequent publication,

(1977). 9780120512508, Academic Press. .
the name Sahul was extended from its previous use for just the to cover the continent.

In 1984, the name Meganesia was suggested, meaning "great island" or "great island-group", for both the Pleistocene continent and the present-day lands, and this name has been widely accepted by biologists.

(1994). 9780730104223, Reed. .
Others have used Meganesia with different meanings: travel writer included New Zealand in his definition
(1992). 9780140159769, Penguin.
and others have used it for Australia, New Zealand and . Another biologist, , coined the name Australinea in 2004.
(2025). 9780618005833, Houghton Mifflin.
Australia–New Guinea has also been used.


History
The Australian continent and Sunda were points of early human migrations after leaving Africa.
(1988). 9780521331098, Cambridge University Press. .
Research points to a planned migration of hundreds of people using bamboo rafts, which eventually landed on Sahul.


Indigenous peoples
Indigenous Australians, that is Aboriginal Australians and Torres Strait Islanders people, are the original inhabitants of the Australian continent and nearby islands. They migrated from Africa to Asia around 70,000 years ago and arrived in Australia at least 50,000 years ago, based on archaeological evidence. More recent research points to earlier arrival, possibly 65,000 years ago.
(2018). 9781760640446, Black Inc..

They are believed to be among the earliest human migrations out of Africa. There is evidence of genetic and linguistic interchange between Australians in the far north and the Austronesian peoples of modern-day and the islands, but this may be the result of recent trade and intermarriage.. (1997). Guns, Germs, and Steel. Random House. London. pp 314–316 The were found at Lake Mungo, a dry lake in the southwest of New South Wales. Remains found at Mungo suggest one of the world's oldest known , thus indicating early evidence for religious ritual among humans.

(1971). 9780708104521, Australian National University Press.
remains a prominent feature of Australian Aboriginal art, the oldest continuing tradition of art in the world.

habitation is estimated to have begun between 42,000 and 48,000 years ago in New Guinea. Trade between New Guinea and neighboring Indonesian islands was documented as early as the seventh century, and archipelagic rule of New Guinea by the 13th. At the beginning of the seventh century, the -based empire of (7th century–13th century) engaged in trade relations with western New Guinea, initially taking items like and birds-of-paradise in tribute to China, but later making slaves out of the natives. The rule of the -based empire of (1293–1527) extended to the western fringes of New Guinea. Recent archaeological research suggests that 50,000 years ago people may have occupied sites in the highlands at New Guinean altitudes of up to , rather than being restricted to warmer coastal areas.


Pre-colonial history
Legends of Terra Australis Incognita—an "unknown land of the South"—date back to Roman times and before, and were commonplace in medieval geography, although not based on any documented knowledge of the continent.Albert-Marie-Ferdinand Anthiaume, "Un pilote et cartographe havrais au XVIe siècle: Guillaume Le Testu", Bulletin de Géographie Historique et Descriptive, Paris, Nos 1–2, 1911, pp. 135–202, n.b. p. 176. Ancient Greek philosopher speculated of a large landmass in the southern hemisphere, saying, "Now since there must be a region bearing the same relation to the southern pole as the place we live in bears to our pole...". His ideas were later expanded by (2nd century AD), who believed that the lands of the Northern Hemisphere should be balanced by land in the south. The theory of balancing land has been documented as early as the 5th century on maps by , who uses the term Australis on his maps.

, a hypothetical first posited in antiquity, appeared on maps between the 15th and 18th centuries.John Noble Wilford: The Mapmakers, the Story of the Great Pioneers in Cartography from Antiquity to Space Age, p. 139, Vintage Books, Random House 1982, Scientists, such as Gerardus Mercator (1569) and Alexander Dalrymple as late as 1767 argued for its existence, with such arguments as that there should be a large in the south as a to the known landmasses in the Northern Hemisphere.Carlos Pedro Vairo, TERRA AUSTRALIS Historical Charts of Patagonia, Tierra del Fuego and Antarctica. Ed. Zagier & Urruty Publicationa, 2010. The cartographic depictions of the southern continent in the 16th and early 17th centuries, as might be expected for a concept based on such abundant conjecture and minimal data, varied wildly from map to map; in general, the continent shrank as potential locations were reinterpreted. At its largest, the continent included Tierra del Fuego, separated from South America by a small strait; ; and what would come to be called Australia. Spieghel der Australische Navigatie; cited by A. Lodewyckx, "The Name of Australia: Its Origin and Early Use", The Victorian Historical Magazine, Vol. XIII, No. 3, June 1929, pp. 100–191.


European exploration
In 1606, Dutch navigator made the first documented European sight and landing on the continent of Australia in Cape York Peninsula.J.P. Sigmond and L.H. Zuiderbaan (1979) Dutch Discoveries of Australia.Rigby Ltd, Australia. pp. 19–30 Dutch explorer circumnavigated and landed on parts of the continental coast and discovered Van Diemen's Land (now ), in 1642, and islands.
(2025). 9781741266887, R.I.C. Publications. .
He was the first known European explorer to reach these islands.

In the quest for , Spanish explorations in the 17th century, such as the expedition led by the Portuguese navigator Pedro Fernandes de Queirós, discovered the and archipelagos, and sailed the between and , named after navigator Luís Vaz de Torres, who was the first European to explore the Strait. When first arrived, inhabitants of New Guinea and nearby islands, whose technologies included bone, wood, and stone tools, had a productive agricultural system. In 1660, the Dutch recognised the Sultan of 's sovereignty over . The first known Europeans to sight New Guinea were probably the Portuguese and navigators sailing in the South Pacific in the early part of the 16th century.

On 23 April 1770, British explorer made his first recorded direct observation of indigenous Australians at near Bawley Point. On 29 April, Cook and crew made their first landfall on the mainland of the continent at a place now known as the Kurnell Peninsula. It is here that James Cook made first contact with an Aboriginal tribe known as the , who he fired upon, injuring one. His expedition became the first recorded Europeans to have encountered the eastern coastline of Australia. Captain led the of 11 ships and about 850 convicts into on 26 January 1788. This was to be the location for the new colony. Phillip described as being "without exception the finest harbour in the world".


Modern history
In 1883, the tried to annex the southern half of eastern New Guinea, but the British government did not approve.John Waiko. Short History of Papua New Guinea (1993) The Commonwealth of Australia came into being when the Federal Constitution was proclaimed by the Governor-General, Lord Hopetoun, on 1 January 1901. From that point a system of federalism in Australia came into operation, entailing the establishment of an entirely new national government (the Commonwealth government) and an ongoing division of powers between that government and the States. With the encouragement of Queensland, in 1884, a British protectorate had been proclaimed over the southern coast of New Guinea and its adjacent islands. British New Guinea was annexed outright in 1888. The possession was placed under the authority of the newly federated Commonwealth of Australia in 1902 and with passage of the Papua Act of 1905, British New Guinea became the Australian Territory of Papua, with formal Australian administration beginning in 1906.

The Bombing of Darwin on 19 February 1942 was the largest single attack ever mounted by a foreign power on Australia. In an effort to isolate Australia, the Japanese planned a seaborne invasion of , in the Australian Territory of New Guinea. Between July and November 1942, Australian forces repulsed Japanese attempts on the city by way of the Kokoda Track, in the highlands of . The Battle of Buna–Gona, between November 1942 and January 1943, set the tone for the bitter final stages of the New Guinea campaign, which persisted into 1945. The offensives in Papua and New Guinea of 1943–44 were the single largest series of connected operations ever mounted by the Australian armed forces.

Following the 1998 commencement of reforms across Indonesia, Papua and other Indonesian provinces received greater regional autonomy. In 2001, "Special Autonomy" status was granted to Papua province, although to date, implementation has been partial and often criticised. U.S. Dept. of Defence; International Crisis Group; and International Crisis Group . Archived 19 August 2014. The region was administered as a single province until 2003, when it was split into the provinces of Papua and West Papua. Elections in 1972 resulted in the formation of a ministry headed by Chief Minister , who pledged to lead the country to self-government and then to independence. Papua New Guinea became self-governing on 1 December 1973 and achieved independence on 16 September 1975. The country joined the (UN) on 10 October 1975.

Migration brought large numbers of southern and central Europeans to Australia for the first time. A 1958 government leaflet assured readers that unskilled non-British migrants were needed for "labour on rugged projects ...work which is not generally acceptable to Australians or British workers".cited in Michael Dugan and Josef Swarc (1984) p. 139 Australia fought on the side of Britain in the two and became a long-standing when threatened by during World War II. Trade with Asia increased and a post-war immigration program received more than 6.5 million migrants from every continent. Supported by immigration of people from more than 200 countries since the end of World War II, the population increased to more than 23 million by 2014.


Geography
The Australian continent, as a whole being part of the , is the lowest, flattest, and oldest landmass on EarthPain, C.F., Villans, B.J., Roach, I.C., Worrall, L. & Wilford, J.R. (2012): Old, flat and red – Australia's distinctive landscape. In: Shaping a Nation: A Geology of Australia. Blewitt, R.S. (Ed.) Geoscience Australia and ANU E Press, Canberra. Pp. 227–275 and it has had a relatively stable geological history. is not part of the continent of Australia, but of the separate, submerged continent of . New Zealand and Australia are both part of the Oceanian sub-region known as , with New Guinea being in .

The continent includes a continental shelf overlain by shallow seas which divide it into several landmasses—the and between mainland Australia and New Guinea, and between mainland Australia and Tasmania. When 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 18,000 to 10,000 years, rising sea levels overflowed the lowlands and separated the continent into today's low-lying to semi-arid mainland and the two mountainous islands of New Guinea and Tasmania. The continental shelf connecting the islands, half of which is less than deep, covers some , including the and .

Geological forces such as of mountain ranges or clashes between tectonic plates occurred mainly in Australia's early history, when it was still a part of . Australia is situated in the middle of the tectonic plate, and therefore currently has no active volcanism.

The continent primarily sits on the Indo-Australian Plate. Because of its central location on its tectonic plate, Australia does not have any active volcanic regions, the only continent with this distinction.

(1996). 9780732931209, Macmillan Education AU. .
The lands were joined with as part of the southern supercontinent until the plate began to drift north about 96 million years ago.

For most of the time since then, Australia–New Guinea remained a continuous landmass. When the last glacial period ended in about 10,000 BC, rising sea levels formed , 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 the Aru Islands, mainland Australia, , and Tasmania.

A northern arc consisting of the New Guinea Highlands, the Raja Ampat Islands, and was uplifted by the northward migration of Australia and subduction of the . The Outer Banda Arc was accreted along the northwestern edge the continent; it includes the islands of , , and . Papua New Guinea has several volcanoes, as it is situated along the Pacific Ring of Fire. Volcanic eruptions are not rare, and the area is prone to and because of this.

(1986). 9781444303810
in Papua New Guinea is the second highest mountain in the continent, and at above sea level, is the .


Ecology

Flora
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 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 forest began to give way to the distinctive hard-leaved plants that characterise the modern Australian landscape.

Typical Southern Hemisphere flora include the (eastern Australia and New Guinea), the rainforest emergents (eastern Australia and New Guinea), (New Guinea and ) and (northern and New Guinea), as well as and several species of Eucalyptus. Prominent features of the Australian flora are adaptations to and fire which include and . These adaptations are common in species from the large and well-known families ( and ), ( or gum trees, and ), ( s or wattles), and ( or she-oaks), which are typically found in the Australian mainland. The flora of New Guinea is a mixture of many tropical rainforest species with origins in Asia, such as Castanopsis acuminatissima, spp., , and , together with typically Australasian flora. In the New Guinean highlands, conifers such as , , and are present.

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 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 that now separates the two main landmasses. The collision also pushed up the islands of , which served as island 'stepping-stones' that allowed plants from '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. Among the fungi, the remarkable association between gunnii (one of the "golf-ball" fungi) and its associated trees in the genus is evidence of that drift: the only other places where this association is known are New Zealand and southern and .

(1983). 9780643035485


Fauna
Due to the spread of animals, fungi and plants across the single Pleistocene landmass the separate lands have a related .
(2025). 9780816039739, Checkmark. .
There are over 300 bird species in West Papua, of which at least 20 are unique to the ecoregion, and some live only in very restricted areas. These include the grey-banded munia, Vogelkop bowerbird, and the king bird-of-paradise. WWF: Bird wonders of New Guinea's western-most province, retrieved 11 May 2010

Australia has a huge variety of animals; some 83% of mammals, 89% of reptiles, 24% of fish and insects and 93% of that inhabit the continent are to Australia.Williams, J. et al. 2001. Biodiversity, Australia State of the Environment Report 2001 (Theme Report), CSIRO Publishing on behalf of the Department of the Environment and Heritage, Canberra. This high level of endemism can be attributed to the continent's long geographic isolation, stability, and the effects of an unusual pattern of climate change on the soil and flora over geological time. Australia and its territories are home to around 800 species of bird;Egerton, p. 122. 45% of these are endemic to Australia.

(2025). 9780642568618, Australian Biological Resources Study. .
Predominant bird species in Australia include the Australian magpie, , the , and the laughing kookaburra.Egerton, L. ed. 2005. Encyclopedia of Australian wildlife. Reader's Digest The , , and are of Australia, and the is also one of the well-known animals in the country. The is a lizard native to the Australian mainland.Underhill D (1993) Australia's Dangerous Creatures, Reader's Digest, Sydney, New South Wales,

As the continent drifted north from Antarctica, a unique fauna, flora and developed. and also existed on other continents, but only in Australia–New Guinea did they out-compete the and come to dominate. New Guinea has 284 species and six orders of mammals: monotremes, three orders of marsupials, and ; 195 of the mammal species (69%) are endemic. New Guinea has a rich diversity of life and 1,200 species of have been found. Also about 600 species of reef-building coral—the latter equal to 75 percent of the world's known total. New Guinea has 578 species of breeding birds, of which 324 species are endemic. life also flourished—in particular, the (order , suborder Passeri) are thought to have evolved 50 million years ago in the part of that later became , New Zealand, , and , before radiating into a great number of different forms and then spreading around the globe.

Animal groups such as , , and are endemic to Australia. There were three main reasons for the enormous diversity that developed in animal, fungal and plant 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 . in Australia–New Guinea, in other words, remained reasonably constant for a very long time, and a vast number of different animal, fungal and plant species were able to evolve to fit particular . 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 activity and/or massive events to turn over fresh, unleached rocks rich in , the rocks and of Australia–New Guinea were left largely untouched except by gradual and deep . In general, fertile soils produce a profusion of life, and a relatively large number of species/level of biodiversity. This is because where are plentiful, competition is largely a matter of outcompeting rival species, leaving great scope for innovative 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.

Although New Guinea is the most northerly part of the continent, and could be expected to be the most 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 population growth.


Climate
In New Guinea, the climate is mostly (December to March), southeast monsoon (May to October), and tropical rainforest with slight seasonal temperature variation. In lower altitudes, the temperature is around year round. But the higher altitudes, such as , are constantly around with cool lows nearing , with abundant rainfall and high humidity. The New Guinea Highlands are one of the few regions close to the that experience , which occurs in the most elevated parts of the mainland. Some areas in the island experience an extraordinary amount of precipitation, averaging roughly of rainfall annually.

The Australian landmass's climate is mostly or semi-arid, with the southern coastal corners having a climate, such as and humid subtropical climate in the east coast and Mediterranean climate in the west. The northern parts of the country have a . falls frequently on the highlands near the east coast, in the states of Victoria, New South Wales, and in the Australian Capital Territory. Temperatures in Australia have ranged from above to well below . Nonetheless, minimum temperatures are moderated. The El Niño-Southern Oscillation is associated with seasonal abnormality in many areas in the world. Australia is one of the continents most affected and experiences extensive droughts alongside considerable wet periods.

(1997). 9780415125192, Routledge. .


Politics
Australia is a parliamentary constitutional monarchy with at its apex as the King of Australia, a role that is distinct from his position as monarch of the other Commonwealth realms. The King is represented in Australia by the Governor-General at the federal level and by the Governors at the state level, who by convention act on the advice of the government's ministers. There are two major political groups that usually form government, federally and in the states: the Australian Labor Party and the Coalition which is a formal grouping of the Liberal Party and its minor partner, the National Party. Within Australian political culture, the Coalition is considered and the Labor Party is considered .
(2025). 9781486001385, Pearson Higher Education AU.

Papua New Guinea is a Commonwealth realm. As such, King is its sovereign and head of state. The constitutional convention, which prepared the draft constitution, and Australia, the outgoing metropolitan power, had thought that Papua New Guinea would not remain a monarchy. The founders, however, considered that imperial honours had a cachet.

(1997). 9781573226004, Riverhead Books. .
The monarch is represented by the Governor-General of Papua New Guinea, currently . Papua New Guinea (along with ) is unusual among Commonwealth realms in that governors-general are elected by the legislature, rather than chosen by the executive branch.


Economy
Australia is the only country on the Australia-New Guinea continent, although the economy of Australia is by far the largest and most dominant economy in the region and one of the largest in the world. Australia's per-capita GDP is higher than that of the , , , and in terms of purchasing power parity. Field listing – GDP (official exchange rate), CIA World Factbook The Australian Securities Exchange in is the largest stock exchange in Australia and in the South Pacific. In 2012, Australia was the 12th largest national economy by nominal GDP and the 19th-largest measured by PPP-adjusted GDP.

Tourism in Australia is an important component of the Australian economy. In the financial year 2014/15, represented 3.0% of 's GDP contributing A$47.5 billion to the national economy. In 2015, there were 7.4 million visitor arrivals. Mercer Quality of Living Survey ranks Sydney tenth in the world in terms of quality of living, making it one of the most livable cities. It is classified as an Alpha+ by GaWC. also ranked highly in the world's most liveable city list, and is a leading in the region. The Global Financial Centres Index 14 (September 2013) . Y/Zen Group. p 15. Retrieved 4 December 2013. 2012 Global Cities Index and Emerging Cities Outlook . A.T. Kearney. p 2. Retrieved 29 December 2013.

Papua New Guinea is rich in natural resources, which account for two-thirds of their export earnings. Though PNG is filled with resources, the lack of country's development led foreign countries to take over few sites and continued foreign demand for PNG's resources and as a result, the United States constructed an oil company and began to export in 2004 and this was the largest project in PNG's history. Papua New Guinea is classified as a developing economy by the International Monetary Fund. World Economic Outlook Database, October 2015, International Monetary Fund. Database updated on 6 October 2015. Accessed on 6 October 2015. Strong growth in Papua New Guinea's mining and resource sector led to the country becoming the sixth fastest-growing economy in the world in 2011. Asian Development Outlook 2015: Financing Asia’s Future Growth. Asian Development Bank (March 2015)


Demographics

Immigration
Since 1945, more than 7 million people have settled in Australia. From the late 1970s, there was a significant increase in immigration from Asian and other non-European countries, making Australia a multicultural country. Sydney is the most city in Oceania, having more than 250 different languages spoken, with about 40 percent of residents speaking a language other than English at home. Furthermore, 36 percent of the population reported having been , with top countries being , , and , among others. is also fairly multicultural, having the largest Greek-speaking population outside of , and the second largest Asian population in Australia after Sydney.


Religion
is the predominant religion in the continent, although large proportions of Australians belong to . Christianity in its Global Context, 1970–2020 Society, Religion, and Mission, Center for the Study of Global Christianity Other religions in the region include , and , which are prominent minority religions in Australia. Traditional religions are often , found in New Guinea. is widespread in the Indonesian New Guinea. Many Papuans combine their Christian faith with traditional indigenous beliefs and practices.


Languages
"Aboriginal Australian languages", including the large Pama–Nyungan family, "" of and neighbouring islands, including the large Trans–New Guinea family, and "Tasmanian languages" are generic terms for the native languages of the continent other than those of Austronesian family. Predominant languages include in Australia, in Papua New Guinea, and Indonesian (Malay) in Indonesian New Guinea. Immigration to Australia have brought overseas languages such as , , , Filipino, Mandarin, Vietnamese and , among others. Contact between Austronesian and Papuan resulted in several instances in such as . is an English spoken in Papua New Guinea. Papua New Guinea has more languages than any other country, with over 820 indigenous languages, representing 12% of the world's total, but most have fewer than 1,000 speakers. Papua New Guinea, Ethnologue


Culture
Since 1788, the primary influence behind Australian culture has been , with some Indigenous influences.Jupp, pp. 796–802.Teo and White, pp. 118–20.
(2025). 9780868405896, UNSW Press. .
The divergence and evolution that has occurred in the ensuing centuries has resulted in a distinctive Australian culture.Teo and White, pp. 125–27.
(2001). 9780195515039 .
Since the mid-20th century, American popular culture has strongly influenced Australia, particularly through television and cinema.Teo and White, pp. 121–23. Other cultural influences come from neighbouring Asian countries, and through large-scale immigration from non-English-speaking nations.Jupp, pp. 808–12, 74–77.
(2025). 9780521807890, Cambridge University Press. .
The Australian Museum in Sydney and the National Gallery of Victoria in Melbourne are the oldest and largest in the continent, as well as in .Australian Museum, A Short History of the Australian Museum, http://australianmuseum.net.au/A-short-history-of-the-Australian-MuseumNational Gallery of Victoria – Victorian Heritage Register Sydney's New Year's Eve celebrations are the largest in the continent.

It is estimated that more than 7,000 different cultural groups exist in Papua New Guinea, and most groups have their own language. Because of this diversity, in which they take pride, many different styles of cultural expression have emerged; each group has created its own expressive forms in , , , and . Papua New Guinea is one of the few cultures in Oceania to practice the tradition of . In particular, Papua New Guinea is world-famous for carved wooden : masks, canoes, story-boards.

Australia has a tradition of Aboriginal art which is thousands of years old, the best known forms being rock art and . Evidence of in Australia can be traced back at least 30,000 years. Examples of ancient Aboriginal rock artworks can be found throughout the continent – notably in national parks such as those of the listed sites at and Kakadu National Park in the Northern Territory, but also within protected parks in urban areas such as at Ku-ring-gai Chase National Park in Sydney. Aboriginal culture includes a number of practices and ceremonies centered on a belief in the . Reverence for the land and oral traditions are emphasised.

File:Kurulu Village War Chief.jpg|Yali Mabel, Anemaugi Village War Chief climbing kayo (traditional watchtower) at in File:Didgeridoo (Imagicity 1070).jpg| player Ŋalkan Munuŋgurr performing with


Sport
Popular sports in Papua New Guinea include various codes of (, , , and Australian rules football), , , , , and . Other are also gaining popularity, such as and weightlifting. is the most popular sport in Papua New Guinea (especially in the highlands), which also unofficially holds the title as the national sport. The most popular sport in Australia is , the most popular sport among Australian women is , while Australian rules football is the most popular sport in terms of spectatorship and television ratings. Australia (Countries & Cultures), Tracey Boraas, Capstone Press (2002), Page 54 Planet Sport, Kath Woodward, 2012 p. 85 Australia (Cultures of the World), Vijeya Rajendra, Sundran Rajendra, 2002, p. 101 Australia has hosted two Summer Olympic Games: Melbourne 1956 and Sydney 2000. Australia has also hosted five editions of the Commonwealth Games (Sydney 1938, Perth 1962, Brisbane 1982, Melbourne 2006, and Gold Coast 2018). In 2006 joined the Asian Football Confederation and qualified for the 2010 and 2014 World Cups as an Asian entrant.


See also


Notes

Bibliography


External links
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