Deserts (primarily the Great Australian Desert) cover about 1,371,000 km2 (529,000 sq mi), or 18%, of the Australian mainland, but about 35% of the Australian continent receives so little rain that it is practically desert (other "deserts"). Collectively known as the Great Australian desert, they are primarily distributed throughout the Western Plateau and interior lowlands of the country, covering areas from South West Queensland, the Far West region of New South Wales and Spencer Gulf in South Australia to the Barkly Tableland in Northern Territory and the Kimberley region in Western Australia. Parts of the Mallee in Victoria are named as deserts; the region is described as semi-desert. By international standards, the Great Australian desert receives relatively high rates of rainfall, around 250 mm (10 in) on average, but due to the high evapotranspiration it would be correspondingly arid. No Australian weather stations situated in an arid region record less than 100 mm (3.94 in) of average annual rainfall. The deserts in the interior and south lack any significant summer rains. The desert in Western Australia is well explained by the little evaporation of the cold sea current of the West Australian Current, of polar origin, which prevents significant rainfall in the interior of the continent. About 40% of Australia is covered by dunes. Australia is the driest inhabited continent, with the least fertile soils. In addition to being mostly uninhabited, the Great Australian Desert is diverse, where it consists of semi-desert grassy or mountainous landscapes, xeric shrubs, salt pans, gibber (stony) deserts, red sand dunes, sandstone mesas, rocky plains, open tree savannahs and bushland with a few rivers and salt lakes, which are mostly seasonally dry and often have no outflow in the east. The 3 million km2 (1.2 million sq mi) desert is among the least modified in the world. The Australian desert has the largest population of feral camels in the world.
History
Geological
The area's geology spans a geological time period of over 3.8 billion years, therefore featuring some of the oldest rocks on earth. There are three main cratonic shields of recognised Archaean age within the Australian landmass: The Yilgarn, the Pilbara and the Gawler cratons. Several other Archaean-Proterozoic orogenic belts exist, usually sandwiched around the edges of these major cratonic shields. The history of the Archaean cratons is extremely complex and protracted. The cratons appear to have been accumulated to form the greater Australian landmass in the late Archaean to meso-Proterozoic, (~2400 Ma to 1,600 Ma). Chiefly the Capricorn Orogeny is partly responsible for the assembly of the West Australian landmass by connecting the Yilgarn and Pilbara cratons. The Capricorn Orogeny is exposed in the rocks of the Bangemall Basin, Gascoyne Complex granite-gneisses and the Glengarry, Yerrida and Padbury basins. Unknown Proterozoic orogenic belts, possibly similar to the Albany Complex in southern Western Australia and the Musgrave Block, represent the Proterozoic link between the Yilgarn and Gawler cratons, covered by the Proterozoic-Palaeozoic Officer and Amadeus basins.
Aboriginal
Indigenous Australians have lived in the desert for at least 50,000 years and occupied all Outback regions, including the driest deserts, when Europeans first entered central Australia in the 1800s. Many Indigenous Australians retain strong physical and cultural links to their traditional country and are legally recognised as the traditional owners of large parts of the Outback under Commonwealth Native Title legislation. Aboriginal tribes and clans have been nomadic in the desert areas for thousands of years. They subsisted on the local flora and fauna, now known as bush food, and made sure that their sources of drinking water remained intact. The nomads moved in clearly demarcated tribal areas. For example, important tribes living in the desert areas include the Arrernte, Luritja and Pitjantjatjara. The latter tribe's sphere of influence extended from Uluṟu to the Nullarbor Plain. The Dieri tribe lives in a large area of the Simpson, Strzelecki and Tirari deserts. The rock art and archaeological site at Karnatukul was, until recently, estimated to have been inhabited for up to 25,000 years, and known as the site of the oldest continuous recorded occupation in the Western Desert cultural region. Karnakatul shows one of the earliest uses of firewood, and habitation continued through times of extreme climate change, when the desertification occurred as the polar ice sheets expanded. The oldest examples of rock art, in Western Australia's Pilbara region and the Olary district of South Australia, are estimated to be up to around 40,000 years old. The oldest firmly dated evidence of rock art painting in Australia is a charcoal drawing on a small rock fragment found during the excavation of the Narwala Gabarnmang rock shelter in south-western Arnhem Land in the Northern Territory. The isolated desert areas remained undeveloped for a long time. For example, the Spinifex people first had contact with whites in the 1950s, when they were expelled from their tribal lands because of nuclear weapons testing (1950–1963) by the British and Australian governments. The Pintupi Nine, a group of nine Aboriginal people of the Pintupi tribe, lived a nomadic hunter-gatherer lifestyle in the Gibson Desert until October 1984, when they first encountered whites as they left the desert. Both discoveries were sensations at the time. Large parts of the Australian desert areas are part of the Desert Cultural Area. Important cultural sites include Uluṟu and Kata Tjuṯa. Aboriginal Australians of the desert produced many important artists, one of the first and most famous being Albert Namatjira, who was born in Hermannsburg in the Great Sandy Desert. About a third of Australia's deserts are now Aboriginal lands. A very large part of it is managed by them as a nature reserve. A number of tribes have land use rights for almost all other desert regions. Today, numerous Aboriginal peoples live in settlements in the deserts.
European
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