The Australian continent is one of the driest in the world apart from Antarctica. Nearly 50% of Australia receives less than 25cms of rainfall in a year. Australian desert areas are extremely warm and are one of the most difficult places for survival of plants, human beings and animals. Most of the Australian deserts are located in central and north-western parts of the country. The total size of the Australian deserts is 2.3 million square kilometre and it occupies 44% of the entire continental area.
There are ten deserts in Australia: the Great Victoria Desert, Great Sandy Desert, Tanami Desert, Simpson Desert, Gibson Desert, Little Sandy Desert, Strzelecki Desert, Sturt Stony Desert, Tirari Desert, Pedirka Desert.
Only 3% of the Australian population live in the desert.
Great Victoria Desert
The Great Victoria Desert is a vast sand dune and sand plain desert, and the largest in Australia. Its area is shared equally by the States of South and Western Australia, north of the Nullarbor Plain and south of the Musgrave Ranges, and is bounded on the west by Laverton and the goldfields and to the east by Mabel Creek Station west of Coober Pedy and the Stuart Highway. The desert was named after Queen Victoria by the explorer Ernest Giles in 1875, and is the largest sand dune desert in Australia. Its dunes trend east west, and aside from the major palaeodrainage basin at Serpentine Lakes it has no major watercourses. Save for a few vehicle tracks, this vast wilderness is virtually untouched by man. The internatonal significance of the Unnamed Conservation Park that lies on the South Australian side of the desert was recognised in 1977 when it was proclaimed a Biosphere Reserve by UNESCO. It is one of the larges arid zone biospheres in the world.
Sandplains and dunefields are the dominant landform, forming the southern part of the anticyclonic whorl of dunes that include the Simpson and Great Sandy Deserts. The dunes are longitudinal, from 5-20 metres in height and can run for up to 100kms. Salt lakes are another feature of the desert, the best known are the Serpentine Lakes, other lake systems are the Nurrari and Wyola Lakes, Lakes Maurice and Bring, and Plumridge Lakes and Yeo Lakes in Western Australia.
There are numerous stony rises and breakaways on the north west edge of the desert, and the Musgrave, Mann, Tomlinson and Everard Ranges contain it to the north. To the south is the vast limestone Nullarbor Plain, and to the south east Tietkins Plain and the Ooldea dunefields.
Great Sandy Desert
The great sandy desert is australias sencond biggest desert. It's made up of dunes and ergs. It is a hot desert that is dry, but when the monsoons cross the north of Australia from September to April it will rain.It has a average yearly rainfall of 250mm. In winter it can get very cold with no cloud cover from above and during the day it gets very hot for the same reason. In summer you are looking at a temperature of 38-42 degrees celcius (100-108 degrees fahrenheit.) In the winter it's a plesant but still hot 25-30 degrees celcius (77-86 degrees fahrenheit.)
The great sandy desert is flat and as the name says sandy. This desert has sand dunes. It also has sandstone country, low hills, and even chains of salt lakes. You can see most of the sand dunes from the rocky ranges and hills in the Kimberley or Pilbara.
The Tanami Desert
The Tanami Desert covers the central region of the Northern Territory and expands over the border into Western Australia. Less than a third of the desert is suitable for pastoral use, the rest made up of Aboriginal lands and Mining leases. The Tanami Road, the major vehicular thoroughfare dissects the desert on a north west, south east axis, with the remote Rabbit Flat Roadhouse about half way between Alice Springs and Halls Creek. The prevailing vegetation is hummock or Spinifex grassland, and the landscape is typified by a profusion of anthills, or termite mounds. There are also rocky outcrops, sand dunes and salt lakes. Gold is mined at the Tanami and Granites mines, as well as the Coyote Field in Western Australia. Major Aboriginal communities in the Tanami are Balgo, famous for its vibrant art, Yuendemu, Lajamanu and Jarra Jarra.
The Simpson Desert
The Simpson Desert is a longitudinal sand dune desert that that occupies an area of 170,000 square kilometres just east of the geographical center of Australia. The southern edge of the desert is bordered by Lake Eyre, to the west stony tablelands and the rivers of the Finke, Macumba, Sevenson and Todd Rivers, to the north the Plenty Highway, and to the east the rivers of the Diamantina, Georgina, Warburton and Goyder's Lagoon. Witjira National Park is on the western boundary, Simpson Desert National Park on the eastern.
The original inhabitants were Wangkangurru Aboriginal people who lived at wells called Mikiri. The main tracks across the Simpson Desert are the French Line, the Rig Road, the WAA Line and the QAA Line. Most of these follow straight lines as they were made by bulldozers following compass bearings, hence they being named lines. The most popular trek through the Simpson Desert is from Oodnadatta to Birdsville. There are other tracks into the desert, some requiring special permission to enter, like the Colson Track and the Hay River Track. There are also endless disused lines, some going nowhere. Whilst the desert has a uniform topography and a severe climate - from below freezing on winter nights to temperatures reaching into the sixty degree Celsius range in summer, it is a place of extraordinary beauty and contains a great diversity of flora and fauna.
Gibson Desert
The Gibson Desert is on the central Western Australia plateau south of the Great Sandy Desert, east of the Little Sandy Desert and north of the Great Victoria Desert. At its highest point it reaches 500 m. Having an area of about 155,000 km2 (60,000 miles2) of Western Australia, the Gibson Desert is the 5th largest in Australia, after the Great Sandy, Great Victoria, Tanami Desert and Simpson deserts, and is still largely in an almost "pristine" state. It is situated between Lake Disappointment and Lake Macdonald on the Tropic of Capricorn. The Gibson bioregion includes extensive areas of undulating sand plains and dunefields, with some low rocky or gravelly ridges, the pebbles have been laterised - an iron coating. There are also large areas of upland and there are some saline lakes in the centre. There is a series of small salt water lakes along a palaeodrainage channel to the southwest. Groundwater is present under the desert where it covers parts of the Officer Basin and the Canning Basin. Large areas of the Gibson have a surface of gravel, as noted by early Australian explorers such as Giles (discussed below). Geographically, the Gibson Desert area forms part of the plateau of central Western Australia.
Little Sandy Desert
The Little Sandy Desert lies south of the Great Sandy Desert and west of the Gibson Desert. It is a cousin of the Great Sandy in so far as it has a similar land form and ecology, but smaller. To the north of the desert is Lake Disappointment, a vast salt lake. Within the Little Sandy Desert are numerous rocky outcrops and small rangeland areas which rise like islands in a sea of sand. The best known of these are the Durba Hills, a popular stopover on the Canning Stock Route, but there are also others, like the Calvert Range and Constance Headland which contain spectacular Aboriginal rock art galleries.
Strzelecki Desert
The dunefields of the Strzelecki Desert fan out from the Naterannie Sandhills in a north easterly trend. The sandhills are intersected with numerous claypans and floodplains.The desert stretches from the western edge of New South Wales across to the Birdsville Track in South Australia. The Birdsville track cuts a swathe between the Tirari Desert and the Strzelecki. The salt lakes Callabonna and Frome mark its southern edge along with the northern tip of the Flinders Ranges. The deserts northern edge is roughly the woodland of the Cooper floodplain, beyond which lies Sturt Stony Desert. Through the middle of the desert runs the Strzelecki Creek, which is a branch of the Cooper that terminates at Lake Blanchewater alongside which runs the Strzelecki Track. The Strzelecki Regional Reserve is within the desert.
Sturt Stony Desert
The red iron clad plains shimmering in the heat haze gives the impression that Sturt Stony Desert is perhaps the most inhospitable place on earth. The Diamantina River flowing into Goyders Lagoon, and beyond that the Simpson Desert borders Sturts Stony Desert to the west. To the south are the dunefields of the Strzelecki Desert. Nothing could have prepared the explorer Captain Charles Sturt for his 1845 encounter with the desert that is named in his honour. Iron clad treeless plains stretch to an eternity, baking in the shimmering heat. The only trees appear to be the occasional grevilleas that line the dry creek lines. Occasionally the iron coloured horizon is punctuated by an orange sand dune that appears through the mirage. Plants and shrubs, especially saltbush and bluebush dominate this hard country, but to the casual observer all one can see is stones. Surprisingly the succulence and nutrients of these plants sustain millions of kangaroos and some profitable cattle stations, like Clifton Hills, the largest on the Birdsville Track, and the historic Cordillo Downs to the east. The southeastern border of the desert includes parts of the Moomba and Jackson gas and oil fields and there are numerous exploration sites,well sites and seismic lines.
Tirari Desert
All the deserts of Australia have their own character, and perhaps none appear as wild and windswept as the little known Tirari Desert, that makes up the dunefields and myriad of salt lakes east of the vast Lake Eyre. Typified by white sands with little vegetation and lots of salt lakes, the desert is the least visited in Australia due to there being no public access routes into its arid heart. The longitudinal dunes trend NNW-SSE, and are quite dense, their spacing around 9 dunes per kilometre on average. The desert is bordered to the south by the Clayton River, to the east by the Birdsville Track and to the north by the Warburton River. The two great rivers the Warburton and the Cooper cut through the Tirari. The Cooper slices through the sand dunes leaving steep gypseous banks. The western side of the desert contains parts of the Lake Eyre National Park. Clayton, Dulkaninna, Etadunna, Mulka, Mungerannie, Cowrie and Kalamurina Stations all contain parts of the desert within their pastoral leaseholds.
Pedirka Desert
The Pedirka Desert is Australia's smallest desert, a longitudinal dunefield to the north east of Oodnadatta. It is bordered to the north by the Hamilton Creek, where the dunes end abruptly. North of the creek are stony tablelands. The dunefield runs east almost to the border with Witjira National Park, the deep red dunes trend north east to south westThere are several bores within the desert for pastoral use. The dunes trend north east to south west, and the interdunal corridors are up to one kilometre wide.. The dunes are deep red sand, and the interdunes are made of deep red sandy loam. A large proportion of the desert lies within the Hamilton Station Pastoral Lease,operated by the Williams Pastoral Company. The land use is rangeland cattle grazing.
The Hamilton Creek is lined with River Red Gums coolibah, mulga, dead finish and prickly wattle. Grasses include silky brown top and native millet. Species such as verbine grow thickly after flooding.
A dense scrub of shrub and grasses is found in the interdune areas. The shrubs include satiny bluebush, Giles emubush, weeping emubush, and spiny saltbush. Woollybutt, broad-leaf wanderrie, mulga grass and bandicoot grass are the most common grasses with annuals like mulga grass growing after rains. The dunes support an open mulga woodland, with an understorey which includes tall kerosene grass and woollybutt.
The Pedirka Desert is accessed by the public road that connects the Oodnadatta Track with Dalhousie Springs and Witjira National Park.
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The main reason for the formation of the Australian deserts is their location. Like most major deserts across the world the they are found around a certain latitude (roughly 30° north/south of the equator) where the weather phenomena create a dry climate.