Western Australia is bounded to the east nominally by longitude 129°E, the meridian 129 degrees east of Greenwich, although the actual border with South Australia and the
Northern Territory (as surveyed and marked or otherwise indicated on the ground) deviates from 129° east and is not a single straight line, and bounded by the Indian Ocean to the west and north. The
International Hydrographic Organization (IHO) designates the
body of water south of the continent as part of the Indian Ocean; in Australia it is officially gazetted as the
Southern Ocean. The total length of the
state's eastern border is . There are of coastline, including of island coastline. The total land area occupied by the state is .
Geology The bulk of Western Australia consists of the extremely old
Yilgarn craton and
Pilbara craton which merged with the
Deccan Plateau of India,
Madagascar and the
Kaapvaal and
Zimbabwe cratons of Southern Africa, in the
Archean Eon to form
Ur, one of the oldest
supercontinents on Earth (3–3.2 billion years ago). In May 2017, evidence of the
earliest known life on land may have been found in 3.48-billion-year-old
geyserite and other related mineral deposits (often found around
hot springs and
geysers) uncovered in the Pilbara craton. Because the only
mountain-building since then has been of the
Stirling Range with the rifting from
Antarctica, the land is extremely eroded and ancient, with no part of the state above 1,249 metres (4,098 ft)
AHD (at
Mount Meharry in the
Hamersley Range of the
Pilbara region). Most of the state is a low plateau with an average elevation of about 400 metres (1,200 ft), very low relief, and no
surface runoff. This descends relatively sharply to the coastal plains, in some cases forming a sharp escarpment (as with the Darling Range/
Darling Scarp near Perth). . The extreme age of the landscape has meant that the soils are remarkably infertile and frequently
laterised. Even soils derived from
granitic bedrock contain an order of magnitude less available
phosphorus and only half as much
nitrogen as soils in comparable climates in other continents. Soils derived from extensive sandplains or
ironstone are even less fertile, nearly devoid of soluble phosphate and deficient in
zinc, copper,
molybdenum and sometimes
potassium and
calcium. The infertility of most of the soils has required heavy application by farmers of fertilisers. These have resulted in damage to
invertebrate and bacterial populations. The grazing and use of hoofed mammals and, later, heavy machinery through the years have resulted in
compaction of soils and great damage to the fragile soils. Large-scale land clearing for agriculture has damaged habitats for native flora and fauna. As a result, the
South West region of the state has a higher concentration of rare, threatened or endangered flora and fauna than many areas of Australia, making it one of the world's biodiversity "hot spots". Large areas of the state's wheatbelt region have problems with
dryland salinity and the loss of fresh water.
Climate in Western Australia The
southwest coastal area has a
Mediterranean climate. It was originally heavily forested, including large stands of
karri, one of the
tallest trees in the world. This agricultural region is one of the nine most bio-diverse terrestrial habitats, with a higher proportion of
endemic species than most other equivalent regions. Thanks to the offshore
Leeuwin Current, the area is one of the top six regions for marine biodiversity and contains the most southerly
coral reefs in the world. Average annual rainfall varies from 300 millimetres (12 in) at the edge of the
Wheatbelt region to 1,400 millimetres (55 in) in the wettest areas near
Northcliffe, but from November to March, evaporation exceeds rainfall, and it is generally very dry. Plants are adapted to this as well as the extreme poverty of all soils. The central two-thirds of the state is
arid and sparsely inhabited. The only significant economic activity is mining. Annual rainfall averages less than 300 millimetres (8–10 in), most of which occurs in sporadic torrential falls related to cyclone events in summer. An exception to this is the northern tropical regions. The
Kimberley has an extremely hot
monsoonal climate with average annual rainfall ranging from 500 to 1,500 millimetres (20–60 in), but there is a very long almost rainless season from April to November. Eighty-five percent of the state's
runoff occurs in the Kimberley, but because it occurs in violent floods and because of the insurmountable poverty of the generally shallow soils, the only development has taken place along the
Ord River. Snow is rare in the state and typically occurs only in the
Stirling Range near
Albany, as it is the only mountain range far enough south and sufficiently elevated. More rarely, snow can fall on the nearby
Porongurup Range. Snow outside these areas is a major event; it usually occurs in hilly areas of southwestern Australia. The most widespread low-level snow occurred on 26 June 1956 when snow was reported in the
Perth Hills, as far north as
Wongan Hills and as far east as
Salmon Gums. However, even in the Stirling Range, snowfalls rarely exceed and rarely settle for more than one day. The highest observed temperature of 50.7 °C (123.3 °F) was recorded in
Onslow on 13 January 2022. The lowest temperature recorded was −7.2 °C (19.0 °F) at
Eyre Bird Observatory on 17 August 2008. The
South Geomagnetic Pole is currently tilted 10 degrees away from the South Pole towards Western Australia, allowing for
aurora australis displays as far north as
Geraldton.
Flora and fauna on
Rottnest Island is the state bird of Western Australia Western Australia is home to around
630 species of birds (depending on the taxonomy used). Of these around 15 are
endemic to the state. The best areas for birds are the southwestern corner of the state and the area around Broome and the Kimberley. The
Flora of Western Australia comprises 10,162 published native
vascular plant species, along with a further 1,196 species currently recognised but unpublished. They occur within 1,543
genera from 211
families; there are also 1,276 naturalised alien or
invasive plant species, more commonly known as weeds. In the southwest region are some of the largest numbers of plant species for its area in the world. Western Australia's
ecoregions include the sandstone gorges of
the Kimberley on the northern coast, and below that the drier
Victoria Plains tropical savanna inland, and the semi-desert
Pilbara shrublands,
Carnarvon xeric shrublands, and
Western Australian mulga shrublands to the southwest. Southwards along the coast are the
Southwest Australia savanna and the
Swan Coastal Plain around Perth, with the
Jarrah-Karri forest and shrublands on the southwest corner of the coast around the
Margaret River wine-growing area. Going east along the Southern Ocean coast is the
Goldfields-Esperance region, including the
Esperance mallee and the
Coolgardie woodlands inland around town of
Coolgardie. Deserts occupy the interior, including the
Great Sandy-Tanami desert,
Gibson Desert,
Great Victoria Desert, and
Nullarbor Plain. In 1831, Scottish botanist
Robert Brown produced a scientific paper, titled
General view of the botany of the vicinity of Swan River. It discusses the vegetation of the
Swan River Colony. ==Demographics==