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Most of the state is subarid, and the combination of low rainfall and high temperatures restricts most of the population and agricultural activities to the so-called comfortable zone southwest of an imaginary line stretching from north of Geraldton on the state’s western coast to Esperance on its southern coast.The overwhelming majority of the population lives in the greater Perth area, which is one of the largest metropolitan regions in Australia. Kimberley region in the far north is a multisectioned plateau.Similarly, soils in the eastern deserts are red, but they are generally sandy.In the central southern region and the Nullarbor plain, calcareous loams and stony soils predominate.Indeed, inland drainage is characteristic of most of Western Australia, and the great majority of the lakes shown on any map of the state are saline playas (dried-up lake beds), not bodies of fresh water (except after major rainfall events).The dry, rough country lying to the south of the Pilbara is drained by the Gascoyne River.

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The northern and southern parts of Western Australia have entirely contrasting climates; the north is tropical, with summer rainfall, while the south has a Mediterranean climate.Western Australia, state of western Australia occupying that part of the continent most isolated from the major cultural centres of the east.The state is bounded to the north by the Timor Sea, to the northwest and west by the Indian Ocean, and to the south by the portion of the Indian Ocean commonly called the Southern Ocean (or Antarctic Ocean) in Australia.Usually dry, these rivers become raging torrents during the cyclone season.To the east of the Pilbara flows the Rudall River, which drains inland to the saline (and usually dry) Lake Dora.

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