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The Eucla Basin is an artesian depression located in Western Australia and South Australia. The onshore-offshore depression covers approximately 1,141,000 km² and slopes southward to an open bay known as the Great Australian Bight.〔The term 'Eucla Basin' was first used by H.Y. L. Brown ( see: - ) on a geological map of South Australia that was published in 1900 - see page 12, of 〕 It extends more than 500 km offshore and about 350 km inland from the coastline. The Eucla Basin is a Cainozoic basin consisting mostly of carbonate sediments and sedimentary rocks. The basin contains a sandstone aquifer at its base (confined), and an unconfined limestone aquifer. The surface area of the basin (and Nullarbor Plain) consists mostly of grazing and rangeland, but nickel and gold are mined at the western end. Very few people live in this part of the country, with most of the region having fewer than one inhabitant per km². In normal years, the area receives less than 250 mm of precipitation. Due to a shortage of regional seals and source rocks, the basin has poor petroleum prospects, but it is forming as a major zircon producing area. ==Physiography== The Eucla Basin is one of the distinct physiographic provinces of the larger West Australian Shield. It includes the smaller Eyre Coastal Plain and Eucla Shelf physiographic sections. The physiographic units within the basin are:〔Chapter 2 Physiography pp. 16 - 36 of 〕 * Bunda Plateau - the plateau * Hampton Range, Wylie Scarp, and Bunda Cliffs - the scarp * Roe Plains and Israelite Plain - the plains * Eucla Shelf - continental shelf 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Eucla Basin」の詳細全文を読む スポンサード リンク
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