Two mountain ranges forming the edges of the Deccan plateau in southern India. The Eastern Ghats extend about 700 mi (1,100 km) along the southeastern and eastern coast north to the mouth of the Mahanadi River; their average elevation is about 2,000 ft (600 m). The Western Ghats run some 800 mi (1,300 km) along the southwestern and western coast north to the mouth of the Tapti River; their average elevations range from 3,000 ft (900 m) to 5,000 ft (1,500 m). Because they receive heavy rainfall during the monsoon season, the Western Ghats comprise peninsular India's principal watershed.
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Two mountain ranges forming the edges of the Deccan plateau in southern India. The Eastern Ghats extend about 700 mi (1,100 km) along the southeastern and eastern coast north to the mouth of the Mahanadi River; their average elevation is about 2,000 ft (600 m). The Western Ghats run some 800 mi (1,300 km) along the southwestern and western coast north to the mouth of the Tapti River; their average elevations range from 3,000 ft (900 m) to 5,000 ft (1,500 m). Because they receive heavy rainfall during the monsoon season, the Western Ghats comprise peninsular India's principal watershed.
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Main watershed of eastern Australia. It consists of a series of plateaus and mountain ranges roughly paralleling the coasts of Queensland, New South Wales, and Victoria that stretches for some 2,300 mi (3,700 km). Beginning in the north on the Cape York Peninsula, Queen., the range heads generally south to become the Australian Alps near the New South Wales–Victoria border. The range bends west in Victoria, ending in the Grampians, while a southern spur emerges from the Bass Strait to form the central uplands of Tasmania. First traversed by Europeans moving into the Australian Outback in 1813, the region is now important for agriculture, lumbering, and mining, and its national parks and other natural areas are major tourist attractions.
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