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Tasmania is well known for its bush walking tracks. Even though Tasmania is a small island, more than forty percent of its land area is protected. Therefore, there are plenty of places to go bush walking in Tasmania.
Overall Tasmania is comparatively low-lying with the highest point at 1,617 metres (5,305 ft). Tasmania has ten peaks over the height of 1,500 metres (4,921 ft). With thirty peaks higher than 1,200 metres (3,937 ft), it is one of the most mountainous islands in the world, and Tasmania is Australia's most mountainous state.
The Wellington Range is home to over 500 unique species of flora, despite being mostly high alpine region. The range forms part of the South-east Tasmania Important Bird Area, identified as such by BirdLife International because of its importance in the conservation of a range of woodland birds, especially the endangered swift parrot and forty-spotted pardalote.
[5]: 192 The best known are Kakadu, Uluru (formerly known as Ayers Rock) and the Great Barrier Reef. The Tasmanian Wilderness is probably the best known of the rest. [6] Tasmania is approximately 296 km (184 mi) north to south and 315 km (196 mi) east to west, [7]: 6 and about 300 km (190 mi) south of mainland Australia. Around 30 per cent of ...
This page was last edited on 2 November 2019, at 16:26 (UTC).; Text is available under the Creative Commons Attribution-ShareAlike 4.0 License; additional terms may apply.
The Abels are a group of 158 Tasmanian mountains above 1100m and with a prominence of at least 150m.. They are listed in the books The Abels. [1] [2] [3]Climbing them all is part of the Tasmanian peakbagging movement. [4]
Protected areas of Tasmania Narawntapu National Park (formerly known as Asbestos Range National Park ) is a national park in the Australian state of Tasmania . It lies on Tasmania's north coast, adjoining Bass Strait , between Port Sorell in the west and the mouth of the Tamar River in the east.
The dolerite is so prominent as the older rocks that overlay them are softer and have been eroded away. In places dolerite columns have collapsed into scree slopes. [10] The face of the tiers has been eroded and retreated approximately 4 miles (6.4 km) since their formation, leaving the mountain Quamby Bluff as a solitary outlier.
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