how was cradle mountain formed

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Located 144 km from Launceston and 83 km from Devonport, Cradle Mountain is the central feature of the Cradle Mountain-Lake St Clair National Park, part of Tasmania's World Heritage area. Cradle mountain, rises above the glacially formed Dove Lake and has 4 summits. The most well known remnants from glaciation in Tasmania are Crater Lake and Dove Lake near Cradle Mountain in the island's central highlands. Cradle Mountain is a 1.5-hr drive from Devonport and a 2.5-hour drive from Launceston. At 1,545 metres (5,069 ft) above sea level, it is the sixth-highest mountain in Tasmania. The Cradle Valley, where the famous Cradle Mountain is located, has been formed and altered by geographical processes in the past 2 million years, over three glacial periods, the most recent one was the last ice age (10000 years ago). Cradle Mountain is a major feature of the Cradle Mountain - Lake St Clair National Park, in north-western Tasmania, 144 km south-west from Launceston, and 83 km south-west from Devonport. Geography and Weather. To the south, the great fissured mass of Cradle Mountain itself rises imperious and awesome, its summit often cloaked in white. Cradle Mountain today is part of the Tasmanian Wilderness World Heritage Area. The mountain rises to 1545 metres (5068 feet) above sea level and is considered to be a must see on one of the worlds best walking tracks, The Overland Track. Cradle Mountain–Lake St Clair National Park is renowned for its glassy lakes and pristine wilderness, with walking trails ranging from a gentle six-kilometre stroll around Dove Lake to the six-day Overland Track trek. Cradle Mountain is a natural feature that draws many people to the Launceston region of Tasmania each and every year. To the west is a steep cone-shaped hollow, hundreds of metres deep with Crater Lake at its base, while on the other side of … The landforms of today are the result of prolonged, continuous processes of movement and erosion over millions of years … The … Cradle Mountain is located at the northern end of Cradle Mountain-Lake St Clair National Park. We have discovered Cradle Mountain has been formed Allah since Cradle Mountain is his creation and so are us humans It is 1.5 hours drive from Devonport and 2.5 hours drive from Launceston via Sheffield. Cradle Mountain History. From Sheffield, take the C136 and C132 to the park entrance. Cradle Mountain is on an alpine plateau at an altitude of 934 metres (3,064 ft). Cradle Mountain (1,545 metres / 5,069 ft) is formed of dolerite columns, and Dove Lake is of glacial origin. During this ice age, a huge 6km ice cap formed. The mountain is frequently climbed by tourists and can generally be accessed all year round. The area was glaciated during the last ice age (about 10 000 years ago) when a huge 6 km ice cap formed and glaciers flowed from its edges carving the landscape into dramatic shapes with their inexorable erosive powers. It is a spectacular mountain of Jurassic dolerite, its present jagged appearance formed by glaciers which gouged and sculpted it about 10 000 years ago. The locality of Cradle Mountain is a rural locality in the local government areas of Meander Valley, Kentish and West Coast in the Launceston and North-west and west local government regions of Tasmania. The locality is about 109 kilometres (68 mi) west of the town of Westbury. McDermotts Coaches runs four Cradle Discoverer buses from the Tasmanian Parks and Wildlife Service visitor centre into Cradle Mountain-Lake St Clair National Park.

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