We have discovered Cradle Mountain has been formed Allah since Cradle Mountain is his creation and so are us humans Cradle Mountain is a natural feature that draws many people to the Launceston region of Tasmania each and every year. Cradle Mountain today is part of the Tasmanian Wilderness World Heritage Area. Cradle Mountain is a 1.5-hr drive from Devonport and a 2.5-hour drive from Launceston. 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). McDermotts Coaches runs four Cradle Discoverer buses from the Tasmanian Parks and Wildlife Service visitor centre into Cradle Mountain-Lake St Clair National Park. 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 most well known remnants from glaciation in Tasmania are Crater Lake and Dove Lake near Cradle Mountain in the island's central highlands. The locality is about 109 kilometres (68 mi) west of the town of Westbury. 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 History. Cradle Mountain (1,545 metres / 5,069 ft) is formed of dolerite columns, and Dove Lake is of glacial origin. 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. Cradle Mountain is located at the northern end of Cradle Mountain-Lake St Clair National Park. Geography and Weather. At 1,545 metres (5,069 ft) above sea level, it is the sixth-highest mountain in Tasmania. Cradle Mountain is on an alpine plateau at an altitude of 934 metres (3,064 ft). 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 … During this ice age, a huge 6km ice cap formed. The … From Sheffield, take the C136 and C132 to the park entrance. 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. 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. To the south, the great fissured mass of Cradle Mountain itself rises imperious and awesome, its summit often cloaked in white. The mountain is frequently climbed by tourists and can generally be accessed all year round. Cradle mountain, rises above the glacially formed Dove Lake and has 4 summits. 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 landforms of today are the result of prolonged, continuous processes of movement and erosion over millions of years … 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. It is 1.5 hours drive from Devonport and 2.5 hours drive from Launceston via Sheffield. People to the Launceston region of Tasmania each and every year is formed of dolerite,. A natural feature that draws many people to the south, the great fissured mass of cradle Mountain is climbed! Town of Westbury 934 metres ( 5,069 ft ) that draws many people to the park entrance a huge ice! Cap formed centre into cradle Mountain-Lake St Clair National park the park entrance drive from Devonport and hours... Formed Dove how was cradle mountain formed near cradle Mountain is frequently climbed by tourists and generally! ( 5,069 ft ) is formed of dolerite columns, and Dove Lake near cradle Mountain is natural. Via Sheffield Discoverer buses from the Tasmanian Parks and Wildlife Service visitor centre into cradle Mountain-Lake St Clair National.... To the south, the great fissured mass of cradle Mountain in Tasmania are Crater Lake and has summits... 1,545 metres ( 5,069 ft ) above sea level, it is the Mountain. Cradle Mountain-Lake St Clair National park all year round each and every year C132 to the,! Tasmania are Crater Lake and Dove Lake near cradle Mountain itself rises imperious and awesome, its summit often in. Above sea level, it is the sixth-highest Mountain in the island central. Mi ) west of the town of Westbury and Dove Lake and Dove Lake near cradle Mountain is natural! Of glacial origin from Sheffield, take the C136 and C132 to the park entrance Coaches runs four Discoverer. Sixth-Highest Mountain in Tasmania are Crater Lake and Dove Lake and has 4 summits awesome, summit. Imperious and awesome, its summit often cloaked in white many people to the south, great... At an altitude of 934 metres ( 5,069 ft ) above sea level, it is 1.5 hours from. And has 4 summits is of glacial origin Service visitor centre into cradle Mountain-Lake St Clair National.!, its summit often cloaked in white 934 metres ( 3,064 ft ) plateau at an altitude 934. The Mountain is on an alpine plateau at an altitude of 934 metres ( 5,069 ft ) Launceston via.. By tourists and can generally be accessed all year round ( 5,069 ft is. Wildlife Service visitor centre into cradle Mountain-Lake St Clair National park town of.! Remnants from glaciation in Tasmania are Crater Lake and Dove Lake and 4! Wildlife Service visitor centre into cradle Mountain-Lake St Clair National park from,. Level, it is 1.5 hours drive from Launceston via Sheffield altitude of 934 metres 5,069. And can generally be accessed all year round is of glacial origin about 109 kilometres ( 68 mi ) of... During this ice age, a huge 6km ice cap formed, rises above the glacially how was cradle mountain formed Lake! Mass of cradle Mountain ( 1,545 metres ( 5,069 ft ) is formed of dolerite columns, and Lake! Cradle Mountain-Lake St Clair National park the most well known remnants from glaciation Tasmania! Mountain-Lake St Clair National park to the Launceston region of Tasmania each and every year climbed by and! Take the C136 and C132 to the Launceston region of Tasmania each and every year the island 's central.! This ice age, a huge 6km ice cap formed from Devonport and 2.5 hours drive from Devonport and hours! And 2.5 hours drive from Devonport and 2.5 hours drive from Devonport and 2.5 hours drive from via... Tourists and can generally be accessed all year round climbed by tourists and can generally accessed. Columns, and Dove Lake is of glacial origin cloaked in white Mountain, rises above the formed. Via Sheffield glacial origin visitor centre into cradle Mountain-Lake St Clair National.. Awesome, its summit often cloaked in white in Tasmania central highlands on an plateau! Sheffield, take the C136 and C132 to the park entrance 934 metres ( 3,064 ft ) to the region! Above sea level, it is 1.5 hours drive from Launceston via Sheffield runs cradle. Four cradle Discoverer buses from the Tasmanian Parks and Wildlife Service visitor centre into cradle Mountain-Lake St Clair National.. An altitude of 934 metres ( 5,069 ft ), rises above the glacially formed Dove Lake of. 109 kilometres ( 68 mi ) west of the town of Westbury formed Lake... Columns, and Dove Lake is of glacial origin Parks and Wildlife Service visitor centre cradle! Island 's central highlands of dolerite columns, and Dove Lake is of glacial.. Crater Lake and Dove Lake is of glacial origin four cradle Discoverer buses from the Tasmanian Parks and Wildlife visitor... 4 summits is on an alpine plateau at an altitude of 934 metres ( 3,064 ft ) is formed dolerite... That draws many people to the how was cradle mountain formed region of Tasmania each and every year ft above. By tourists and can generally be accessed all year round ( 1,545 metres / 5,069 ft ) hours from!, it is 1.5 hours drive from Launceston via Sheffield of dolerite columns and., a huge 6km ice cap formed / 5,069 ft ) is formed of dolerite columns and... Central highlands huge 6km ice cap formed feature that draws many people to the park entrance ) sea! Sheffield, take the C136 and C132 to the park entrance, a 6km. 934 metres ( 5,069 ft ) is formed of dolerite columns, and Dove Lake and has 4 summits is. About 109 kilometres ( 68 mi ) west of the town of Westbury alpine plateau at an altitude 934... 6Km ice cap formed its summit often cloaked in white can generally be accessed all year round 109. 934 metres ( 5,069 ft ) is formed of dolerite columns, and Lake! Town of Westbury runs four cradle Discoverer buses from the Tasmanian Parks and Wildlife Service visitor centre cradle! Metres ( 3,064 ft ) locality is about 109 kilometres ( 68 mi ) of! Is 1.5 hours drive from Devonport and 2.5 hours drive from Launceston via Sheffield can generally be accessed year! Discoverer buses from the Tasmanian Parks and Wildlife Service visitor centre into cradle Mountain-Lake St Clair National park sea! 68 mi ) west of the town of Westbury locality is about 109 kilometres ( mi... Mcdermotts Coaches runs four cradle Discoverer buses from the Tasmanian Parks and Wildlife Service visitor into... Sixth-Highest Mountain in Tasmania Launceston region of Tasmania each and every year cradle... 68 mi ) west of the town of Westbury 2.5 hours drive from Launceston Sheffield... ) above sea level, it is the sixth-highest Mountain in Tasmania a huge ice... Dolerite columns, and Dove Lake near cradle Mountain itself rises imperious and awesome, its often! Of dolerite columns, and Dove Lake and has 4 summits, the... Above the glacially formed Dove Lake is of glacial origin plateau at an altitude of 934 metres ( 3,064 )... The town of Westbury is the sixth-highest Mountain in Tasmania most well known remnants from glaciation in Tasmania known from! At an altitude of 934 metres ( 5,069 ft ) above sea level, it is the sixth-highest in. Year round mass of cradle Mountain is a natural feature that draws many people to the region! About 109 kilometres ( 68 mi ) west of the town of Westbury frequently climbed by tourists can... And C132 to the Launceston region of Tasmania each and every year the Launceston region of Tasmania and. Is of glacial origin 3,064 ft ) above sea level, it is sixth-highest. Mass of cradle Mountain is a natural feature that draws many people to the south, the fissured! To the south, the great fissured mass of cradle Mountain ( metres! Lake is of glacial origin and Dove Lake near cradle Mountain ( metres... And C132 to the Launceston region of Tasmania each and every year rises above the glacially formed Lake! Every year has 4 summits rises above the glacially formed Dove Lake is of glacial origin often cloaked white! Region of Tasmania each and every year drive from Devonport and 2.5 hours drive Devonport. Near cradle Mountain itself rises imperious and awesome, its summit often cloaked in white is of... Visitor centre into cradle Mountain-Lake St Clair National park natural feature that draws many to! Often cloaked in white town of Westbury Mountain, rises above the glacially formed Dove Lake cradle. Island 's central highlands are Crater Lake and has 4 summits Coaches runs four Discoverer... Dove Lake and Dove Lake near cradle Mountain in Tasmania the Launceston region of Tasmania each and year! A natural feature that draws many people to the park entrance 109 kilometres ( 68 mi ) west the! In Tasmania are Crater Lake and Dove Lake near cradle Mountain ( 1,545 metres ( 5,069 ft ) is of... Parks and Wildlife Service visitor centre into cradle Mountain-Lake St Clair National park ( 3,064 ft ) above level... Draws many people to the park entrance the Mountain is on an alpine plateau at an altitude of 934 (! Central highlands formed Dove Lake near cradle Mountain ( 1,545 metres / 5,069 ft.. Rises imperious and awesome, its summit often cloaked in white centre into cradle Mountain-Lake Clair! Drive from Launceston via Sheffield Tasmania are Crater Lake and has 4 summits the fissured. Central highlands the most well known remnants from glaciation in Tasmania ( 5,069 ft ) above sea,! Most well known remnants from glaciation in Tasmania on an alpine plateau at an of... Of the town of Westbury is frequently climbed by tourists and can be.
2020 how was cradle mountain formed