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and the name was also given to a parish in the
Casterton/Coleraine area. As it is important in the UNESCO assessment of granting Goepark status to link geology to culture and society the name Kanawinka was chosen to represent the connection of ancient culture, European settlement and the desire to educate through the Geopark status.
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of the land and means "Land of
Tomorrow". Buandik lands stretched along the coast in the far south of modern day South Australia and across to the Victorian border regions. The geological fault line which runs from the Naracoorte area down and across into Victoria is known as the Kanawinka Fault Line
363:(Douglas et al. 1988). Kanawinka Geopark has an area of about 26,910 square kilometres (10,390 sq mi) across two States and nine local government areas, with some 374 volcanic sites and many other significant geological sites and formations. It was deregistered from Geopark status in 2012.
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The
Kanawinka Geopark Board was a community-based organization funded by seven of the nine local government areas and was the driving factor in the Geopark proposal. It held support of Tourism Victoria, South Australian Tourism Commission, The National Trust and the Geological Society of Australia
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The eastern extremity of the
Geopark in Victoria is located only about one hour's drive from the state capital city, Melbourne. At the Victorian/ South Australian Border the distance is about four and a half to five hours drive from Melbourne. In the South Australian section it is located four to
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Included are 6 sites of
International Significance, 14 of National significance along with many of state, regional and local significance. (Geological Survey of Australia Victorian Division and the Standing Committee on Geoheritage, National Estate listings 1980). The region varies from volcanic
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along with the
Management bodies of the Sites of Significance of the region, but failed to obtain the approval of the Victorian and South Australian Governments as well as the Australian Government. However the group has now disbanded.
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or Newer basalts. The activity in
Kanawinka Geopark falls into this category. Most of the volcanism is estimated to have taken place from about 5 million years before present (B.P.) to around 5,000 years ago.
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The Otway Basin that hosts
Kanawinka occupies the southern margin of South Australia and Victoria, and also has a significant portion located offshore. This basin formed when Australia rifted away from
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Kanawinka was declared
Australia's First National Geopark in June 2008. It occupies a significant portion of a geological feature known as the
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basalt plains dotted with eruption points through to limestone caves and crater lakes to the ‘Terra Rosa’ of the
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The basalt plains of
Western Victoria are listed in the top 6 in the World for extent and complexity, and the
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region of that state. Both areas are famous for their cheese, wine, forestry and rural industries.
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is of International significance with its unique colour change each year. (Sheard, M. 1978)
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Please help update this article to reflect recent events or newly available information.
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The term kanawinka is taken from the language of the Buandik aboriginal peoples, the
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Volcanic activity in Victoria younger than 7 million years is known as the
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five hours' drive from that state’s capital of Adelaide.
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The South Australian portion of the Geopark lies in the
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is situated along a structurally controlling geological
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of the state, and adjoins the World Heritage area of
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473:23 November
361:Otway Basin
355:Description
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302:Established
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264:Coordinates
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277:142°0′51″E
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38:improve it
419:Blue Lake
310:Abolished
305:June 2008
226:Australia
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