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The large granite massifs of Strzelecki National Park dominate the southern part of Flinders Island and offer amazing views.
The spectacular Devonian granite forms part of a much larger series of granite bodies extending from north-eastern Tasmania to Wilsons Promontory in Victoria. These granite massifs formed during a major continental collision in eastern Australia, approximately 370 million years ago.
This page produced by the Parks & Wildlife Service,
a unit of the Department of Primary Industries, Parks, Water and Environment This page was last modified on Tuesday, 14 May 2013