Planning for the future at the Walls of Jerusalem
Mt Field gallery to showcase hidden gems
A big effort for Low Head's little penguins
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