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Hallett Cove is situated on the coastal cliffs just south of Adelaide. It is a relatively small but highly concentrated area of geomorphic and geological interest. Landforms derived from glacial events are prominent at Hallett Cove, exposed by recent erosion. Features from the Permian Glaciation (about 280my ago) are found here; they are of considerable local interest and subject to study by researchers from Australia and overseas. Evidence of other geomorphic events (including a newer glaciation and an older glaciation) can also be found here.
Perhaps the best known feature of Hallett Cove Conservation Park is the Sugarloaf. It is a residual landform, exposed as surrounding material has been weathered and removed. It sits within a depression called the Ampitheatre. The coloured layers hold the key to understanding the original formation of these features. Words from http://www.vnc.qld.edu.au/enviro/flinders/f-p-shc.htm
Perhaps the best known feature of Hallett Cove Conservation Park is the Sugarloaf. It is a residual landform, exposed as surrounding material has been weathered and removed. It sits within a depression called the Ampitheatre. The coloured layers hold the key to understanding the original formation of these features. Words from http://www.vnc.qld.edu.au/enviro/flinders/f-p-shc.htm
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