Our Latest News

West Point Road improvements

29/06/2009

Access to a popular coastal recreational destination, the West Point State Reserve on Tasmania's West Coast, has been improved with the completion of roadworks by the Parks and Wildlife Service.
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Strong commercial interest in proposed Three Capes Track

25/06/2009

There has been an encouraging response to the recent Identification of Commercial Interest for the proposed Three Capes Track.
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Maria Island access

18/06/2009

The Parks and Wildlife Service wishes to advise that the Maria Island Ferry and Eco Cruises will not be operating its ferry service to Maria Island during the period 23rd June to 14 July, 2009.
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Painted Cliffs

32. Painted Cliffs

time 2 - 2.5 hours return
access A ferry operates to Maria Island. The ferry departure point is at Triabunna. For ferry bookings and timetables see www.mariaislandferry.com.au. See our "Visitors Guide to Maria Island" for further access details.
fees Park entry fees apply, ferry charges and camping fees apply
facilities Picnic, toilet and gas barbecue facilities. There are no shops on the island. Basic hut and camping accommodation (own bedding, stove and food required)
grade Moderate grade with no steep sections
what to take Group A items
cautions Beach area; please supervise children
prohibited Pets or firearms not allowed. Bicycles may be ridden on the formed road sections of the walk but not on the beaches or foot track areas

This walk is on Maria Island and can be enjoyed as part of a day or overnight visit to the island. Day visitors could combine the walk with another Great Short Walk, the Fossil Cliffs walk and/or exploring the historic Darlington area.

Highlights

The geology of Maria Island is of great interest as it contains features from many geological ages. The Triassic sandstones of the Painted Cliffs is one such feature.

Although this sort of rock formation is not uncommon, it is rare in a natural situation for it to be so extensively and beautifully exposed. The wonderful patterns are caused by ground water percolating down through the already formed sandstone and leaving traces of iron oxides, which have stained the rock formation. This probably occurred millions of years ago in a monsoonal climate.

More recently, sea spray hitting the rock face has dried, forming crystals of salt. These crystals cause the rock to weather in the honeycomb patterns that you see. Wave action has also created some interesting features. Rock fragments moved around by the water have gradually worn small potholes and notches into the cliff face, eventually resulting in the undercutting of the cliff. This is a continual process and as you walk further along you can see how quite recently the cliff top has collapsed, plunging sandstone blocks and she-oaks down to the sea.

This is a very fragile environment so please do not walk on the cliffs or scratch the formation.