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Family fun day at Hastings Thermal Springs

13/11/2009

Hastings Cave is throwing open the doors to the thermal springs pool for a family fun day on Saturday, 28 November.
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Planned fuel reduction burn in the southwest

29/10/2009

The Parks and Wildlife Service and Forestry Tasmania are conducting a planned burn in the Southwest National Park and on lands managed by Forestry Tasmania today.
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Volunteer Campground Hosts Sought for Cockle Creek

21/10/2009

The Parks and Wildlife Service (PWS) is seeking people with a passion for the beautiful Cockle Creek area in Tasmania's far south area to be volunteer campground hosts for several weeks during the coming summer.More

Painted Cliffs

59. 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. See map.
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 Level 2 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.