Our Latest News

Toilet construction works continue at Cosy Corner South campsite

14/05/2012

On Monday 14 May, work will commence on the upgrade of the toilet block at the Cosy Corner South campsite in the Bay of Fires Conservation Area. Builders are expected to be on site for two to three weeks.More

Toilet construction works begin at Cosy Corner North campsite

27/04/2012

On Monday 30 April, work will commence on the construction of a new toilet block at the Cosy Corner North campsite in the Bay of Fires Conservation Area. Builders are expected to be on site for two to three weeks.More

Sixteen new reserves for King Island

20/04/2012

As part of the ongoing Crown Land Assessment and Classification (CLAC) 16 new reserves have recently been proclaimed for King Island.More

Fossil Cliffs

60. Fossil Cliffs

time 1.5 – 2 hours return
access A ferry operates to Maria Island. The ferry departure point is at Triabunna. For ferry bookings, timetables and further access details, see our "Visitors Guide to Maria Island".
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 with no steep sections
what to take Group B items
cautions Dangerous cliffs; please supervise children and keep away from cliff edges.
prohibited Pets or firearms not allowed. Bicycles may be ridden on this track

This walk is in the Maria Island National Park and can be enjoyed as part of a day or overnight visit to the island.

Highlights

Along the way to Fossil Cliffs you will pass many reminders of the rich cultural heritage of Maria Island. Our web site has full details of this heritage.

The cliff exposure in the Fossil Bay area is recognised as the best example of lower Permian strata in Tasmania, if not the world.

At Fossil Cliffs you will discover the prolific occurrence of fossils of the thick-shelled mussel Eurydesma. The soft parts of the creatures have rotted away, leaving only the hard shells, which have lasted almost 300 million years.

On the lower rock shelf you can see a variety of fossils including sea fans, coral-like creatures, scallop shells and sea lilies. It is thought that such an extensive accumulation of fossils may be related to the cold conditions associated with the polar sea of the time. Amongst the fossils are some large rocks, called dropstones. These have been transported by floating ice. As the ice begins to melt, the stones fall to the sea floor and settle amongst the finer sediments. The stones consist of different rock types, including granite and quartzite, and may have come from nearby, or from great distances away.