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Fly Neighbourly Advice for the Tasman National Park

24/08/2019

Public comment is invited on the draft Tasman National Park Fly Neighbourly Advice. The draft Fly Neighbourly Advice has been prepared by the Tasmania Parks and Wildlife Service in response to increasing air traffic over the Tasman National Park.More

Hybrid diesel-electric shuttle buses at Cradle Mountain - a first for National p

19/08/2019

When you next visit Cradle Mountain you will be able to step aboard one of the new hybrid, diesel-electric, shuttle buses on your trip to Dove Lake. These new buses will reduce emissions and deliver a quieter, all mobility friendly, visitor experience.More

AFAC Independent Operational Review of the 2018-19 bushfires

08/08/2019

Following the 2018-19 bushfires the Tasmanian Government commissioned an independent report by the Australasian Fire and Emergency Service Council to review the overall response and identify areas where more can be done to improve the State's response andMore

Liffey Falls

42. Liffey Falls

time 45 minutes return (1km one way)
access
Road C513. Approach from Bracknell, Deloraine or Great Lake. See map
facilities Gas barbecues, picnic shelters, toilets and drinking water
grade Level 2
what to take Group A items
cautions Supervise children, weather may change quickly, flowing waters
prohibited Pets, firearms or bicycles are not allowed.
Access road is not suitable for buses and caravans

There are two walking tracks to Liffey Falls.  The walk described here is from the top car park where there are developed picnic facilities and a shorter, and higher grade walking track.  An alternative track is from the lower car park where there are minimal facilities and a longer and lesser grade walking track.  The lower car park may be accessed by buses and caravans.

Liffey Falls is within the Liffey Falls State Reserve.

Highlights

Water collected on the Great Western Tiers washes into the Liffey River. As it rushes downslope it erodes away the softer mudstone sediments exposing sandstone steps. These give rise to a series of waterfalls culminating in Liffey Falls.

The exposed sandstone was laid down over 250 million years ago when this region lay further south, covered by sea and ice. As icebergs melted, rocks were freed and plunged as 'dropstones' into the marine sediments below. These embedded dropstones, which are paler, roundish and flattened in shape, can be seen in the river along the track to Liffey Falls. Made of quartzite, these dropstones may have come from as far away as Cradle Mountain! Also embedded in the rocks exposed by the erosive force of the Liffey River are tiny marine fossils.