Purnululu National Park is a world heritage site in Western Australia, 2054 km northeast of Perth. The nearest town is Kununurra which is a good 300 kilometres away, making this park pretty isolated, even more so than Uluru. Interestingly, before 1983, the Bungle Bungle Range had not been known to outsiders, although the Indigenous Karjaganujaru peoples have lived in this park for over 40,000 years.
Purnululu is the name given to the sandstone area of the Bungle Bungle Range by the Kija Aboriginal people, and the national park is also known as the Bungles National Park. The range is situated within the park, rises up to 578 m (1896 feet) above sea level and is famous for the unusual and striking sandstone domes striped with alternating orange and grey bands. The banding of the domes is due to differences in clay content and porosity of the sandstone layers. The grey banding is cyanobacteria which grows on the layers where moisture accumulates. The orange bands are layers of oxidised iron compounds that dry out too quickly for the cyanobacteria to form.
The term Purnululu National Park is actually quite a new one. Apart from the indigenous people, no one had known about the Bungle Bungle ranges until the 1980s, which is fairly recent as to land discovery. However, nevertheless to say, the area does have a rich indigenous history with several Aboriginal art and burial sites are numerous in this area.
The name "Purnululu" means sandstone in the language of the local Kija tribe. It is believed that it was either misinterpreted as "Bungle Bungle" or that it is a misspelling of the common Kimberley Grass Bundle. However, rumors still circulate as to the real origin and meaning of Bungle Bungle, making this "lost world" seem even more mysterious.
The park became a UNESCO World Heritage Site in 2003.
The Bungle Bungle Range is one of the most extensive and impressive occurrences of sandstone tower (or cone) karst terrain in the world. The Bungle Bungles were a plateau of Devonian sandstone, carved into a mass of beehive-shaped towers with regularly alternating, dark grey bands of cyanobacterial crust (single cell photosynthetic organisms). The plateau is dissected by 100–200-metre (330–660 ft) deep, sheer-sided gorges and slot canyons. The cone-towers are steep-sided, with an abrupt break of slope at the base and have domed summits. How they were formed is not yet completely understood. Their surface is fragile but stabilised by crusts of iron oxide and bacteria. They provide an outstanding example of land formation by dissolutional weathering of sandstone, with removal of sand grains by wind, rain and sheet wash on slopes.
The plateau and domes themselves are devoid of vegetation, but there are islands of green with more than 600 documented plant species both between the beehives and at the gorge entrances. Some of the plants in the park don't even have a name yet, as they were only recently discovered.
The fan palm (Livistona victoriae) is particularly eye-catching; it clings to walls and crevices in dangerously steep places, especially in the northwest, and reaches heights of up to twelve metres. Tree species that cling to rocks with their roots include the rock fig, the milkwood tree and the dwarf tropical red box gum.
Much of the park consists of undulating, deep red or yellow sandy plains overgrown with acacia and silver tree bushes, eucalyptus forests, spinifex and other grasses. Kapok bushes, Kimberley bauhinia, Kimberley heather and Grevillea species mix up the savannah with colour.
When it comes to fauna, the biodiversity in the park is remarkable; particularly related to the boundary between the tropical and arid climate zones, which ensures that species from both climate zones coexist. Over 40 species of mammals and over 80 species of reptiles are documented in the park.
For example, the flat-toed kangaroo comes from tropical latitudes, while the mountain kangaroo comes from stony dry zones. The frilled lizard is native to the north, the brown snake is adapted to both wet and dry habitats.
The animals that are the easiest to spot in the park are the birds. There are around 150 species, including spinifex pigeons and flocks of brightly coloured budgerigars. Other species such as the nocturnal swallowtail, white- tipped pigeon, and brown-breasted fathead are so well camouflaged that they barely stand out against the rocks they inhabit.
Access to the park by road is via Spring Creek Track from the Great Northern Highway approximately 250 km south of Kununurra. The track is 53 km (33 miles) long and is only passable in the dry season for 4WD vehicles. It will take approximately 3 hours to negotiate that distance to the visitor centre. Access by air is less painful and helicopter flights are available from Turkey Creek Roadhouse (Warmun), 187 km south of Kununurra, or by light aircraft from Kununurra.
During the monsoon season (from November and April 1) or the summer months, it is not possible to enter the park and the park is closed during then.
The Bungle Bungle section of the park has a fee, although the fees tend to get a little bit complicated. Up to date fee info can be found on the park's website.
All the roads in Purnululu National Park past the caravan park are unpaved so you will need a 4WD to get around most of the time.
Budgerigars, wallabies, bungle bungle range, gorges, rock pools, sandstone towers and fan palm trees in crevices in rocks.
The only shop of any kind in the park is at the visitor centre.
There are two public campgrounds in the park - Walardi to the south, near Cathedral Gorge and Picaninny Creek, and Kurrajong to the north near Echidna Chasm. They are basic campgrounds which offer water, shared fireplaces with a limited supply of wood provided (no collecting because it's a national park) and pit toilets. Booking ahead is advisable since you don't want to be turned back after the long drive in from the highway.
Backcountry camping is generally not advised due to safety concerns and is prohibited in large parts of the park.
Primary administrative division