Wolfe creek where is it

Climbing down into the crater is not permitted because the steep terrain and loose rocks make it dangerous. This is the second largest meteorite crater on Earth. The ridge of the crater stands about 35 metres above the surrounding flat sand plain.

The outer edges slope at a gradual 15 degrees, but the much steeper inner walls fall away at about a 50 degree angle. The crater is known as Janyil in Jaru and as Karntimarlarl in Walmajarri. Traditional Owners believe this circular crater was formed when a giant mythological snake raised its head from the ground back long ago at the time of creation. Aboriginal people understand many natural features, such as rivers and creeks, are the tracks left by giant ancestral snakes that once weaved their way across the desert.

Scientists believe Wolfe Creek was formed by the impact of a meteorite as long as , years ago. Among the broken rocks on the crater wall you may see a brown ringtail dragon stalking insects that frequent the flowering shrubs.

Mammals are active at dawn and dusk, avoiding the heat of the day. Spectacular and noisy Major Mitchell cockatoos harvest seeds from the wattles and paperbarks of the crater floor.

The best time to visit the park is from May to October, when the weather is fine and temperatures are moderate. The park is generally only accessible to conventional vehicles during the dry season.

No water is available so please bring ample supplies with you. Leave rocks and cultural artefacts as you find them. No bins are provided so please take your rubbish with you. Wolfe Creek Crater National Park lies km from Halls Creek via the Tanami Road and access road gravel and only accessible to conventional vehicles during the dry season , a two to three hour drive.

All access within the national park is on foot. The Atlas of Living Australia Atlas contains information on all the known species in Australia aggregated from a wide range of data providers: museums, herbaria, community groups, government departments, individuals and universities.

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