NLC Logo NLCLink to About the NLCLink to Media / PublicationsLink to Caring for CountryLink to Land & Sea RightsLink to Visiting Aboriginal LandLink to Doing Business on Aboriginal LandLink to ContactsLink to Photo Gallery
Caring for Country Caring for Country
NLC Logo Spacer

Home Page : Search : Site Map : Permits

Rock Introduction Rock Connection to Land Rock Climate & Landscape
Rock Sea Management Rock Land Management Rock Feral Animal Management


 

 

 

   

Climate and Landscape


Rock In the Tropics Rock Landscape Rock Stories Rock Coping with Change

   
Rock

In the Tropics

 

The Northern Territory's Top End is generally regarded as being the area north of the 16th parallel of latitude.

Arnhem Land floodplain
Arnhem Land floodplain

The Top End is situated in the wet-dry tropics of Australia.

In the wet season, from November to April, 93% of the annual rainfall occurs; most rain is brought by the South-East Asian Monsoon when monsoonal troughs lie over the Top End coast for extended periods. Humidity is very high during the wet season and cloudy conditions keep maximum daily temperatures near the coast to 33-34 degrees Celsius.

The dry season, May to October, is marked by steady east to south-east winds and dry conditions with lower humidity and slightly lower temperatures than the wet season.

Rainfall in Darwin, the capital of the Northern Territory, is approximately 1,600mm per annum and decreases inland towards the south. For example at Katherine, approximately 300km inland, the annual rainfall is about 960mm.

Maximum temperatures increase and minimum temperatures decrease inland.

To Top of Page

 

Rock

Landscape

 

The Top End coastline is backed by landscapes of generally low relief, seldom reaching elevations exceeding 30m.

Further from the coast, plains rise slowly in height towards the south. The most significant departures from this general pattern involve areas of rugged sandstone plateau, the most significant extending from Kakadu National Park south-eastwards through Arnhem Land.

Top End wetlands are concentrated in the areas of low relief near the northern coast. They are some of the most extensive and remote wetlands in Australia and compared to those in southern Australia are generally in good condition.

Closer to the coast there are large mangrove swamps, salt marshes and seagrass beds, while major river systems have freshwater floodplains, covering thousands of square kilometres. These have permanent or seasonal swamps and can be dry or under several metres of water, depending on the season. They are home to large numbers of waterbirds, fish, mammals and reptiles, and are still widely used by Aboriginal people.

The Australian land mass has been subject to dramatic and dynamic changes over the past 20,000 years.

About 18,000 years ago, the wetlands of Kakadu National Park were at the northern edge of the desert zone and sandstone outcrops like Ubirr and Nourlangie, which now overlook Kakadu's wetlands, were drier inland sites.

Today, standing on the rim of the escarpment around the Arafura Swamp in Central Arnhem Land, you look out over the largest paperbark swamp in northern Australia. There is nothing in the visible landscape to suggest that much of this vast freshwater wetland used to be a large saltwater estuary associated with tidal creeks fringed by mangrove.

To Top of Page

 

Rock

Stories

 

There are stories, in both secular and sacred Aboriginal tradition, which refer to those dramatic changes and show the depth of Aboriginal cultural continuity along the dynamic northern coastline.

Contemporary science reinforces the likelihood that these stories refer to real situations from thousands of years in the past:

Rock  

inhabited islands, which no longer exist, some 60 kilometres off the central Arnhem Land coast;

Rock  

the disappearance of large freshwater swamps under the sea;

Rock  

the separation of a larger island mass into two halves

- these are but a few such stories.

To Top of Page

 

Rock

Coping with Change

 

Accepting the evidence for cultural continuity and the speed of coastal change makes you realise the ability and capacity of the Aboriginal nations of the ancient coasts to respond to change.

Look at rock art. It shows how Aboriginal technology has changed in parallel to these geographical changes and demonstrates the capacity to respond rapidly to dramatic change in the landscape affecting huge areas.

For more information on the Top End's climate and landscape, visit: www.savanna.ntu.edu.au

To Top of Page

   

 

  Home Page : Search : Site Map : Permits

An Overview : About the NLC : Jobs : Media/Publications
Caring for Country : Land & Sea Rights : Visiting Aboriginal Land
Doing Business on Aboriginal Land : Contacts : Photo Gallery

© Northern Land Council 2003 : Disclaimer : Privacy

CLICK HERE to increase text size