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MacDonnell Ranges

 

Mountain system, south-central Northern Territory, Australia. Extending east and west of the town of Alice Springs for some 250 mi (400 km), its highest peak is Mount Ziel (4,954 ft [1,510 m]). The mountains were first explored in 1860 by John McDouall Stuart and were named after Richard Macdonnell, governor of South Australia.

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MacDonnell
Range
This Landsat image shows how the northern and southern parts of Alice Springs are connected by Heavitree Gap that passes through the MacDonnell Ranges.
Country Australia
State Northern Territory
Highest point
 - location Mount Zeil
 - elevation 1,531 m (5,023 ft)
Length 644 km (400 mi), E/W
Period Carboniferous

The MacDonnell Ranges of the Northern Territory, are a 644 km (400 mile) long series of mountain ranges located in the centre of Australia (23°42′S 132°30′E / 23.7°S 132.5°E / -23.7; 132.5), and consist of parallel ridges running to the east and west of Alice Springs. The mountain range contain many spectacular gaps and gorges as well as areas of aboriginal significance.

The ranges were named after Sir Richard MacDonnell (the Governor of South Australia at the time) by John McDouall Stuart, whose 1860 expedition reached them in April of that year. The Horn Expedition investigated the ranges as part of the scientific expedition into central Australia. Other explorers of the range included David Lindsay and John Ross.

The ranges are home to a large number of endemic species including the Centralian Tree Frog. This is mostly due to the micro climates that are found around the cold rock pools. Some pools are so cold that hypothermia can set in after a few minutes of swimming.[1]

The MacDonnell Ranges were often depicted in the paintings of Albert Namatjira.[2]

Contents

Geography

The highest peaks are Mount Zeil (1,531 m AHD/ 5,023 ft), Mount Giles (1389 m) and Mount Sonder (1,380 m / 4,528 ft). These are the tallest mountains in the Northern Territory.[3] The MacDonnell Ranges are the headwaters of the Todd River, Finke River and Sandover Rivers. The range is crossed by the Australian Overland Telegraph Line and the Stuart Highway.

Geology

350-300 million years ago a mountain building event created the MacDonnell Ranges.[3] Since that time, folding, faulting and erosion have shaped the range and created numerous gaps and gorges.[3][1] The ranges are composed of many rock types, but are most famous for their red quartzite peaks and gorges. Other rock types include granite, limestone, sandstone and siltstone.[1] Some of the valleys of the range contain fossil evidence of the inland sea that once covered central Australia.[1]

Tourist attractions

Simpsons Gap
Ellery Creek Big Hole
Ochre Pits
View along the West MacDonnell Ranges from the Larapinta Trail, near Glen Helen

The West MacDonnell National Park was established in 1984 to protect the numerous parks and reserves of the range.[1] It also facilitated the development of the Larapinta Trail.

To the east of Alice Springs, within an hours drive, are sites important to the local Arrernte people, many of which contain examples of Aboriginal rock art. These include:

  • Emily Gap
  • Jessie Gap
  • Trephina Gorge
  • N’Dhala Gorge

To the west of Alice Springs is

See also

References

  1. ^ a b c d e f Hema Maps (1997). Discover Australia's National Parks. Milsons Point, New South Wales: Random House Australia. pp. 242—246. ISBN 1975992472. 
  2. ^ Joanne Lane (5 September 2009). "Drawn by a legend". theage.com.au. Fairfax Digital. http://www.theage.com.au/travel/drawn-by-a-legend-20090902-f7s0.html. Retrieved 2009-11-17. 
  3. ^ a b c "Rangelands - Overview - MacDonnell Ranges". Australian Natural Resources Atlas. Department of the Environment, Water, Heritage and the Arts. http://www.anra.gov.au/topics/rangelands/overview/nt/ibra-mac.html. Retrieved 2009-11-17. 

External links


 
 

 

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