Arthur Range (Tasmania)

Arthur Range

Looking across High Moor from Mount Columba towards Mount Capricorn and Mount Pegasus
Highest point
Elevation 1,224 m (4,016 ft) AHD [1]
Parent peak Federation Peak
Coordinates 43°16′17″S 146°28′32″E / 43.27139°S 146.47556°E / -43.27139; 146.47556 
Geography
Location in Tasmania, Australia
Country Australia
State Tasmania
Region South West
Range coordinates 43°12′S 146°25′E / 43.200°S 146.417°E / -43.200; 146.417Coordinates: 43°12′S 146°25′E / 43.200°S 146.417°E / -43.200; 146.417

The Arthur Range is a mountain range in the South West Wilderness, located in south-west Tasmania, Australia. The range is broken into two main section, the Western Arthurs and the Eastern Arthurs. Both sections of the range are popular overnight bushwalking destinations, generally in summer.

History

The range was named by George Augustus Robinson who climbed Mount Frederick (now Mount Hayes) in March 1830.[2]

Geology

It is mainly composed of Quartzite and features evidence of past glaciation such as moraines and hanging valleys.

Flora/Fauna

Federation Peak within the Eastern Arthur Range

Much of the Arthur Range and the area surrounding land is covered by button grass wet sedgelands. Most of the remainder of the land is covered by eucalypt.

Birds are the most common animals (e.g. Yellow-tailed Black Cockatoos). In dryer areas, Pademelons may also be seen.

Climate

The climate in the Arthur Range is extremely unstable – weather predictions are virtually useless here, as it is very common to have sun, heavy rain, cloud, strong winds, even snow all in the same day. The top of the range is classed as Sub-Alpine or Alpine. During winter these mountains are snow-capped. Snow has been experienced every season, with regular snowfalls during summer, though many of these snowfalls don't settle. The climate is mostly decided by the wind. The temperature can change very quick with warm air from Northern Tasmania, or very cold from the Southern Ocean and Antarctica.

Walking

As with other parts of Tasmania's south-west, the trails are extremely muddy – very frequently it is more than ankle deep. The mud does not dissipate with altitude up the mountain range either, except where there is bare rock.

Like many other parts of Tasmania, this area is susceptible to Phytophthora (root rot). To avoid spreading it, walkers are encouraged to stay to the main trail. In order to reduce mechanical damage to plants, walkers are also encouraged to wade through the middle of muddy track sections.

Hikers should ensure they are well prepared for any weather conditions, and have enough food for one or two extra days.

Western Arthurs

The Western Arthurs extends generally East-West from Mount Hesperus to West Portal. This section of the range was first traversed in the early 1960s.[3]

Access to the Western Arthurs is usually from the Scotts peak dam camp site (43°02′15″S 146°17′52″E / 43.03750°S 146.29778°E / -43.03750; 146.29778) via part of the Port Davey Track.

The Western Arthur range can be seen on the left hand side

Lakes

The Western Arthurs are studded with many lakes formed from ice-age glaciers. Among these are:

Mountains

From the north western end, closest to the Port Davey Track:[4]

Eastern Arthurs

The Eastern Arthurs runs North-South from the end of the Western Arthurs and includes the highest peak of the range, the striking Federation Peak. This section of the range was first traversed in December 1947 by a group from the Hobart Walking Club.[5]

Lakes

From the north include:

Mountains

From the north:

named features

See also

References

  1. ↑ "Federation Peak, Australia". Peakbagger.com. Retrieved 5 June 2017.
  2. ↑ Doran, Kevin (2004). Federation: Australia's Adventure Peak. Desdichado. p. 14. ISBN 0-9586935-1-X.
  3. ↑ Chapman, John (1998). South West Tasmania (4 ed.). JOHN CHAPMAN. p. 12. ISBN 0-9596129-5-5.
  4. ↑ refer to Tasmap 1:25,000 'Crossing', Razorback, Glovers - or to map on page 150 of Chapman's South West Tasmania book
  5. ↑ Chapman, John (1998). South West Tasmania (4 ed.). JOHN CHAPMAN. p. 144. ISBN 0-9596129-5-5.
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