Mount Wellington (Tasmania)

Tasmania Wellington Range Hobart

kunanyi / Mount Wellington
Mount Wellington.jpg
Mount Wellington viewed from Lindisfarne Bay on the Eastern Shore of the River Derwent
Highest point
Elevation1,271 m (4,170 ft) [2]
Prominence693 m (2,274 ft) [2]
Isolation47.56 km (29.55 mi) [2]
Listing49th highest mountain of Tasmania
Coordinates42°53′24″S 147°13′48″E / 42.89000°S 147.23000°E / -42.89000; 147.23000Coordinates: 42°53′24″S 147°13′48″E / 42.89000°S 147.23000°E / -42.89000; 147.23000[3]
kunanyi / Mount Wellington is located in Tasmania
kunanyi / Mount Wellington
kunanyi / Mount Wellington
Location in Tasmania
LocationSouth East Tasmania, Australia
Parent rangeWellington
Mountain typeDolerite
First ascent
Easiest routeHike, road

Mount Wellington, officially kunanyi / Mount Wellington /kˈnɑːn/,[4] incorporating its Palawa kani name (Nuenonne: unghbanyahletta or poorawetter[5]), is a mountain in the southeast coastal region of Tasmania, Australia. It is the summit of the Wellington Range and is within the Wellington Park reserve. Located at the foothills of the mountain is much of Tasmania's capital city, Hobart.

The mountain rises to 1,271 metres (4,170 ft) above sea level[2] and is frequently covered by snow, sometimes even in summer, and the lower slopes are thickly forested, but crisscrossed by many walking tracks and a few fire trails.[6] There is also a sealed narrow road to the summit, about 22 kilometres (14 mi) from Hobart central business district. An enclosed lookout near the summit has views of the city below and to the east, the Derwent estuary, and also glimpses of the World Heritage Area nearly 100 kilometres (62 mi) west. From Hobart, the most distinctive feature of Mount Wellington is the cliff of dolerite columns known as the Organ Pipes.


Greater Hobart area from Mount Wellington

The low-lying areas and foothills of Mount Wellington were formed by slow geological upsurge when the whole Hobart area was a low-lying cold shallow seabed. The upper reaches of the mountain were formed more violently, as a Sill with a tabular mass of igneous rock that has been intruded laterally between layers of older rock pushing upwards by upsurges of molten rock as the Australian continental shelf tore away from Antarctica, and separated from Gondwana over 40 million years ago.

Indigenous history

Mount Wellington was originally referred by the original Tasmanian nations of the area as unghbanyahletta (or ungyhaletta), poorawetter (or ‘'pooranetere'’, also pooranetteri),[1] or kunanyi to the indigenous people of Tasmania. The Palawa, the surviving descendants of the original indigenous Tasmanians, tend to prefer the latter name. In 2013, a Tasmanian dual naming policy was announced and "kunanyi / Mount Wellington" was named as one of the inaugural dual named geographic features.[4][7]

European history

The first recorded European in the area Abel Tasman probably did not see the mountain in 1642, as his ship was quite a distance out to sea as he sailed up the South East coast of the island – coming closer in near present-day North and Marion Bays.[8]

No other Europeans visited Tasmania until the late eighteenth century, when several visited southern Tasmania (then referred to as Van Diemens Land) including Frenchman Marion du Fresne (1772), Englishmen Tobias Furneaux (1773), James Cook (1777) and William Bligh (1788 and 1792), and Frenchman Bruni d'Entrecasteaux (1792–93). In 1793 Commodore John Hayes arrived at the Derwent River, naming the mountain Skiddaw, after the mountain in the Lake District, although this name never gained popularity.[citation needed]

In 1798 Matthew Flinders and George Bass circumnavigated the island. Whilst they were resting in the area Flinders named the river the Derwent River (the name John Hayes had given only to the upper part of the river),[9] Flinders referred to the mountain as ‘Table Mountain’ (the name given to it by Bond and Bligh – young Matthew Flinders was with them in 1791) for its similarity in appearance to Table Mountain in South Africa. Bruni d'Entrecasteaux's men were the first European to sail up the river and chart it. Later Nicholas Baudin led another French expedition in 1802, and whilst sheltering in the Derwent River (which they referred to as ‘River du Nord’ – the name d'Entrecasteaux had given to it) Baudin also referred to the mountain as ‘Montagne du Plateau’ (also named by d'Entrecasteaux). However, the British first settled in the Hobart area in 1804, resulting in Flinders’ name of ‘Table Mountain’ becoming more popular. Table Mountain remained its common name until in 1832 it was decided to rename the mountain in honour of the Duke of Wellington who, with Gebhard Leberecht von Blücher finally defeated Napoleon at the Battle of Waterloo in present-day Belgium on 18 June 1815.[citation needed]

A small waterfall in New Town Rivulet near the head of the rivulet on the slopes of Mt Arthur, a sub-peak of Mt Wellington.

In February 1836, Charles Darwin visited Hobart Town and climbed Mount Wellington. In his book The Voyage of the Beagle, Darwin described the mountain thus;

"... In many parts the Eucalypti grew to a great size, and composed a noble forest. In some of the dampest ravines, tree-ferns flourished in an extraordinary manner; I saw one which must have been at least twenty feet high to the base of the fronds, and was in girth exactly six feet. The fronds forming the most elegant parasols, produced a gloomy shade, like that of the first hour of the night. The summit of the mountain is broad and flat, and is composed of huge angular masses of naked greenstone. Its elevation is 3,100 feet [940 m] above the level of the sea. The day was splendidly clear, and we enjoyed a most extensive view; to the north, the country appeared a mass of wooded mountains, of about the same height with that on which we were standing, and with an equally tame outline: to the south the broken land and water, forming many intricate bays, was mapped with clearness before us. ..."

The first weather station was set up on Mount Wellington in 1895 by Clement Lindley Wragge.

Mount Wellington has played host to some notorious characters over time, especially the bushranger 'Rocky' Whelan, who murdered several travelers in the middle of the 19th century. The cave where he lived is known appropriately as 'Rocky Whelan's Cave', and is an easy walk from the Springs.[10]


Organ Pipes at the top of the mountain.
The lookout building near the summit, with the main radio and television transmitter in the background.

Throughout the 19th and into the 20th centuries, the mountain was a popular day-resort for residents of Hobart. To that end, many excursion huts were built over the lower slopes of the mountain. However, none of these early huts survive as they were all destroyed during the disastrous bushfires of 1967, though modern huts are open to the public at the Springs, the Pinnacle, the Chalet – a picnic spot about halfway between the Springs and the Pinnacle – and elsewhere.[11] Sadly, many of the more remote huts have suffered from vandalism, and some are virtually derelict.

The road to the summit was constructed in the early 1930s as a relief scheme for the unemployed, an idea initiated by Albert Ogilvie, the premier of Tasmania of the day. While the road is officially known as the Pinnacle Drive, it was, for some time, also widely known among residents of Hobart as 'Ogilvie's Scar' because at the time it was constructed 'the Mountain' was heavily logged and almost bare, and the road was an all-too-obvious scar across the already denuded mountain. Today the trees have grown again, but the 'scar' most people see today is not actually the road but a line of large rocks with no trees 50–100 m above the road, provided as an easement for power lines. The road itself was opened on 23 January 1937, after two years of work, by Governor Sir Ernest Clark.[12]

The road carries tourist traffic during the day, and sections may be closed at any time of the year due to snowfalls or icy conditions. Halfway up this road (at 720 metres) is a picnic area called "The Springs", near the site of a chalet/health spa that was destroyed by bushfire in 1967.

Mount Wellington was selected by many broadcasters as the site of broadcast radio and television transmitters because it provides line-of-sight transmission to a much larger area of Hobart and surrounding districts than any other point in the region. The first television stations to transmit from there were TVT-6 (now WIN Television) and ABT-2 (the ABC) in 1960. The mountain has two main transmission towers located at its pinnacle. One is the concrete and steel constructed Broadcast Australia Tower (sometimes referred to as the NTA Tower) and one owned by WIN television which is of steel construction. The NTA tower broadcasts all of Hobart's high-power FM radio stations plus the digital TV services for ABC and SBS. The NTA tower also has a small accommodation area at its base with kitchen and workshop area. The WIN TV tower broadcasts the digital TV services from Southern Cross, Win TV, and Tasmanian Digital Television. The site also contains a small kitchen area and contains some data links from local Hobart businesses. An amateur radio repeater is also installed on the mountain.

Lyle Closs jumps to Albert's Tomb, Organ Pipes on Mount Wellington, 1974
Bryan Kennedy solo climbing on Battlements, Organ Pipes on Mount Wellington, 1977

Cable car proposals

See Mount Wellington cable car proposals

An aerial cableway (cable car) has been proposed for the mountain on four occasions.


Mount Wellington has a Tundra Climate (Köppen: ET ). The mountain significantly influences Hobart's weather, and intending visitors to the summit are advised to dress warmly against the often icy winds at the summit, which have been recorded at sustained speeds of over 157 kilometres per hour (98 mph), with rare gusts of up to 200 kilometres per hour (120 mph). In the winter it frequently snows and the mountain is often snowcapped. Lighter snowfalls in spring, summer and autumn are also common. A day on the summit can consist of clear sunny skies, then rain, snow, icy winds and clear again.

Climate data for Mount Wellington
Month Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec Year
Record high °C (°F) 29.8
Average high °C (°F) 13.4
Average low °C (°F) 4.7
Record low °C (°F) −3.4
Average precipitation mm (inches) 91.2
Average precipitation days 16.7 15.3 17.1 18.3 18.9 16.9 19.0 17.6 18.6 19.1 18.3 19.5 215.3
Average relative humidity (%) 74 75 79 83 87 90 93 89 88 83 80 76 83
Source: Bureau of Meteorology[13]

See also


  1. ^ a b Milligan, Joseph (1858). "On the dialects and languages of the Aboriginal Tribes of Tasmania, and on their manners and customs". Papers of the Royal Society of Tasmania: 432.
  2. ^ a b c d "Mount Wellington, Australia". Retrieved 7 June 2015.
  3. ^ "Mount Wellington (TAS)". Gazetteer of Australia online. Geoscience Australia, Australian Government.
  4. ^ a b "Tasmanian dual naming policy announced atop kunanyi". Australian Broadcasting Corporation. 13 March 2013. Retrieved 20 November 2014.
  5. ^ Milligan, Joseph (1858). "On the dialects and languages of the Aboriginal Tribes of Tasmania, and on their manners and customs" (PDF). Papers of the Royal Society of Tasmania: 432.
  6. ^ "Wellington Park – Bush walking". Retrieved 24 October 2013.
  7. ^ "kunanyi / Mount Wellington". Hobart City Council. Retrieved 9 June 2015.
  8. ^ "The curious story of the Dutch explorer who found Tasmania, but missed Australia". The Telegraph. 1 February 2019. Retrieved 4 October 2019.
  9. ^ Flinders, Matthew (1801). Observations on the coasts of Van Diemen's Land, on Bass's Strait and its islands, and on parts of the coasts of New South Wales; intended to accompany the charts of the late discoveries in those countries. John Nichols. p. 5.
  10. ^ "Mount Wellington – Rocky Whelan's Cave". Retrieved 24 October 2013.
  11. ^ "Wellington Park – Sightseeing and facilities". Retrieved 24 October 2013.
  12. ^ "The Pinnacle Road, Mt Wellington". Australian Bureau of Statistics. 22 January 2013. Retrieved 24 October 2013.
  13. ^ "Climate Statistics for Mount Wellington". Bureau of Meteorology. Retrieved 16 April 2013.