Snowy Mountains

The Snowy Mountains experience large natural snowfalls for several months of the year; with significant accumulation during May, June, July, August, September and October with the snow cover usually melting by November (although it can occasionally persist through high summer and the next autumn).

It is considered to be one of the centres of the Australian ski industry during the winter months, with all four snow resorts in New South Wales being located in the region.

The area was first explored by Europeans in 1835, and in 1840, Edmund Strzelecki ascended Mount Kosciuszko and named it after the Polish patriot.

Recreational skiing began at Kiandra in the 1860s and experienced a boom in the 20th century following the commencement of the construction of the Snowy Mountains Hydro-Electric Scheme between 1949 and 1976 which brought many European workers to the district and opened up access to the ranges.The discovery of gold at Kiandra (elevation 1,400 m or 4,600 ft), in 1859, briefly enticed a population of thousands above the snowline and saw the introduction of recreational skiing to the Snowy Mountains around 1861.

Australia's first T-bar lift was installed at Kiandra in 1957, but the ski facilities were finally shifted up the hill to Selwyn Snowfields in 1978.

[6] The Kosciuszko Chalet was built at Charlotte Pass in 1930, giving relatively comfortable access to Australia's highest terrain.

[7] In 1964, Australia briefly boasted the "World's Longest Chairlift", designed to carry skiers from the Thredbo Valley to Charlotte Pass, but technical difficulties soon closed the facility.

[8][9] At 1,760 m (5,774 ft), Charlotte Pass has the highest village base elevation of any Australia ski resort and can only be accessed via over-snow transport in winter.

[14] Anton also recognised the potential of the Thredbo Valley for construction of a major resort and village, with good vertical terrain.

The project began in 1949 employing 100,000 men, two-thirds of whom came from thirty other countries during the post-World War II years.

[18][19] Improved vehicular access to the High Country enabled ski-resort villages to be constructed at Thredbo and Guthega in the 1950s by ex-Snowy Scheme workers, who realised the potential for expansion of the Australian ski industry.

The 'David Moraine', a one kilometre long ridge running across Spencers Creek valley seems to indicate a larger glacier existed in this area at some time, however the glacial origin of this feature is disputed.

The windswept feldmark ecotope is endemic to the alpine region, and covers a mere 300,000 square metres (3,200,000 sq ft).

Montane and wet sclerophyll forests also occur across the ranges, supporting large stands of alpine ash and mountain gum.

In November 2004, a committee "The Snowy Mountains Bushfire Recovery Taskforce" was set up by the NSW State Premier's Department to help residents in the region recover from the fires.

The Taskforce commissioned Louise Darmody from Sound Memories to produce a documentary involving 26 people from the Snowy Mountains to talk about their experiences.

[28] The interviewees included farmers, school children, volunteers and employees from the NSW Rural Fire Service and National Park Snowy Hydro.

Skiing in Australia began in the goldrush town of Kiandra around 1861.
Sunrise over Mount Jagungal
Charlotte Pass is a popular ski area in the upper Snowy Mountains
Map of Snowy Mountains Scheme
Tumut 3 generating station
Blue Lake in the characteristically U-shaped glacial valley, Kosciuszko National Park.
Snow Gum at tree line along Dead Horse Gap Walk, Kosciuszko National Park.
Dead Horse Gap, overlooking the Thredbo Valley
Aftermath of the 2003 Eastern Victorian alpine bushfires showing the burnt out hillsides alongside the Omeo Highway , near Anglers Rest, Victoria , Australia.