Upper half of the Tasman Glacier
|Area||101 km2 (39 sq mi)|
|Length||27 km (17 mi)|
|Thickness||600 m (2,000 ft)|
The Tasman Glacier is the largest of several glaciers which flow south and east towards the Mackenzie Basin from the Southern Alps in New Zealand's South Island. It is New Zealand's longest glacier.
At 27 kilometres (17 mi) in length, Tasman Glacier is New Zealand's longest glacier. It is as much as 4 kilometres (2.5 mi) wide and 600 metres (2,000 ft) thick, and lies entirely within the borders of Aoraki/Mount Cook National Park. The glacier covers an area of 101 square kilometres (39 sq mi) and starts at a height of 3,000 metres (9,800 ft) above sea level. Snowfall during the winter and spring seasons accumulates to 50 metres (160 ft). After the summer melt, 7 metres (23 ft) remains.
Although its upper reaches are snow-covered, rocks carried by the glacier are exposed by ablation along its course, and the lower glacier is entirely rock-covered. It is almost met near its end by the meltwater of the Murchison Glacier, which approaches from the northeast before turning to flow beside the Tasman Glacier outside the moraine wall.
The waters from both these glaciers pool at the end of the glacier in Lake Tasman, before flowing south to join the outflow from the nearby Hooker and Mueller Glaciers in the wide valley of the Tasman River, whose braided streams flow south into Lake Pukaki. They eventually flow into the Waitaki River and to the Pacific Ocean north of Oamaru.
Between 2000 and 2008, the glacier terminus receded 3.7 km. Since the 1990s the terminus has retreated about 180 metres (590 ft) a year on average. The glacier is now in a period of faster retreat where the rate of retreat is calculated to be between 477 to 822 metres (1,565 to 2,697 ft) each year. It is estimated that the Tasman Glacier will eventually disappear and the terminal Tasman Lake will reach a maximum size in 10 to 19 years time. In 1973 Tasman Glacier had no terminal lake and by 2008 Tasman Lake was 7 kilometres (4.3 mi) long, 2 kilometres (1.2 mi) wide, and 245 metres (804 ft) deep.
A large calving event was possibly triggered, or at least contributed to, by the 2011 Canterbury earthquake on 22 February 2011. On this day 30,000,000 metric tons (33,000,000 short tons) to 40,000,000 metric tons (44,000,000 short tons) of ice dropped from the terminal face of the Tasman Glacier and fell into the Tasman Lake. Boats were hit with tsunami waves of up to 3.5 metres (11 ft) as the ice fell into the Tasman Lake under the glacier. Similar events in the past have been attributed to buoyancy effects, a result of high basal water pressures and increased lake level following heavy rainfall events.
- "Place Name Detail: Tasman Glacier". New Zealand Geographic Placenames Database. Land Information New Zealand. Retrieved 18 April 2008..
- "Aoraki/Mount Cook National Park". Tourism New Zealand. Retrieved 14 July 2010.
- "Aoraki/Mount Cook Education Resource" (PDF). Department of Conservation. 2009. p. 8. Retrieved 14 July 2010.
- This excludes glaciers in New Zealand's Antarctic claim, the Ross Dependency.
- "Twenty-First Century Calving Retreat of Tasman Glacier, Southern Alps, New Zealand".
- "Tasman Glacier retreat extreme". Massey University. 23 April 2008. Retrieved 24 April 2008.
- Staff (22 February 2011). "Quake shakes 30m tonnes of ice off glacier". New Zealand Herald. Retrieved 22 February 2011.
- "A 40 Million Tonne Iceberg Dumped in Lake by NZ Earthquake". Important Media Network, Clean Technica. 23 February 2011.
- "Earthquake causes glacier to calve". Fairfax NZ News. 23 February 2011.
- Satellite Image Atlas of Glaciers of the World, Glaciers of New Zealand, Chinn, T.H., USGS Professional Paper 1386, 1988.
|Wikimedia Commons has media related to Tasman Glacier.|
- Department of Conservation - Tasman Valley walking tracks