Tasman glacier

from Wikipedia, the free encyclopedia
Tasman glacier
LandSat image of the Southern Alps with Aoraki / Mount Cook.  The Tasman Glacier is to the north of the image

LandSat image of the Southern Alps with Aoraki / Mount Cook . The Tasman Glacier is to the north of the image

location South Island (New Zealand)
Mountains New Zealand Alps
length 27 km
width Max. 3 km
Coordinates 43 ° 33 ′  S , 170 ° 16 ′  E Coordinates: 43 ° 33 ′  S , 170 ° 16 ′  E
Tasman Glacier (New Zealand)
Tasman glacier
drainage Tasman River
The tongue of the Tasman Glacier and Tasman Lake

The tongue of the Tasman Glacier and Tasman Lake

From left to right: The Müller, Hooker and the Tasman Glacier in the Southern Alps, as can be seen from the retreat in the years from around 1990 to 2000.

From left to right: The Müller , Hooker and the Tasman Glacier in the Southern Alps, as can be seen from the retreat in the years from around 1990 to 2000.

Template: Infobox Glacier / Maintenance / Image description missing

The Tasman Glacier ( Tasman Glacier ) is the largest of a group of glaciers in the New Zealand Alps on New Zealand's South Island . These extend south and east facing the Mackenzie Basin .

The Tasman Glacier is 27 km long, up to 3 km wide and lies entirely within the area of Mount Cook National Park .

The glacier extends in a southerly direction on the southern slopes of the minarets and the eastern flank of the Aoraki / Mount Cook , the summit of which is only 5 km away from the glacier. From the northeast, the Tasman Glacier meets the meltwater of the Murchison Glacier .

The meltwater from both glaciers flows into the Tasman River , which flows southward and flows into Lake Pukaki , just like the water from the Hooker Glacier and Müller Glacier . The water north of Oamaru reaches the Pacific Ocean via the Witaki River .

The retreat of the glaciers

Noticeable are the growing tongue basin lakes , the decline of the "white ice" (ice without moraine material ) and the growth of the moraine in comparison to the ice melt. The glacier is on the retreat. In the period from 1976 to 2007 he lost around 5 kilometers.

From the merging of several small meltwater lakes, Tasman Lake was created by 1990 , which by 2008 had reached 7 km in length, 2 km in width and 245 m in depth and is still growing.

In the wake of the Christchurch earthquake in February 2011 , a piece of ice with an estimated mass of 30 million tons broke off the Tasman Glacier. It plunged into the lake at the end of the glacier, creating a three and a half meter high tidal wave.

Web links

Commons : Tasman Glacier  - Collection of Images, Videos and Audio Files

Individual evidence

  1. http://earthobservatory.nasa.gov/IOTD/view.php?id=49553
  2. Quake shakes 30m tonnes of ice off glacier (English) , New Zealand Herald. February 22, 2011. Retrieved February 28, 2011.