ski the tasman run map - head of the tasman glacier
EVERY FINE DAY WE SKI 2 RUNS ON THE GLACIER
TAKING A DIFFERENT LINE AND STARTING FROM A DIFFERENT LANDING SPOT FOR EACH RUN.
The average run length is about 8 km - and up to 10 km in some seasons.
Highest landing: Tasman Saddle 2,400 metres
Lowest aircraft pick up: Malte Brun strip 1,500 metres
The South Island of New Zealand is unique for a temperate climate zone in that the glaciers here come almost to sea level.
There are approximately 178 separate glaciers in Aoraki/Mount Cook National Park. The two main systems are the Tasman and the Godley.
Two million years of history
The Tasman Glacier's story goes back 2 million years - to the Pleistocene ice ages. The glacier has advanced and retreated several times, leaving behind great moraine deposits, and carving out Lake Pukaki.
CLIMATE CHANGE AND THE TASMAN GLACIER
Over recent years the affects of climate change on the Tasman Glacier have been evident. The growing terminal lake and increasing amounts of moraine on the lower glacier are the most obvious signs.
Scientists from GNS New Zealand have been surveying the Tasman, the local mountains and other glaciers. Read about their work on the GNS website.
- 23 km long
- 600 metres deep (nearly 2000 ft) in the middle, and 200 metres deep at the nevé
- An average width of 1.6 km (a mile)
- Average daily surface motion 35-40 cm (over a foot)
- Annual snowfall depth at the nevé - up to 70 metres!