Kōrero: Geology – overview

Moraines at Tasman Glacier

Moraines at Tasman Glacier

Although the climate has been relatively warm and stable over the last 6,000 years, there have been cool periods when glaciers expanded in their upper reaches. The most recent of these, sometimes called the ‘little ice age’, began about the 13th century and continued until the 1890s. Since then, warmer temperatures have caused the glaciers to retreat.

Tasman Glacier (foreground) has been gradually melted and thinned, and its surface has become covered in moraines – piles of rocks and sediment deposited by the glacier. A lake began to form at the front of the glacier in the mid-1980s, and the ice is now thin enough to break off and float away, accelerating the rate of retreat. Most of the large glaciers in the Mt Cook area are now retreating.

Te whakamahi i tēnei tūemi

GNS Science
Reference: CN22243
Photograph by Lloyd Homer

Permission of GNS Science must be obtained before any use of this image.

Ngā whakaahua me ngā rauemi katoa o tēnei kōrero

Te tuhi tohutoro mō tēnei whārangi:

Eileen McSaveney and Simon Nathan, 'Geology – overview - Holocene – the last 10,000 years', Te Ara - the Encyclopedia of New Zealand, http://www.TeAra.govt.nz/mi/photograph/8403/moraines-at-tasman-glacier (accessed 12 August 2020)

He kōrero nā Eileen McSaveney and Simon Nathan, i tāngia i te 12 Jun 2006