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Kōrero: Geology – overview

Moraines at Tasman Glacier

Image
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

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

Me pēnei te tohu i te whārang

Eileen McSaveney rāua ko Simon Nathan, Geology – overview – Holocene – the last 10,000 years, Te Ara – the Encyclopedia of New Zealand, https://teara.govt.nz/mi/photograph/8403/moraines-at-tasman-glacier (accessed 4 June 2026).

He kōrero nā Eileen McSaveney rāua ko Simon Nathan, i tāngia i te 2 March 2009.

Comments

Harvey Brown
09 March 2013
This is a fascinating introduction to the geological history of New Zealand; the combination of text and images is very effective.