Glaciated upland landscapesArêtes and pyramidal peaks

Corries, pyramidal peaks and U-shaped valleys form due to glaciation. Glaciated uplands are used for different land uses which can lead to conflict. Strategies must be adopted to deal with these.

Part ofPhysical environments

Arêtes and pyramidal peaks

A view of the Himalayas showing an arête and pyramidal peak
Figure caption,
A view of the Himalayas showing an arête and pyramidal peak

An is a knife-edge . It is formed when two neighbouring corries run back to back. As each glacier erodes either side of the ridge, the edge becomes steeper and the ridge becomes narrower.

U-shaped valley in Hola Valley, Norway
Figure caption,
U-shaped valley in Hola Valley, Norway

A is formed where three or more corries and arêtes meet. Glaciers erode backwards towards each other, carving out the rocks by and abrasion. Freeze thaw weathers the top of the mountain, creating a sharply pointed .