Showing posts with label Glacial troughs. Show all posts
Showing posts with label Glacial troughs. Show all posts

Sunday, 19 January 2014

Glacial troughs, Truncated spurs, Hanging Valleys, Ribbon lakes

Glacial Troughs, Truncated spurs and Hanging Valleys

Located: Nant Ffrancon Valley, Wales

When The glacier moves downhill through a V-shaped valley it abrades the sides and base using frost-shattered material, picked up via plucking. This turns the V-shaped into a U-shaped valley which is flat-bottomed and steep-sided. This also causes the formation truncated spurs.


Where the glacier cuts through another higher V-shaped valley it can lead to the formation of a hanging valley. If the V-shaped valley contains a river then a waterfall is additionally formed as the river is cut off mid-stream.

Ribbon Lakes

Located: Llyn Ogwen, Windermere, Wales



It is parallel sided and can only occur when there is a change in geology.