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.

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