The glacial trough, often more simply called a U-shaped valley, is an impressive landscape feature. These glaciated valleys can be hundreds of metres deep with vertical rock walls, down which waterfalls cascade from hanging valleys.On the top of the valley sides the land often flattens out to form a high-level bench, known as an 'alp' in the Alps of Switzerland. The width and flatness of the valley floor are in marked contrast to the steepness of the sides.
These valleys are drained by misfit streams which are dwarfed by the size and scale of the new glaciated valley. In some glacial troughs, lakes ill parts or all of the valley floor; these lakes are ribbon lakes, so-called because of their shape, which is long and thin.
In the lower parts of the valley, examples of landforms of glacial deposition, such as terminal moraines, are found.
The valley's long profile is characterized by its irregular shape providing many hollows for lake formation.
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