A U-shaped valley, also known as a glacial trough, is a classic landform created by the erosive action of glaciers. Unlike V-shaped valleys, which are carved by rivers and have sharp, narrow profiles, U-shaped valleys are characterized by their broad, rounded profiles. These valleys form as glaciers move through pre-existing valleys, eroding the sides and bottom equally.
The powerful grinding action of the glacier scrapes and polishes the valley floor and sides, widening and deepening it in the process. The outcome is a smooth, U-shaped cross-section. Typical features within U-shaped valleys often include:
- Hanging valleys - smaller tributary valleys elevated above the main U-shaped valley
- Glacial troughs - the deep, main valley itself
- Striations - scratches or grooves on the valley floor, left by moving glaciers