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Glaciated Valley

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Glaciated Valley
Glaciated Valley

A Glaciated Valley is also known as U-Shaped Valleys due to its shape, being steep sides and having a flat bottom. This type of valley would have been formed through the assistance of glaciers, hence the name glaciated valley, this would have been classified it as being formed through a chemical weathering process. A U valley always starts as a typical V shaped valley however through the shape of the glacier, it uniformly turns the landscape into a U shape.

A Glaciated Valley forms when a glacier travels down a slope. A glacier is a slow moving mass of ice that is formed by the accumulated and compacted snow on the mountains. When this glacier travels down the slope, through abrasion and glaciation (plucking) the glacier forms the valley. This means that through the violent nature in which the glacier travels downslope, it weakens and takes off some of the rock from the mountain. Along with this, glaciers have a much greater viscosity than a river, which restricts the course of the glacier, keeping it relatively straighter and smoother. Through this abrasion and glaciation, the ice sometimes begins to thaw. This then allows the large rocky material, now small boulders to be deposited on the floor of the valley.
A Glaciated Valley forms when a glacier travels down a slope. A glacier is a slow moving mass of ice that is formed by the accumulated and compacted snow on the mountains. When this glacier travels down the slope, through abrasion and glaciation (plucking) the glacier forms the valley. This means that through the violent nature in which the glacier travels downslope, it weakens and takes off some of the rock from the mountain. Along with this, glaciers have a much greater viscosity than a river, which restricts the course of the glacier, keeping it relatively straighter and smoother. Through this abrasion and glaciation, the ice sometimes begins to thaw. This then allows the large rocky material, now small boulders to be

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