A stream shaped valley is usually 'V' shaped. A glacier formed valley is usually 'U' shaped.
The shape of a valley carved by a glacier is U shaped. A valley carved by a river is V shaped.
A glacier valley typically has a U-shape, with steep sides and a flat bottom. This shape is the result of the erosion and scouring action of the glacier as it moves downhill, carving out the landscape over time.
Glacially eroded valleys are normally U-shaped.
As a glacier moves through a valley, it digs deep into the walls and floor . A once-narrow valley that had a V shape becomes wider. As a glacier moves through, the valley becomes U shape .
When the glacier is moving down the side of the valley it scrapes of the rocks. The grinding changes the shape of the valley so that it is rounded.
A glacier-eroded valley will typically have a U-shape with steep sides and a flat bottom, while a stream-eroded valley usually has a V-shape with a narrow channel and wider floodplain. Glacier-eroded valleys are often much larger in scale and can be sculpted by the movement of thick ice over long periods of time, whereas stream-eroded valleys are shaped by the gradual erosion caused by flowing water.
A stream valley typically has a V-shape, while a glacial valley has a U-shape. This difference in shape is due to the different erosional processes involved. Stream valleys are eroded mainly by flowing water, while glacial valleys are shaped by the movement of glaciers that scrape and pluck rock and sediment.
The shape of a valley carved by a glacier is U shaped. A valley carved by a river is V shaped.
A U-shaped valley is typically formed through glacial erosion, as the moving glacier carves out the valley floor and sides, creating the characteristic U shape. Deposition may also occur within the valley, when the glacier deposits sediment it has eroded from elsewhere.
A glacier valley typically has a U-shape, with steep sides and a flat bottom. This shape is the result of the erosion and scouring action of the glacier as it moves downhill, carving out the landscape over time.
Glacially eroded valleys are normally U-shaped.
As a glacier moves through a valley, it digs deep into the walls and floor . A once-narrow valley that had a V shape becomes wider. As a glacier moves through, the valley becomes U shape .
U Wide
When the glacier is moving down the side of the valley it scrapes of the rocks. The grinding changes the shape of the valley so that it is rounded.
When the glacier is moving down the side of the valley it scrapes of the rocks. The grinding changes the shape of the valley so that it is rounded.
A fjord is a valley whose characteristic shape was created by a glacier, so it is a valley after it was glaciated.
a "V"