A stream shaped valley is usually 'V' shaped. A glacier formed valley is usually 'U' shaped.
The terms U-shaped and V-shaped are descriptive terms of geography to characterize the form of valleys. Most valleys belong to one of these two main types or a mixture of them, at least with respect of the cross section of the slopes or hillsides. A valley formed by flowing water, or river valley, is usually V-shaped. The exact shape will depend on the characteristics of the stream flowing through it. A valley carved by glaciers, or glacial valley, is normally U-shaped. The valley becomes visible upon the recession of the glacier that forms it.
The shape of a valley carved by a glacier is U shaped. A valley carved by a river is V shaped.
V-valley refers to a type of valley on a topographic map that has a V-shaped profile, typically formed by erosion from a river or stream. U-valley refers to a valley with a U-shaped profile, typically formed by glacial erosion. V-valleys are more narrow and have steeper sides compared to U-valleys.
A long valley profile shows the cross-sectional view of a valley from its headwaters to its mouth. It typically displays the variations in elevation and slope along the length of the valley, often revealing features such as V-shaped valleys, interlocking spurs, and river meanders. This profile is useful for analyzing the geological and geomorphological history of a valley.
I would say the waterfall and the rapids are the most prominent features of a narrow V - Shaped valley where the stream profile drops rapidly.
A V-shaped valley eroded by a river is called a canyon.
You can transform a v-shaped valley into a u-shaped valley by a glacier.
A V-shaped valley has been formed by a river. A U-shaped valley has been formed by a glacier.
You can transform a v-shaped valley into a u-shaped valley by a glacier.
You can transform a v-shaped valley into a u-shaped valley by a glacier.
A 'V' shaped valley is formed by streams and water action. A 'U' shaped valley is formed by the gouging out of the valley walls by a glacier. A hanging valley is where side valleys are cut across by the main glacier. Hanging valleys often have waterfalls that fall into the main valley over a cliff.
The most prominent features of a narrow V-shaped valley with a rapidly dropping stream profile are steep valley walls, narrow width of the valley bottom, and a pronounced V shape that indicates erosion by the stream. These valleys often exhibit vertical erosion and can be associated with fast-flowing water and a high energy environment.
V-shaped Valley
a valley , that'll work , or a V shaped Valley.
A 'V' shaped valley is formed by streams and water action. A 'U' shaped valley is formed by the gouging out of the valley walls by a glacier. A hanging valley is where side valleys are cut across by the main glacier. Hanging valleys often have waterfalls that fall into the main valley over a cliff.
The glacier was huge.A v-shaped valley is a valley that was shaped by a glacier.