Mountainous areas typically form V-shaped stream valleys. These valleys are created by the erosional forces of fast-flowing rivers and streams that cut down into the landscape, carving steep sides as they flow through the mountainous terrain. The steep gradient and high energy of the water contribute to the characteristic V-shape, as opposed to broader, flatter valleys found in more gentle landscapes.
As a glacier moves into a stream valley, it can create a U-shaped valley by eroding the valley floor and walls. The glacier may also deposit sediment along the valley as it retreats, forming features like moraines and outwash plains. Additionally, meltwater from the glacier can lead to the formation of kettle lakes and braided streams in the valley.
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.
dew, ice, stream and snow are all forms of water. Cold is not.
a. deepens itb. straightens itc. all of thesed. only deepens it and widens itC.) all of these
The type of glacier that forms when ice and snow accumulate in a mountain valley on a continent is called a valley glacier, or alpine glacier. These glaciers flow down the valley, shaped by the terrain and gravitational forces, and are typically found in mountainous regions. They can vary in size and are often a key feature of mountainous landscapes.
As a glacier moves into a stream valley, it can create a U-shaped valley by eroding the valley floor and walls. The glacier may also deposit sediment along the valley as it retreats, forming features like moraines and outwash plains. Additionally, meltwater from the glacier can lead to the formation of kettle lakes and braided streams in the 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.
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.
A stream valley forms through the process of erosion, where flowing water carves out the landscape, creating a channel and shaping the surrounding terrain. The depth of downcutting depends on factors such as the stream's velocity, sediment load, and the geology of the area; streams in soft rock may create deeper valleys than those in harder rock. Over time, the valley may widen and evolve through various processes, including lateral erosion and sediment deposition. Ultimately, the depth and profile of a stream valley can vary significantly based on these environmental factors.
water
ruhr valley
Rift valley
A river valley forms from a river from the river going into a valley
A rift valley.
A rift valley forms at a convergent boundary.
Answer:Rift Valley
a rift valley