i think its the farts in this world
A stream valley landform is the most common result of erosion by flowing water over a long period of time. Water shapes the land by cutting through rock and soil, creating a valley with a stream or river running through it.
A V-shaped valley is primarily formed by erosion, specifically by the action of a river or stream wearing away rock and sediment over time. The force of flowing water scours the landscape, carving out the valley shape. While some sediment may be deposited along the valley floor, the overall formation is due to erosion.
The stream valley will likely have a V-shaped profile characterized by steep sides and a narrow channel due to the primary work of downward erosion cutting towards base level. This shape results from the stream's ability to efficiently remove material through hydraulic action, abrasion, and corrosion. As the stream continues to erode downwards, the valley may deepen and widen over time.
Headward erosion is a fluvial process of erosion that lengthens a stream, a valley or a gully at its head and also enlarges its drainage basin. The stream erodes away at the rock and soil at its headwaters in the opposite direction that it flows. Once a stream has begun to cut back, the erosion is sped up by the steep gradient the water is flowing down. As water erodes a path from its headwaters to its mouth at a standing body of water, it tries to cut an ever-shallower path. This leads to increased erosion at the steepest parts, which is headward erosion. (wikipedia)When this happens, the erosion can break through into another stream and the water from the stream is diverted. So the stream is "stealing" the other stream's water.
the uplift of the surrounding landmass. The stream erodes downward, carving a V-shaped valley, while the landmass rises due to tectonic movement. Over time, this combination results in the formation of V-shaped stream valleys.
A stream valley is usually 'V' shaped, formed by erosion from a stream. A glacial valley is usually 'U' shaped, formed by the action of a glacier.
wind erosion
a stream is most likely widen by erosion
A mature stream causes more erosion than a young stream, due to the pure fact that theres more curve in a mature stream causing the sediments to shift more frequently.
It is because if a stream gets bigger, it is allowed to carry more sediment. More sediment means more erosion.
the headward erosion hat brings about the formation of a river valley is an important factor in a process called stream piracy.
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.
A stream valley landform is the most common result of erosion by flowing water over a long period of time. Water shapes the land by cutting through rock and soil, creating a valley with a stream or river running through it.
Gravity causes rock to fall away from steep mountains or cliffs and even by Landslides.
A 'V' shaped valley is typically formed by the erosion of a river or stream cutting through elevated land over time. The flowing water carves out the valley by gradually wearing away the surrounding rock and soil, creating steep, sloping sides that converge at the bottom in a V shape.
When a stream cuts into a steep slope, it often creates a feature known as a "stream valley" or "gorge." This process leads to vertical erosion, which can result in steep, rugged terrain along the banks of the stream. Over time, this erosion can deepen the valley and shape the landscape, potentially forming features like cliffs or waterfalls. The surrounding area may display a distinct contrast between the steep slopes and the flatter valley floor.
A valley is a stretch of lowland located between hills and mountains formed by erosion. It usually contains a river or stream running through it.