an erosion by the movement of an can produce a you- shaped valley
A U-shaped valley is typically formed by erosion, specifically by the movement of glaciers over time. Glaciers carve out the valley through abrasion and plucking, removing rock and sediment from the valley walls and floor. This process results in the distinctive U-shape of the valley.
A U-shaped valley produced by the erosion of a valley glacier is called a glacial trough. This distinct feature is carved out by the movement of ice over time, shaping the landscape into a broad and deep valley with steep sides.
Stream erosion is mainly caused by the force of flowing water, which carries sediment and particles and can wear away the land it passes through. Valley erosion is a result of various factors, including the flow of water in streams and rivers, weathering of rocks, freeze-thaw cycles, and the movement of glaciers. Over time, these processes can shape and reshape the landscape of a valley.
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.
The formation of valleys can be caused by different types of erosion, primarily by the flowing of water (fluvial erosion) or by glaciers (glacial erosion). Fluvial erosion occurs when water flows through a valley, gradually wearing down the rock and soil. Glacial erosion happens when moving glaciers cut and shape the land as they advance and retreat.
A U-shaped valley is typically formed by erosion, specifically by the movement of glaciers over time. Glaciers carve out the valley through abrasion and plucking, removing rock and sediment from the valley walls and floor. This process results in the distinctive U-shape of the valley.
A U-shaped valley produced by the erosion of a valley glacier is called a glacial trough. This distinct feature is carved out by the movement of ice over time, shaping the landscape into a broad and deep valley with steep sides.
The entire valley is from erosion and glaciers.
Erosion!
A 'U' shaped valley indicates glacial erosion.
Water erosion
After glaciation, a valley can become a U-shaped valley, which is wider and shallower compared to the original V-shaped valley. This transformation is due to the erosion caused by the movement of glaciers, which tend to widen and deepen valleys as they erode and transport material.
Erosion played a crucial role in shaping Death Valley through a combination of weathering, water runoff, and the movement of ice and wind. Over millions of years, rainwater and meltwater from surrounding mountains eroded the rock and soil, carrying sediment into the valley. Additionally, wind erosion helped to sculpt the landscape, creating the valley's iconic features such as dunes and salt flats. Tectonic activity also contributed by lowering the valley floor while raising the surrounding mountains, intensifying the erosive processes.
Stream erosion is mainly caused by the force of flowing water, which carries sediment and particles and can wear away the land it passes through. Valley erosion is a result of various factors, including the flow of water in streams and rivers, weathering of rocks, freeze-thaw cycles, and the movement of glaciers. Over time, these processes can shape and reshape the landscape of a valley.
glacier erosion
Erosion.
Gully Erosion