Glacial Trough (U-shaped valleys) - Flat-bottomed valley with steep sides produced by the erosion of the floor and sides of the valley by an alpine glacier as its sediment abrades while the glacier flows downhill. On the topographic maps they are recognized by closely spaced contours along the valley sides and widely spaced contours on the valley floor.
Hanging Glacial Troughs - Formed when the down-cutting erosion of the main valley glacier exceeds that by the tributary glacier. The tributary glacier flows onto the main glacier and thus has an erosional base level of the elevation of the main valley glacier. After melting, the lower portion of the tributary glacial trough is then left hanging above the main floor of the glaciated valley. On maps they are recognized by more widely spaced contours across a stream in the upper portion than in the lower portion (where the modern stream cascades into the main valley below).
If it is inundated by the sea it is called a "Fjord", if not is just a glacial valley.
A U-Shaped Valley is formed by glacial erosion.
It's called a "hanging valley". Many waterfalls occur at hanging valleys.
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.
A glacial valley typically has a U-shaped cross-section, with steep walls and a flat or gently sloping bottom. These valleys often have a wide floor and are characteristic of being carved out by the movement of glaciers.
hanging valley
A glacial trough is a U-shaped valley carved out by a glacier as it moves downhill. It forms through a process called glacial erosion where the glacier scours and deepens the valley over time by plucking and grinding the bedrock beneath it. The vast weight and movement of the glacier cause it to scrape and shape the landscape into a distinctive U-shaped trough.
They are called hanging valleys. The smaller glacier valleys are the hanging walls that join the deeper main valley called the U-shaped valley.
arete-steep sided ridge corries-hollows containing small glaciers ribbon lakes-formed by glacial retreat glacial trough-steep flat bottomed valleys hanging valleys-valleys formed by tributary glaciers truncated spurs-cliff like edges of a valley pyramidal peak -mountain with 3 sides
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.
A 'U' shaped valley indicates glacial erosion.
A glacier trough is also known as a U-shaped valley and is formed when a glacier passes through it. The glacier erodes the bottom of the valley through abrasion, and the sides of the valley through freeze-thaw weathering. It wears away the softer rock but when it gets to the harder, tougher rock it can't erode it to give the glacial trough its shape. Hope this helps!
If it is inundated by the sea it is called a "Fjord", if not is just a glacial valley.
Erosional features in areas with valley glaciers include U-shaped valleys, cirques (bowl-shaped hollows at the head of glaciers), arêtes (sharp ridge between cirques), and hanging valleys (smaller valleys that join a main glacier valley). Glacial striations (scratches on bedrock caused by moving glacier ice) and moraines (piles of debris deposited by glaciers) are also common erosional features.
No. The Grand Canyon was carved by the Colorado River.
The Hanging Valley was created in 1989.
U-shaped valleys, moraines, cirques, and hanging valleys are typical landforms that indicate the prior existence of a valley glacier. Additionally, striations (scratches left on bedrock), glacial till, and erratic rocks deposited in the area are also signs of past glacial activity.