The term "valley walls" is metaphorical; valleys do not actually have walls, they have hills. Valleys are between hills, that's why they are valleys. If there were no hills, the valley would just be a plain.
As a glacier moves through a valley, it digs deep into the walls and floor . A once-narrow valley that had a V shape becomes wider. As a glacier moves through, the valley becomes U shape .
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 U-shaped valley is formed when glaciers carve out a valley. As glaciers move down mountainous terrains, they erode the landscape, widening and deepening the valley floor while creating steep, rugged side walls. This distinctive U-shape contrasts with the V-shaped valleys typically formed by river erosion, highlighting the powerful impact of glacial activity on the topography.
The choices for this question are either a: U cross-Valley Profile, Y Cross-Valley Profile, V cross-valley profile, or S Cross Valley Profile.The answer to this question is a: U cross-valley profile is typical of canyons and valleys eroded by alpine or valley glaciers.
Cirques are the rounded basins carved into the sides of mountains by valley glaciers. They are typically characterized by steep walls and a bowl-like shape. The process of glacial erosion forming cirques is known as plucking and abrasion.
The bed of a youthful valley will be steeper than the remainder of the watercourse, and the valley walls will be steeper than the remainder of the watercourse.
Sure, very common! Rainwater running down valley's walls end up in the center as a lake.
To help survive during floods .
Round the walls of the tombs of the Pharaohs in the valley of the kings.
The term "valley walls" is metaphorical; valleys do not actually have walls, they have hills. Valleys are between hills, that's why they are valleys. If there were no hills, the valley would just be a plain.
The Indus people probably wanted privacy or they used the outer walls forsomething else,maybe they put decor on the outer walls
As a glacier moves through a V-shaped river valley, it erodes the valley walls, transforming the V shape into a broader U shape. The immense weight and movement of the glacier scrape and pluck rock and sediment from the sides, leading to steepened and smoothened valley walls. This process also results in the widening of the valley floor, creating a more expansive glacial trough. Over time, the glacier's movement reshapes the landscape, leaving behind features such as hanging valleys and moraines.
A glaciated mountain valley typically has a U-shaped profile with steep, smooth walls and a flat bottom due to the scouring action of the glacier. In contrast, a mountain valley that was not glaciated usually has a V-shaped profile with more rugged and uneven walls, shaped primarily by flowing water and tectonic forces.
They are called hanging valleys. The smaller glacier valleys are the hanging walls that join the deeper main valley called the U-shaped valley.
The proper name for a wide valley floor is typically referred to as the valley bottom or valley floor. It is the flat or gently sloping area between the valley walls where rivers or streams may flow.
A rift valley looks like a very huge trench. There is a wide opening at the centre of the two escarpment walls on either sides.
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.