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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.

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What is the movement of a glacier?

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 .


Which forms as a glacier moves into a stream valley?

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.


What shaped valley is carved when glaciers carve out a 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.


What cross valley profile is typical of canyons and valleys eroded and deepened by alpine or valley glaciers?

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.


What are the rounded basins carved into the sides of mountains by 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.

Related Questions

What are characteristics of a youthful valley?

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.


Can there be a lake in a valley?

Sure, very common! Rainwater running down valley's walls end up in the center as a lake.


Why did the indus valley have so many walls?

To help survive during floods .


Where can you read the book the dead?

Round the walls of the tombs of the Pharaohs in the valley of the kings.


What are valley's?

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.


Why did the indus valley people have no windows on the outer walls of the buildings?

The Indus people probably wanted privacy or they used the outer walls forsomething else,maybe they put decor on the outer walls


What happens to the walls of a V shaped river valley as a glacier moves through it?

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.


8.How does a glaciated mountain valley differ in appearance from a mountain valley that was not glaciated?

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.


What are smaller glacial valleys that join the deeper main valley?

They are called hanging valleys. The smaller glacier valleys are the hanging walls that join the deeper main valley called the U-shaped valley.


What is the proper name for the wide valley floor?

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.


What does a rift valley look like?

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.


What forms as a glacier moves into a stream 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.