What are Erosional Landforms?

Erosional Landforms

Erosional landforms refer to the various landforms that have developed on the earth’s surface as a result of erosion. Erosion is the process by which the terrain is modeled away by numerous forces, including water, wind, and ice. Erosion-related landforms include valleys, potholes, rooted meanders, and river terraces, among others.

Cave:

• Waves often find some weakness or crack in the rock and widen it through hydraulic action.
• It often leads to the formation of caves on the headland.

Arches:

• The waves can then infiltrate the cave and erode the headland until they finally break through to produce an arc.
• For example, Durdle Door, Dorset, UK.

Stacks and stumps:

• As a result of constant weathering and erosion, the roof eventually collapses, leaving a tall, lonely stack.
• For example, Old Harry, Dorset coast.

Cliffs:

• The most prevalent type of coastal erosion on land is sea cliffs.
• When destructive waves hit the base of the rock wall between the high and low water marks, the reefs start to form.

Wave Cut Platforms:

• A wave notch results from processes like corrosion and hydraulic action that undercut the reef’s foundation.
• The boulder above hangs over the notch, and as the wave surge continues, the gap widens, eventually causing the overhang to fall due to gravity.
• The waves gently removed the tailings before attacking the fresh cliff face.

Summary:

What are Erosional Landforms?

The numerous landforms that have emerged on the surface of the earth as a result of erosion are known as erosional landforms. Erosion is the process by which the terrain is destroyed by various forces, including water, wind, and ice.

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