Question

Difficulty: MediumOceans, Coastal Processes, and Coastal Landforms

Which of the following options represents the correct sequential order of physical stages involved in the landward retreat of a rocky cliff and the formation of a wave-cut platform?

  1. 1Concentrated marine erosion, mainly hydraulic action and abrasion, attacks the base of the cliff between high and low tide marks.
  2. 2Persistent undercutting along the cliff foot leads to the excavation of a wave-cut notch.
  3. 3The weight of the unsupported overhanging rock exceeds its tensile strength, causing it to collapse under gravity.
  4. 4Repeated cliff collapse causes the cliff face to recede landward, exposing a gently sloping bedrock terrace known as a wave-cut platform.

Answer

The correct sequence of stages in cliff retreat and wave-cut platform formation begins with concentrated wave erosion attacking the cliff base between tide marks, followed by the development of a basal wave-cut notch, the subsequent gravitational collapse of the unsupported overhang, and ultimately the landward retreat of the cliff face leaving an exposed wave-cut platform.
Cliff retreat begins when concentrated wave action (hydraulic force and abrasion) attacks the cliff base in the intertidal zone. Persistent undercutting carves a horizontal recess called a wave-cut notch. As erosion deepens the notch, the overhanging rock face loses structural support and eventually collapses under gravity. Over extended periods, this cycle of undercutting, overhang collapse, and cliff recession leaves behind a wide, gently sloping bedrock terrace termed a wave-cut platform.

Step-by-Step Solution

1
Identify the primary process initiating basal cliff erosion.
Marine erosion mechanisms (hydraulic action and abrasion) concentrate impact along the intertidal zone.
Wave energy is most potent between high and low tide levels.
2
Determine the micro-landform created by sustained undercutting.
A wave-cut notch is hollowed out at the base of the cliff face.
Continuous localized erosion carves a horizontal cavity into the rock base.
3
Identify the gravitational response to prolonged notch deepening.
The unsupported cliff overhang collapses under gravity.
Rock stability fails once the overhang exceeds critical mass without underneath support.
4
Establish the cumulative result of ongoing cliff collapse and retreat.
The cliff face moves inland, leaving behind a smooth, gently sloping wave-cut platform.
Repeated cliff retreat exposes the former rock base as a exposed bedrock bench at low tide.

Key Concept

Coastal Cliff Retreat and Wave-Cut Platform Formation
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