Coastal Landforms Codexery

Wave-cut platform

Erosional flat rock at cliff base, often exposed at low tide.

A wave-cut platform is a narrow, flat area of rock found at the base of a sea cliff or along a shoreline, created by erosion. It is often most visible at low tide, when extensive areas of flat rock are exposed. In some cases, the landward side may be covered by sand forming a beach, revealing the platform only during low tides or after storms.

Quick Facts

Alternate names
  • shore platform
  • coastal bench
  • wave-cut cliff
Primary erosional agents
  • abrasion
  • corrosion
  • hydraulic action
Additional weathering processes
freeze-thaw, biological weathering

Facts from the source article.

Did You Know?

Formation

Destructive waves striking a cliff face cause undercutting between high and low water marks through abrasion, corrosion, and hydraulic action, forming a wave-cut notch. This notch enlarges into a cave, and the roof eventually collapses under pressure from freeze-thaw or biological weathering, causing the cliff to retreat landward. The cave floor becomes the wave-cut platform as collapsed material is broken down by attrition, with some debris washed into the sea or deposited as an offshore beach. The constant wave action makes the platform a hostile environment, supporting only certain organisms.

Use of ancient examples

Ancient wave-cut platforms serve as evidence of past sea and lake levels. Raised, abandoned platforms found behind modern beaches indicate higher sea levels in the geological past and help identify areas of isostatic adjustment. Scientific dating or examination of marine fossils on the platform allows determination of when it formed, providing information about historical sea levels. In the United Kingdom and other previously glaciated areas, this has been used to calculate current land uplift rates. Where seismic activity alters coastlines, a series of platforms may record earlier sea levels and earthquake-related uplift.

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