Sea cliffs are dynamic landforms that recede landward as waves erode the base of the cliff, causing overβsteepening and collapse. The speed of this retreat is a key indicator of coastal vulnerability and is driven by the balance between material removal and addition.
The primary drivers include the mechanical erosion caused by wave impact, the chemical weakening of rock, and the amount of sediment that is redeposited at the cliff toe. When erosion exceeds deposition, the cliff retreats; when deposition dominates, the retreat can be slowed or even halted.
E = erosion rate (m/yr)
D = deposition rate (m/yr)
T = time period (yr)
By inserting measured values for erosion, deposition, and the time interval, the formula yields the expected landward shift of the cliff line, allowing planners to assess risk and design mitigation strategies.
What causes sea cliffs to recede?
How does wave impact affect cliff retreat?
What role does chemical weakening play in cliff erosion?
How does sediment deposition influence cliff retreat?
What is coastal vulnerability?
How do I use this calculator for my project?
Can this calculator predict future cliff positions?
Results are for informational purposes only and do not constitute professional advice.
