Figure 1 shows the rate of cliff retreat at two villages on a soft-rock coast, where longshore drift moves sediment from north to south. Groynes and rock armour were built at Village A in 2000. Village B is 3 km south of Village A.
Using Figure 1, describe the changes in the rate of cliff retreat at the two villages and suggest reasons for them.
Model answer
Before 2000 the cliffs at both villages retreated at about 1.5 m a year. After the defences were built at Village A in 2000, its rate of retreat fell sharply to about 0.3 m a year by 2005 and to about 0.1 m a year by 2020. At Village B the opposite happened: the rate increased to about 2.4 m a year by 2005 and about 3.4 m a year by 2020, more than twice the rate before 2000.
The rock armour at Village A absorbs wave energy at the foot of the cliffs, and the groynes trap sediment carried south by longshore drift, building a wider beach that protects the cliffs. Because the sediment is trapped at Village A, less reaches Village B, so its beach becomes narrower and its cliffs are attacked by more powerful waves. This is similar to what happened at Mappleton and Cowden on the Holderness coast.
Explanation
A Level 2 answer describes both lines with data (before and after 2000) and links the reasons together: the defences protect A, but by trapping sediment they starve B's beach, increasing erosion there. Describing the graph without suggesting reasons, or giving reasons for only one village, stays in Level 1.