Question 1Two fictional coasts have the same offshore wave height. Coast A faces a long fetch and frequent onshore winds; coast B lies behind an offshore barrier. At A, permeable sandstone overlies clay and the cliff becomes saturated after prolonged rain. (a) Explain how wind duration, speed, fetch, bathymetry, refraction and shelter can produce different nearshore waves despite the equal offshore height. (b) Distinguish weathering from marine erosion and explain how water may trigger a rotational failure on this cliff. (c) Evaluate how stronger waves and rainfall could interact through toe removal and reduced strength, stating why the descriptions do not permit a numerical retreat forecast. Show your reasoning on a labelled cliff cross-section.6 indicative marks
Two fictional coasts have the same offshore wave height. Coast A faces a long fetch and frequent onshore winds; coast B lies behind an offshore barrier. At A, permeable sandstone overlies clay and the cliff becomes saturated after prolonged rain. (a) Explain how wind duration, speed, fetch, bathymetry, refraction and shelter can produce different nearshore waves despite the equal offshore height. (b) Distinguish weathering from marine erosion and explain how water may trigger a rotational failure on this cliff. (c) Evaluate how stronger waves and rainfall could interact through toe removal and reduced strength, stating why the descriptions do not permit a numerical retreat forecast. Show your reasoning on a labelled cliff cross-section.
Cambridge 2027: Partial conceptual match
Wave controls and subaerial processes: the prompt and worked answer explicitly demonstrate these selected concepts. Remaining material: g-8.1.1: measured wave/tide/current resources and constructive/destructive regimes; g-8.1.3: wider physical/chemical/biological weathering and mass-movement examples. Fictional data are not real named-case evidence. Independent teacher review pending.
- 9696: 8.1.1: Waves and coastal controls
- 9696: 8.1.3: Subaerial coastal processes
AI-assisted placement. Independent teacher approval pending.
Show indicative guidance
Worked guidance
- Trace energy from wind generation through bathymetric transformation to the cliff rather than equating an offshore measurement with cliff impact. Explicitly label the sheltering barrier and differing approach directions.
- On the cross-section draw permeable over less-permeable strata, possible perched water, a curved slip surface and a threatened toe. These are hypotheses about the fictional lithology, not a claim that all sandstone-clay cliffs fail identically.
- Evaluate a coupled event chain: waves remove toe support, water reduces resistance and a failure provides debris that may temporarily protect the toe. Feedback and time lag make a single-driver explanation inadequate.
- Primary references (theory or real case, not sources of fictional numbers): US National Park Service: Coastal Landforms: https://www.nps.gov/subjects/geology/coastal-landforms.htm; USGS Fact Sheet 2004-3072: Landslide Types and Processes: https://pubs.usgs.gov/fs/2004/3072/fs-2004-3072.html
Self-marking points
View marking points
- Offshore height alone omits wave period/direction and nearshore transformation; long fetch does not guarantee identical waves at every point.
- Shoaling/refraction and barriers redistribute energy; wave approach and beach slope affect swash/backwash and cliff exposure.
- Weathering breaks down material in place; marine erosion removes material through water/load action.
- Water can perch above clay, raise pore pressure and reduce effective resistance, favouring curved-surface rotational movement where conditions allow.
- Toe erosion can remove support while rainfall weakens the slope; drainage, bedding and engineering modify the interaction.
- Retreat needs repeat surveys and event/geotechnical evidence; no deterministic rate follows from this schematic.
Examiner tip
Wave height offshore is not cliff erosion rate. Weathering, marine removal and mass movement are related but distinct processes. Indicative practice points only; independent teacher approval pending.