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S4 Geography: River Landforms – Challenge Practice (10 Questions)

S4 Geography: River Landforms – Challenge Practice (10 Questions)

  • 2026-11-06

S4 Geography: River Landforms – Challenge Practice (10 Questions)

Ten harder items cover flood plains, graded profiles, waterfall retreat, sediment yield, return-period probability, point bars, terraces, delta classification and urban hydrology.

Quick answer 1. fine alluvium left by floods; 2. a smooth concave-up curve; 3. 150 m; 4. 1 095 000 tonnes; 5. about 9.6 per cent; 6. point bar of sand and gravel; 7. renewed downcutting strands the old flood plain; 8. balance of supply against waves and tides; 9. higher peak, shorter lag; 10. armouring only slows erosion.

01 Paper details (check answers afterwards)

Item Detail
Questions 10 questions
Suggested time about 30 minutes
Difficulty mix Foundation 2 · Intermediate 2 · Challenge 5 · Error redo 1
Chapter Chapter: S4 Geography | River Landforms: erosion, transport, deposition and valley development
Level S4

02 Questions (10 items)

  1. FoundationWhat is a flood plain?
  2. FoundationWhat shape does a river long profile normally take?
  3. IntermediateA waterfall retreats 1.5 m a year. How far has it retreated in 100 years?
  4. IntermediateA river carries 3 000 tonnes of suspended load a day. What is the annual total over 365 days?
  5. ChallengeA flood has a 100-year return period. What is the chance of at least one such flood in the next 10 years?
  6. ChallengeWhat depositional feature builds on the inside of a meander bend, and of what is it made?
  7. ChallengeHow does a river terrace form?
  8. ChallengeWhat mainly controls the shape of a delta?
  9. ChallengeHow do peak discharge and lag time change after urbanisation?
  10. Error redoA student says an armoured bed means the river has stopped eroding. What is wrong?

03 Answers and one-line notes

# Answer One-line note
1 The flat lowland built of fine alluvium laid down when a river overtops its banks. Each flood leaves a thin sheet of silt, and the layers build into a flat fertile plain.
2 A smooth concave-up curve, steep near the source and gentle near the mouth. The graded profile is the ideal form reached when erosion and deposition balance.
3 150 m. The fall retreats because soft rock beneath is hollowed out and the hard cap collapses.
4 1 095 000 tonnes. Suspended load usually dominates total load, though the share varies with basin geology.
5 About 9.6 per cent, from 1 minus 0.99 to the power 10. A 100-year event has a 1 per cent annual exceedance probability, not one guaranteed hit every century.
6 A point bar, built of coarser sand and gravel. The slow inner bend drops the coarser load first, building a shoal that slopes toward the channel.
7 The river renews its downcutting and leaves an old flood plain standing as a bench above the new level. Uplift or a larger discharge makes the river cut down again, stranding the former flood plain on the valley side.
8 The balance between river sediment supply and the destructive power of waves and tides. River-dominated deltas prostrate, wave-dominated ones are smoothed, and tide-dominated ones are cut into funnels.
9 The peak becomes higher and arrives sooner, so lag time shortens. Impermeable surfaces cut infiltration, and rain reaches the channel quickly, giving a flashier flood.
10 Armouring only shields the bed with a coarse surface layer, so erosion continues but more slowly. Fine grains are winnowed away and a gravel lag remains, which needs a higher velocity to move.

04 What to do after marking

  • After marking, redo only the wrong items and write down which step went wrong (formula, unit, or misread number).
  • Repeat the same item two days later; move to the next paper only when both attempts are correct.
  • Parents only need the answer and note columns; there is no need to explain every item.

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