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S5 Geography Rivers, Paper 4: landforms and human activity

S5 Geography Rivers, Paper 4: landforms and human activity

  • 2026-11-02

S5 Geography Rivers, Paper 4: landforms and human activity

Paper 4 covers gradient, waterfalls and flood plains, then calculates discharge, catchment runoff, flood peak reduction and velocity at a narrowing, and interprets reservoir and runoff coefficient figures.

Focus Gradient is fall over length, discharge is cross section times velocity, runoff volume is area times rainfall times the coefficient, and a fixed discharge speeds up where the section narrows.

01 Paper details (check answers afterwards)

Item Detail
Questions 10
Suggested time 25
Difficulty mix Foundation 4 · Intermediate 3 · Challenge 2 · Error redo 1
Chapter Chapter: S5 Geography: Rivers
Level S5

02 Questions (10 items)

  1. FoundationA river runs 180 km with a fall of 720 m. What is its average gradient in metres per kilometre?
  2. FoundationHow does a waterfall normally form?
  3. FoundationHow is a flood plain formed?
  4. FoundationIn which course of a river is deposition strongest?
  5. IntermediateA channel is 18 m wide and 2.5 m deep with a velocity of 1.6 m per second. What is the discharge?
  6. IntermediateA catchment of 60 square kilometres receives 120 mm of rain that all runs off. What is the runoff volume?
  7. IntermediateA reservoir cuts the flood peak from 120 cubic metres per second to 78. By what percentage is the peak reduced?
  8. ChallengeA channel narrows from 24 m to 8 m while discharge stays at 96 cubic metres per second and the depth there is 2.5 m. What is the velocity?
  9. ChallengeA basin of 350 square kilometres has 2200 mm of rain a year and a runoff coefficient of 0.35. What is the annual runoff volume?
  10. Error redoError: a student says erosion is strongest in the lower course. What is correct?

03 Answers and one-line notes

# Answer One-line note
1 4 m per km Gradient is fall over length, and 720 divided by 180 is 4.
2 Hard rock caps softer rock, the soft layer is eroded into a step, and the river plunges over it Rock of differing resistance creates the step, and as the face retreats the fall slowly migrates upstream.
3 Flood water spills over the banks, slows sharply and drops its fine sediment on both sides Each flood lays down a thin sheet of silt, and repeated layers build a flat fertile plain.
4 The lower course, where velocity and carrying power are lowest The slower the flow the finer the load it can hold, so sand and silt settle in the lower course and at the mouth.
5 72 cubic metres per second The cross section is 18 times 2.5, which is 45 square metres, and times 1.6 gives 72.
6 7 200 000 cubic metres Sixty square kilometres is sixty million square metres, and times 0.12 m gives seven million two hundred thousand cubic metres.
7 Reduced by 35 per cent The difference is 42, and 42 over 120 is 0.35, so the peak is a third lower and flood risk falls.
8 4.8 m per second The section is 8 times 2.5, which is 20, and 96 over 20 is 4.8, so this reach erodes strongly.
9 269 500 000 cubic metres Three hundred and fifty square kilometres is 350 million square metres, times 2.2 m gives 770 million, and 0.35 of that is 269.5 million.
10 Erosion is strongest upstream through downcutting and headward erosion, while the lower course is dominated by lateral erosion and deposition Steep fast headwaters spend their energy cutting down, while the gentle lower course mostly transports and finally deposits.

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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