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

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

  • 2026-11-06

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

Ten items focus on valley development and simple calculations: lateral erosion, downcutting rates, Strahler order, meander migration, runoff volume, flood peaks, sinuosity and the effect of dams.

Quick answer 1. broad shallow trough, lateral erosion; 2. 5 cm; 3. second order; 4. 100 m; 5. about 2 × 10⁸ m³; 6. four times; 7. 1.5; 8. supply trapped, deposition lags erosion; 9. gravel, sand, silt, clay; 10. energy depends on discharge and gradient.

01 Paper details (check answers afterwards)

Item Detail
Questions 10 questions
Suggested time about 25 minutes
Difficulty mix Foundation 3 · Intermediate 4 · Challenge 2 · Error redo 1
Chapter Chapter: S4 Geography | River Landforms: erosion, transport, deposition and valley development
Level S4

02 Questions (10 items)

  1. FoundationWhat shape is a lower-course valley cross-section, and which erosion dominates?
  2. FoundationA river bed is downcut by 0.5 cm each year. How much lowering after 10 years?
  3. FoundationTwo first-order tributaries join. What is the Strahler order of the stream below the junction?
  4. IntermediateA meander outer bank retreats 2 m a year. How far has it moved in 50 years?
  5. IntermediateA 250 km² basin receives 2 000 mm of rain a year with a runoff coefficient of 0.4. What is the annual runoff volume?
  6. IntermediatePeak discharge rises from 20 m³/s to 80 m³/s. By what factor has it increased?
  7. IntermediateSinuosity is channel length divided by valley length. With 12 km of channel in an 8 km valley, what is the value?
  8. ChallengeWhy does a delta retreat after a dam is built upstream?
  9. ChallengeWhat is the correct order of sediment from coarsest to finest?
  10. Error redoA student claims river energy depends only on gradient. What is wrong?

03 Answers and one-line notes

# Answer One-line note
1 Broad and shallow, trough-shaped, dominated by lateral erosion. On a gentle lower course the river swings sideways, so the valley is much wider than upstream.
2 5 cm. Multiply the rate by the number of years, though armouring and base level eventually slow it.
3 Second order. Equal orders add one, while unequal orders keep the higher value, so 2 plus 1 stays 2.
4 100 m. Meander migration accumulates over decades and can finally cut off an oxbow lake.
5 About 2 × 10⁸ m³. Convert the area to 2.5 × 10⁸ m², multiply by 2 m of rain and by 0.4.
6 Four times. A fourfold rise in discharge greatly increases both transport power and flood risk.
7 1.5. A value near 1 means a straight channel; above 1.5 is strongly meandering.
8 The dam traps sediment, so downstream supply collapses and deposition can no longer match erosion and wave attack. A delta balance depends on river supply against marine removal, and cutting the supply makes it shrink.
9 Gravel, sand, silt, clay. Finer grains settle more slowly and travel farther, which is why river mouths are built of fine sediment.
10 Energy depends on discharge as well as gradient, so a large slow river can still move far more load. Discharge means mass, so a big gentle river can carry more total energy than a steep small stream.

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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