S5 Geography Rivers, Paper 3: base level and oxbow lakes
- 2026-11-02
S5 Geography Rivers, Paper 3: base level and oxbow lakes
Paper 3 starts from base level and sediment sorting, then calculates discharge, catchment runoff and velocity at a narrowing, and explains how a dam affects the bed and the delta.
Focus Gradient is fall over length, discharge is cross section times velocity, a fixed discharge means a narrower section flows faster, and base level limits downcutting.
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)
- FoundationA river runs 300 km with a fall of 450 m. What is its average gradient in metres per kilometre?
- FoundationWhat is base level, and why can a river no longer cut down once it reaches it?
- FoundationWhy is a river bed full of boulders upstream but fine sand downstream?
- FoundationHow does an oxbow lake form?
- IntermediateA channel is 22 m wide and 1.5 m deep with a velocity of 1.2 m per second. What is the discharge?
- IntermediateA catchment of 25 square kilometres receives 80 mm of rain that all runs off. What is the runoff volume?
- IntermediateA basin of 120 square kilometres has 1800 mm of rain a year and a runoff coefficient of 0.5. What is the annual runoff volume?
- ChallengeA channel narrows from 30 m to 15 m while discharge stays at 45 cubic metres per second and the depth there is 1.5 m. What is the velocity?
- ChallengeWhat does an upstream reservoir do to the lower course of a river?
- Error redoError: a student says river velocity depends only on slope. What is correct?
03 Answers and one-line notes
| # | Answer | One-line note |
|---|---|---|
| 1 | 1.5 m per km | Gradient is fall over length, and 450 divided by 300 is 1.5. |
| 2 | The surface of the water body it enters, usually sea level, and with no remaining fall the river stops downcutting | Erosion needs water driven by gravity, and once the channel reaches base level no fall is left to use. |
| 3 | Fast upper water carries coarse material that drops out as the flow slows, leaving fine sand to travel furthest | A stone the fast upper course can move settles where the flow slows, so particles grow finer downstream. |
| 4 | Erosion narrows the neck of a meander until a flood cuts it through, and the abandoned loop silts up into a lake | Meanders grow until only a narrow neck remains, which a flood cuts through and leaves the old loop abandoned. |
| 5 | 39.6 cubic metres per second | The cross section is 22 times 1.5, which is 33 square metres, and times 1.2 gives 39.6. |
| 6 | 2 000 000 cubic metres | Twenty five square kilometres is twenty five million square metres, and times 0.08 m gives two million cubic metres. |
| 7 | 108 000 000 cubic metres | One hundred and twenty square kilometres is 120 million square metres, times 1.8 m gives 216 million, and half of that is 108 million. |
| 8 | 2 m per second | Velocity is discharge over cross section, and 45 divided by 22.5 is 2. |
| 9 | Discharge falls and becomes steady, sediment supply is cut so the bed incises, and the delta at the mouth shrinks | A dam stores flood water and sediment, so the lower course keeps a steady flow but loses the sand that builds its bed and delta. |
| 10 | Velocity depends on slope, cross section, bed roughness and discharge together | At the same slope a narrower or smoother channel flows faster, so slope alone does not set velocity. |
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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