How do drainage basins work, and what causes rivers to flood?
Drainage basins and flooding: the drainage basin as an open system (inputs, stores, transfers, outputs), the storm hydrograph, the physical and human causes of river flooding, the impacts of flooding, and a UK flood event.
An Eduqas GCSE Geography A (C111) answer to drainage basins and flooding in Theme 1, covering the drainage basin as an open system, the storm hydrograph, the physical and human causes of river flooding, the social, economic and environmental impacts, and a UK flood event.
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What this dot point is asking
This is part of Eduqas GCSE Geography A (C111) Theme 1, Landscapes and Physical Processes, assessed in Component 1. Eduqas expects you to understand the drainage basin as an open system (inputs, stores, transfers and outputs), to read and interpret a storm hydrograph, to explain the physical and human causes of river flooding, to describe the impacts of flooding (social, economic and environmental), and to study one UK flood event in detail.
The drainage basin as an open system
A drainage basin is the area of land drained by a river and its tributaries, separated from the next basin by a ridge of high land called the watershed. Eduqas treats it as an open system with four parts.
The storm hydrograph
A storm hydrograph shows how a river's discharge (the volume of water passing a point, in cumecs) responds to a rainfall event over time.
- The rising limb shows discharge increasing after rain; the peak discharge is the maximum; the falling (recession) limb shows it returning to normal.
- The lag time is the gap between the peak rainfall and the peak discharge. A short lag time with a steep rising limb and high peak means a flashy river that floods easily.
- Lag time is shortened by impermeable rock, steep slopes, saturated or frozen ground, sparse vegetation, urbanisation and intense rainfall, because all of these speed water to the channel.
Physical causes of flooding
Some flood causes are natural.
- Prolonged rainfall saturates the soil until no more can infiltrate, so extra rain runs straight off.
- Intense rainfall (a heavy storm) falls faster than the ground can absorb it.
- Snowmelt releases a large volume of water quickly in a thaw.
- Impermeable rock (clay, granite) stops infiltration, so water runs off the surface.
- Steep relief speeds overland flow into the valley.
Human causes of flooding
People can make floods more likely and more damaging.
- Urbanisation replaces permeable ground with impermeable concrete and tarmac and adds drains, so water reaches rivers faster.
- Deforestation removes trees that intercept rain and take up water, so more reaches the channel sooner.
- Building on the floodplain puts homes and businesses in harm's way and covers the natural flood store with hard surfaces.
- Reduced dredging of channels lowers their capacity, so they overtop sooner.
The impacts of flooding
Eduqas classifies flood impacts under three headings.
- Social: homes flooded and people made homeless, lives lost, water supplies contaminated, disruption to schools and hospitals, stress and ill health.
- Economic: the cost of repairs, lost business and farmland, damaged roads, railways and bridges, and rising insurance premiums.
- Environmental: soil eroded from fields, rivers polluted by sewage and chemicals, and habitats destroyed (though floodplains are also enriched by silt).
A UK flood event
Eduqas requires one UK flood studied in detail. A common choice is the 2015 Cumbria floods, when Storm Desmond dropped record-breaking rainfall (over 340 mm in 24 hours at Honister) onto already saturated, steep, impermeable upland catchments. Rivers including the Eden and Kent burst their banks, around 5,000 homes flooded in places such as Carlisle and Kendal, bridges were destroyed, and the damage ran to hundreds of millions of pounds. Another popular study is the 2014 Somerset Levels floods, where prolonged rain, a low flat landscape and reduced dredging left land underwater for weeks. Learn the causes, the impacts and the responses for your chosen event.
Try this
Q1. Describe the four parts of the drainage basin system. [4 marks]
- Cue. Inputs (precipitation), stores (interception, soil, groundwater), transfers (infiltration, throughflow, channel flow) and outputs (discharge, evapotranspiration).
Q2. Explain how urbanisation increases flood risk. [4 marks]
- Cue. Impermeable surfaces and drains stop infiltration and speed runoff, shortening lag time and raising peak discharge.
Exam-style practice questions
Practice questions written in the style of WJEC Eduqas exam questions on this dot point, with worked answer explainers. The year tag is the paper they imitate, not the source.
Eduqas 2018 (style)4 marksExplain how human activity can increase the risk of river flooding. (Component 1)Show worked answer →
A 4-mark "Explain" question assessing AO1 and AO2. Markers reward causal links, not a list of activities.
Award credit for: urbanisation replaces permeable soil and vegetation with impermeable concrete and tarmac, so rainwater cannot infiltrate; it runs off quickly into drains and rivers, raising discharge fast. Deforestation removes trees that would have intercepted rain and taken up water, so more reaches the channel sooner. Both reduce lag time and raise the peak discharge, increasing flood risk. A strong answer makes the link from the human action to faster runoff to higher, quicker peak discharge.
Eduqas 2022 (style)8 marksFor a UK flood event you have studied, assess the extent to which its impacts were caused by human activity rather than physical factors. (Component 1)Show worked answer →
An 8-mark "Assess" question marked by levels of response, assessing AO1, AO2 and AO3, with SPaG credit. Markers reward a named UK flood, a balance of physical and human factors, and a judgement.
Strong answers take a studied flood (such as the 2015 Cumbria floods or the 2014 Somerset Levels floods) and weigh the two sides. Physical causes: prolonged, intense rainfall (Storm Desmond dropped record rainfall on saturated ground), steep impermeable upland catchments, and low-lying floodplains. Human causes: building on the floodplain, reduced river dredging, deforestation of upland catchments, and impermeable urban surfaces speeding runoff. The impacts (homes flooded, roads and bridges destroyed, farmland ruined, the cost running into hundreds of millions of pounds) were worsened by where and how people had built and managed the land, but the trigger was an extreme physical event. A top answer reaches a clear, supported judgement on the balance rather than sitting on the fence. Markers reward the named event, balanced causes and a justified conclusion.
Related dot points
- River landforms and processes: weathering, mass movement, erosion, transport and deposition; the long profile and changing valley cross-profile; upper-course landforms (V-shaped valleys, waterfalls, gorges) and lower-course landforms (meanders, ox-bow lakes, floodplains, levees); and a UK river landscape.
An Eduqas GCSE Geography A (C111) answer to river landforms and processes in Theme 1, covering weathering and mass movement, the river processes of erosion, transport and deposition, the long profile, upper-course landforms (V-shaped valleys, waterfalls, gorges), lower-course landforms (meanders, ox-bow lakes, floodplains, levees) and a UK river landscape.
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An Eduqas GCSE Geography A (C111) answer to the distinctive landscapes of the UK in Theme 1, covering the distribution of upland and lowland landscapes, how geology, climate and human activity make them distinctive, and one landscape where human activity has created environmental challenges.
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An Eduqas GCSE Geography A (C111) answer to managing river and coastal landscapes in Theme 1, covering hard and soft engineering for river flooding and coastal erosion, their costs and benefits, stakeholder conflicts, and how to evaluate the strategies.
- Coastal landforms and processes: waves, marine and sub-aerial processes, erosional landforms (headlands and bays, caves, arches, stacks, stumps, wave-cut platforms) and depositional landforms (beaches, spits, bars), and a UK coastal landscape.
An Eduqas GCSE Geography A (C111) answer to coastal landforms and processes in Theme 1, covering constructive and destructive waves, marine and sub-aerial processes, erosional landforms (headlands, caves, arches, stacks, wave-cut platforms), depositional landforms (beaches, spits, bars) and a UK coastal landscape.
- Numerical and statistical skills: calculating and interpreting measures of central tendency (mean, median, mode) and spread (range, interquartile range), percentages and percentage change, ratios and proportions, and reading data from tables and graphs.
An Eduqas GCSE Geography A (C111) guide to the numerical and statistical skills assessed across every component, covering the mean, median, mode, range and interquartile range, percentages and percentage change, ratios and proportions, and interpreting data from tables and graphs.
Sources & how we know this
- WJEC Eduqas GCSE (9-1) Geography A specification (C111) — WJEC Eduqas (2016)