Rivers have gravitational
energy so they transport load
(boulders, gravel, sand, silt)
downstream
When rivers have high energy (eg after heavy rainfall or if it flows
quickly), they erode. When rivers have low energy, they deposit
Erosion
Abrasion- Scraping, scouring and smashing
action of the load carried onto the river banks
Attrition- When pebbles and rocks carried
smash against one another so they get
smaller and more rounded
Hydraulic action- When friction and pressure cause
water to be forced into cracks of the river bank and
bed, causing the particles to break apart
Corrosion- When weak acidic water disscolve rocks such as limestone and chalk
Transportation
Solution- Dissolved minerals carried within water
Suspension- When small particles such as sand and silt are carried by the flow
Saltation- Small stones are bounced along the river bed
Traction- Large stones and boulders are rolled along the river bed
Factors affecting transportation
Size of particles
Type of rock as sofer rocks like limestone
are more like to be dissolved as they are
soluble
The velocity of the river
Deposition
Caused by a decrease in the gradient or
velocity of the river
In floooding, rivers overflow
onto the floodplain so they
deposit material after floding
An increase in the size of
sediment casues deposition
When there is shallow water (eg in the
inside of a meander bend) rivers deposit
its load
River landforms
V-shaped valleys
Formed in the upper course
The water erodes sharply
downwards(vertical erosion) and
cuts the bed like a knife, forming a
steep valley
Rain washes stones ans soil from the sides so the valley becomes V-shaped
Steep gradient+high energy= lots of erosion
The river winds and bends and avoids areas of hard rock, creating interlocking spurs
Meanders and oxbow lakes
Water flows faster on the outer curve of
its bend and slower on the inner curve
The outer bend is eroded whilst the
lower bed has depsoited materials
As the outer bend gets eroded (forms a river cliff),
the inner bedn grows (forms a point bar)
Over time, the process continues so the
meander becomes more loopy
An oxbow lake is a cut-off meander
As erosion continues, the neck of the meander gets narrower
During flooding the river takes a shortcut
stright across the neck
The loop of the meander gets sealed off
In time, the lake gets covered by
weeds and soil and disappears
Happens in the middle course
Waterfalls and gorges
Water tumbles over a ledge of hard
rock and erodes the sofer rock
underneath it faster
This leaves a ledge
of hard rockand a
plunge pool
Overhang makes the ledge unstable
so it falls into the plunge pool
This is repeated so the
water reatrests upstream
and carves out a gorge
Happens upstream
Floodplains
In the lower course, the river has a high voulme and a
large discharge and deposition happens
A floodpalin is an area around a river that is covered in times of flood
Very fertile as it has alluvium deposits
More deposition= build-up of alluvium, which
creates levees, which raise the river bank
Estuaries
it is where the river meets the sea.
The river here is tidal so during high tides, large
areas of valey floor will be flooded.
As the tide falls, materila will be deposited, creating
mudflats, which are important habitats fro wildlife
The Drainage Basin
Factors affecting the drainage basin
Geology- Impermeable rocks and clay soils do not allow
precipiation to inflitarte, increasing surface runoff, which can
increase the discharge and thus increase flooding risk
Deforestion+Afforestation- Trees reduce surface runoff due to interception as
well as soaking up groundwater. More trees= less discharge and vice versa
Urbanisation- Buildings and roads are impermeable, increasing
surface runoff sue to less inflitartion. Also, drains remove rainwater
quickly from urban areas towrds rivers, increasing discharge
Amount and duration of rainfall- Haevy
rain can cause floods as there is too mich
water to infiltarte into the ground so more
surface runoff. Long rain times causes the
soil to get oversatuared so more surface
runoff so higher discharge
Definitions
Drainage basin- an area of land drained by a river and its tribuateries
Watershed- The boundary between 2 drainage basins
River channel- Where the water flows
Confluence- Where two rivers meet
Source- the start of a river
Tribuateries- A small river joining the mian river
Mouth- Where the river meets the sea
Interception storage- Water stopped by vegetation
Surface storage- Water stored on the surafce of the eartg
Infiltartion- Water that soaks from the surface to soil
Percolation- Water travelling from soil to rock
Soil storage- Water stored in the soil
Groundwater storage- Water stored in rocks
Through flow- Water that travels through soil
Groundwater flow- Water that flows through the soil
Storm hydrographs
A hydrogarph is a way of displaying
hwo the discharge of a river can
chnage over a ranfall event
Discharge is the voulme of water flowing in a
river and is measured in cumecs. Peak
discharge is when a river is at its mots full
Lag time is the time taken for a channel to reach peak discharge after peak rainfall
Rising limb can be steeper due to less inflitartion
Peak discharge can be higher due to less infliltartion
Lag time also depends on the factors affecting a
draingae basin eg longer lagtime due to more
infiltration and groundwater flow
Case Study- The Cumbrian Floods-
2015
Cause
The warm air from the mid-atlantic caused relief
rainfall over the Cumbrain mountains. The warmer the
air, the more moisture it has
Event
In December 2015, Storm Desmond set a new
record with 341.4mm of rain faling over 24 hours
Cockermouth was mainly affected despite its
flood defences in response to previous floods
Previous flood
defences
River dredging took place after 2009 to increase the capacity of the river
A self-closing flood barrier was installed in
2013 to increase the height of the river banks
The Environmental Agency moniters the area for potential flooding and issues flood warnings (RAG)
The government has peldged to spend £2.3 billion on flood defences between 2016 and 2022
Impacts
Social
Over 43,000 homes suffered from
power cuts
5200 homes were affected by flooding
One person died
Economic
Many businesses suffered from property damage
Estimated cost was £500 million
across Cumbria. Government
provided £50 million for flood
victims and businesses
Environmental
Vegetation was flooded, causing habitat loss
Heavy rain washed nutrients fro soil
Rivers were largely altered sue to more erosion
Flood
management strategies
Hard Engineering
Embankments- Raising the banks of a river so it can hold more water.
Pros- Allows for floodwater to be contained within a river.
Cons- Water speeds up, increasing flood risk
downstream+ looks unnatural
Levees- Embankments built along rivers so river can hold more
water
Pros- Allows the floodplain to be built upon.
Cons- If levees are breached, there is a risk
of severe flooding+ expnsive
Dams- Huge walls built across rivers and resevoirs are
built behind dams. Floodwater is caught by dams and
is realesed by a steady flow throughout the year
Pros- Resevoirs provide a reliable water source and turbines in dams generate electricity. Also allows for irrigation.
Cons- Wildlife affected as fish migrate upstream to breeding groungs+ very expensive
Straightening- River seppeds up the water so
high volumes of water can pass quickly
Pros- Reduces flood risk in built-up areas.
Cons- Increases flood risk downstream due
to speeding of river
Dredging- Makes the river deeper to hold more water
Pros- More water held into the channel.
Cons- Needs to be done frequently
Flood relief channels- Water is diverted from areas being protected
Pros- Removes excess water from the river channel to reduce flooding.
Cons- Expensive+ relief channel can also flood if water levels continue to rise
Soft engineering
Flood plain zoning- Allowing only ceratin
land uses on the flodplain to reduce
flooding risk on buildings
Pros- Costlier buildings moved further from river so
lower flood risk.+ less damage= less insurance claims
Cons- Not always possible to change current land uses+
restricts development of an area
Wetalnd and river banck conservation- Wetland store water
ad slow it down so planting vegetaion increases interception,
increasing lagtime and reducing discharge
Pros- Creates wildlife
habitats+ vegetation
protects against soil erosion.
Cons- Less alnd available for
farming
Flood warnings and prepartion- Environmentqal
agencies monitor rivers and issue warning via th
emedia so people can prepare for floods
Pros- People have time to protect theor properties and evacuate+ reduces insurance claims.
Cons- Some people can't access warnings and flash floods happen to fast for a warning to
be effecive
River restoration- Making the river more natural though man-made levees and allowing natural flooding
Pros- Less maintainacne needed as river is left in its
natural state+ river provides a better habitat to wildlife.
Cons- Local flood risk increases
Views on flood defences
For
Planners advice that permeable
materials such as gravel are used
for more infiltartion
Soft engineering moves flooding away from urban areas
Expensive defences guarenatee home protection (home owner)
Peat bogs allow for more water to
soak into marshland and protects
habitats (envoronmnetalist)
Against
Motorists want impermeable materials
such as tarmac on roads
Hard engineering increases discharge downstream
and affects other towns (River scientist)
Floodplains must not be built upon
as there is a higher flooding risk
(housing minister)
Drains carry water downstream, increasing flooding risk (environmentalist)
The River Tees Case Study
Upper Course
Rises from the Penines and is located in the moorlands of Cumbria in soggy land
Annual rainfall is 1200mm and altitude is 800m
Bedload is large and angular and land is
mainly made of impermeable rocks
There is a V shaped valley
A resevoir is built to store water for urban areas downstream
Middle Course
Bedload is medium and rounded and altitude is 350m
V-shaped valley becomes flatter and meanders and floodpalins forms
Highforce Waterfall is made of Whin sill (hard rock) and is 21m high and forms a gorge
Lateral erosion happens so more depsoition
happens and river is wided and meanders erode
the valley floor, creating a U shaped valley
More land is used for farming and pasture
Flood defences-Yarm
Cost of defences was £2.1 million
Embankmenst installed to increase the level of river banks
Gabions reduce erosion along river banks
Street lighting and flower bed placed to
visually improve the area
Lower Course
Channel becomes wider and deeper
Bedload made of fine silt
Land use is mainly industrial (steel and iron
factories) and there is a nuclear power plant
Levees formed sue to flooding
Estuary important for wildlife such as birds
River has been straightened for navigation+ to reduce flooding
Flood defence- Tees Barrage
Barrage stops tidal flows upstream and has opened 25km clean navigable waterway for leisure
Regeneration of derelict land and attracted new jobs and businesses. Also led to increased tourism
Barrage cost £54 million
Around barrage there is a caranvan site, restaurants, woodlands, encouraging tourism