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Geography
Paper 1
River Landscapes
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Cards (32)
Hard engineering examples:
Dams
and reservoirs,
channelisation
Soft engineering examples:
flood plain zoning, Washlands
Upper course of river
Relatively
high
above sea level
More
gravitational
potential energy
Vertical
(downwards)
erosion
dominates
Middle and lower courses of river
Relatively
low
Erodes more
laterally
(side to side)
Water joining river
1. From
tributary
streams
2. Surface
runoff
3.
Through
flow
4.
Base
flow
River velocity
Affected by how efficient the river is in overcoming
friction
with
bed
and banks
Sediments
Become
smaller
and
rounder
due to attrition
Deposition creating river landforms
1.
Flood
plains
2.
Levees
Flood plains
Lateral erosion
on the outside bends of
meanders
Valley floor
becomes more wide and
flat
During floods, the flood waters spread out across the
valley floor
As they slow down with
less energy
for transport, the river deposits fine sediments called
alluvium
Flood waters move very
slowly
, because they counter in
friction
Levees
In times of
flood
, water and
sediment
come out the channel as the river overflows its banks
As it overflows the river immediately releases
velocity
, energy and deposits the larger and heavier sediment first, on its
banks
Repeated flooding causes these banks to get
higher
forming
levees
Erosion and deposition creating river landforms
1.
Meander
, river cliffs and point bars
2.
Oxbow
lakes
Meander, river cliffs and point bars
As water approaches a meander it is thrown towards the outside of the bend
Current is
faster
here and erosion occurs to form a
river cliff
On the inside of a bend a current is
slower
and deposition occurs due to
increased friction
Oxbow
lakes
Meander
is being
eroded
Water
takes the
quickest route
Deposition
takes place cutting off the
meander
Meander
rock cut off completely
Oxbow lake
is left behind
Physical causes of flooding in Loughton Brook drainage basin
Impermeable Geology
Steep slopes
Small drainage basin
Impermeable Geology
Reduces infiltration
and
accelerates surface run-off
Steep
Slopes
Speed up
run-off
into the river
Small Drainage Basin
Drainage is
faster
because of the
small
size
Human causes of flooding in Loughton Brook drainage basin
Deforestation
Urbanisation
Deforestation
Reduces infiltration because the soil becomes more compact and
rainwater
reaches the surface
faster
Interception
is reduced
Urbanisation
Spreads
impermeable
surfaces (less infiltration)
Many
drains
to quickly transport rainwater into the
river
Dams and reservoirs and how they work
barriers
constructed to hold back
water
Dams and reservoirs benefits and advantages
They are long-lasting also produce
hydro-electric
power, provide local
water
supply. Can be used for water sports
Dams and reservoirs costs and disadvantages
They are expensive to build and can cause the
displacement
of people and ruin the environment. Some lakes suffer from the growth of
Algae
Channelisation Costs and disadvantages:
Water taken
downstream
may put
other
places at risk. It doesn't look natural.
Channelisation benefits
and
advantages
This involves more water to run through more quickly taking it away from places at risk concrete reducing friction increasing velocity.
Channelisation and how it works
this involves deepening and or straightening the river.
Flood plain zoning and how it works
governments
allocate areas of land to different uses according to their level of
flood risk.
Flood plain zoning Benefits and advantages
Food risk
management aims to prevent building homes and businesses for leisure and recreation are allowed because of
flooding
Flood plain zoning Costs and disadvantages
These may not be for the best places for different activities in terms of public accessibility
Washlands and how they work
areas on the
flood plain
are allowed to
flood
Washlands Costs and disadvantages:
Allowing land to
flood
may limit use of land for
recreation
for example or mean change of land use, for example a change of farmland
Washlands Benefits and advantages:
give a safe place for
floodwater
to of and help slow floodwaters down. Also improves a river
natural sediment process