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Geography GCSE
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The main types of
renewable energy
are
solar
,
wind
,
hydroelectricity
,
geothermal
,
tidal
,
wave
,
biomass
, and
biofuels.
Solar power
is generated using photovoltaic cells or
concentrated solar panels
that
convert sunlight
into
electricity.
Geothermal energy
uses
heat
stored within the Earth's
crust
to create
steam
, which drives
turbines
to generate
electricity.
Nigeria
is a
LIC
that hires migrant workers from other countries (
HICs
) using
TNCs
because they are
unable
to
afford resources
to get
oil
themselves
A
floodplain
is a wide,
flat
area of
marshy
land on either side of a river, and is found in the
middle
and
lower
courses.
Floodplains
are made of
alluvium
, a
sediment
deposited by a
river
when it
floods.
Floodplains
are used for
farming
as the
soils
are very
fertile.
Meanders
migrate across the
floodplain
due to
lateral
erosion.
When
meanders
reach the edge of the floodplain they
erode
the
valley side
(
bluff
).
This explains why
floodplains
are very
wide.
When the river floods it
deposits silt
, creating a very
flat
floodplain.
Layer
upon
layer
builds up over many
years
to form a thick
deposit
of
fertile alluvium.
A
levee
is a
raised
river bed (
levé
in French means
'rise'
) found alongside a river in its
lower
course.
A
ridge
of
sediment
is
deposited
naturally to build up the
levee.
During
low
flow conditions
deposition
takes place,
raising
the river bed and
reducing
the capacity of the channel.
When
flooding
occurs, water flows over the
sides
of the channel.
The
velocity
of the river
decreases
rapidly leading to
deposition
of
sediment
on the river
banks.
First the
coarser
sands are
deposited
and then the
finer
silt and
mud.
Gradually after many
floods
the
height
of the
banks
can be
raised
by as much as
two
metres.
In the UK most river
mouths
form wide tidal
estuaries
, especially in areas where
sea levels
have
risen.
Estuaries
are
transitional
zones between
river
and
coastal
environments and are affected by
wave
action as well as
river
processes.
The main process operating in
estuaries
is
deposition.
During a
rising
tide
river water is unable to be
discharged
into the sea.
The river's
velocity
falls
and sediment is
deposited.
At
low
tide these fine
deposits
form extensive
mudflats.
Over time, mudflats develop into important natural habitats called
saltmarshes.
The
upper
course of a river is characterized by a
steep
sided
V
shaped valley.