RiversIGCSE
M Ralph
Topic Outline
• Explain the main hydrological characteristics and processes which
operate within rivers and drainage basins
• Demonstrate an understanding of the work of a river in eroding,
transporting and depositing
• Describe and explain the formation of the land forms associated
with these processes.
• Demonstrate and understanding that rivers present hazards and
offer opportunities for people.
• Explain what can be done to manage the impacts of river flooding
• Know a case study of the opportunities presented by a river, the
hazards associated with it and their management.
STARTER
Are there any rivers
in the UAE? explain
your answer!
Learning Objectives
•All – identify the different
features of a river
•Most – can discuss the
journey of a river from source
to mouth
•Some – can define what each
key feature is.
Common River Terms
•Source – The place where a river begins.
•Course – The route the river takes to the sea
•Tributary – A small river that joins a larger
river.
•Confluence – The point where the tributary
joins the river.
Common River Terms
•Mouth – The point where the river enters the
sea.
•Estuary – The part of the mouth that is tidal.
•Basin – The area of land drained by a river.
•Watershed – The high ground separating one
river basin from another.
The River’s Journey
• Rivers usually begin in the mountains.
• They flow downhill onto flat land and into the sea.
The Stages of a River’s Journey
As the river flows from it’s
source to the sea it goes
through 3 stages. These
are:
1. The Upper or Youthful
Stage
2. The Middle or Mature
Stage
3. The Lower or Old Stage
4 Processes of River Erosion
•Hydraulic Action – The force of the moving
water wears away the banks and bed of
the river.
•Abrasion – Small stones carried by the river
wear away at the banks and bed of the
river.
4 Processes of River Erosion
•Attrition – The small stones in the river are
worn down and broken up as they hit off
each other.
•Solution – Rocks and soil are dissolved by
acids in the water.
The Youthful River
•The youthful river has a small amount of water
but it travels very quickly down the steep
mountain slope.
•Most of its energy is used to erode (wear away)
the landscape.
•This erosion (wearing away) occurs in 4 ways.
Landforms of the Youthful Stage
• All of the erosion by the river creates features or
landforms on the landscape.
Three features created in the youthful stage are,
1. V-shaped Valleys
2. Interlocking Spurs
3. Waterfalls
V-Shaped Valleys
• V-shaped valleys get their name from their shape.
The river erodes the landscape and creates a valley
in the shape of a V.
• This occurs because of Vertical Erosion. The river cuts
down into the river bed, making it deeper. It creates
a narrow deep valley. Mechanical weathering and
mass movement create the V shape. See Diagram.
V-Shaped Valleys
Interlocking Spurs
•As the rivers flows it
meets areas of hard
rock. It cannot erode
these so it flows
around them.
•This creates a zigzag
course.
Waterfalls
• Waterfalls are formed when
rivers flow over areas of hard and
soft rock.
• The river erodes the soft rock but
cannot erode the hard rock. This
creates a step which the water
starts to fall over.
• The falling water erodes deeper
into the bed. The rivers load
creates a Plunge Pool as it falls.
See Diagram.
Video clip
• https://www.youtube.com/
watch?v=fOI7aKvrFn4
Write down 5 facts
you learned from the
video clip!
Starter
List the 4 types of
river erosion
…write it down!
Learning Objectives
•All – can identify features
at the middle course of the
river
•Most – Can explain how the
river transports its load
•Some – can describe what
the rivers load consists of.
The Mature Stage
• We now know that during the youthful stage the
river is mainly eroding the landscape.
• Erosion breaks off particles of rock and soil from the
bed and banks of the river. They are carried along by
the river and are known as the Load.
• The load is carried from upland to lowland areas.
This process is called River Transportation.
River Transportation
• All rivers carry material in them. This material is carried by
• the river as it flows along.
• Rivers can carry large stones, small stones, sand, and
• other dissolved minerals.
• All of this material in the river is called the river’s Load
• When the river moves its load we call this River
Transportation
River Transportation
•Transportation occurs in 4 ways.
•1. Rolling
•2. Bouncing
•3. Suspension
•4. Solution
Rolling
The large stones are rolled along
the bed of the river.
Rolling
Bouncing
The smaller pebbles are bounced
along the bed of the river.
Bouncing
Suspension
Light material like sand and silt are
carried along (floating) in the water.
Solution
Dissolved materials are carried along by the river.
Solution
Starter
What is a Wadi?
Where is the closest
one to the school?
…Write it down!
Learning Objectives
•All – can identify all features at
the mature and old stage of
the river
•Most – can explain with the aid
of a diagram how meanders
form
•Some – can discuss how ox-
bow lakes, levees and deltas
form.
Landforms of the Mature Stage
In the Mature Stage the river begins to slow down,
and so it begins to deposit some of its load. It
creates the following features.
1. Wide river valley
2. Meanders
3. Flood plain
Wider River Valley
• In the mature stage the river
moves from side to side and
the valley becomes wide and
flat.
• Weathering and Mass
Movement continue to wear
away at the sides of the valley.
Meanders
Meanders are bends or
curves along the river.
They are formed by
erosion and deposition.
Erosion occurs on one
side of the river while
deposition occurs on
the opposite side. This
continues, making the
bends sharper. See
diagrams.
Flood Plain
A flood plain is the flat area of
land on either side of the river.
After heavy rain the river
sometimes floods. The water
spreads out over the land on
either side of the river. When
the river retreats it leaves
behind a thin layer of
alluvium. After many floods a
thick layer of alluvium is
created. This is very fertile soil.
The Old Stage
• In the Old Stage the river is
carrying lots of sand and silt. It
is now flowing over flat land
and so it is moving slowly.
Therefore it begins to drop off
its load. This is called
deposition. Like erosion in the
Youthful Stage, deposition also
creates many features or
landforms.
Landforms of the Old Stage
The following features or landforms are
created by river deposition in the Old Stage.
1. Ox-Bow Lakes
2. Levees
3. Delta
Ox-Bow Lakes
An ox-bow lake is a horseshoe
shaped lake found beside a
river. Ox-bow lakes are formed
when continued erosion and
deposition create very
pronounced meanders.
Eventually the river cuts through
the neck of the meander.
Deposition then occurs which
leaves the ox-bow lake
separated from the river.
How an Ox-Bow Lake is Made
Levees
Levees are raised banks of deposited
material found along the banks of
the river. When the river floods and
spreads out over the floodplain, the
heaviest material is deposited close
to the river.
Over time and after many periods of
flooding this deposited material
forms levees along the banks of the
river.
Delta• A Delta is a triangular shaped piece of
land which is formed at the mouth of the
river.
• As the river enters the sea it drops off all
the
• remaining material it is carrying.
• This material builds up to form new land.
• The river is forced to break up into smaller
channels called distributaries.
StarterLast year we
experienced some
flooding at school
what was the main
cause of it?
... Write it down
Learning Objectives
•All – identify the main causes
of flooding
•Most - can explain the
impacts of flooding in an area
•Some – can describe how the
flood was responded to
•Extension – what are the long
and short term effects?
Causes of Flooding• Heavy Rainfall
• Loss of Trees
• Tributaries
• Flat Land
• Impermeable Rock
• Steep Slopes
• Soggy Soil
• Built Up Areas
• Snow Melt
What is a flash flood?
Boscastle Flood MEDC
Background
• Boscastle is situated on the
northwest coast of Cornwall,
near Bude
• It is situated at the confluence
of the River Valency and its
tributaries
• It happened on Monday 16th
August 2004
What were the Causes?
• The day had been very warm, drawing
in sea breezes along the coast. When
they joined forces with a wet
southerly air flow they shot upwards
with a dangerous mix of warm, moist,
highly unstable air.
• The thunderclouds grew so tall that
they created intense rain leading to
more than 5 inches falling around
Boscastle in just a few hours.
• With the ground already saturated
from recent rains, the storm waters
were funneled down steep river
valleys and burst
Video clip
• http://www.bbc.co.uk/lear
ningzone/clips/why-did-
boscastle-flood/14072.html
Write down 5 facts
you learned from the
video clip!
Reasons For Flooding in Boscastle
• Heavy rainfall - is less likely to infiltrate into the soil and will reach the river
quickly. This will result in a rapid increase in river discharge.
• Relief of the surrounding area - Boscastle is in a valley, flanked on either side
by high ground. The slopes of the valley are very steep and the river
becomes narrower in the approach to the mouth.
• Impermeable ground - The underlying strata are mostly shales and slate,
with some sandstone beds which break down in weathering to give clay-rich
soils.
• Confluence of two rivers - Boscastle stands where two valleys meet, formed
by the rivers Valency and Jordan. A third river, Paradise, also flows through
the village.
• Bridge - This constricted the flow of the water through the village, forcing
the river to burst its banks.
What were the effects?
• 90% of Boscastle’s economy is dependent on tourism.
• After the flood, more than 20 accommodation providers were
forced to shut
• Seven helicopters from the Coastguard, the Royal Navy and the
Royal Air Force hovered overhead, winching people to safety
• Cars, boulders and uprooted trees were strewn through the streets.
• Cars were swept out to sea, bridges were washed away and people
clung to rooftops and trees
• Work has started on new £4.5m flood defences to protect the
Cornish village of Boscastle from flooding.
Video clip
https://www.youtube.
com/watch?v=xrb0Ea0
OkKU
What do you think the
immediate impacts of
the Boscastle floods
were?
Mozambique LEDC Flooding
Background
• 9th Feb – 27th Feb 2000
• 40 million population
• Zambezi was 2.5 m over
flood level
Mozambique LEDC Flooding
Hazards
•Destroy infrastructure
•Death
•Destroy services
•Disease
•Damage to field
•Damage to communication
Mozambique LEDC Flooding
Opportunities
• Fertile land (alluvium)
• LEDCs make money from
subsistence farming
• Water for irrigation
• Transport - Travel by boat
along river
• Flat land for building
• River source of fish (food)
Mozambique LEDC Flooding
Impacts
• Social – 180,000 fled, 81
dead, 150,000 in danger from
starvation, 23,000 lost
everything they had
• Economic – Roads and
bridges destroyed, transport
links cut off
• Environmental – 7,000
trapped in trees
Igcse rivers

Igcse rivers

  • 1.
  • 2.
    Topic Outline • Explainthe main hydrological characteristics and processes which operate within rivers and drainage basins • Demonstrate an understanding of the work of a river in eroding, transporting and depositing • Describe and explain the formation of the land forms associated with these processes. • Demonstrate and understanding that rivers present hazards and offer opportunities for people. • Explain what can be done to manage the impacts of river flooding • Know a case study of the opportunities presented by a river, the hazards associated with it and their management.
  • 3.
    STARTER Are there anyrivers in the UAE? explain your answer!
  • 4.
    Learning Objectives •All –identify the different features of a river •Most – can discuss the journey of a river from source to mouth •Some – can define what each key feature is.
  • 6.
    Common River Terms •Source– The place where a river begins. •Course – The route the river takes to the sea •Tributary – A small river that joins a larger river. •Confluence – The point where the tributary joins the river.
  • 7.
    Common River Terms •Mouth– The point where the river enters the sea. •Estuary – The part of the mouth that is tidal. •Basin – The area of land drained by a river. •Watershed – The high ground separating one river basin from another.
  • 8.
    The River’s Journey •Rivers usually begin in the mountains. • They flow downhill onto flat land and into the sea.
  • 9.
    The Stages ofa River’s Journey As the river flows from it’s source to the sea it goes through 3 stages. These are: 1. The Upper or Youthful Stage 2. The Middle or Mature Stage 3. The Lower or Old Stage
  • 10.
    4 Processes ofRiver Erosion •Hydraulic Action – The force of the moving water wears away the banks and bed of the river. •Abrasion – Small stones carried by the river wear away at the banks and bed of the river.
  • 11.
    4 Processes ofRiver Erosion •Attrition – The small stones in the river are worn down and broken up as they hit off each other. •Solution – Rocks and soil are dissolved by acids in the water.
  • 12.
    The Youthful River •Theyouthful river has a small amount of water but it travels very quickly down the steep mountain slope. •Most of its energy is used to erode (wear away) the landscape. •This erosion (wearing away) occurs in 4 ways.
  • 13.
    Landforms of theYouthful Stage • All of the erosion by the river creates features or landforms on the landscape. Three features created in the youthful stage are, 1. V-shaped Valleys 2. Interlocking Spurs 3. Waterfalls
  • 14.
    V-Shaped Valleys • V-shapedvalleys get their name from their shape. The river erodes the landscape and creates a valley in the shape of a V. • This occurs because of Vertical Erosion. The river cuts down into the river bed, making it deeper. It creates a narrow deep valley. Mechanical weathering and mass movement create the V shape. See Diagram.
  • 15.
  • 16.
    Interlocking Spurs •As therivers flows it meets areas of hard rock. It cannot erode these so it flows around them. •This creates a zigzag course.
  • 17.
    Waterfalls • Waterfalls areformed when rivers flow over areas of hard and soft rock. • The river erodes the soft rock but cannot erode the hard rock. This creates a step which the water starts to fall over. • The falling water erodes deeper into the bed. The rivers load creates a Plunge Pool as it falls. See Diagram.
  • 18.
    Video clip • https://www.youtube.com/ watch?v=fOI7aKvrFn4 Writedown 5 facts you learned from the video clip!
  • 19.
    Starter List the 4types of river erosion …write it down!
  • 20.
    Learning Objectives •All –can identify features at the middle course of the river •Most – Can explain how the river transports its load •Some – can describe what the rivers load consists of.
  • 21.
    The Mature Stage •We now know that during the youthful stage the river is mainly eroding the landscape. • Erosion breaks off particles of rock and soil from the bed and banks of the river. They are carried along by the river and are known as the Load. • The load is carried from upland to lowland areas. This process is called River Transportation.
  • 22.
    River Transportation • Allrivers carry material in them. This material is carried by • the river as it flows along. • Rivers can carry large stones, small stones, sand, and • other dissolved minerals. • All of this material in the river is called the river’s Load • When the river moves its load we call this River Transportation
  • 23.
    River Transportation •Transportation occursin 4 ways. •1. Rolling •2. Bouncing •3. Suspension •4. Solution
  • 24.
    Rolling The large stonesare rolled along the bed of the river. Rolling
  • 25.
    Bouncing The smaller pebblesare bounced along the bed of the river. Bouncing
  • 26.
    Suspension Light material likesand and silt are carried along (floating) in the water.
  • 27.
    Solution Dissolved materials arecarried along by the river. Solution
  • 28.
    Starter What is aWadi? Where is the closest one to the school? …Write it down!
  • 29.
    Learning Objectives •All –can identify all features at the mature and old stage of the river •Most – can explain with the aid of a diagram how meanders form •Some – can discuss how ox- bow lakes, levees and deltas form.
  • 30.
    Landforms of theMature Stage In the Mature Stage the river begins to slow down, and so it begins to deposit some of its load. It creates the following features. 1. Wide river valley 2. Meanders 3. Flood plain
  • 31.
    Wider River Valley •In the mature stage the river moves from side to side and the valley becomes wide and flat. • Weathering and Mass Movement continue to wear away at the sides of the valley.
  • 32.
    Meanders Meanders are bendsor curves along the river. They are formed by erosion and deposition. Erosion occurs on one side of the river while deposition occurs on the opposite side. This continues, making the bends sharper. See diagrams.
  • 34.
    Flood Plain A floodplain is the flat area of land on either side of the river. After heavy rain the river sometimes floods. The water spreads out over the land on either side of the river. When the river retreats it leaves behind a thin layer of alluvium. After many floods a thick layer of alluvium is created. This is very fertile soil.
  • 35.
    The Old Stage •In the Old Stage the river is carrying lots of sand and silt. It is now flowing over flat land and so it is moving slowly. Therefore it begins to drop off its load. This is called deposition. Like erosion in the Youthful Stage, deposition also creates many features or landforms.
  • 36.
    Landforms of theOld Stage The following features or landforms are created by river deposition in the Old Stage. 1. Ox-Bow Lakes 2. Levees 3. Delta
  • 37.
    Ox-Bow Lakes An ox-bowlake is a horseshoe shaped lake found beside a river. Ox-bow lakes are formed when continued erosion and deposition create very pronounced meanders. Eventually the river cuts through the neck of the meander. Deposition then occurs which leaves the ox-bow lake separated from the river.
  • 38.
    How an Ox-BowLake is Made
  • 39.
    Levees Levees are raisedbanks of deposited material found along the banks of the river. When the river floods and spreads out over the floodplain, the heaviest material is deposited close to the river. Over time and after many periods of flooding this deposited material forms levees along the banks of the river.
  • 40.
    Delta• A Deltais a triangular shaped piece of land which is formed at the mouth of the river. • As the river enters the sea it drops off all the • remaining material it is carrying. • This material builds up to form new land. • The river is forced to break up into smaller channels called distributaries.
  • 41.
    StarterLast year we experiencedsome flooding at school what was the main cause of it? ... Write it down
  • 42.
    Learning Objectives •All –identify the main causes of flooding •Most - can explain the impacts of flooding in an area •Some – can describe how the flood was responded to •Extension – what are the long and short term effects?
  • 43.
    Causes of Flooding•Heavy Rainfall • Loss of Trees • Tributaries • Flat Land • Impermeable Rock • Steep Slopes • Soggy Soil • Built Up Areas • Snow Melt What is a flash flood?
  • 44.
    Boscastle Flood MEDC Background •Boscastle is situated on the northwest coast of Cornwall, near Bude • It is situated at the confluence of the River Valency and its tributaries • It happened on Monday 16th August 2004
  • 46.
    What were theCauses? • The day had been very warm, drawing in sea breezes along the coast. When they joined forces with a wet southerly air flow they shot upwards with a dangerous mix of warm, moist, highly unstable air. • The thunderclouds grew so tall that they created intense rain leading to more than 5 inches falling around Boscastle in just a few hours. • With the ground already saturated from recent rains, the storm waters were funneled down steep river valleys and burst
  • 47.
  • 48.
    Reasons For Floodingin Boscastle • Heavy rainfall - is less likely to infiltrate into the soil and will reach the river quickly. This will result in a rapid increase in river discharge. • Relief of the surrounding area - Boscastle is in a valley, flanked on either side by high ground. The slopes of the valley are very steep and the river becomes narrower in the approach to the mouth. • Impermeable ground - The underlying strata are mostly shales and slate, with some sandstone beds which break down in weathering to give clay-rich soils. • Confluence of two rivers - Boscastle stands where two valleys meet, formed by the rivers Valency and Jordan. A third river, Paradise, also flows through the village. • Bridge - This constricted the flow of the water through the village, forcing the river to burst its banks.
  • 49.
    What were theeffects? • 90% of Boscastle’s economy is dependent on tourism. • After the flood, more than 20 accommodation providers were forced to shut • Seven helicopters from the Coastguard, the Royal Navy and the Royal Air Force hovered overhead, winching people to safety • Cars, boulders and uprooted trees were strewn through the streets. • Cars were swept out to sea, bridges were washed away and people clung to rooftops and trees • Work has started on new £4.5m flood defences to protect the Cornish village of Boscastle from flooding.
  • 50.
    Video clip https://www.youtube. com/watch?v=xrb0Ea0 OkKU What doyou think the immediate impacts of the Boscastle floods were?
  • 51.
    Mozambique LEDC Flooding Background •9th Feb – 27th Feb 2000 • 40 million population • Zambezi was 2.5 m over flood level
  • 52.
    Mozambique LEDC Flooding Hazards •Destroyinfrastructure •Death •Destroy services •Disease •Damage to field •Damage to communication
  • 53.
    Mozambique LEDC Flooding Opportunities •Fertile land (alluvium) • LEDCs make money from subsistence farming • Water for irrigation • Transport - Travel by boat along river • Flat land for building • River source of fish (food)
  • 54.
    Mozambique LEDC Flooding Impacts •Social – 180,000 fled, 81 dead, 150,000 in danger from starvation, 23,000 lost everything they had • Economic – Roads and bridges destroyed, transport links cut off • Environmental – 7,000 trapped in trees