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CHAPTER 2
LIVING WITH
TECTONIC HAZARDS
Risk or Opportunity?
In this Chapter, you will explore three key
questions:
1.Why are some areas more prone to tectonic
hazards?
2.What landforms and associated tectonic
phenomena are found at plate boundaries?
3.How do people prepare for and respond to
earthquakes?
CHAPTER 2 LIVING WITH
TECTONIC HAZARDS
CHAPTER 2 LIVING WITH
TECTONIC HAZARDS
Gateway 2: What landforms and associated
tectonic phenomena are found at plate
boundaries?
The sea started to recede. I remember
learning in a geography lesson that this
happens before a tsunami. I shouted to tell
everyone a tsunami was coming and for
them to run!
Quoted from a survivor of the tsunami that took place at Mai Khao
Beach , Thailand on 26 December 2004.
In December 2004, The Tsunami swamps Phuket's Chedi resort (AFP/Joanne Davis)
Gateway 2: What landforms and associated
tectonic phenomena are found at plate
boundaries?
After the tsunami, authorities have now
installed signs along this coastline.
• What symbols and words would you expect to
see on these signs. Sketch the signs you
expect to see at the beach.
• Explain why you thought the signs are
important.
CHAPTER 2 LIVING WITH
TECTONIC HAZARDS
Gateway 2: What landforms and associated
tectonic phenomena are found at plate
boundaries?
a.Why are different landforms found at different plate
boundaries and how are they formed?
b.What phenomena are found at plate boundaries and how are
they formed?
What could have happened here?
Fold mountains
• Over millions of years, the folding of rocks creates a
landform called fold mountains.
• The Himalayas, the Rocky Mountains and the Andes
are examples of fold mountains.
• Fold mountains are formed along convergent
plate boundaries.
• The compressional force causes the layers of
rocks to buckle and fold.
• This process is known as folding.
Fold mountains
• The upfold is called the anticline and
• The downfold is the syncline.
• When there is increasing compressional force on one
limb of a fold, the rocks may buckle until a fracture
forms.
• The limb may then move forward to ride over the
other limb
Fold mountains
Fold mountains
The Himalayas
Peak : Mount Everest (between
Nepal and Tibet)
Elevation : 8,848 metres
• Fold mountains are located along convergent plate
boundaries
Describe the distribution of FM shown.
What could have happened here?
Describe what you see. [4]
Rift valleys and block mountains
• Rift valleys and block mountains are formed at
divergent plate boundaries.
• A fault is a fracture in the rocks along which
the rocks are displaced.
• The tensional forces result in parts of the
crust being fractured.
• This process is called faulting.
Rift valleys and block mountains
• A rift valley is a valley with steep sides formed along
fault lines.
• E.g. East African Rift Valley
Rift valleys and block mountains
• A block mountain is a block of land with steep sides.
It is formed when sections of the crust extend along
fault lines and rock masses surrounding a central
block sink due to tensional forces.
Rift valleys and block mountains
Explain the formation of Block
Mountains and Rift Valleys
Divergent plate
boundaries
Parts of crust
fractured in
faulting
Tensional
Forces
Pull apart Within a plate
Between
parallel faults
Form rift valley Sections of
crust extend
along fault
lines
Tensional
forces
Central block of
land subside
However When
tensional
forces
surround a
block of land
to subside
Block mountain
is form
Between
parallel fault
cause land
masses
Explain the formation of Block
Mountains and Rift Valleys
Divergent plate
boundaries
1
Parts of crust
fractured in
faulting
5
Tensional
Forces
2
Pull apart
4
Within a plate
3
Between a pair
of parallel
faults
To form a rift
valley
When Sections
of crust extend
along fault
lines
Tensional
forces
Can cause a
Central block of
land subside
However when
tensional
forces
surround a
block of land
to subside
A block
mountain is
form
Between
parallel fault
cause land
masses
Explain the formation of Block
Mountains and Rift Valleys
Divergent plate
boundaries
1
Parts of crust
fractured in
faulting
5
Tensional
Forces
2
Pull apart
4
Within a plate
3
Between a pair
of parallel
faults
4
To form a rift
valley
5
When Sections
of crust extend
along fault
lines
1
Tensional
forces
2
Can cause a
Central block of
land subside
3
However when
tensional
forces
surround a
block of land
to subside
A block
mountain is
form
Between
parallel fault
cause land
masses
Explain the formation of Block
Mountains and Rift Valleys
Divergent plate
boundaries
1
Parts of crust
fractured in
faulting
5
Tensional
Forces
2
Pull apart
4
Within a plate
3
Between a pair
of parallel
faults
4
To form a rift
valley
5
When Sections
of crust extend
along fault
lines
1
Tensional
forces
2
Can cause a
Central block of
land subside
3
However when
tensional
forces
1
surrounding a
block of land
to subside
3
A block
mountain is
form
4
Between
parallel fault
5
cause land
masses
2
Rift valleys and block mountains
The East African Rift Valley
Is formed from the Nubian
section of the African Plate and
the Somalian section of the
African Plate pulling away from
one another.
• Describe the distribution of rift valleys
and block mountains
What could have happened here?
Volcanoes
• A volcano is a landform formed by magma ejected
from the mantle onto the earth’s surface.
Mount Saint Helens volcano before and after an eruption in May
1980
• Magma is molten rock found below the earth’s
surface.
• Parts of a Volcano
- magma chamber
- vents
• Magma that is ejected onto the surface is known
as lava.
Volcanoes
Volcanoes
Formation, structure of, and features of a volcano
Shapes and sizes of volcanoes
• Volcanoes vary in shapes and sizes due to the
characteristics of the lava.
• Viscosity refers to the stickiness of the lava
• The most common types of volcanoes are:
- Shield volcanoes; and
- Stratovolcanoes
Volcanoes
Shield volcanoes
• Shield volcanoes have gently sloping sides and a broad
summit
• The low silica lava flows easily and spreads over a large
area before solidifying.
• As lava do not trap much gas, eruptions are generally not
explosive.
• Successive eruption cause the base of the volcano to
increase in size.
Volcanoes
E.g. Mount
Washington,
United States
of America
Why are shield volcanoes shaped
with a broad based and gentle
sloping sides?
Stratovolcanoes
• Stratovolcanoes develop from successive eruptions of lava
and ash.
• Initital explosion of pyroclastic flow because the high silica
lava traps gases.
• Followed by alternate layers of lava and pyroclastic flow
again.
• The lava prevents the pyroclasts from being eroded away.
• Successive eruptions build high volcano.
Volcanoes
E.g. Mount
Mayon,
Philippines
Compare between Shield and Stratovolcanoes
Characteristics Shield Volcanoes Stratovolcanoes
Shape Broad summit
Broad base
High volcano with slightly
concave profile
Height? x x
RELIEF Gentle sloping sides Steeper at the top
Gentler at the base
Type of lava Low silica content
Low viscosity
High silica content
High viscosity
Type of eruption Gentle Explosive
Frequency of eruption X X
Where it occurs? Usually at Oceanic-
Oceanic plate divergence
Or at hotspots
Usually at Continental-
Oceanic plate convergence
Volcanoes
Distribution of earth’s major active volcanoes
• An earthquake is a vibration in the earth’s crust caused by the
sudden release of stored energy in the rocks found along
fault lines.
b. What phenomena are found at plate
boundaries and how are they formed?
• Measuring earthquakes
- A seismograph records the seismic waves released
by an earthquake.
Earthquakes
• Extent of earthquakes
- The Richter Scale is used to measure the magnitude
of an earthquake
Earthquakes
Ecuador Earthquake 17 April 2016
7.8 Ritcher Scale – 11.26 p.m.
• http://www.mapsofworld.com/thematic-maps/earthquake/ecuador.html
1) What is the
extent of the
damage / impact
of the the EQ?
2) How long do
you think the
aftershocks may
last?
3) Why would
Ecuador suffer a
greater impact
than compared to
Taiwan?
Date Ritcher
Scale
Death
estimate
Injured
estimate
17 April (Sat) 7.8 272 2500
18 April 7.8 272 (am)
410 (pm)
Over 2000
20 April 6.1 Over 2000
21 April 6.0 Over 2000
Ecuador Earthquake 17 April 2016
7.8 Ritcher Scale – 11.26 p.m.
• https://www.youtube.com/watch?v=bWzruH2KcR8
• Three Deadly Earthquakes Strike in 3 Days
1) Do you think there might be patterns involved in the movements of the
plates?
• Apart from its magnitude, the extent of damage
caused by an earthquake may vary based on other
factors:
- Population density
- time of occurrence
- level of preparedness
- distance from the epicentre
- type of soil
Earthquakes
Describe distribution of the earth’s major earthquakes
Earthquakes
Hazards associated with living in earthquakes zones
- Threat of tsunamis
- Disruption of services
- Fires
- Landslides
- Destruction of properties
- Destruction of infrastructure
- Loss of lives
Earthquakes
What happened here?
Threat of tsunamis
• Tsunami refers to an usually large sea wave.
• Tsunamis may be formed by:
- The movement of the sea floor during a large earthquake
at subduction zones;
- An underwater volcanic eruption;
- An underwater landslide; and
- A landslide above sea level which causes materials to
plunge into the water.
Hazards associated with earthquakes
Hazards associated with earthquakes
• In 2004, a 9.2 magnitude triggered a tsunami with
waves spreading throughout the Indian Ocean.
Aceh before and after the tsunami hit the area
Hazards associated with earthquakes
The spread of the tsunami waves caused by the tsunami
Hazards associated with earthquakes
What happened here?
What happened here?
What happened here?
What happened
here?
Disruption of services
• An earthquake can disrupt services such as the
supply of electricity, gas and water.
• The earthquake in Kobe, Japan, in 1995 disrupted
electricity, gas and water supplies to about a million
of Kobe city’s 1.4 million residents.
Hazards associated with earthquakes
Fire
• Earthquakes may rupture gas pipes and this can
provide fuel to start fires.
• For example, the earthquake in Kobe, Japan, in 1995
caused extensive fires.
Hazards associated with earthquakes
Landslides
• Landslides are rapid downslope movements of soil,
rock and vegetation. Mudflows may also occur when
there is heavy rainfall.
Hazards associated with earthquakes
Destruction of properties
• Earthquakes can cause destruction to many homes.
• People may be without homes after the disaster.
Hazards associated with earthquakes
Destruction of infrastructure
• Earthquakes may cause cracks to form in
infrastructure such as roads and bridges.
• Transportation can be disrupted as it is unsafe to use
the damaged roads.
Hazards associated with earthquakes
Loss of lives
• Earthquakes and their associated hazards often
threaten the lives of those living in earthquake zones.
Hazards associated with earthquakes
Hazards associated with earthquakes
Volcanic eruptions
- Occurs on land occur on the sea floor.
Active, dormant or extinct
• Active volcanoes refers to volcanoes which are currently
erupting or are expected to erupt in the future.
• Dormant volcanoes are currently inactive but may erupt
in the near future.
• Extinct volcanoes refers to volcanoes without current
seismic activity
b. What phenomena are found at plate
boundaries and how are they formed?
Risks of living near volcanic areas
Some of the risks associated with living near volcanic
areas include:
• Destruction by volcanic materials
• Landslides
• Pollution
• Effects on weather
Volcanic eruptions
Destruction by volcanic materials
• Volcanic materials can lead to widespread damage of
property.
Volcanic eruptions
Some Volcanic Hazards
Volcanic Gases
Mudflows
Lava flow
Ash fall
Lightning strikes
Pyroclastic flows / surges
(high-density mixtures of hot, dry rock fragments
and hot gases that move away from the vent that
erupted them at high speeds)
Landslides
• Landslides can occur due to the structural collapse of a
volcanic cone.
• Obstruct the flow of rivers which causes floods,
• block roads, and
• bury villages and farmlands.
Volcanic eruptions
Pollution
• Ash particles may block sunlight, suffocate crops, and
cause severe respiratory problems for people and
animals.
• Release of gases may be harmful to people.
Volcanic eruptions
Volcanic eruptions
Eruption of Eyjafjallajokull affected jets.
http://mountaincatgeology.wordpress.com/2011/02/19/the-
2010-eruptions-ofeyjafjallajokull
Effects on weather
• Sulphur dioxide released from volcanic eruptions
has impacts on the environment
• It may react with water vapour and other
chemicals in the atmosphere to form sulphur-
based particles.
• These particles reflect the sun’s energy back into
space and temporarily cool the earth for periods
of time.
Volcanic eruptions
Benefits of living near volcanic areas
• Fertile volcanic soil
• Building materials, and precious stones and
materials
• Tourism
• Geothermal energy
Volcanic eruptions
Fertile volcanic soil
• Lava and ash from the volcanic eruptions break
down to form fertile volcanic soils.
• Favourable to agriculture
Volcanic eruptions
Precious stones and minerals, building materials
• Volcanic rocks can be rich in precious stones and
minerals.
• These resources can only be from a volcanic area
after millions of years.
• An example is diamond.
Volcanic eruptions
Tourism
• Volcanic areas offer a variety of activities for
tourists to engage in.
• The ruins of Pompeii, Italy, is one such example.
Volcanic eruptions
Pompeii was partially destroyed and buried under 4
to 6 m (13 to 20 ft) of ash and pumice in the
eruption of Mount Vesuvius in CE 79.
Volcanic eruptions
Geothermal energy
• Geothermal energy is derived from the heat in the
earth’s crust.
• The hot water or steam can be harnessed to produce
electricity.
Volcanic eruptions
CHAPTER 2 LIVING WITH
TECTONIC HAZARDS
Gateway 2: What landforms and associated
tectonic phenomena are found at plate
boundaries?
a. Why are different landforms found at different plate
boundaries and how are they formed?
b. What phenomena are found at plate boundaries and how are
they formed?
Practice Questions
• Describe the types of impacts of volcanic
eruptions. (6)
• Clue : How can you classify impacts?
Practice Questions
“The amount of damage and the number of
deaths is dependent on the strength of the
earthquake.” Discuss. (8)
•Clue 1 : What is the relationship between the
variables? Support
•high magnitude earthquakes vibrate and shake the
ground more violently, causes greater destruction
•Clue 2 : Is this relationship always the way it is?
•Clue 3 : Why not? Dependent on …
• reasons for exceptions:
– type of soil,
– level of preparedness (incl. education),
– distance from epicenter,
– earthquake resistance infrastructure,
– population density

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Geography Elective/Pure Chapter 2: Plate tectonic

  • 1. CHAPTER 2 LIVING WITH TECTONIC HAZARDS Risk or Opportunity?
  • 2. In this Chapter, you will explore three key questions: 1.Why are some areas more prone to tectonic hazards? 2.What landforms and associated tectonic phenomena are found at plate boundaries? 3.How do people prepare for and respond to earthquakes? CHAPTER 2 LIVING WITH TECTONIC HAZARDS
  • 3. CHAPTER 2 LIVING WITH TECTONIC HAZARDS Gateway 2: What landforms and associated tectonic phenomena are found at plate boundaries? The sea started to recede. I remember learning in a geography lesson that this happens before a tsunami. I shouted to tell everyone a tsunami was coming and for them to run! Quoted from a survivor of the tsunami that took place at Mai Khao Beach , Thailand on 26 December 2004.
  • 4. In December 2004, The Tsunami swamps Phuket's Chedi resort (AFP/Joanne Davis) Gateway 2: What landforms and associated tectonic phenomena are found at plate boundaries?
  • 5. After the tsunami, authorities have now installed signs along this coastline. • What symbols and words would you expect to see on these signs. Sketch the signs you expect to see at the beach. • Explain why you thought the signs are important.
  • 6. CHAPTER 2 LIVING WITH TECTONIC HAZARDS Gateway 2: What landforms and associated tectonic phenomena are found at plate boundaries? a.Why are different landforms found at different plate boundaries and how are they formed? b.What phenomena are found at plate boundaries and how are they formed?
  • 7. What could have happened here?
  • 8. Fold mountains • Over millions of years, the folding of rocks creates a landform called fold mountains. • The Himalayas, the Rocky Mountains and the Andes are examples of fold mountains.
  • 9. • Fold mountains are formed along convergent plate boundaries. • The compressional force causes the layers of rocks to buckle and fold. • This process is known as folding. Fold mountains
  • 10. • The upfold is called the anticline and • The downfold is the syncline. • When there is increasing compressional force on one limb of a fold, the rocks may buckle until a fracture forms. • The limb may then move forward to ride over the other limb Fold mountains
  • 11. Fold mountains The Himalayas Peak : Mount Everest (between Nepal and Tibet) Elevation : 8,848 metres
  • 12. • Fold mountains are located along convergent plate boundaries Describe the distribution of FM shown.
  • 13. What could have happened here? Describe what you see. [4]
  • 14. Rift valleys and block mountains • Rift valleys and block mountains are formed at divergent plate boundaries.
  • 15. • A fault is a fracture in the rocks along which the rocks are displaced. • The tensional forces result in parts of the crust being fractured. • This process is called faulting. Rift valleys and block mountains
  • 16. • A rift valley is a valley with steep sides formed along fault lines. • E.g. East African Rift Valley Rift valleys and block mountains
  • 17. • A block mountain is a block of land with steep sides. It is formed when sections of the crust extend along fault lines and rock masses surrounding a central block sink due to tensional forces. Rift valleys and block mountains
  • 18. Explain the formation of Block Mountains and Rift Valleys Divergent plate boundaries Parts of crust fractured in faulting Tensional Forces Pull apart Within a plate Between parallel faults Form rift valley Sections of crust extend along fault lines Tensional forces Central block of land subside However When tensional forces surround a block of land to subside Block mountain is form Between parallel fault cause land masses
  • 19. Explain the formation of Block Mountains and Rift Valleys Divergent plate boundaries 1 Parts of crust fractured in faulting 5 Tensional Forces 2 Pull apart 4 Within a plate 3 Between a pair of parallel faults To form a rift valley When Sections of crust extend along fault lines Tensional forces Can cause a Central block of land subside However when tensional forces surround a block of land to subside A block mountain is form Between parallel fault cause land masses
  • 20. Explain the formation of Block Mountains and Rift Valleys Divergent plate boundaries 1 Parts of crust fractured in faulting 5 Tensional Forces 2 Pull apart 4 Within a plate 3 Between a pair of parallel faults 4 To form a rift valley 5 When Sections of crust extend along fault lines 1 Tensional forces 2 Can cause a Central block of land subside 3 However when tensional forces surround a block of land to subside A block mountain is form Between parallel fault cause land masses
  • 21. Explain the formation of Block Mountains and Rift Valleys Divergent plate boundaries 1 Parts of crust fractured in faulting 5 Tensional Forces 2 Pull apart 4 Within a plate 3 Between a pair of parallel faults 4 To form a rift valley 5 When Sections of crust extend along fault lines 1 Tensional forces 2 Can cause a Central block of land subside 3 However when tensional forces 1 surrounding a block of land to subside 3 A block mountain is form 4 Between parallel fault 5 cause land masses 2
  • 22. Rift valleys and block mountains The East African Rift Valley Is formed from the Nubian section of the African Plate and the Somalian section of the African Plate pulling away from one another.
  • 23. • Describe the distribution of rift valleys and block mountains
  • 24. What could have happened here?
  • 25. Volcanoes • A volcano is a landform formed by magma ejected from the mantle onto the earth’s surface. Mount Saint Helens volcano before and after an eruption in May 1980
  • 26. • Magma is molten rock found below the earth’s surface. • Parts of a Volcano - magma chamber - vents • Magma that is ejected onto the surface is known as lava. Volcanoes
  • 27. Volcanoes Formation, structure of, and features of a volcano
  • 28. Shapes and sizes of volcanoes • Volcanoes vary in shapes and sizes due to the characteristics of the lava. • Viscosity refers to the stickiness of the lava • The most common types of volcanoes are: - Shield volcanoes; and - Stratovolcanoes Volcanoes
  • 29. Shield volcanoes • Shield volcanoes have gently sloping sides and a broad summit • The low silica lava flows easily and spreads over a large area before solidifying. • As lava do not trap much gas, eruptions are generally not explosive. • Successive eruption cause the base of the volcano to increase in size. Volcanoes E.g. Mount Washington, United States of America
  • 30. Why are shield volcanoes shaped with a broad based and gentle sloping sides?
  • 31. Stratovolcanoes • Stratovolcanoes develop from successive eruptions of lava and ash. • Initital explosion of pyroclastic flow because the high silica lava traps gases. • Followed by alternate layers of lava and pyroclastic flow again. • The lava prevents the pyroclasts from being eroded away. • Successive eruptions build high volcano. Volcanoes E.g. Mount Mayon, Philippines
  • 32. Compare between Shield and Stratovolcanoes Characteristics Shield Volcanoes Stratovolcanoes Shape Broad summit Broad base High volcano with slightly concave profile Height? x x RELIEF Gentle sloping sides Steeper at the top Gentler at the base Type of lava Low silica content Low viscosity High silica content High viscosity Type of eruption Gentle Explosive Frequency of eruption X X Where it occurs? Usually at Oceanic- Oceanic plate divergence Or at hotspots Usually at Continental- Oceanic plate convergence
  • 33. Volcanoes Distribution of earth’s major active volcanoes
  • 34. • An earthquake is a vibration in the earth’s crust caused by the sudden release of stored energy in the rocks found along fault lines. b. What phenomena are found at plate boundaries and how are they formed?
  • 35. • Measuring earthquakes - A seismograph records the seismic waves released by an earthquake. Earthquakes
  • 36. • Extent of earthquakes - The Richter Scale is used to measure the magnitude of an earthquake Earthquakes
  • 37. Ecuador Earthquake 17 April 2016 7.8 Ritcher Scale – 11.26 p.m. • http://www.mapsofworld.com/thematic-maps/earthquake/ecuador.html 1) What is the extent of the damage / impact of the the EQ? 2) How long do you think the aftershocks may last? 3) Why would Ecuador suffer a greater impact than compared to Taiwan?
  • 38. Date Ritcher Scale Death estimate Injured estimate 17 April (Sat) 7.8 272 2500 18 April 7.8 272 (am) 410 (pm) Over 2000 20 April 6.1 Over 2000 21 April 6.0 Over 2000
  • 39. Ecuador Earthquake 17 April 2016 7.8 Ritcher Scale – 11.26 p.m. • https://www.youtube.com/watch?v=bWzruH2KcR8 • Three Deadly Earthquakes Strike in 3 Days 1) Do you think there might be patterns involved in the movements of the plates?
  • 40. • Apart from its magnitude, the extent of damage caused by an earthquake may vary based on other factors: - Population density - time of occurrence - level of preparedness - distance from the epicentre - type of soil Earthquakes
  • 41. Describe distribution of the earth’s major earthquakes Earthquakes
  • 42. Hazards associated with living in earthquakes zones - Threat of tsunamis - Disruption of services - Fires - Landslides - Destruction of properties - Destruction of infrastructure - Loss of lives Earthquakes
  • 44. Threat of tsunamis • Tsunami refers to an usually large sea wave. • Tsunamis may be formed by: - The movement of the sea floor during a large earthquake at subduction zones; - An underwater volcanic eruption; - An underwater landslide; and - A landslide above sea level which causes materials to plunge into the water. Hazards associated with earthquakes
  • 45. Hazards associated with earthquakes
  • 46. • In 2004, a 9.2 magnitude triggered a tsunami with waves spreading throughout the Indian Ocean. Aceh before and after the tsunami hit the area Hazards associated with earthquakes
  • 47. The spread of the tsunami waves caused by the tsunami Hazards associated with earthquakes
  • 52. Disruption of services • An earthquake can disrupt services such as the supply of electricity, gas and water. • The earthquake in Kobe, Japan, in 1995 disrupted electricity, gas and water supplies to about a million of Kobe city’s 1.4 million residents. Hazards associated with earthquakes
  • 53. Fire • Earthquakes may rupture gas pipes and this can provide fuel to start fires. • For example, the earthquake in Kobe, Japan, in 1995 caused extensive fires. Hazards associated with earthquakes
  • 54. Landslides • Landslides are rapid downslope movements of soil, rock and vegetation. Mudflows may also occur when there is heavy rainfall. Hazards associated with earthquakes
  • 55. Destruction of properties • Earthquakes can cause destruction to many homes. • People may be without homes after the disaster. Hazards associated with earthquakes
  • 56. Destruction of infrastructure • Earthquakes may cause cracks to form in infrastructure such as roads and bridges. • Transportation can be disrupted as it is unsafe to use the damaged roads. Hazards associated with earthquakes
  • 57. Loss of lives • Earthquakes and their associated hazards often threaten the lives of those living in earthquake zones. Hazards associated with earthquakes
  • 58. Hazards associated with earthquakes
  • 59. Volcanic eruptions - Occurs on land occur on the sea floor. Active, dormant or extinct • Active volcanoes refers to volcanoes which are currently erupting or are expected to erupt in the future. • Dormant volcanoes are currently inactive but may erupt in the near future. • Extinct volcanoes refers to volcanoes without current seismic activity b. What phenomena are found at plate boundaries and how are they formed?
  • 60. Risks of living near volcanic areas Some of the risks associated with living near volcanic areas include: • Destruction by volcanic materials • Landslides • Pollution • Effects on weather Volcanic eruptions
  • 61. Destruction by volcanic materials • Volcanic materials can lead to widespread damage of property. Volcanic eruptions
  • 62. Some Volcanic Hazards Volcanic Gases Mudflows Lava flow Ash fall Lightning strikes Pyroclastic flows / surges (high-density mixtures of hot, dry rock fragments and hot gases that move away from the vent that erupted them at high speeds)
  • 63.
  • 64.
  • 65.
  • 66.
  • 67.
  • 68.
  • 69.
  • 70.
  • 71.
  • 72. Landslides • Landslides can occur due to the structural collapse of a volcanic cone. • Obstruct the flow of rivers which causes floods, • block roads, and • bury villages and farmlands. Volcanic eruptions
  • 73. Pollution • Ash particles may block sunlight, suffocate crops, and cause severe respiratory problems for people and animals. • Release of gases may be harmful to people. Volcanic eruptions
  • 74. Volcanic eruptions Eruption of Eyjafjallajokull affected jets. http://mountaincatgeology.wordpress.com/2011/02/19/the- 2010-eruptions-ofeyjafjallajokull
  • 75. Effects on weather • Sulphur dioxide released from volcanic eruptions has impacts on the environment • It may react with water vapour and other chemicals in the atmosphere to form sulphur- based particles. • These particles reflect the sun’s energy back into space and temporarily cool the earth for periods of time. Volcanic eruptions
  • 76. Benefits of living near volcanic areas • Fertile volcanic soil • Building materials, and precious stones and materials • Tourism • Geothermal energy Volcanic eruptions
  • 77. Fertile volcanic soil • Lava and ash from the volcanic eruptions break down to form fertile volcanic soils. • Favourable to agriculture Volcanic eruptions
  • 78. Precious stones and minerals, building materials • Volcanic rocks can be rich in precious stones and minerals. • These resources can only be from a volcanic area after millions of years. • An example is diamond. Volcanic eruptions
  • 79. Tourism • Volcanic areas offer a variety of activities for tourists to engage in. • The ruins of Pompeii, Italy, is one such example. Volcanic eruptions
  • 80. Pompeii was partially destroyed and buried under 4 to 6 m (13 to 20 ft) of ash and pumice in the eruption of Mount Vesuvius in CE 79. Volcanic eruptions
  • 81. Geothermal energy • Geothermal energy is derived from the heat in the earth’s crust. • The hot water or steam can be harnessed to produce electricity. Volcanic eruptions
  • 82. CHAPTER 2 LIVING WITH TECTONIC HAZARDS Gateway 2: What landforms and associated tectonic phenomena are found at plate boundaries? a. Why are different landforms found at different plate boundaries and how are they formed? b. What phenomena are found at plate boundaries and how are they formed?
  • 83. Practice Questions • Describe the types of impacts of volcanic eruptions. (6) • Clue : How can you classify impacts?
  • 84. Practice Questions “The amount of damage and the number of deaths is dependent on the strength of the earthquake.” Discuss. (8) •Clue 1 : What is the relationship between the variables? Support •high magnitude earthquakes vibrate and shake the ground more violently, causes greater destruction •Clue 2 : Is this relationship always the way it is? •Clue 3 : Why not? Dependent on …
  • 85. • reasons for exceptions: – type of soil, – level of preparedness (incl. education), – distance from epicenter, – earthquake resistance infrastructure, – population density