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VIOLENT VOLCANOES…
What is a volcano?

  A volcano is an opening or vent in the earth’s surface
  through which molten material erupts and solidifies as lava.




                                        Volcanic vent




http://www.youtube.com/watch?v=NBPwwt0HuVo&feature=fvst
Label this cross section of a volcano


                                        Volcanic
         Crater                         bombs, ash,
                                        lava, gases



                                             Parasitic
                                             cone
   Main vent
                                         •Volcanic bombs,
                                         ash, lava, gases
                                         •Magma chamber
                                         •Parasitic cone
   Magma                                 •Crater
   chamber
                                         •Main vent
What comes out of a volcano?
Do all volcanoes erupt?
    Active volcano – liable to erupt
    e.g. Mt Etna & Mt. Merapi in
    Indonesia.
    Dormant (sleeping) volcano – a
    volcano which has not erupted for
    many years. For example, Mt
    Pinatubo erupted in 1991 after 500
    years of dormancy.
     Extinct volcano – a volcano which
     has not erupted for many
     thousands or millions of years e.g.
     Edinburgh.      http://www.bbc.co.uk/learningzone/clips/volcanic-scotland/9116.html



  However, it is often very difficult to tell whether a volcano
  will erupt again…El Chichon, Mexico erupted in 1982
  after being dormant for approximately 1200 years!
Why do they happen?
Can you remember what is happening to the plates at a
CONSTRUCTIVE plate boundary?


The two plates are moving apart…


What comes up through the gap created in the crust?
A volcano….
Volcanoes at constructive plate boundaries don’t tend to be very
spectacular or explosive. As the crust moves apart for the
magma it is easily able to escape and just trickles out the top.
The lava here tends to be runny and flows some distance from
the crater before it solidifies. So, these volcanoes tend to be
shallow sided, or SHIELD volcanoes.
Volcanoes also form at DESTRUCTIVE plate boundaries.
 Where one plate is forced down under the other (called subduction).




What happens to the crust that is forced down into the mantle?

It melts…

What does this create?

Excess magma…

What do you think happens to this extra magma?

Pressure builds and eventually there is a violent, explosive, volcanic eruption!

Volcanoes at destructive plate boundaries tend to be very explosive! The lava is thick
and so does not flow far from the crater. These volcanoes build up layers with each
eruption. These are called   COMPOSITE volcanoes.
Example of a shield volcano- Mauna
Kea, Hawaii
Example of a composite volcano- Mt.
Merapi – Indonesia
Where in the world are volcanoes found?




       Around which plate do we find most volcanoes?
Where do Earthquakes and volcanoes form?




The ‘ring of
fire’ is an
area around
the Pacific
Ocean, prone
to                 A map to show the
earthquakes                              Ring of fire
                 spread of Earthquakes
and               and volcanoes around
volcanoes              the earth
The Ring of Fire
Hawaii
 The Hawaiian islands are a chain
 of volcanoes in the Pacific Ocean.
 Look at their location on the map below.
 Why is this an unusual place for them to
 be located?
Hot spot volcanoes




  In the animation above, why are the volcanoes to the left of
  the ‘hot spot’ extinct?
HOT SPOT volcanoes are found in the middle of a plate.
Here the crust is weaker than usual. There is a plume of hot magma rising from
the mantle and it is able to push through the crust at this point.
The plate moves across this ‘hotspot’ forming a chain of volcanoes over millions
of years e.g. Hawaii.
Your tasks:
•    You have one side of A3 paper on which to
     produce a ‘fact sheet’ about volcanoes. You
     need to include:
1.   Completed ‘pop-up’ volcano.
2.   An explanation as to how volcanoes form. Try
     to include information about both constructive
     and destructive plate boundaries and what the
     different volcanoes are known as (shield and
     composite).
3.   An explanation as to what is meant by active,
     dormant and extinct volcanoes.
4.   An explanation of ‘hot-spot’ volcanoes.
Lesson 2 volcanoes

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Lesson 2 volcanoes

  • 2. What is a volcano? A volcano is an opening or vent in the earth’s surface through which molten material erupts and solidifies as lava. Volcanic vent http://www.youtube.com/watch?v=NBPwwt0HuVo&feature=fvst
  • 3.
  • 4. Label this cross section of a volcano Volcanic Crater bombs, ash, lava, gases Parasitic cone Main vent •Volcanic bombs, ash, lava, gases •Magma chamber •Parasitic cone Magma •Crater chamber •Main vent
  • 5. What comes out of a volcano?
  • 6. Do all volcanoes erupt? Active volcano – liable to erupt e.g. Mt Etna & Mt. Merapi in Indonesia. Dormant (sleeping) volcano – a volcano which has not erupted for many years. For example, Mt Pinatubo erupted in 1991 after 500 years of dormancy. Extinct volcano – a volcano which has not erupted for many thousands or millions of years e.g. Edinburgh. http://www.bbc.co.uk/learningzone/clips/volcanic-scotland/9116.html However, it is often very difficult to tell whether a volcano will erupt again…El Chichon, Mexico erupted in 1982 after being dormant for approximately 1200 years!
  • 7. Why do they happen? Can you remember what is happening to the plates at a CONSTRUCTIVE plate boundary? The two plates are moving apart… What comes up through the gap created in the crust? A volcano…. Volcanoes at constructive plate boundaries don’t tend to be very spectacular or explosive. As the crust moves apart for the magma it is easily able to escape and just trickles out the top. The lava here tends to be runny and flows some distance from the crater before it solidifies. So, these volcanoes tend to be shallow sided, or SHIELD volcanoes.
  • 8. Volcanoes also form at DESTRUCTIVE plate boundaries. Where one plate is forced down under the other (called subduction). What happens to the crust that is forced down into the mantle? It melts… What does this create? Excess magma… What do you think happens to this extra magma? Pressure builds and eventually there is a violent, explosive, volcanic eruption! Volcanoes at destructive plate boundaries tend to be very explosive! The lava is thick and so does not flow far from the crater. These volcanoes build up layers with each eruption. These are called COMPOSITE volcanoes.
  • 9. Example of a shield volcano- Mauna Kea, Hawaii
  • 10. Example of a composite volcano- Mt. Merapi – Indonesia
  • 11. Where in the world are volcanoes found? Around which plate do we find most volcanoes?
  • 12. Where do Earthquakes and volcanoes form? The ‘ring of fire’ is an area around the Pacific Ocean, prone to A map to show the earthquakes Ring of fire spread of Earthquakes and and volcanoes around volcanoes the earth
  • 13. The Ring of Fire
  • 14. Hawaii The Hawaiian islands are a chain of volcanoes in the Pacific Ocean. Look at their location on the map below. Why is this an unusual place for them to be located?
  • 15. Hot spot volcanoes In the animation above, why are the volcanoes to the left of the ‘hot spot’ extinct?
  • 16. HOT SPOT volcanoes are found in the middle of a plate. Here the crust is weaker than usual. There is a plume of hot magma rising from the mantle and it is able to push through the crust at this point. The plate moves across this ‘hotspot’ forming a chain of volcanoes over millions of years e.g. Hawaii.
  • 17.
  • 18.
  • 19. Your tasks: • You have one side of A3 paper on which to produce a ‘fact sheet’ about volcanoes. You need to include: 1. Completed ‘pop-up’ volcano. 2. An explanation as to how volcanoes form. Try to include information about both constructive and destructive plate boundaries and what the different volcanoes are known as (shield and composite). 3. An explanation as to what is meant by active, dormant and extinct volcanoes. 4. An explanation of ‘hot-spot’ volcanoes.

Hinweis der Redaktion

  1. This ‘conveyor belt’ animation is a simplified version of the formation of hot spot volcanoes/ chains of islands. Internet Links – US Geological Survey Hawaiian volcanoes http://hvo.wr.usgs.gov/ While all care is taken to ensure web links contain useful information, Boardworks does not take responsibility for the content or accuracy of external web sites.