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3.4.1.4  Tectonic processes  Volcanic hazards
Syllabus… ,[object Object],[object Object],[object Object],[object Object]
References ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Volcanic activity – What you already know ,[object Object],[object Object],Animated guide: Volcanoes
Syllabus details: Relate the distribution and nature of volcanic activity to plate margins and hot spots.  Identify the types of eruption and volcanic forms as basic, acid, fissure and composite.  Identify primary hazards (such as ash, lava, directed blast, nuée ardente and pyroclastic flows) and secondary hazards (such as landslides, lahars (mudflows) and atmospheric impacts).
terminology ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Relate the distribution and nature of volcanic activity to plate margins and hot spots
[object Object],[object Object],[object Object]
The shape of a volcano depends on the: ,[object Object],[object Object],[object Object]
[object Object],Constructive plate boundaries 73% of magma which reaches the earth’s surface occurs along these boundaries.  The main areas are the mid ocean ridges where melting of the upper mantle produces basaltic magma.  The eruptions tend to be  non-violent (=effusive)  and as most occur on the sea floor they do not represent a major hazard to people except where portions of ocean ridge emerge above sea level to form inhabited islands such as  Iceland Continental constructive boundaries occur where continental crust is being moved apart e.g. the  East African rift valley  system.
 
[object Object],Destructive plate boundaries 80% of the world’s active volcanoes occur along destructive boundaries.  As the oceanic plate descends into the mantle and melts basic magma rises upwards and mixes with continental crust to produce  magma with a higher silica content  than along the oceanic ridges (Mt Cotopaxi – Ecuador).  These  andesitic and rhyolitic magmas result in violent activity .  Volcanic island arcs (Japan – Mt Fujiyama, Mt Unzen) form where two oceanic plates are colliding the resulting volcanic activity is of andestitic magmas.
 
Hot spots  Hotspots are small areas of the crust with an  unusually high heat flow  and are found  away from plate boundaries .  Slowly rising mantle rocks create volcanic activity on the surface.  The movement of the lithospheric plates over the hot spot produces a  chain  of what are mainly  now extinct volcanoes .  Examples of hot spots are  Hawaiian Islands , Maldives, Azores.  Eruptions are normally of  low viscosity basaltic magmas, effusive eruptions
Identify the types of eruption and volcanic forms as basic, acid, fissure and composite ,[object Object]
How can volcanoes be classified: 1. Shape ,[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
[object Object],[object Object],[object Object],[object Object],[object Object]
The nature of the eruption ,[object Object],[object Object]
Why volcanoes explode
[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Ref Waugh pg 28
Summary table:
Tasks: ,[object Object],[object Object],[object Object]
Identify primary hazards and secondary hazards ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Lava flows ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Pyroclastic flows and surges = nuees ardentes   ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
 
Ash and tephra fall ,[object Object],[object Object],[object Object],[object Object]
The largest fragment is about 5 mm in diameter. Tephra between 2 and 64 mm in diamter is called lapilli; tephra <2 mm in diamter is called ash.
Volcanic gases ,[object Object],[object Object]
 
Secondary  volcanic hazards. ,[object Object],[object Object],[object Object],Identify secondary volcanic hazards pg 68  - 70
Lahars ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Early war n ing for volcanic mudslides Deadly mudslide at Ecuador volcano Mount Pinatubo: Lahars could devastate the surrounding country
Mud slide fears over Mexico volcano
landslides ,[object Object],[object Object],[object Object],[object Object]
tsunami
Nevado del Ruiz Volcano, Colombia, 1985  USGS website
Tasks ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
references ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Case studies ,[object Object],[object Object],[object Object],[object Object]

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  • 1. 3.4.1.4 Tectonic processes Volcanic hazards
  • 2.
  • 3.
  • 4.
  • 5. Syllabus details: Relate the distribution and nature of volcanic activity to plate margins and hot spots. Identify the types of eruption and volcanic forms as basic, acid, fissure and composite. Identify primary hazards (such as ash, lava, directed blast, nuée ardente and pyroclastic flows) and secondary hazards (such as landslides, lahars (mudflows) and atmospheric impacts).
  • 6.
  • 7. Relate the distribution and nature of volcanic activity to plate margins and hot spots
  • 8.
  • 9.
  • 10.
  • 11.  
  • 12.
  • 13.  
  • 14. Hot spots Hotspots are small areas of the crust with an unusually high heat flow and are found away from plate boundaries . Slowly rising mantle rocks create volcanic activity on the surface. The movement of the lithospheric plates over the hot spot produces a chain of what are mainly now extinct volcanoes . Examples of hot spots are Hawaiian Islands , Maldives, Azores. Eruptions are normally of low viscosity basaltic magmas, effusive eruptions
  • 15.
  • 16.
  • 17.
  • 18.
  • 19.
  • 21.
  • 23.
  • 24.
  • 25.
  • 26.
  • 27.  
  • 28.
  • 29. The largest fragment is about 5 mm in diameter. Tephra between 2 and 64 mm in diamter is called lapilli; tephra <2 mm in diamter is called ash.
  • 30.
  • 31.  
  • 32.
  • 33.
  • 34. Mud slide fears over Mexico volcano
  • 35.
  • 37. Nevado del Ruiz Volcano, Colombia, 1985 USGS website
  • 38.
  • 39.
  • 40.