Hazards 3 Volcanic Hazards

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Nature and Distribution:

  • Ocean Ridges:
    • Plates are moving apart and magma is moving to the surface
    • Gentle sloped sides because the basaltic lava has a low viscosity 
    • Eruptions are frequent but a relatively effusive
    • e.g. Eyjafjallajökull, Iceland, on the Mid-Atlantic Ridge
  • Subduction Zones:
    • e.g. the Ring Of Fire in the Pacific Ocean

Primary Impacts:

  • tephra: solid material of varying in grain size ranging from volcanic bombs to ash, all ejected into the atmosphere
  • Nuées ardentes: very hot, gas charged, high-velocity flows made up of a mixture of gas and tephra. These usually hug the ground and flow down the sides of a volcano
  • Lava flows
  • Volcanic gases: these include carbon dioxide, carbon monoxide, hydrogen sulphide, sulphur dioxide and chlorine

Secondary Effects:

  • Lahars: melted snow and ice as a result of the volcanic ash forms mud flows that can move down the course of the river valley at high speeds
  • Flooding: when an eruption melts glaciers and ice caps, serious flooding can occur
  • Volcanic landslides:
  • Tsunamis: sea wave generated by violent volcanic eruptions
  • Acid rain: volcanoes emit gases including sulphur, when this mixes with atmospheric moisture, acid rain can form
  • Climatic Change: the ejection of huge amounts of volcanic debris into the atmosphere can reduce global temperatures and is believed to have been an agent in past climatic

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