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What is a volcano? A point on the earths crust where magma forces - PowerPoint PPT Presentation

What is a volcano? A point on the earths crust where magma forces its way to the surface Ash and gases may also escape Where do they occur? On subduction zones On constructive plate boundaries On hot spots What types of


  1. What is a volcano? • A point on the earth’s crust where magma forces its way to the surface • Ash and gases may also escape

  2. Where do they occur? • On subduction zones • On constructive plate boundaries • On hot spots

  3. What types of volcanoes are there? Basa salti ltic c vo volc lcano anoes es Acid id vo volc lcano anoes es • Highly explosive • Less explosive* • Magma/lava is viscous • Magma/lava less viscous (thick) (runny) • Found where oceanic crust is • Found at rift zones (constructive boundaries) and hotspots subducted under continental crust * Continental hotspots are basaltic but potentially highly explosive

  4. Acid (rhyolitic) volcanoes Lava va dom omes Stratovo atovolcanoes lcanoes • Formed of layers of lava high in • Also called composite silica volcanoes • Lava is viscous and does not run • Formed of layers of lava and ashes very far • Lava is viscous • Rounded form • composed completely of lava • Distinct cone shape

  5. Example – lava dome • Mount St Helens - Washington state, USA befo fore re dur urin ing after ter

  6. Example - stratovolcano • Mount Pinatubo, Luzon, Philipines before During … after

  7. Other famous stratovolcanoes Fuji, dormant Vesuvius, active Kilamanjaro, Krakatoa, dormant active

  8. Location of stratovolcanoes • Along subduction zones • Often found in volcanic arcs* • E.g. Cascade range, USA

  9. Ba Basic sic (ba basalti saltic) c) vo volc lcanoes anoes  Also known as shield volcanoes  Formed of widespread layers of lava low in silica – low viscsity, lava travels very far  Low form spread over a great distance

  10. Exa Examp mple le – basi asic c vo volca lcano no • Eyjafjallajökull, Iceland

  11. Ex Exam ample 2 ple 2 • Kilauea, Hawaii

  12. Calderas • Collapsed volcanoes • Magma chamber has emptied and the ground has sunk • Often becomes a lake • New volcanoes can form, or pressure can build from below, lifting the ground • If acidic, this can cause a catastrophic eruption in the form of a ”super -volcano volcano ”

  13. Caldera - Santorini • Destroyed the Minoan civilization due to tsunamis circa 1600BC • May have given rise to the Atlantis myth

  14. Yellowstone national park

  15. Yellowstone is a hotspot

  16. Hotspots • Tectonic plate moves over a magma ”plume” • Occasionally erupts, creating a volcano • Hawaii – basic • Yellowstone - acid

  17. Volcanic hazards • Most hazards during eruptions are caused by what comes out of a volcano • In worst case scenarios then a volcano may violently explode

  18. Hazards – ash clouds • Slow moving • Weight of ash can collapse buildings • Destroys crops, pollutes water • Affects air traffic • Can enter high atmosphere and cause cooling – disrupting climate

  19. Hazards – lava bombs • Molten rocks thrown out of volcano • Pummice – smaller rocks • Travel short distances • Can start fires

  20. An acid volcano • Potential for violent eruptions • Slow moving lava • Explosions • Hot ash/cinders • Pyroclastic flows • Real danger!

  21. History of eruptions • 1800 BC – destruction of Bronze age settlements – then several more times • 79 AD – destruction of Pompeii • At least 40 times until the last eruption in 1944 – witnessed by allied troops towards the end of WWII • = once every 40-50 years

  22. Buried alive!

  23. Reducing the risks • Round-the-clock monitoring of the volcano – Tremors, gasses, changes in water • Identifying hazard areas – Weak spots, secondary vents, predicting routes of pyroclastic flows • Creating an evacuation plan – Zoning, warning systems, public education

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