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Restless Earth
                                What I should know…
       o   What oceanic and continental tectonic plate are and how and why are they
           different
       o   The different layers of the Earth’s interior and how they differ

       o   Why the asthenosphere is an important part of the mantle

       o   How convection in the mantle drives plate tectonic motion

       o   That there are different types of plate margins

       o   How new oceanic crust is subducted at destructive plate margins

       o   How earthquakes and volcanoes form at destructive plate margins

       o   Why earthquakes occur along conservative plate margins

       o   Why fold mountains form in collision zones

       o   How destructive collision zone earthquakes can be

       o   How to explain the global pattern of earthquakes and volcanoes

       o   How shield volcanoes and composite volcanoes form from different types of
           magma
       o   How hazards are measured using VEI, Richter and Mercalli scales

       o   The difference between primary and secondary impacts

       o   Detailed causes and impacts for two named volcanoes

       o   Detailed causes and impacts for two named earthquakes

       o   How earthquakes and volcanoes can be planned for and even predicted

       o   The different types of hazard response, both short and long term


                                             Key terms
Asthenosphere          Collision plate boundary     Conservative margin Long-term planning
Constructive margin Continental crust                Convection currents Magnitude
Core                   Destructive margin            Evacuation               Oceanic crust
Plate margin           Prediction                    Preparation              Response
Tectonic hazard        Short-term emergency relief

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Restless earth what I should know

  • 1. Restless Earth What I should know… o What oceanic and continental tectonic plate are and how and why are they different o The different layers of the Earth’s interior and how they differ o Why the asthenosphere is an important part of the mantle o How convection in the mantle drives plate tectonic motion o That there are different types of plate margins o How new oceanic crust is subducted at destructive plate margins o How earthquakes and volcanoes form at destructive plate margins o Why earthquakes occur along conservative plate margins o Why fold mountains form in collision zones o How destructive collision zone earthquakes can be o How to explain the global pattern of earthquakes and volcanoes o How shield volcanoes and composite volcanoes form from different types of magma o How hazards are measured using VEI, Richter and Mercalli scales o The difference between primary and secondary impacts o Detailed causes and impacts for two named volcanoes o Detailed causes and impacts for two named earthquakes o How earthquakes and volcanoes can be planned for and even predicted o The different types of hazard response, both short and long term Key terms Asthenosphere Collision plate boundary Conservative margin Long-term planning Constructive margin Continental crust Convection currents Magnitude Core Destructive margin Evacuation Oceanic crust Plate margin Prediction Preparation Response Tectonic hazard Short-term emergency relief