Tectonic hazards

Subdecks (1)

Cards (38)

  • Atmospheric hazards are driven by processes at work in the atmosphere eg: air
  • Inner core
    • mostly solid
    • made of iron and nickel
    • slowly growing
  • Continental crust
    • granite rocks
    • known as sial layer as well
    • over 1500 million years old
    • subducts the oceanic crust
  • Primoridial is the heat left over from the Earth’s formation
  • Radiogenic is the heat produced from radioactive decay of isotopes
  • Ridge push is when new crust is formed due to tension forces.
    • mantle rock rises and experiences a reduction in pressure
  • Father of plate tectonic theory is Alfred Wegner
  • Harry Hess updated the plate tectonic theory in 1962
  • Constructive plate boundary
    • plates moving away from each other
    • both plates are either oceanic or continental
    • magma rises - filling the void and creating new crust
    • basaltic lava fills the gap
    • oceanic ridges made
  • Oceanic ridges:
    • formed from the basaltic lava that comes up
    • ridges can have breaks in them called transform faults
    • these ridges and faults wider at different rates meaning there will be frictional stress causing earthquakes
    • higher than other area - it is buoyant
  • Collision plate boundary
    • usually continental and continental
    • crusts need to be the same density
    • two plates collide and crumple upwards
    • forms fold mountains eg: Himalayas
  • A magma plume is extremely hot magma that breaks through the oceanic crust and and cools to form a small volcano
    • the volcano gets bigger over time
    • it later becomes extinct as the plates moves
    • the volcano moves off the plate boundary and the hot spot
  • Extinct volcanoes sink as they become heavy and they also become smaller due to erosion
  • Tephra
    • fragments of volcanic rock and lava thrown into the air
  • Crater
    • main opening of the volcano
  • Pyroclastic flow (speeds of 50mph)
    • rock fragments, gases and ash which destroys everything in its path
  • Andesitic lava:
    • viscous
    • high silica content
    • cooler
    • loses gas quickly
  • Caldera volcanoes: (shield)
    • large circular/oval depressions
    • some filled with lakes
    • often surrounded by steep cliffs
    • formed by the inward collapse of a volcano
  • Vulcanian volcanoes: (composite)
    • thick lava, basaltic/andesitic/rhyolitic
    • less frequent, violent eruptions of gases
  • Vesuvian volcanoes: (composite)
    • thick lava, basaltic/andesitic/rhyolitic
    • long periods of inactivity
    • very violet has explosions
  • Peléan volanoes: (composite)
    • andesiitic and rhyolitic
    • violent eruptions
  • Plinian volcanoes: (composite)
    • rhyolitic - viscous, tend to form thick blocky lava flows
    • violent
    • erupt gas, ash and pumice
    • rainstorms cause lahars
  • Evidence for continetal drift:
    • if the continents were pieced together, they would fit almost perfectly
    • fossil remains - identically evolved repitle fossils found in both South America and Africa
    • coal found in Antartica - coal needs tropical climates and dense vegetation
  • Hawaiian volcanoes: (shield)
    • non-explosive eruptions
    • generate red hot lava rivers - basaltic lava
    • sloping mountains