The Energy of the Christchurch Earthquake and the Slapdown Effect

Sdílet
Vložit
  • čas přidán 13. 03. 2011
  • GNS Science seismologist Dr Martin Reyners explains why this earthquake was so damaging for its comparatively low magnitude
  • Věda a technologie

Komentáře • 7

  • @FortitudoDei
    @FortitudoDei Před 13 lety +2

    Great explanation - one of the best I've heard.

  • @maurasmith-mitsky762
    @maurasmith-mitsky762 Před měsícem

    Wonderful video. I had never heard of the slap down effect.

    • @Kiwigeo8339
      @Kiwigeo8339 Před měsícem

      In this article there's a photo that was taken of the CBD during the quake which shows rising dust plumes due to the "slapdown effect"...also called a "trampoline effect".
      nzhistory.govt.nz/culture/february-2011-christchurch-earthquake

  • @richardpope3063
    @richardpope3063 Před 3 lety

    @5.24 the script doesn't correspond to what GNS speaker said. Script 'the ground was...' the GNS speaker said the ground wasn't...'

  • @roastedpeas
    @roastedpeas Před 13 lety

    cheers ,is Christchurch now going to be more "earthquake active" or will it go back to a shake now and then ?

  • @notwowe
    @notwowe Před 12 lety

    Convection currents within the earth's mantle. If you've learnt physics, The hotter magma near the core rises up and then cools down, which moves to the side before sinking. Whichever direction the magma goes before cooling will affect the direction of the plate's direction.

    • @Kiwigeo8339
      @Kiwigeo8339 Před měsícem

      Mantle convection currents are only one of three drivers of plate tectonic movement. The other two are plate push at spreading ridge systems and plate pull down at subduction zones.