The Energy of the Christchurch Earthquake and the Slapdown Effect

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  • เผยแพร่เมื่อ 15 ต.ค. 2024
  • GNS Science seismologist Dr Martin Reyners explains why this earthquake was so damaging for its comparatively low magnitude

ความคิดเห็น • 7

  • @FortitudoDei
    @FortitudoDei 13 ปีที่แล้ว +2

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

  • @maurasmith-mitsky762
    @maurasmith-mitsky762 4 หลายเดือนก่อน

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

    • @Kiwigeo8339
      @Kiwigeo8339 3 หลายเดือนก่อน

      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

  • @roastedpeas
    @roastedpeas 13 ปีที่แล้ว

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

  • @richardpope3063
    @richardpope3063 3 ปีที่แล้ว

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

  • @notwowe
    @notwowe 12 ปีที่แล้ว

    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 3 หลายเดือนก่อน

      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.