Japan 10th Anniversary of 2011 Earthquake—Lessons learned from seismogeodesy

10min 31s Novice

How can we improve earthquake and tsunami warnings?

The March 11, 2011 earthquake and tsunami was a tragedy.  Research carried out since that earthquake happened has revealed ways in which earthquake and tsunami alerts can be sent much more quickly, by understanding how energy is stored between plates in a subduction zone, and how that energy is released.


Lessons from the 2011 Tohoku-oki earthquake are being applied to earthquake and tsunami warning systems worldwide.


Scientific lessons learned and described here include:

Scientific lessons learned and described here include:

  • Tsunami geology can extend the earthquake record by centuries or millenia.
  • Earthquake Early Warning can mitigate damage and save lives, but the 2011earthquake revealed limitations of a system using only seismometers.
  • Adding Global Positioning System observations of earthquake ground motion improves accuracy of earthquake early warning, and is essential to tsunami warnings.

Related Animations

Japan has more measurable earthquakes than any other country and has over 100 active volcanoes. These both result from Japan being wedged among four major tectonic plates. The tectonics are complicated, but in this animation we attempt to look at the basic mechanics of the region. We focus on two famous earthquakes: the 1995 Kobe (Great Hanshin) earthquake and the 2011 Tohoku Oki earthquake.

Animation Novice

Subduction-zone megathrust earthquakes, the most powerful earthquakes in the world, can produce tsunamis through a variety of structures that are missed by simple models including: fault boundary rupture, deformation of overlying plate, splay faults and landslides. From a hazards viewpoint, it is critical to remember that tsunamis are multiple waves that often arrive on shore for many hours after the initial wave.

Animation Novice