Not exact matches
However, the seismic
potential of crustal faults within the forearc of the northern Cascadia
subduction zone in British Columbia has remained elusive.
Therefore developing a better understanding of earthquake and tsunami behavior and
potential is a priority for local communities, for the wider Indian Ocean, and for related
subduction zones.»
This
subduction has created a collision
zone with the
potential to generate huge earthquakes and accompanying tsunamis, which happen when faulted rock abruptly shoves the ocean out of its way.
For example, the Caribbean coast of northern Colombia resembles a classic
subduction zone with the
potential for tsunamigenic M > 8 earthquakes at millennial time scales, but the absence of a large earthquake since 1492 is cause for complacency among local populations.
When experts talk about the
potential «Big One,» they mean a Cascadia
subduction zone earthquake.