@littlek,
Quote:And the waves bounce back and forth on the various landmasses?
Yes, the site of the event probably caused an underwater ripple just like a pebble going into a pond, but much larger of course.
The ripples (quite sizable) radiated out in a spherical form as you would expect, but where they entered the channels they were compressed and amplified as they approached the shore. I think this is how the Bay of Funde works as well, except that it's an amplification of the standard tidal cycle because it's a much larger channel.
Based on where the events were reported you can kind of imagine where the source must have been, and about how large it must have been.