Yes, <b><span style="color:cyan">sloracer</span></b>, I saw the same program. The islands were the Canary Islands. However, the scientists asked about it were divided, some cited that landslide-induced tsunami are much more localized events and would not be transoceanic.<br /><br />I want to thank everyone who took time to answer my question, particularly <span style="color:red"><b>meteo</b></span>, whose answers were superb.<br /><br />I'd have to agree with him, that it's more reasonable to think of it using the Skater model. Suppose the plate on top were to jut upward by 1 mile (I know it was probably only feet, which is why the change is so miniscule), and the plate subducted thrust 1 mile deep. That's like increasing the Earth's diameter by a mile at that point, and it is like extending an arm (it may be easier to visualize by thinking of the movement in terms of a larger distance, like miles ... if a mountain shot up out of the water 15,000 feet high.. it's <i>like an arm</i>).<br /><br />There would be no counter-acting force from the Mid--Atlantic Ridge, <b>maddad</b>. The subducted rock would push more rock into the mantle, where it would liquefy, and circulate along the currents and eddies deep within the Earth. But the mantle circulates very slowly. So the time until some counter-acting event happens could be considerable.<br /><br />I guess I also disagree that taken over a long enough period of time (if you take enough samples, as <b><span style="color:cyan">maddad</span></b> suggests), the effect must cancel itself out. Hasn't the Earth's rotation slowed down over the past several billion years? Can this effect be solely due to mass being added to the Earth by meteorites?<br /><br />Nobody really knows what's floating around deep within the Earth. I don't think there's any finding that the Mantle and Core must be made up of a distribution of materials with homogeneous density. Heavy elements could congregate and bob and weave and flow around, clos