Thursday, August 12, 2004

SCIENCE

Daily Express: A Wave of Destruction Will Destroy America's East Coast

Around this time of the year many Britons look towards the Canary Islands for a sunshine break. What most don't know, however, is that on one of the Canary Islands lies a major global catastrophe in the making, a natural disaster so big that it could flatten the Atlantic coastlines of Britain, Europe, North Africa and the United States of America and cause enormous damage to London and other UK cities.

Recently, scientists have realised that the next Mega Tsunami is likely to begin on one of the Canary Islands

Dr. Day says: "If the volcano collapsed in one block of almost 20 cubic kilometres of rock, weighing 500 billion tonnes - twice the size of the Isle of Wight - it would fall into water almost 4 miles deep and create an undersea wave 2000 feet tall. Within five minutes of the landslide, a dome of water about a mile high would form and then collapse, before the Mega Tsunami fanned out in every direction, travelling at speeds of up to 500 mph. A 330ft wave would strike the western Sahara in less than an hour."

Guardian: Tidal Wave Disaster Just
Waiting To Happen


It has everything you could wish for in a cliche-ridden disaster movie. A beautiful volcanic island in the Atlantic is on the brink of catastrophic collapse, threatening to unleash giant waves that will wreak havoc around the globe within hours. And while scientists try in vain to make their concerns heard, the world's governments look the other way.

But yesterday a leading expert claimed the doom-laden scenario was not only real but was being almost completely ignored by people in power.

When - Professor McGuire says it is not a matter of if - the rock plunges into the ocean it will trigger giant waves called mega-tsunamis.

Travelling at speeds of up to 560mph, the huge walls of water will tear across the ocean and hit islands and continents, leaving a trail of destruction.

Mega-tsunami waves are much longer than the ones we are used to.



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