Tsunami - What is it?
The word tsunami (pronounced soo-NAH-mee) is Japanese, and it means ‘harbour wave’.
A tsunami is a huge volume of moving seawater. These giant waves can travel for thousands of miles across the sea and still have enough energy and force to destroy buildings, trees, wildlife and people.
If you throw a stone in a pond it will create a series of ripples. A tsunami is just like those ripples but the disturbance that sets them moving is much greater than a small stone. It can be triggered by an undersea earthquake, landslide or volcanic eruption.
In deep water tsunami waves can extend thousands of feet into the sea, and reach speeds of 500mph, almost fast enough to keep up with a jet airplane. There can be up to a hundred miles between each wave, which may be just a few feet above the sea.
Japan Tsunami, 11 March 2011
This image shows sediment (light brown & green colour) left after the tsunami along the northeast coast of Sri Lanka. (Image courtesy of ESA, Envisat MERIS image dated 28 December 2004)
Most Tsunamis are caused by undersea earthquakes. These underwater earthquakes cause disruption to the seafloor and, in turn, the overlying water. A tsunami and has nothing to do with tides although it is sometimes mistakenly called a tidal wave.
How and where do these undersea earthquakes occur?
The earth is made up of several pieces of hard rock that fit together a bit like a jigsaw. These are called tectonic plates and they move very slowly. Oceanic plates are denser/heavier than continental plates and so they slide under the continental plates. Where this happens it is called a subduction zone. There are subduction zones off Chile, Nicaragua, Mexico and Indonesia. These areas are prone to earthquakes, which happen when the plates suddenly move against each other.
What other things could create a tsunami?
Sometimes when an ocean island collapses it causes a huge displacement of water which can also create a tsunami. Very rarely, a tsunami can be created by a giant meteor hitting the sea!
Scientists found traces of a huge meteor rock that collided with the Earth 3.5 billion years ago and landed in the sea, which may have created a giant tsunami that drastically changed coastlines and wiped out almost all life on land.
On Friday 11 March 2011 an underwater earthquake triggered a tsunami which hit Japan’s north-east coast. The earthquake was the most powerful ever recorded in Japan causing a 10 metre tsunami wave to hit the city of Sendai and further devastate several coastal communities. The death toll is still rising but is expected to exceed 10,000.
to read an article on the Japanese tsunami from YPTE's blog
Asian Tsunami in Sumatra, Indonesia - 26 December 2004
On 26th December 2004 a devastating tsunami hit Indonesia and affected several countries. The tsunami was caused by an underwater earthquake which measured 9.15 on the Richter scale. Amongst the affected countries was Somalia in Africa which is almost 3000 miles from the epicenter of the earthquake.
The initial tsunami waves took a little over 2 hours to reach the teardrop-shaped island of Sri Lanka. Additional waves continued to arrive for many hours afterward.
NASA's Terra satellite passed overhead capturing this image of deep sea tsunami waves about 30-40 kilometers from Sri Lanka's southwestern coast. The image covers an area of 129 miles x 128 miles. (Image courtesy of NASA Jet Propulsion Laboratory (NASA-JPL)
The Pacific Ocean experiences more tsunamis than anywhere else in the world. Tsunamis have also occurred in the Caribbean and Mediterranean Seas, and the Indian and Atlantic Oceans.
The December 2004 Asian tsunami is the deadliest in recorded history with a death toll of nearly 300,000. It was triggered by the fourth most powerful earthquake since 1900, estimated to measure 9.15 on the Richter scale.
Many people were killed by the Asian tsunami because they went down to the beach to see the exposed seafloor caused by the retreating of the sea. If you see the sea receding unusually quickly or far it’s a good sign that a big wave is on its way.
Before 2004 the most damaging tsunami on record was in 1782, following an earthquake in the South China Sea, which killed an estimated 40,000 people.
The Indian Ocean tsunami travelled as much as 3,000 miles to Africa and still had enough force to cause enormous destruction. For example, Somalia was hit harder than Bangladesh despite being much further away.
An earthquake off the coast of Chile in 1960 produced a tsunami that had enough force to kill 150 people in Japan after a journey of 22 hours and 10,000 miles.
In 1775, the Lisbon earthquake created a tsunami in the North Atlantic that killed as many as 60,000 people in Portugal, Spain and North Africa. This quake caused a tsunami as high as 23 feet in the Caribbean.
Another of the most deadly tsunamis in recorded history followed the eruption of the volcano Krakatoa in 1883, which destroyed the volcano completely and killed more than 36,500 people across the South Java Sea.
Sources of information:
Updated 14 March 2011 EB