As prescribed by Paulina Constancia
ALL ABOUT TSUNAMIS
Info from National Geographic
What is a TSUNAMI? A tsunami is a series of ocean waves that sends surges of water, sometimes reaching heights of over 100 feet (30.5 meters), onto land. These walls of water can cause widespread destruction when they crash ashore.
What causes a TSUNAMI? These awe-inspiring waves are typically caused by large, undersea earthquakes at tectonic plate boundaries. When the ocean floor at a plate boundary rises or falls suddenly it displaces the water above it and launches the rolling waves that will become a tsunami.
Where do most Tsunamis happen? Most tsunamis, about 80 percent, happen within the Pacific Ocean’s “Ring of Fire,” a geologically active area where tectonic shifts make volcanoes and earthquakes common.
What else can trigger a TSUNAMI? Tsunamis may also be caused by underwater landslides or volcanic eruptions. They may even be launched, as they frequently were in Earth’s ancient past, by the impact of a large meteorite plunging into an ocean.
How fast do TSUNAMIS go? Tsunamis race across the sea at up to 500 miles (805 kilometers) an hour—about as fast as a jet airplane. At that pace they can cross the entire expanse of the Pacific Ocean in less than a day. And their long wavelengths mean they lose very little energy along the way.
Describe the appearance of TSUNAMIS. In deep ocean, tsunami waves may appear only a foot or so high. But as they approach shoreline and enter shallower water they slow down and begin to grow in energy and height. The tops of the waves move faster than their bottoms do, which causes them to rise precipitously.
Describe the nature of TSUNAMIS. A tsunami’s trough, the low point beneath the wave’s crest, often reaches shore first. When it does, it produces a vacuum effect that sucks coastal water seaward and exposes harbor and sea floors. This retreating of sea water is an important warning sign of a tsunami, because the wave’s crest and its enormous volume of water typically hit shore five minutes or so later. Recognizing this phenomenon can save lives.
Is a TSUNAMI made up of only one wave? No. A tsunami is usually composed of a series of waves, called a wave train, so its destructive force may be compounded as successive waves reach shore. People experiencing a tsunami should remember that the danger may not have passed with the first wave and should await official word that it is safe to return to vulnerable locations.
Are TSUNAMIS always large towering waves? No. Some tsunamis do not appear on shore as massive breaking waves but instead resemble a quickly surging tide that inundates coastal areas.
What’s the best defense against a TSUNAMI? The best defense against any tsunami is early warning that allows people to seek higher ground. The Pacific Tsunami Warning System, a coalition of 26 nations headquartered in Hawaii, maintains a web of seismic equipment and water level gauges to identify tsunamis at sea. Similar systems are proposed to protect coastal areas worldwide.
|Image from decodedscience|
Although there is no absolute size rule, an underwater earthquake of around M7.0 might be considered capable of producing the required displacement. And an M7.0 earthquake is very large – ten times the size of an M6.0 and 100 times the size of an M5.0 (the earthquake scale is logarithmic).
Large earthquakes, however, do not always generate tsunamis – for example, an M8.6 off Sumatra in 2005 caused a 3m tsunami which killed over 1300 people, while another in the same region and of the same magnitude in 2012 generated no tsunami. Although both occurred in deep water (another necessary condition), they were characterised by different types of earth movement. The first involved sudden vertical movement over a long area of a fault: the second involved lateral (strike-slip) faulting within a tectonic plate.
In summary, then, it’s clear that not all earthquakes generate tsunamis. The International Tsunami Warning Center identifies the main causes of tsunamis as “large, shallow earthquakes with an epicentre or fault line near or on the ocean floor.” So a small earthquake, even if it fulfills all the other conditions, will not generate a major tsunami – and, in reality, such major disasters are mercifully few and far between. Read more…
Read about the 10 Most Destructive TSUNAMIS in History on Australian Geographic, List of Historic Tsunamis on Wikipedia, History’s Biggest Tsunamis on LiveScience
Here are a few educational videos to help you better understand TSUNAMIS.
Please choose the appropriate one for you (or your audience).
1. What is a Tsunami? Educational video for Kids
by Mocomi Kids
I have also attached a video of the 3.11.2011 TOHOKU Earthquake & Tsunami in Japan. It’s a 5-Part Feature, so if you wish to continue watching please click the succeeding links.
Japan’s Tsunami: How it happened – Part 1 of 5
Please click on the links below to continue watching…
(Part 2 of 5)
( Part 3of 5)
( Part 4of 5)
(Part 5of 5)
Many countries and agencies have developed their teaching/learning resources on the topic of earthquakes and TSUNAMIS. Here are some that I have gathered for you:
From The Caribbean, Emergency Management BC(Canada), Australia, Discovery Education, Red Cross, IRIS , USGS, NY Times…