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Cause and effect of tsunamis
The cause and effect of tsunami
Physics of tsunami
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What are Tsunamis?
Tsunamis (pronounciation: soo-ná-mees), are a progression or series of huge and gigantic waves formed by underwater disturbances such as • Landslides
• Earthquakes
• Volcanic eruptions
• Meteorites Tsunamis are also called “Seismic sea waves.” A tsunami can move hundreds of miles per hour in the open sea and crash into the land with waves as high as 100 feet or more.
The Word
The word “Tsunami” has been derived from the Japanese language meaning “harbor wave,” due to the devastating effects these waves have had on low-lying Japanese coastal communities.
Speed of Tsunamis
The speed of tsunami waves relies upon ocean depth rather than the distance from the source of the wave. Tsunami waves may travel as fast as jet planes over profound waters, only slowing down when reaching shallow waters.
Size of Tsunamis
From the region where the tsunami forms, waves travel outward in all directions. Once the wave approaches the shore, it builds in height. The geography of the coastline and the ocean floor affects the size of the wave.
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What damage can tsunamis do?
The impact of a tsunami is usually limited to coastal areas but the destruction could be immense. Buildings and anything in the path of the waves is in danger of being destroyed and washed away, such is the force of the wave. The 2004 Indian Ocean earthquake and tsunami, which struck off the west coast of Indonesia with a magnitude of 9.1-9.3, left 250,000 people killed or missing in 14 different countries including Indonesia, Sri Lanka, India and Thailand.
More Tsunamis in the Pacific than the Atlantic Ocean
Tsunamis occur more frequently in the Pacific Ocean as compared to the Atlantic Ocean. The main reason behind this is the “Ring of Fire.”
The Ring of
Earthquakes, by Webster’s dictionary definition, are, “a shaking or trembling of the earth that is volcanic or tectonic in origin.” World Book Encyclopedia reports scientists believe that more than 8,000 earthquakes occur each day without causing damage. A little more than 1,000 each year are strong enough to be felt. Earthquakes occur in the general sense, anywhere on land. Other earthquakes go by different names, such as volcanic eruptions and tsunamis, large tidal wave storms that occur underwater, primarily in the Pacific Ocean.
Imagine if a 9.0 earthquake struck the West Coast today, resulting in a giant tsunami. Coastal towns would be washed away or completely isolated, and electricity would be lost (FOX5). There would be $70 billion in damage and people would only have 15 minutest to evacuate or move to higher ground resulting in 10,000 deaths (FOX5). This sounds like a plot for a scary movie, but this is actually a reality. The Oregon Coast in located on a subduction zone, which makes it very susceptible to major earthquakes and tsunamis. With the Cascadia subduction zone running along he West Coast the threat of a major tsunami is very real.
Tsunamis can go the same speed as a jetliner and that massive wave can out run the fastest runner. When there is a lot of waves at once, or the water goes back that is a sign that a tsunami is coming. If that tsunami is far then people need to get to the tallest and strongest building there is in the city that way they are safe and helicopter can pick them up. Tsunamis can wipe out an entire city or 1/4 of the country. Tsunamis can last up to an hour, or more.
A tsunami is a series of waves “created by an underwater disturbance such as an earthquake, landslide, volcanic eruption, or meteorite” (ready.gov). Tsunami waves are quite different from normal waves. Once a tsunami is set in motion there is no way to really “prevent” it fully, or to stop such an event. Precautionary steps can be taken, such as in Japan where a sea wall was built to protect people and property. However, this was a futile attempt since in 2011 a tsunami was able to surge over the wall, with the water building up and rushing over the top. The lesson learned is that one should not
Sara M. Evans, in her book, Tidal Wave: How Women Changed America at Century’s End, chronicles feminist activities over several decades from just before the beginning of the women’s liberation movement in the 1960’s through the 1990’s. Doctor Evans was born in 1943 and currently teaches at the University of Minnesota in the history department after receiving both her B.A. and M.A. at Duke University and then later her PhD from the University of North Carolina Chapel Hill.
According to the article, “Indian Ocean tsunami: Then and now” It states that “About 228,000 people were killed as a result of the 9.1 magnitude quake and the giant waves that slammed into coastlines on 26 December 2004.” From this quote, Is similar to the quote in the book because in the book the author says “The pick up truck was leaving to dump all the corpses so no one gets a disease.” In conclusion, you should always be thankful for what you have now because you might not have it in the
Over the course of Japanese history, arguably, no artist is more famous for their works than Katsushika Hokusai. During his 88 years of life, he produced over 30,000 pieces of artwork, and heavily influenced Western styles of art. His most famous piece was created around 1831, a Japanese styled piece titled, The Great Wave off Kanagawa. This piece has stood as a defining piece of artwork in the Japanese culture for over 180 years, analyzed by students and authors for the interpretations filling the paper. The relationship between Hokusai’s painting has directly affected the Western point of view of Japanese style. The English author, Herbert Read’s novel interprets the painting distinctly differently from a Japanese point, American poet,
Additionally, this earthquake occurred on a thrust fault. This fault was a subduction zone slip which occurred primarily beneath the ocean were the Pacific plate plunges underneath the North American plate. This sudden upward movement of the sea floor along the rupturing fault generated a massive tsunami. This vertical deformation
After researching and reading I found that one of the major effects of the Moon on the Earth and its inhabitants is its gravitational influence on the tides of Earth. The tidal effect of the moon usually affects the largest bodies of water, like the main oceans. The gravity of the moon pulls the water in the oceans toward it. As the Earth rotates, the knot shifts through the different areas of the globe. Tides appear on both sides of the Earth because of the pull of the sun. The flow of the oceanic tides helps the movement of heat from the equator north and south to the poles.
While the early warning saved thousands of people, the Japan’s Meteorological Agency underestimated this earthquake as the subduction zone of Japan should not produce the magnitude 9.0 quake (Oskin, 2013a). The Tohoku Earthquake and its tsunami approximately killed 16 thousand people, injured 6 thousand people and around 3 thousand people were missing. Most people died from drowning. Around 300 thousand buildings, 4000 roads, 78 bridges, and many more were affected by the earthquake, tsunami, and fires from leaking oils and gas. Electricity, telecommunication, and railways were severely damaged. The debris of 25 million tons was generated and carried out to the sea by water (BBC News, 2012). The country’s authorities estimated more than 309 billion US dollars of damages. Landslides occurred in Miyagi and liquefaction in Chiba, Tokyo, Odaiba, and Urayasu (USGS, 2013). Furthermore, the tsunami destroyed protective tsunami seawalls. Approximately 217 square miles of Japan covered in water (Oskin,
Unlike a tsunami being a giant wave that sinks a piece of land, a flood is a temporary overflow of water on usually dry land. Floods can come from heavy rain, storm surges, waterway block and many more. They can occur in a slow pace, taking days, or happen at an instant, becoming a flash flood (Flood).
At first, tsunami, also known as seismic sea waves, are a series of enormous waves created by an underwater disturbance such as earthquake, landslide, volcanic eruption, or meteorite. A tsunami can move hundreds of miles per hour in the open ocean and smash into land with waves as high as 100 feet or more.
Tsunamis are barely noticeable in deep ocean water; however when it starts approaching the land and shallow water the waves start to slow down and the height starts increase sometimes reaching heights of over 100 feet (30.5 meters).
The death toll climbs to over 10,000 and is still rising (Branigan 2). The disaster in Japan began without warning on Friday March 11, 2011 at 2:46pm with a 9.0 magnitude earthquake, the strongest ever recorded in the country (Fackler 3). A massive thirty-three foot high tsunami, generated by the earthquake, swept over lands in northern Japan, taking objects and debris with it. To make matters worse, the tsunami caused the cooling systems at several nuclear power plants to fail. The disaster in Japan was a tragic event, and it had a plethora of causes and effects.
Seismic waves are energy waves that are caused by the sudden breaking of rock in the earth’s crust, or because of an explosion caused by man; these waves travel through the earth and can be recorded by seismographs. There are many different types of seismic waves, but the two main types are surface waves, which can only move on the earth’s surface like a sort of ocean wave, and body waves, that travel through the earth’s innermost layers. Earthquakes make up both surface and body waves. Both surface and body waves can be broken down to two main