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COSMOS_Project7
COSMOS_Project7

... What is an Earthquake? An earthquake is a trembling of the Earth's surface Usually caused by stress that is released along the fault lines as pressure builds up over time Shock waves will be generated by the movement of the masses of rock and crust. ...
6 WATER WAVES - MIT OpenCourseWare
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... Most important from a design point of view, it has been observed that extreme events do NOT follow the Rayleigh distribution - they are more common. Such dangers are well documented in data on a broad variety of processes including weather, ocean waves, and some social systems. In the case of ocean ...
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... This is more information on the effects of earthquakes in developed and developing countries: The 2010 Christchurch earthquake was a 7.1 magnitude earthquake which struck the South Island of New Zealand at on 4 September 2010. The earthquake was caused by the collision of the Australian and Pacific ...
Chapter21 - Cobb Learning
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... Energy is transferred from stone to floating log, but only the disturbance travels. Actual motion of any individual water particle is small. Energy propagation via such a disturbance is known as mechanical wave motion. ...
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Locating the Epicenter (modified for ADEED)

... Explain that scientists consider three important factors when determining the likelihood of an earthquake to generate a tsunami. First, they determine whether the earthquake had a magnitude greater than 7.0. Magnitude describes the amount of shaking and energy released during a quake. On average, on ...
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...  Know where the risk of earthquakes is highest in the United States and why  Know where the risk of earthquakes is lowest in the United States and why  Be able to describe why the eastern United States has experienced some of the most powerful quakes in the nation’s history  Know the four types ...
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Potential for Tsunami Generation along the Makran Subduction Zone

... Effects of the November 28, 1945 Tsunami in Pakistan, India, Iran, and Oman PAKISTAN - The tsunami reached a maximum run up height of 13 m (40 feet) along the Makran coast. The waves destroyed fishing villages and caused great damage to port facilities. More than 4,000 people died from the combined ...
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... This picture shows the EM Spectrum. In the middle is visible light. Between 400nm and 700nm (nano metres or 1x10-9m = 0.000000001m). The eye is sensitive to this light and by monitoring the reflection of light from the objects around us we are able to distinguish the distance of the objects and the ...
EARTHQUAKES
EARTHQUAKES

...  Scientists use the principle that the speed and direction of a seismic wave depends on the material it travels through. Because of the behavior of these different waves, scientists have indirect evidence for the solid inner core and liquid outer core of Earth; because earthquake waves travel fas ...
Abbott_6e_IM
Abbott_6e_IM

... distinct from wind-blown waves and from tidal waves. The common usage in the media of the term tidal wave as a synonym for tsunami is deplorable. Tidal waves draw their energy from gravitational attraction; tsunami do not. Tsunami can travel almost 500 mph and can have periods up to one hour. Tsunam ...
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Tsunami



A tsunami (plural: tsunamis or tsunami; from Japanese: 津波, lit. ""harbor wave"";English pronunciation: /tsuːˈnɑːmi/), also known as a seismic sea wave, is a series of waves in a water body caused by the displacement of a large volume of water, generally in an ocean or a large lake. Earthquakes, volcanic eruptions and other underwater explosions (including detonations of underwater nuclear devices), landslides, glacier calvings, meteorite impacts and other disturbances above or below water all have the potential to generate a tsunami. In being generated by the displacement of water, a tsunami contrasts both with a normal ocean wave generated by wind and with tides, which are generated by the gravitational pull of the Moon and the Sun on bodies of water.Tsunami waves do not resemble normal sea waves, because their wavelength is far longer. Rather than appearing as a breaking wave, a tsunami may instead initially resemble a rapidly rising tide, and for this reason they are often referred to as tidal waves, although this usage is not favored by the scientific community because tsunamis are not tidal in nature. Tsunamis generally consist of a series of waves with periods ranging from minutes to hours, arriving in a so-called ""wave train"". Wave heights of tens of meters can be generated by large events. Although the impact of tsunamis is limited to coastal areas, their destructive power can be enormous and they can affect entire ocean basins; the 2004 Indian Ocean tsunami was among the deadliest natural disasters in human history with at least 230,000 people killed or missing in 14 countries bordering the Indian Ocean.The Greek historian Thucydides suggested in his late-5th century BC History of the Peloponnesian War, that tsunamis were related to submarine earthquakes, but the understanding of a tsunami's nature remained slim until the 20th century and much remains unknown. Major areas of current research include trying to determine why some large earthquakes do not generate tsunamis while other smaller ones do; trying to accurately forecast the passage of tsunamis across the oceans; and also to forecast how tsunami waves would interact with specific shorelines.
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