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msphillipsonline

Irresistible Ideas for play based learning - 0 views

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    Good ideas for play based learning.
msphillipsonline

Best content in Fourth Grade Chadwick | Diigo - Groups - 0 views

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    Google doc book of project based learning
msphillipsonline

Project Based Learning | BIE - 0 views

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    Comprehensive site for PBL
msphillipsonline

LearnZillion - 0 views

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    Videos for learning.
emily hough

The World & I Genes and Biotechnology: Past & Present, Special Collection, Educational ... - 2 views

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    Learn about Earthquakes and Plate Tectonics 
msphillipsonline

Learning science vocabulary through knowledge of Greek and Latin roots - 2 views

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    Excellent power point for understanding how to teach greek and latin roots
msphillipsonline

How to Read Mathematics - 0 views

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    Good article as introduction to interesting sounding education book on math education
Katie Jeon

Simple machines - 0 views

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    This website tells us about simple machines...
Katie Jeon

all about simple machines - 0 views

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    you could find all about simple machines! I hope you like it!
msphillipsonline

What's Going On in This Picture? | April 15, 2013 - NYTimes.com - 2 views

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    VTS takes a position in the NYT everyday.  Yay!
Katie Jeon

dictionary - 0 views

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    type a phrase and find a definition!
msphillipsonline

The Role of Mathematics, HK Feb.2013 | Trello - 1 views

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    All the doc's from the IB math workshop
Tonya Low

Recycling for Kids - Fun Experiments, Free Games, Cool Projects, Science Online - 0 views

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    Explore the amazing world of recycling for kids with our range of fun experiments, free games, crazy facts, cool projects, interesting videos, quizzes and more! Learn why we recycle, where it happens, how it happens, what materials are easiest to recycle, how much energy it can save and much more.
msphillipsonline

Geology of a Tsunami - 1 views

  • On May 22, 1960, a huge earthquake off the coast of Chile generated tsunami waves that traveled across the Pacific Ocean and reached Japan twenty-three hours later, causing damage and killing 122 people. In Chile itself, the earthquake and tsunami together killed two thousand people, injured three thousand people, and made two million people homeless.
  •   The outermost layer of our rocky planet is made up of a dozen tectonic plates which constantly move relative to one another at rates of one or several inches per year. The boundaries of these tectonic plates are marked by numerous active faults and earthquakes. When a fault on the ocean floor rapidly moves, it rises or collapses one block of rock against another. This creates an earthquake, disrupts the overlying water, and sends fast moving tsunami waves. Although large undersea earthquakes and water-column displacements are responsible for most tsunamis, there have been tsunami events in which the earthquake occurred on islands or near the coastal areas. It is thus possible that seismic (earthquake-generated) waves traveling along the Earth's surface also play a role in tsunamis, propagating energy from rocks to ocean water.
  •  Human response to tsunamis should be viewed at different levels--global, regional, local, and individual. There are already some major endeavors to study tsunamis and to reduce their harm. These efforts need to be strengthened and we need to be aware of them.
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  •  The destructive effects of tsunamis on islands and coastal areas directly result from three factors: (1) inundation (flooding and floating debris); (2) wave impact on structures, ships, and port facilities, and (3) erosion of foundations leading to collapse of bridges, seawalls, and buildings.                Indirect factors of tsunami casualties come from (1) fires initiated in buildings, ships, oil tanks, and gas stations; (2) environmental pollution caused by sewage, oil, and dangerous chemicals; and (3) outbreak of epidemic diseases. All these lead to tragic loss of life, damage to property, and destruction of ports, towns, and villages.
  • All along the margin of the Pacific Ocean, there are subduction zones where the denser oceanic plate descends under the lighter continental plate. This has created the Ring of Fire--a circum-Pacific belt of numerous volcanic eruptions and earthquakes. Almost 80 percent of tsunamis in the world take place in the Pacific Ocean. However, there are subduction zones in the Indian Ocean and in the Caribbean Sea too; these regions are prone to earthquakes and tsunamis as well. Destructive tsunamis are usually generated by undersea earthquakes with magnitudes exceeding 7 on the Richter scale.
  •  Currently scientists cannot predict exactly when an earthquake will occur. However, we know where earthquakes mostly take place on Earth. In addition, the time lapse between the occurrence of an undersea earthquake and the tsunami waves hitting land gives a window of opportunity to evacuate people from hazard zones.
  • Since 1997, a new type of tsunami warning device has been developed that consists of a pressure sensor placed on the ocean floor, and a surface "buoy" that transmits the pressure readings to a U.S. weather satellite named GEOS. This modern system is called DART (Deep-ocean Assessment and Reporting of Tsunamis).
  •  While international and national programs are crucial to mitigate tsunami hazards, communities and individuals living in coastal areas or on islands prone to tsunamis can equally play an important role. Some useful tips are:                -- Learn tsunami facts and recognize tsunami warning signs;                -- Be familiar with your environment and community;                -- Participate in activities related to tsunami preparations and emergency plans in your family, school, workplace, religious congregation, etc.                -- If there is a large earthquake, get the latest information from a radio or TV;                -- If you are near the ocean and the ground shakes, evacuate at once;                -- When there is a tsunami warning, never go to the beach to watch the tsunami;                -- Remember the highest ground or the farthest place from the beach is the safest when a tsunami strikes.
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    Article describing how a tsunami works, how they are measured and the new technology, and what to watch for.
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