Current Events

  • Kansas Legislator Proposes Bill to Outlaw Sustainability Education
    A bill has been introduced in the Kansas legislature this week that would prohibit the promotion of ...Read more

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    Kansas Legislator Proposes Bill to Outlaw Sustainability Education

    A bill has been introduced in the Kansas legislature this week that would prohibit the promotion of sustainability. Here is a link to the one-page bill: http://www.kslegislature.org/li/b2013_14/measures/documents/hb2366_00_0000.pdf. See report on Bloomberg News.
  • Earth's Center Is 1,000 Degrees Hotter Than Previously Thought, Synchrotron X-Ray Experiment Shows
    Scientists have determined the temperature near the Earth’s center to be 6000 degrees Celsius, 1000 ...Read more

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    Earth's Center Is 1,000 Degrees Hotter Than Previously Thought, Synchrotron X-Ray Experiment Shows

    Scientists have determined the temperature near the Earth’s center to be 6000 degrees Celsius, 1000 degrees hotter than in a previous experiment run 20 years ago. These measurements confirm geophysical models that the temperature difference between the solid core and the mantle above, must be at least 1500 degrees to explain why the Earth has a magnetic field. For more information about this study, see the press release from the European Synchrotron Radiation Facility.
  • Ocean Volcanic Rocks Contain Samples of Recycled Crust
    Scientists have long believed that lava erupted from certain oceanic volcanoes contains materials fr...Read more

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    Ocean Volcanic Rocks Contain Samples of Recycled Crust

    Scientists have long believed that lava erupted from certain oceanic volcanoes contains materials from the early Earth’s crust. But decisive evidence for this phenomenon has proven elusive. New research from a team including Carnegie’s Erik Hauri demonstrates that oceanic volcanic rocks contain samples of recycled crust dating back to the Archean era 2.5 billion years ago. Their work is published in Nature. Oceanic crust sinks into the Earth’s mantle at so-called subduction zones, where two plates come together. Much of what happens to the crust during this journey is unknown. Model-dependent studies for how long subducted material can exist in the mantle are uncertain and evidence of very old crust returning to Earth’s surface via upwellings of magma has not been found until now. For more information about these results, see the press release from the Carnegie Institution.
The picture above shows how the shape of a tsunami wave changes as it moves into shallower water.
Click on image for full size
NOAA

What Is a Tsunami?

A tsunami (pronounced tsoo-NAH-mee) is a series of waves, generated in an ocean or other body of water by a disturbance such as an earthquake, landslide, volcanic eruption, or meteorite impact. Tsunamis can savagely attack coastlines, causing devastating property damage and loss of life. Some people call tsunamis “tidal waves”, but these monstrously large waves really have little to do with tides, so the term “tidal wave” is not really appropriate.

Tsunami waves are different from the waves you can find rolling into the coast of a lake or ocean. Those waves are generated by wind offshore. The wavelength of regular wind-generated waves, that is the distance between the crests or highest points of the waves, might a just a few meters for small waves or about 100 meters for large waves. But a tsunami in the open ocean can have a wavelength of more than 100 km. Tsunami waves have huge wavelengths, but they are typically less than a meter high in the open ocean. A tsunami can travel over the open ocean at about 700 km/hr.

As a tsunami travels into the shallower water near the coast, it transforms. As a tsunami approaches shore, it’s height increases and wavelength decreases. Therefore, even though a tsunami may be imperceptible at sea, it may grow to be several meters or more in height near the coast and have a tremendous amount of energy. When it finally reaches the coast, a tsunami may appear as a rapidly rising or falling tide or a series of waves with a maximum height of up to 30 meters above sea level.

A few minutes before a tsunami wave hits, the water near shore may recede, exposing the ocean floor. Often the first wave may not be the largest. Additional waves may arrive at the coast every 10 to 60 minutes and move much faster than a person can run. The danger from a tsunami can last for several hours after the arrival of the first wave. Unlike other waves, tsunami waves typically do not curl and break.

Coasts affected by a tsunami will be severely eroded. A tsunami can cause flooding hundreds of meters inland. The water moves with such force that it is capable of crushing homes and other buildings.

Last modified May 21, 2008 by Lisa Gardiner.

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