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Tsunami
The term tsunami comes from the Japanese,
composed of the two kanji. Tsu meaning
“harbor” and nami meaning “wave”
Tsunami is a series of water waves caused by the
displacement of a large volume of a body of
water, generally an ocean or a large lake.
Earthquakes, volcanic eruptions and other
underwater explosions, above or below water
all have the potential to generate a tsunami
Tsunamis cause damage by two mechanisms:
the smashing force of a wall of water travelling
at high speed, and the destructive power of a
large volume of water draining off the land.
A tsunami in the deep ocean has a much larger
wavelength of up to 200 kilometers (120 mi).
Such a wave travels at well over 800
kilometers per hour (500 mph).
As the tsunami approaches the coast and the
waters become shallow, wave
shoaling compresses the wave and its speed
decreases below 80 kilometers per hour
(50 mph). Its wavelength diminishes to less
than 20 kilometers (12 mi) and its amplitude
grows enormously.
Open bays and coastlines adjacent to very deep
water may shape the tsunami further into a
step-like wave with a steep-breaking front.
About 80% of tsunamis occur in the Pacific
Ocean, but they are possible wherever there
are large bodies of water, including lakes. They
are caused by earthquakes, landslides,
volcanic explosions, glacier calving,
and bolides.
A tsunami cannot be precisely predicted, even if
the magnitude and location of an earthquake
is known. Geologists, oceanographers,
and seismologists analyze each earthquake
and based on many factors may or may not
issue a tsunami warning.
However, there are some warning signs of an
impending tsunami, and automated systems
can provide warnings immediately after an
earthquake in time to save lives.

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Tsunami

  • 2. The term tsunami comes from the Japanese, composed of the two kanji. Tsu meaning “harbor” and nami meaning “wave” Tsunami is a series of water waves caused by the displacement of a large volume of a body of water, generally an ocean or a large lake. Earthquakes, volcanic eruptions and other underwater explosions, above or below water all have the potential to generate a tsunami
  • 3. Tsunamis cause damage by two mechanisms: the smashing force of a wall of water travelling at high speed, and the destructive power of a large volume of water draining off the land. A tsunami in the deep ocean has a much larger wavelength of up to 200 kilometers (120 mi). Such a wave travels at well over 800 kilometers per hour (500 mph).
  • 4. As the tsunami approaches the coast and the waters become shallow, wave shoaling compresses the wave and its speed decreases below 80 kilometers per hour (50 mph). Its wavelength diminishes to less than 20 kilometers (12 mi) and its amplitude grows enormously. Open bays and coastlines adjacent to very deep water may shape the tsunami further into a step-like wave with a steep-breaking front.
  • 5. About 80% of tsunamis occur in the Pacific Ocean, but they are possible wherever there are large bodies of water, including lakes. They are caused by earthquakes, landslides, volcanic explosions, glacier calving, and bolides.
  • 6. A tsunami cannot be precisely predicted, even if the magnitude and location of an earthquake is known. Geologists, oceanographers, and seismologists analyze each earthquake and based on many factors may or may not issue a tsunami warning. However, there are some warning signs of an impending tsunami, and automated systems can provide warnings immediately after an earthquake in time to save lives.