Friday, 8 June 2012

Tsunami


Tsunami
   Tsunami, Japanese word, meaning “harbor wave” and used as the scientific term
for seismic sea waveGenerated by an undersea earthquake or possibly an undersea
landslide or volcanic eruption. When the Ocean floor is tilted or offset during an
earthquake; a set of waves is created similar to the concentric   Waves generated by
an object dropped into the water. Most tsunamis originate along the ring of fire, a
zone of volcanoes and seismic activity , 32500 km (24,000mi) long, that encircles
the pacific ocean. Since1819, about 40 tsunamis have struck the Hawallan islands.

A Tsunami can have wavelengths, or widths, of 100 to 200 km (60 to 120 mi), and
 may travel hundreds Of kilometers across the deep ocean, reaching speeds of
  about 725 to 800 km/h (about 450 to 500 mph)
Upon entering shallow coasted wasters, the wave which may have been only about
half a meter (a foot Or two) high out at sea, suddenly grows rapidly. When the
 wave reaches the shore, it may be 15 m (50ft) high or more. Tsunamis have
 tremendous energy because of the great volume of water affected. They are
Capable of obliterating coastal settlements.
Tsunami should not be confused with storm surges, which are domes of water that
rise underneath hurricanes or cyclones and cause extensive coastal flooding when
 the storms reach land. Storm surges are particularly devastating if they occur at
 high tide. A cyclone and accompanying storm surge killed an estimated
500,000people in Bangladesh in 1970.

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