Tsunami! - HRSBSTAFF Home Page

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Tsunami!
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What happened & why
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Tsunami: causes
•Undersea
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earthquake
(most
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often) must be above
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6.75 on richter scale
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•Volcanic eruption
•Undersea rockslide
NOAA
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Tsunamis are
created when:
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styles
quickly
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changes shape
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Anthony Liekens 15:30, 28 Dec 2004 (UTC)
•Water is
displaced (pushed
up)
•Waves are
formed as gravity
tries to move the
water back into
place
Earthquakes and
tsunamis
Crust is stuck 
• Pressure from moving
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plates builds
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• When crust slips
energy
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level is
Crust slips
released (elastic– rebound
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theory)
energy
• This energy is transferred to
the water as it gets pushed
up
Energy
• Gravity pushes it back down transferred
starting the tsunami
to water
Subduction and Tsunamis
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Anthony Liekens 15:30, 28 Dec 2004 (UTC)
Landslides and
tsunamis
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tooccur
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• Landslides
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on their own
or be level
triggered by• an
Third level
earthquake
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• Energy released by
shifting land displaces
surrounding water
creating a ripple effect
• Like dropping a rock
into a pond
Volanoes and tsunamis
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• The explosive eruption of Krakatau in August
1883 created a tsunami that claimed more than
36,000 lives
Wave Characteristics
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Crest: top of wave
Trough: bottom of wave
Wavelength: Length of one complete cycle
Wave Height: measured from trough to crest
Amplitude: ½ height of wave
Tsunami Wave Characteristics
• Speed:
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– can•move
overMaster
970 km/h
(faster than a
jet) – Second level
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– Regular wave
generated
by wind 90km/h
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level
• Distance:
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– Can travel across entire oceans with little
energy loss
• Size:
– Long, shallow waves in open ocean, decrease
in length and increase in height as you
approach the shore
Wave Characteristics
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Wave Characteristics
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• When the trough of the wave hits the
ocean floor the speed decreases and wave
height increases
• Runup is a temporary increase in sea level;
can occur without the ‘huge’ tsunami waves
Wave Characteristics
Wave height increases as it reaches land
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Wave Characteristics
Wave speed decreases as it approaches the
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shore
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Warning Systems
Many countries
around the Pacific
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have warning
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systems –and
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evacuation
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procedures in the
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event of a serious
tsunami.
Tsunamis travel fast, but there is enough
time to evacuate all areas except those
that are nearest the epicenter
•Monitor seismic
activity
(seismograph)
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•Monitor changes
in
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sea level off– the
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coast using a series
of buoys
•Difficult because
tsunamis have such
small height in open
ocean
Effects of Tsunamis
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– Second level of human life
• Destruction
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(100,000+)
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• Destruction of property and
infrastructure
• Increase spread of disease
• Destruction of ecosystems
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http://msnbc.msn.com/id/6770108/
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http://msnbc.msn.com/id/6770108/
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