What is a tsunami?
A tsunami is a tidal wave that may be caused by a variety of geophysical events. The word tsunami comes from the Japanese words tsu, meaning "harbor" and nami, meaning wave. Origins of a tsunami include earthquakes, volcanic eruptions, landslides beneath the ocean or an asteroid striking the earth.Some useful sites about tsunami include:
Tsunami!: The WWW
Tsunami Information Resource
Google
News Coverage
Google's Tsunami Relief
Site
The South-East Asia Earthquake and
Tsunami Blog
Donations to Tsunami relief programs in Southeast Asia can be made though these
organizations:
Action Against
Hunger
American
Red Cross (via
Amazon)
American Jewish World Service
BAPS
Care International
CARE
Direct Relief International
GOAL
Habitat
for Humanity International
International
Federation of Red Cross and Red Crescent
Islamic Relief Worldwide
Karuna Trust
Network
for Good
Oxfam International (US
page)
Sarvodaya
Save the Children
UNICEF (US
page)
World Food Programme (UN)
World Vision
How large are tsunami?
In the open ocean, tsunami may have wave-lengths of up to several hundred miles
and travel at speeds up to 450 mi per hr (720 km per hr). Despite these remarkable
features, a tsunami may have wave heights of less than 3 feet (1 meter) that
pass unnoticed beneath a ship at sea.
The period between wave-crests varies from 5 minutes to about 1
hour. When tsunami approach shallow water along a coast, their speed slows,
causing their length to shorten and their height to rise sometimes to as high
as 100 feet (30 meters). When they break, they often destroy anything in their
path - piers, buildings and beaches - and take human life. The wave height as
they crash upon a shore depends almost entirely upon the underwater topography
offshore. Waves tend to rise to greater heights along gently sloping shores,
along ridges or in coastal embayments.
Is it possible to predict a tsunami?
There is little warning of a tsunami's approach. When a "train"
of tsunami waves approaches a coastline, the first indication is often a sharp
swell, similar to an ordinary storm swell, followed by a sudden outrush of water
that often exposes offshore areas as the first wave trough reaches the coast.
After several minutes, the first huge wave crest strikes, inundating the newly
exposed beach and rushing inland to flood the coast. Generally, the third to
eighth wave crests are the largest.
Since tsunami principally occur in the Pacific Ocean following shallow-focus
earthquakes over magnitude 6.5 on the Richter scale, one of the best means of
prediction is the detection of such earthquakes on the ocean floor with a seismograph
network (see seismology).
Tsunami may be detected by wave gauges, such as those emplaced as part of the
Tsunami Warning System operating in the Pacific regions. Measurement of sudden
sea level changes from satellites can also warn of potential tsunami.
When was the largest tsunami recorded?
Probably the most destructive tsunami occurred following the explosive eruption of the volcano Krakatoa in the East Indies on August 27, 1883, when over 36,000 people were killed as a result of the wave. Waves were up to 100 feet (30 meter) high with speeds between 350 and 450 miles per hour (560-720 km per hr). Its passage was traced as far away as Panama. It is believed that a 0.6-mile-wide (1-kilometer-wide) asteroid that struck the ocean southwest of New Zealand about AD 1500 created tsunami that reached heights of more than 425 feet (130 meters).

