Tsunami
 
 

A tsunami (pronounced tsoo-nah-mee) is a wave train, or series of waves, generated in a body of water
by an impulsive disturbance that vertically displaces the water column. Earthquakes, landslides, volcanic
eruptions, explosions, and even the impact of cosmic bodies, such as meteorites, can generate tsunamis.
Tsunamis can savagely attack coastlines, causing devastating property damage and loss of life.
 

What causes a tsunami?

A tsunami can be generated by any disturbance that displaces a large water mass from its equilibrium
position. In the case of earthquake-generated tsunamis, the water column is disturbed by the uplift or
subsidence of the sea floor. Submarine landslides, which often accompany large earthquakes, as well as
collapses of volcanic edifices, can also disturb the overlying water column as sediment and rock slump
downslope and are redistributed across the sea floor. Similarly, a violent submarine volcanic eruption can
create an impulsive force that uplifts the water column and generates a tsunami. Conversely, supermarine
landslides and cosmic-body impacts disturb the water from above, as momentum from falling debris is
transferred to the water into which the debris falls. Generally speaking, tsunamis generated from these
mechanisms, unlike the Pacific-wide tsunamis caused by some earthquakes, dissipate quickly and rarely
affect coastlines distant from the source area.
 
 

Important Facts to Know about Tsunamis

     Tsunamis that strike coastal locations in the Pacific Ocean Basin are most always caused by
     earthquakes. These earthquakes might occur far away or near where you live.

     Some tsunamis can be very large. In coastal areas their height can be as great as 30 feet or more
     (100 feet in extreme cases), and they can move inland several hundred feet.

     All low-lying coastal areas can be struck by tsunamis.

     A tsunami consists of a series of waves. Often the first wave may not be the largest. The danger
     from a tsunami can last for several hours after the arrival of the first wave.

     Tsunamis can move faster than a person can run.

     Sometimes a tsunami causes the water near the shore to recede, exposing the ocean floor.

     The force of some tsunamis is enormous. Large rocks weighing several tons along with boats and
     other debris can be moved inland hundreds of feet by tsunami wave activity. Homes and other
     buildings are destroyed. All this material and water move with great force and can kill or injure
     people.

     Tsunamis can occur at any time, day or night.

     Tsunamis can travel up rivers and streams that lead to the ocean.
 
 

What does "tsunami" mean?
 

Tsunami is a Japanese word with the English translation, "harbor wave."
Represented by two characters, the top character, "tsu," means harbor, while
the bottom character, "nami," means "wave." In the past, tsunamis were
sometimes referred to as "tidal waves" by the general public, and as "seismic sea
waves" by the scientific community. The term "tidal wave" is a misnomer;
although a tsunami's impact upon a coastline is dependent upon the tidal level at
the time a tsunami strikes, tsunamis are unrelated to the tides. Tides result from
the imbalanced, extraterrestrial, gravitational influences of the moon, sun, and
planets. The term "seismic sea wave" is also misleading. "Seismic" implies an
earthquake-related generation mechanism, but a tsunami can also be caused by a
nonseismic event, such as a landslide or meteorite impact.


Back to main