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This
data
tip
describes
the
science
behind
the
tsunamis
caused
by
the
great
earthquake
of
December
26,
2004,
which
caused
catastrophic
damage
and
loss
of
life
throughout
the
Indian
Ocean
basin.
The
discussion
centers
on
how
tsunamis
are
generated
and
how
great
quakes
and
resulting
tsunamis
occur
at
subducting
plate
boundaries.
Links
to
more
detailed
information
are
embedded
in
the
text.
An
exercise
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This
resource
discusses
the
relationship
between
earthquakes
and
tsunamis,
and
the
connection
between
the
shape
of
the
ocean
bottom
and
the
height
of
the
waves.
The
article
is
supported
by
an
animation
showing
the
origin
and
conclusion
of
a
tsunami,
a
video
interview
with
a
tsunami
survivor,
and
three
photographs.
There
are
two
sidebars,
called
'Catching
a
Tsunami
in
the
Act'
and
'Remembrance
of
Waves
...
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A comprehensive list of federal, state, and international tsunami links and publications. Links are both internal and external and provide a wealth of information concerning tsunami causes, preparedness, prediction, effects, and more.
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This interactive from NOVA Online shows how the 2004 Indian Ocean tsunami was triggered, how its waves traveled thousands of kilometers largely unchanged, and what happened once the waves reached coastlines both near and far from their source. Users can click on highlighted points on the map to see animations and written narrative describing the tsunami's effects.
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A
general
introduction
to
tsunamis
including
information
about
the
mechanisms
of
tsunami
generation
and
propagation,
the
impact
of
tsunamis
on
humankind,
and
the
Tsunami
Warning
System.
Sections
include
information
on
what
tsunami
means,
how
earthquakes,
landslides,
volcanic
eruptions
and
meteorites
generate
tsunamis,
and
what
happens
when
a
tsunami
approaches
and
encounters
land.
Also
included
is
...
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Since
the
Indian
Ocean
tsunami
of
December
26,
2004,
scientists
have
tried
to
retrace
the
path
of
the
giant
waves
to
learn
how
and
why
the
water
moved
in
unexpected
directions,
even
turning
corners
and
producing
simultaneous
wavefronts
coming
from
different
directions.
This
radio
broadcast
describes
efforts
to
measure
the
strength,
distance
traveled
inland,
and
height
of
the
tsunami,
as
well
as
mapping
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In
this
activity,
students
study
seismograms
from
three
different
seismic
stations
that
recorded
the
magnitude
9.0
Sumatra
earthquake
of
December
26,
2004.
By
comparing
the
arrival
times
of
the
P
and
S
waves
on
each
seismogram,
they
can
determine
the
distance
from
the
epicenter
to
each
station
and
accurately
map
its
location.
Using
this
information,
they
also
calculate
the
position
of
the
quake-generated
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This
radio
broadcast
covers
two
topics-
the
massive
undersea
earthquake
and
tsunami
that
devastated
coastal
communities
in
much
of
Asia
on
December
26,
2004,
and
an
update
on
the
annual
Audubon
Christmas
Bird
Count.
The
tsunami
segment
discusses
how
tsunamis
are
created,
what
their
effects
are,
and
whether
an
effective
system
can
be
created
to
provide
warning
of
these
killer
waves
in
the
Indian
Ocean,
...
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This
report
contains
true
stories
that
illustrate
how
to
survive
(and
how
not
to
survive)
a
tsunami.
It
is
meant
for
people
who
live,
work,
or
play
along
coasts
that
tsunamis
may
strike.
The
stories
are
personal
accounts
selected
from
interviews
with
people
who
survived
a
Pacific
Ocean
tsunami
generated
by
the
magnitude
9.5
earthquake
that
occurred
along
the
coast
of
Chile
on
May
22,
1960.
Important
...
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The
Plymouth
Wave
Lab
is
a
series
of
movies
of
waves
on
a
string
intended
for
middle
school
students.
The
reference
material
at
the
site
explains
the
relationship
between
the
behavior
of
the
string
in
the
six
examples
and
the
behavior
of
a
tsunami.
The
December
26,
2004
tsunami
that
was
generated
from
the
M9.0
Sumatra
earthquake
has
raised
public
awareness
worldwide
of
the
disastrous
consequences
...
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