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In
this
activity,
students
examine
a
seismogram
display
called
a
seismic
record
section
in
which
each
trace
is
a
seismogram
recorded
at
a
specific
seismograph
station.
The
seismograms
are
plotted
according
to
the
distance
(in
degrees,
geocentric
angle)
from
the
earthquake
location
and
time
from
the
earthquake
origin.
The
traces
are
of
the
vertical
component
of
ground
motion,
and
have
been
filtered
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Choosing & Using this resource...
Educational standards associated with this resource:
National Science Education Standards (NSES): Read
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This resource is referenced by :
Explorations in Earth Science: Earth Science Education Demonstrations, Lessons and Activities -
http:/
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In
this
activity,
students
construct
a
model
that
will
allow
them
to
experiment
with
thermal
convection,
illustrating
how
thermal
energy
can
generate
a
flowing
motion
in
a
fluid.
The
thermal
convection
in
this
model
is
similar
to
the
convection
that
is
inferred
for
the
Earth's
mantle
and
can
produce
horizontal
flow
that
can
cause
or
is
related
to
plate
motions.
Students
will
investigate
the
viscosity
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Choosing & Using this resource...
Educational standards associated with this resource:
National Science Education Standards (NSES): Read
Related resources and collections
This resource is referenced by :
Explorations in Earth Science: Earth Science Education Demonstrations, Lessons and Activities -
http:/
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Users
can
access
the
array
of
seismometers
operated
by
the
the
University
of
California
at
Berkeley's
Seismological
Laboratory
in
northern
and
central
California.
The
Berkeley
Digital
Seismic
Network
is
an
array
of
high-dynamic
range,
broadband
seismometers.
Data
from
these
instruments
are
transmitted
continuously
to
UC
Berkeley
for
processing
and
analysis.
Using
the
interface,
visitors
may
create
...
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Choosing & Using this resource...
Educational standards associated with this resource:
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This radio broadcast explains how the North Pole is constantly moving due to the rotation of the Earth, which in turn is determined by any changes in the mass distribution of the Earth. The clip is 2 minutes in length.
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In
this
activity
students
plot
the
latitude
and
longitude
involved
in
the
movement
of
the
Magnetic
North
Pole
over
a
period
of
time,
predict
its
location
by
the
year
2000,
and
justify
their
reasoning.
Students
will
discover
that
the
Magnetic
North
Pole
has
been
charted
over
the
past
several
hundred
years
and
that
the
pole
shifts
an
average
of
15
kilometers/
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Choosing & Using this resource...
Educational standards associated with this resource:
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In
this
activity
students
learn
about
Earth's
magnetic
reversals
by
reading
two
fiction
stories
and
a
scientific
summary
of
past
reversals,
including
graphical
information.
This
will
help
students
discriminate
between
factual
and
fictional
descriptions
of
a
natural
phenomenon,
which
has
been
scientifically
studied
from
the
fossil
and
geologic
record
of
Earth,
and
found
to
be
a
lot
less
frightening
...
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Choosing & Using this resource...
Educational standards associated with this resource:
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The
Earth
hums,
emitting
a
tone
too
low
for
human
ears
to
detect.
Geophysicists
have
finally
located
the
source
of
the
noise.
As
this
radio
broadcast
reports,
it
comes
from
the
largest
oceans
during
winter,
apparently
the
result
of
powerful
winter
storms.
The
hum
comes
from
the
surface
of
the
Earth
rising
and
falling
less
than
a
millionth
of
a
meter,
vibrating
once
per
300
seconds.
The
clip
is
3
minutes
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This
is
the
homepage
of
the
Marine
Seismic
Data
Center
(MSDC)
of
the
University
of
Texas
Institute
for
Geophysics
(UTIG).
MSDC's
purpose
is
to
organize
seismic
reflection
and
refraction
data
into
a
modern
relational
database
management
system
accessible
through
the
Internet.
The
web
site
provides
access
to
metadata,
SEG-Y
(seismic
shot
record
conversion)
files,
navigation
files,
seismic
profile
images,
...
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This set of animations, accompanied by an audio narrative, shows the four types of wave motion seen in an earthquake: P waves, S waves, Love waves, and Rayleigh waves. A brief written narrative and a set of study questions are also included.
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This
tutorial
provides
information
on
the
four
types
of
wave
motion
seen
in
earthquakes
(S,
P,
Love,
and
Rayleigh
waves).
A
table
accompanied
by
text
describes
their
particle
motion,
typical
veolcity,
and
other
characteristics.
The
four
animations
show
a
rectangular
block
of
material
with
outlined
with
grid
lines
and
a
filled-in
grid
square
to
highlight
the
particle
motion
and
direction
of
propagation.
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