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This
magazine
article
describes
how
two
high-magnitude
earthquakes
(7.6
in
both
instances)
triggered
landslides
in
El
Salvador
and
Taiwan
which
caused
extensive
damage
and
loss
of
life,
apart
from
the
shaking
of
the
earthquakes
themselves.
The
article
points
out
that
the
two
areas
have
common
features-
tectonically
very
active,
high
steep
slopes
and
deeply
weathered
material,
that
made
the
landslides
...
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This
hands-on
activity
demonstrates
the
abrasive
power
of
glaciers
carrying
rocks
and
sand.
Its
purpose
is
to
illustrate
the
concept
that
glaciers
change
the
Earth's
surface
through
the
processes
of
erosion
and
deposition.
Students
construct
model
glaciers
by
freezing
water
with
sand
and
pebbles
at
the
bottom
to
represent
the
rock
fragments
carried
by
a
real
glacier.
They
then
rub
their
'glacier'
...
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Users
can
choose
a
time
in
geologic
history,
select
the
link,
and
see
what
the
Earth
looked
liked
in
the
far
distant
past.
Each
map
features
a
brief
written
description
of
the
events
occurring
at
that
time,
and
a
link
to
additional
information
on
the
geologic
era
or
period
being
shown.
There
are
also
maps
that
show
what
the
Earth
might
look
like
in
the
future,
50,
100,
and
150
million
years
from
now.
...
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This isoseismal map shows shows regions of different intensities according to the Modified Mercalli Intensity Scale. These zones were defined using the felt reports from the Charlevoix-Kamouraska earthquake of February 1925, which occurred in central Quebec, Canada.
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This isoseismal map shows the distribution of Modified Mercalli values compiled from questionnaires distributed after the largest shock of the January 1988 Tennant Creek earthquake, which occurred in Northern Territory, Australia.
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In
this
exercise,
students
will
study
the
three
types
of
faults,
investigate
the
association
between
faults
and
earthquakes,
and
examine
the
relationship
between
earthquakes
and
plate
tectonics.
There
is
a
set
of
animations
that
illustrate
the
types
of
seismic
waves,
an
exercise
in
which
students
determine
the
location
of
an
earthquake
epicenter
using
arrival
times
of
P
and
S
waves,
and
an
exercise
...
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In
this
activity,
students
gather
data
and
compare
the
shaking
intensities
of
the
1906
San
Francsico
and
1989
Loma
Prieta
earthquakes.
They
compare
shaking
intensity
maps
from
the
two
earthquakes
using
the
Modified
Mercalli
Shake
Intensity,
examine
the
lengths
of
fault
ruptures,
and
examine
seismograph
traces
from
each
earthquake.
Links
to
additional
information
and
to
lesson
plans
that
use
these
...
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This resource references :
Lesson 5: A Whole Lot of Shakin? Goin? On! -
http:/
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This interactive feature provides an introduction to the theory of plate tectonics. Topics include the history of ideas on plate tectonics, some evidence that the continents were once connected to each other, what happens when plates move and collide, and a description of the internal structure of the Earth. Interactive illustrations and animated maps are included to help reinforce these concepts.
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This page provides an introduction to plate tectonics for secondary students. Topics include plate motions, the layers of the Earth and oceanic versus continental plates. A set of links provides access to material on the processes of plate tectonics occuring at plate boundaries, zones of movement and instability.
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This page discusses the three main forces (compression, tension, and shear) that drive deformation within the Earth. Students can click on an animation to see illustrations of each type. Links to a glossary are embedded in the text.
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This resource is part of :
The Southern California Integrated GPS Network Education Module -
http:/
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