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This
introduction
to
plate
tectonics
covers
plates
and
boundaries,
subduction
zones,
colliding
continents,
plumes,
and
earthquakes.
There
is
also
more
advanced
material
on
buoyancy,
floating
continents,
and
rates
of
isostasy;
sedimentation,
continental
growth,
rifts
and
creation
of
continental
margins,
passive
and
active
margins,
and
island
arcs
and
back-arc
basins;
continental
collision,
folding
...
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This
bulletin
discusses
the
magnitude
7.9
earthquake
that
shook
the
islands
of
Tonga
in
May
2006.
Topics
include
the
tectonic
setting
of
the
islands,
at
the
boundary
of
the
Pacific
and
Australian
plates,
the
frequent
seismic
activity
at
this
location,
how
earthquakes
are
produced
at
subduction
zones,
and
how
they
can
reveal
information
about
the
Earth's
interior.
There
is
also
information
about
the
...
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Recordings
on
this
site
present
164
aftershocks
as
they
were
heard
at
one
seismic
recording
station.
They
occurred
after
an
earthquake
with
a
magnitude
of
6.2
beneath
and
near
New
Zealand.
All
events
are
heard
in
rapid
sequence,
without
the
true
time
intervals
between
them.
The
main
shock
was
at
a
depth
of
30
kilometers,
10
kilometers
below
the
interface
between
the
subducting
Pacific
Plate
and
the
...
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This
map
of
world
seismicity
illustrates
earthquake
data
for
the
years
1991
through
1996.
It
is
intended
to
provide
a
sense
of
the
depth
distribution
of
earthquakes.
Plate
boundaries
are
shown,
along
with
diffuse
regions
of
seismicity,
such
as
in
central
Asia,
and
earthquake
locations
are
color-coded
to
indicate
the
depths
at
which
they
occurred.
In
addition
to
the
map,
selected
cross-sections
of
...
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Early
evidence
showing
striking
similarities
between
regions
on
opposite
sides
of
vast
oceans
suggested
that
in
Earth's
distant
past
what
are
now
separate
continents
may
once
have
been
connected.
However,
this
evidence
said
nothing
about
how
the
continents
could
have
moved
to
their
present
positions.
This
video
shows
how
seafloor
spreading
creates
new
oceanic
crust
and
how
the
crust
is
destroyed
by
...
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This
demonstration
models
the
manner
in
which
the
convection
currents
in
the
mantle
of
the
Earth
cause
movement
of
the
plates.
Convection
currents
in
the
mantle
were
thought,
for
many
years,
to
be
solely
responsible
for
plate
tectonic
movements,
with
the
movement
taking
rocks
down
at
destructive
margins
and
new
rocks
forming
when
plates
spread.
It
is
now
thought
likely
that
there
are
three
possible
...
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On
the
Pacific
Northwest
an
oceanic
tectonic
plate
(Juan
de
Fuca)
is
being
pulled
and
driven
(subducted)
beneath
the
North
American
continental
plate.
Earthquakes
generated
along
that
fault
may
produce
local
tsunamis.
Local
tsunamis
are
those
generated
by
earthquakes
near
the
coast.
This
site
provides
links
to
external
webpages
describing
the
physics
behind
a
tsunami.
Resources
featured
in
the
links
...
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This
resource
provides
general
information
about
volcanoes.
It
illustrates
the
growth
of
a
volcano,
using
Paricutin
and
Mt.
St.
Helens
as
examples
of
an
active
volcano
and
a
lava
dome.
The
terms
extinct
and
dormant
are
also
discussed.
This
site
provides
an
explanation
of
why
and
how
volcanoes
form,
zones
of
subduction,
mid-ocean
ridges,
and
hot
spots.
Deadly
dangers
associated
with
eruptions
are
discussed
...
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This
link
takes
you
to
the
download
page
for
Tanya
Atwater's
plate
tectonics
animations.
Users
must
register
before
using
the
site,
but
it
is
free
of
charge.
The
site
contains
a
series
of
QuickTime
movies
illustrates
the
movement
and
tectonic
history
of
the
Pacific-North
America
plate
from
85
million
years
ago
to
present.
The
movies
show
the
tectonic
evolution
of
California,
evolution
of
the
San
Andreas
...
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This
resource
offers,
among
other
things,
a
collection
of
journal
entries
from
scientists
reporting
on
their
personal
experiences
of
the
volcanoes
of
Costa
Rica.
Reference
sections
include
an
introduction
to
volcanoes
and
Central
America,
the
anatomy
of
subduction
zones,
the
source
of
volatiles,
sampling
volatiles,
recycling
elements,
and
isotope
geochemistry
(geochemical
tracers).
There
is
a
short
...
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