Inside Planet Earth Page #5
- Year:
- 2009
- 120 min
- 461 Views
They go with a bang.
The old ocean floor carries
water into the mantle,
which mixes with the magma.
When the pressure
can no longer be contained,
it explodes in that most awesome
of natural events,
a volcanic eruption.
Most of the world's volcanoes
are in subduction zones,
but there are exceptions.
Kilauea is on
the Big Island of Hawaii,
the middle of the Pacific Ocean,
thousands of miles away
from any subduction zone.
But the whole chain is formed
entirely from volcanoes
whose rivers of fire
heave and bubble
at temperatures
of 2,000 degrees.
What provides the furnace
for all this outpouring
if it's not the crashing
of the tectonic plates?
The volcanologists
have an explanation.
The lava that's flowing
and spattering behind me
is the surface manifestation
of a thermal anomaly,
or a hot spot,
that's deep within the earth
beneath my feet.
Where we are now--
on Kilauea Volcano
on the Big Island of Hawaii--
is at the southeast end of
a 6,000-kilometer-long chain
of seamounts and volcanic
islands that have formed
as the Pacific plate
has moved north and westward
over the last
80 million years or so
at a rate of around
9 or 10cm per year.
So as the plate
moves over this hot spot,
you burn through
the lithosphere,
forming a volcanic island.
And then the plate moves on,
and a new island forms
further to the southeast.
The hot spot has made Kilauea
the tallest mountain
in the world--
30,000 feet
from its base on the seafloor.
Taller even than Everest.
It's also one of
the most studied.
But scientists can't always wait
for the lava to come to them.
They must catch it as it bursts
through the crust.
Carl Thornber often goes fishing
with a cable in a red-hot pond.
And sometimes
he has to get even closer.
It's extremely dangerous.
At any moment, the lava may
spurt out unexpectedly,
leaving Thornber
with nowhere to run.
Behind me is a perched lava pond
that's being fed from a vent
off to my left.
You can see
that there's lava spattering
and overflowing on its edges.
I'm gonna attempt to scoop
a sample of molten lava--
hopefully with a hammer
so I won't have to use
a long cable to throw it in.
And it'll be extremely hot.
We have to worry about gases.
And we have to worry
about breakouts
near the edge of the pond.
So we'll see how it goes.
Thornber is risking his life.
But unless scientists can learn
how to forecast eruptions,
volcanoes will continue to be
an uncontrollable threat.
Okay, we'll take this sample
back to the USGS observatory,
and we'll prepare it
for chemical analysis.
The chemistry
of Hawaiian basalts is unique
compared to volcanic deposits
near subduction zones
or near mid-ocean ridges.
And that will be reflected
in the chemistry that we see.
More importantly,
we're looking at very subtle
variations in chemistry
that can be correlated
with the eruptive history
of this volcano.
So it will allow us to predict
what may happen next.
High on Maui,
the next island in the chain,
NASA scientists at the satellite
laser ranging station
are preparing
for a long night's work.
They're setting up to fire
a laser beam
at a satellite target
orbiting the Earth.
The information they gain
will tell them, to the inch,
how fast the island, and the
Pacific plate on which it rests,
are moving across the ocean.
They have to time
the firing exactly
to be sure
that no planes are passing.
any pilot
who might look at it directly.
Okay, we're at 227 Azimuth.
18 degrees ''L''.
This is starlit.
Culmination's at 74 degrees.
We're rotating clockwise.
Okay, you'll be clear to fire.
We're at 21.
Going down.
and bounces back,
pinpointing their location.
22 years of calculations confirm
that Maui and the Pacific plate
are moving northwest at the
rate of 2.5 inches a year--
amazingly fast.
This is the absolute proof
that the surface of our planet
is in constant motion.
Tectonic theory says that the
volcanoes of the Hawaiian chain
should get progressively older
and become more eroded
the further they travel
from the hot spot.
And they do.
One day,
the raging fires of Kilauea
will be as silent and cold
as these dead cones.
But the heir to them all
is already emerging.
As one island dies,
a new one is formed.
The hot spot is currently moving,
or manifesting itself,
at Lo'ihi,
which is a submarine seamount
to the south
of the Big Island of Hawaii
and still more than 3,000 feet
beneath the surface
of the ocean.
It may be another 100,000 years
before we see Lo'ihi surface.
At the same time,
the hot spot is causing
destruction elsewhere,
the pressure of the continual
input of magma from below
is bulldozing open
this great crack
which stretches across
the length of the island.
It is more than 80 feet deep,
and it's splitting away
at 3 inches a year.
Eventually, the whole side
of the mountain will fail
and collapse into the sea.
It will send a giant wave
racing away to the Pacific Rim,
to reach the west coast
of the Americas in a few hours,
causing massive destruction.
We can't predict or prevent
these catastrophes.
The geological truce
between ourselves
and our restless planet
may be coming to an end.
Cataclysms may have caused
extinctions and disasters,
but they have also shaped
the Earth
and produced an environment
in which human life
could flourish--
the air breathable,
the seas are warm,
climate mild, the ice rooted
firmly at the poles.
In fact, a geological truce.
But that truce
may be coming to an end.
The forces that drive the Earth
are impervious to our needs.
With man so widely spread
across the planet,
cataclysms of nature will turn
into human catastrophes.
Every movement of the plates
brings the danger
of disaster nearer.
50 million years ago,
the Asian and Indian plates
were about to clash.
Separated by a dying ocean,
they collided
with fantastic force.
Neither would give way,
and the land had
only one way to go-- up.
This is the world's highest
mountain range, the Himalayas.
This entire area was uplifted
from sea level
to over 5 miles high
in less than 30 million years.
How do the scientists know?
From the evidence of the rocks.
There's dramatic evidence
for this uplift
right in the face of Everest,
in Lhotse.
The famous yellow band
that you can see cutting across
is actually a marine limestone.
It was formed
in the bottom of the ocean.
So 50 million years ago,
the tops of these mountains
were at the bottom of the sea.
It's hard to believe.
We have similar evidence
from Tibet,
Where we find things
like this--
ammonite fossils
of marine creatures
that now are more than
4,000 meters above sea level.
Certainly these tell us
that plate tectonics
supplies enough force
to lift things
from the bottom of the ocean
all the way to here,
the top of the world.
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