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Earth, a 4.5- Billion-year-old planet,
still evolving.

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As continents shift and clash, volcanoes
erupt, glaciers grow and recede,

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the Earth's crust is carved
in countless fascinating ways,

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leaving a trail of geological
mysteries behind.

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Water.

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One of the most powerful
forces on the planet.

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It plays a crucial role in creating life
and destroying it,

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in forging landscapes
and in breaking apart the Earth.

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In its most dramatic form, it becomes
a killer wave known as a tsunami.

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Until recently, predicting when
these monsters may next strike

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has been impossible.

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But today, scientists are starting
to understand these giant waves.

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By connecting clues as varied as ancient
Japanese writings and landslides,

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ancient corals and buried
Native American settlements,

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the secrets of tsunamis
are finally being unlocked.

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Tsunamis. One of the most
deadly forces of nature.

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Giant waves that travel faster
than a jet plane,

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they can cross entire oceans
in just hours.

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They have the power to smash buildings,
vehicles, anything in their way.

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MAN: By itself, you wouldn't
think that water just streaming

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into the coast would necessarily
cause so much damage.

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But in fact, they are very fast moving
and they pick up everything in its path,

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so it's not the water by itself,
it's what comes with the water

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that is also a part of the big hazard.

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A tsunami isn't over
in just a few seconds,

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it is a torrent of raging water
that keeps coming.

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The main thing about a tsunami
is the persistence.

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It comes on and on and on,
and just when you think it has to quit,

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it keeps coming, and it's the
power plus the... the duration

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that is unstoppable, really.

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Tsunamis have ravaged
the Earth for billions of years.

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When the Earth was first created,
the moon was much closer.

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It filled the sky.

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Its gravitational pull
was much stronger,

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and it generated towering waves
over half a mile high

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that raced across the primeval oceans.

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MAN: Oh, my God!

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(SCREAMING)

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Today, tsunamis are still a threat
to coastlines all over the world.

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MOONEY: Tsunamis will always occur,
and have always occurred,

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throughout Earth's history.

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But it's only been more recently,
as population densities have increased

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and people have moved
and migrated to the coastal regions,

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that we've become much
more aware of the tsunami hazards.

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The investigation into what
caused these monster waves

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began over a thousand years ago

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on the islands of Japan.

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This country is the world's
tsunami hotspot.

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Its coasts have been pounded
with these enormous waves

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more than anywhere else on the planet.

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Evidence for this
is the word tsunami itself.

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It is Japanese and literally
means "harbour wave".

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Japan has the longest written tsunami
record of anywhere in the world.

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The records go back as far as 684 A.D.

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By studying these records,
it is possible to work out that,

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on average, this country has been
struck nearly every seven years.

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Samurai writings speak of people
living on the coasts

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running for higher ground
as soon as they felt an earthquake.

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The Japanese knew this was a clue,

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a warning sign that a deadly
tsunami would soon follow.

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But despite their attempts to escape,

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tsunamis have continually brought death
and destruction to these islands.

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In 1896, a wave that hit Honshu
in the northeast

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claimed the lives of 27,000 people.

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In 1933, the same area
was smashed again.

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This time, 3,000 people
were swept away.

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And in 1993, the island of Okushiri
was rocked by an enormous earthquake

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measuring 7.8 on the Richter scale.

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Buildings were levelled and fires raged.
But worse was to come.

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Minutes after the shaking had subsided,

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an ominous white crest
appeared on the horizon - a tsunami.

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A gigantic wave swept in,
flattening any buildings still standing.

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In Japan, the locals had already
worked out the connections

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between earthquakes and tsunamis.

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But there's another hotspot on Earth
where tsunamis regularly strike -

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the Hawaiian islands.

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But very few of them were preceded
by an earthquake.

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The city of Hilo on the Big Island
has been dubbed

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the Tsunami Capital of the World.

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Dozens of these enormous waves
have hit these beautiful islands,

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and the mystery is why.

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With no natural warning to go on,

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the people of Hawaii must rely

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on the world's biggest
tsunami monitoring station.

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Set up in 1949, it is connected
to a network of buoys

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spread across the Pacific Ocean.

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These buoys provide important clues.

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They monitor changes in sea level

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that indicate the approach
of any potential tsunamis.

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In 1960, scientists got the breakthrough
they were looking for.

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They were finally able to work out
the type of event

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at the root of Hawaii's
mystery tsunamis.

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An enormous quake on the coast of
Chile, the biggest recorded of all time,

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with a factor 9.5 on the Richter scale,

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triggered a tsunami that swept
across the entire Pacific Ocean

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in just a few hours.

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The islands of Hawaii were thousands
of miles away, directly in its path.

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The Tsunami Warning Center
was monitoring its progress,

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revealing for the first time
that a single massive wave

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crossed thousands of miles of ocean.

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The warning centre was a success.

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They were able to evacuate
the communities closest to the shore

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before the wave struck.

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But the homes they left
behind were decimated.

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In Hilo, the tsunami was so strong
it even bent parking metres in half.

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The wave continued
past Hawaii to Japan.

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It had lost none of its power.

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Pacific-wide, this tsunami
cost more than 2,000 lives

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and caused millions of dollars' worth
of damage.

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Devastating as it was,

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the 1960 event was a turning point
in the study of tsunamis.

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It was the first time that scientists
could accurately measure

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how the size of
an underwater earthquake

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directly affected the size of a tsunami.

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And conclusive proof
that a tsunami can travel

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thousands of miles across the Earth.

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And It was with this Chilean earthquake
that we really could prove

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that the, uh, undersea motions
associated with the earthquake

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are generating these huge effects.

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Now scientists had
the evidence to confirm

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that undersea earthquakes were
directly responsible for tsunamis.

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The ancient Japanese suspicion
was now scientific fact.

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In terms of modern tsunami study,
the 1960 wave was year zero.

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MOONEY: The Chilean earthquake
was, you might say, the perfect storm,

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it's when scientific understanding
had advanced to the point

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where scientists had begun to see
the link connecting everything,

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so it's a new science,
we're talking about something

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which is really only
less than 50 years old.

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There are more tsunamis in
the Pacific Ocean than any other.

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So in 2004, the world
was taken by surprise

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when one of the largest
recorded tsunamis of all time

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took place in the Indian Ocean.

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On December 26th, 2004,

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Indonesia was rocked by the second
largest recorded earthquake ever,

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9.2 on the Richter scale.

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Minutes later,

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a 90-foot tsunami slammed into
the South-East Asian coastline.

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225,000 men, women
and children lost their lives.

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The Indonesian earthquake
had as much energy in it

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as the total energy consumption
in the United States in one year.

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This enormous burst of energy
had been released in just seconds.

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Once again,
the world had been reminded

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of the Earth's awesome power.

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In the last 50 years, scientists were
finally able to confirm a solid link

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between earthquakes and tsunamis.

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By monitoring the size of the
Chilean earthquake in 1960,

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scientists were able to prove
conclusively that earthquakes

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triggered these gigantic waves.

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By following the path of this tsunami,
they were able to prove

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that a tsunami could travel
thousands of miles from its origin.

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Monitoring the earthquakes that
cause this incredible devastation

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involves looking many miles
underground.

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By investigating the power at
the root of these giant waves,

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scientists can begin to figure out when
and where these waves may strike next.

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These dramatic pictures
of the aftermath

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of the 2004 Indian Ocean tsunami
show the havoc a tsunami can unleash.

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It's almost impossible to
imagine something like that

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happening here in the Pacific Northwest.

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But Professor Brian Atwater believes
that events like the 2004 tsunami

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could one day happen right here too.

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He was intrigued

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by early settlers' accounts
of Native American folklore tales

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that spoke of great waves
sweeping inland.

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They convinced him that
huge, locally generated tsunamis

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have struck here before,
and could strike again,

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posing a threat to tens
of thousands of people

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living on the Pacific Northwest coast.

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To find out if he was right, he needed
to uncover evidence of past giant waves

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hidden in this landscape.

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To be really sure it's a tsunami, though,
he would also have to find evidence

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of the earthquake that caused it.

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Atwater's starting point is the
Copalis River in Washington State,

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just a couple of miles
from the long sandy beaches

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that make this area
a thriving tourist resort.

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In the banks of this estuary lie
buried thousands of years of history.

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This is one of the dirtiest jobs in science.

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Hunting for evidence of earthquakes
is a muddy business, but it's worth it.

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Atwater has found signs
of a potential tsunami.

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There's a clue in this bank
that nature has provided, it's this notch.

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And notches like this are common

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where tsunamis have
laid out sheets of sand

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and then later currents

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and... and waves come along

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and they pluck the sand grains
out of the bank, but they leave the mud.

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Atwater has to dig deeper
to find what he is looking for,

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a layer of sand that could have
been swept miles inland by a tsunami.

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OK, so now you can see the sand.
What deposited this sand?

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Maybe it was a tsunami.

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To prove that this was
sand from a tsunami,

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Atwater's muddy quest must continue.

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He also needs to find proof
that the land here around the river

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has moved up or down -
a sure sign of an earthquake.

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After some hard work, Atwater
finds what he has been looking for -

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clear evidence of both
an earthquake and a tsunami.

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This time, there was
a human cost as well.

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Here we have evidence
for abrupt lowering of land,

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and we also have evidence
for the associated tsunami.

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In this case, humans are involved -
this was a fishing camp.

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Here you have the remains
of that fishing camp

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in the form of fire-cracked rocks
which were...

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The rocks were used
to heat water, mainly.

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OK, so fishing camp,
overrun by tsunami.

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Because the land dropped
after the tsunami,

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the tides came in
and covered the fishing camp site

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and made sure
that people wouldn't use it again.

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The land the fishing camp
was built on was dragged down

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during the earthquake.

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The tsunami deposited sand
over the remains,

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and finally, the tide
covered the settlement with mud,

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where it remained undisturbed -
until now.

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Atwater finally had
the proof he needed.

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00:14:28,807 --> 00:14:34,598
His Native American myths
of giant waves were no mere legend.

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00:14:36,207 --> 00:14:39,327
But what was it
that caused the earthquake?

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The prime suspect lay 50 miles
offshore - the Cascadia fault.

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Cascadia is a major weakness
in the Earth's crust.

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Although the Earth may
seem to be a solid sphere,

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beneath the oceans
and continents it is divided

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into eight major and many minor
segments known as tectonic plates.

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Where they meet, they can grind and
jostle against each other at fault lines,

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causing earthquakes.

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Geologists had long thought
that the Cascadia fault line

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was incapable of generating
a major quake.

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But Atwater's investigation
has proved that it was highly active.

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The big worry for Atwater
and the thousands of people

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who live in this region
is that the Cascadia fault line

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bears an uncanny resemblance
to another highly active fault line,

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the Sunda Megathrust.

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It was an earthquake along
this fault that was responsible

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for the Indian Ocean tsunami that killed
nearly a quarter of a million people.

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Where we get two tectonic plates
coming together,

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such as the case of
the Indonesian tsunami in 2004,

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one plate pushes beneath the other plate

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and creates lots and lots
of friction and tension

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and drags the upper plate down with it,

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and that process can take
hundreds of years,

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even thousands of years.

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It's a very slow process.

238
00:16:04,287 --> 00:16:07,727
But eventually the pressure of this
one trying to push back up again wins,

239
00:16:07,727 --> 00:16:09,718
and it flips like that.

240
00:16:11,567 --> 00:16:14,767
And that creates a megathrust,
a sudden movement of the seabed,

241
00:16:14,767 --> 00:16:18,167
and that's what creates
a phenomenal tsunami.

242
00:16:18,167 --> 00:16:22,967
Two factors made this Sunda
Megathrust earthquake so deadly.

243
00:16:22,967 --> 00:16:24,727
The first was its size.

244
00:16:24,727 --> 00:16:26,967
At factor 9.2 on the Richter scale,

245
00:16:26,967 --> 00:16:31,447
this was the largest
in nearly 50 years.

246
00:16:31,447 --> 00:16:36,767
The second was that it took place
not far below the surface.

247
00:16:36,767 --> 00:16:38,567
BOXALL: When we talk
about a megathrust,

248
00:16:38,567 --> 00:16:41,767
that's really where the seabed
is disturbed dramatically.

249
00:16:41,767 --> 00:16:44,127
Sometimes, if the earthquake
is deep in the Earth's crust,

250
00:16:44,127 --> 00:16:47,487
then you see very little surface
manifestation of that earthquake.

251
00:16:47,487 --> 00:16:50,127
If it's quite close to the surface
or very intense,

252
00:16:50,127 --> 00:16:52,607
then quite often you'll see
the seabed itself moving,

253
00:16:52,607 --> 00:16:55,758
and that's what creates
a powerful tsunami.

254
00:16:57,447 --> 00:17:00,167
Investigating the ocean floor
after the quake

255
00:17:00,167 --> 00:17:04,527
revealed that more than 1,000 miles
of fault line had fractured

256
00:17:04,527 --> 00:17:07,367
and sprung up by 60 feet.

257
00:17:07,367 --> 00:17:11,727
This massive jolt pushed up
billions of tons of water,

258
00:17:11,727 --> 00:17:17,006
enough to cover Manhattan
to a depth of nearly five miles.

259
00:17:19,687 --> 00:17:22,567
The rift zone itself was about
a thousand miles long.

260
00:17:22,567 --> 00:17:26,287
We had this entire stretch
of subsea moving,

261
00:17:26,287 --> 00:17:28,287
which creates a huge wave.

262
00:17:28,287 --> 00:17:31,647
So the whole thing
was a phenomenal size

263
00:17:31,647 --> 00:17:34,286
and certainly one of the biggest
tsunamis in living memory.

264
00:17:35,487 --> 00:17:39,607
Atwater's determined research
showed that the Pacific Northwest

265
00:17:39,607 --> 00:17:42,804
was at risk from this level
of devastation too.

266
00:17:43,807 --> 00:17:48,127
But he didn't want to unnecessarily
alarm the coastal inhabitants

267
00:17:48,127 --> 00:17:51,087
until he had collected
all the evidence he could.

268
00:17:51,087 --> 00:17:56,527
Atwater needed to find out precisely
when this tsunami struck this coastline

269
00:17:56,527 --> 00:17:58,767
to see if there could be more.

270
00:17:58,767 --> 00:18:03,527
He first tried radiocarbon dating the soil
along the Copalis River.

271
00:18:03,527 --> 00:18:06,487
But the result could only take him so far.

272
00:18:06,487 --> 00:18:09,007
They showed that the earthquake
and tsunami occurred

273
00:18:09,007 --> 00:18:13,447
somewhere between 1680 and 1720.

274
00:18:13,447 --> 00:18:19,238
More importantly, Atwater still needed
precise evidence of how big it had been.

275
00:18:20,727 --> 00:18:26,287
But so far, his investigation has
uncovered two extraordinary facts.

276
00:18:26,287 --> 00:18:29,687
By unearthing
the abandoned fishing camp,

277
00:18:29,687 --> 00:18:32,407
Atwater could see that
a Cascadia earthquake here

278
00:18:32,407 --> 00:18:35,167
had caused the land to drop.

279
00:18:35,167 --> 00:18:37,527
The notch in the bank was proof

280
00:18:37,527 --> 00:18:40,807
that this same earthquake
had generated a tsunami.

281
00:18:40,807 --> 00:18:46,287
But what these clues didn't tell Atwater
was just how big the tsunami was.

282
00:18:46,287 --> 00:18:51,647
He had no way of pinning down the size
of the threat to the Pacific Northwest.

283
00:18:51,647 --> 00:18:55,767
His investigation was about
to take an unexpected turn,

284
00:18:55,767 --> 00:18:59,807
with clues coming from not
only thousands of miles away,

285
00:18:59,807 --> 00:19:02,879
but also from hundreds of years ago.

286
00:19:05,447 --> 00:19:10,687
Japan has the oldest record of tsunamis
of anywhere in the world.

287
00:19:10,687 --> 00:19:15,087
Samurai writings told of
a huge tsunami in 1700

288
00:19:15,087 --> 00:19:18,247
that had swept over
the east coast of Japan.

289
00:19:18,247 --> 00:19:23,367
It hit without warning,
and destroyed entire settlements.

290
00:19:23,367 --> 00:19:27,407
Japanese scientists were baffled
as to where this wave had come from.

291
00:19:27,407 --> 00:19:33,007
There had been no earthquake to warn
the villagers to make for higher ground.

292
00:19:33,007 --> 00:19:37,125
The mystery wave was dubbed
an orphan tsunami.

293
00:19:40,007 --> 00:19:41,447
Back in the U.S.,

294
00:19:41,447 --> 00:19:45,367
Brian Atwater's investigation into
the mysterious Cascadia earthquake

295
00:19:45,367 --> 00:19:47,801
and tsunami needed more evidence.

296
00:19:49,807 --> 00:19:55,723
He had no accurate way to pin down
either the size or the date of the event.

297
00:19:56,887 --> 00:20:03,167
All he knew was that it had taken place
sometime between 1680 and 1720.

298
00:20:03,167 --> 00:20:07,887
But Atwater's dates were a revelation
to the Japanese scientists.

299
00:20:07,887 --> 00:20:14,047
Could this event be the birthplace of
their 300-year-old orphan tsunami?

300
00:20:14,047 --> 00:20:16,567
And they said,
"By the way, we have this tsunami

301
00:20:16,567 --> 00:20:20,487
"we've been trying to, uh,
find a home for in 1700,

302
00:20:20,487 --> 00:20:23,967
"so we think your... your earthquake
happened in 1700,

303
00:20:23,967 --> 00:20:27,607
"specifically in the evening
of the 26th of January 1700,

304
00:20:27,607 --> 00:20:29,643
"and it was of magnitude nine."

305
00:20:31,527 --> 00:20:35,447
A Cascadia earthquake that
produced a wave with enough power

306
00:20:35,447 --> 00:20:38,127
to cross the entire Pacific Ocean
to Japan

307
00:20:38,127 --> 00:20:42,006
would have had to be a factor nine
at the very least.

308
00:20:43,087 --> 00:20:48,207
This is roughly equivalent to the
enormous Indian Ocean earthquake.

309
00:20:49,807 --> 00:20:52,487
Earthquakes like this
have so much power

310
00:20:52,487 --> 00:20:58,007
that they can send a tsunami
across an entire ocean with ease.

311
00:20:58,007 --> 00:21:00,807
BOXALL: The amount of energy
involved is very hard to estimate,

312
00:21:00,807 --> 00:21:04,447
and it's hard to put it into sort of terms
that people can understand.

313
00:21:04,447 --> 00:21:08,167
We are looking at the phenomenal
forces of several Hiroshimas,

314
00:21:08,167 --> 00:21:10,317
hundreds of Hiroshimas, in fact.

315
00:21:11,327 --> 00:21:16,967
But tsunamis are not just
a very big wave, they're fast.

316
00:21:16,967 --> 00:21:18,887
The big difference
is the scale of the wave -

317
00:21:18,887 --> 00:21:22,687
it's typically three
or four hundred miles long.

318
00:21:22,687 --> 00:21:24,607
It's also not very high -

319
00:21:24,607 --> 00:21:28,287
when it starts off life,
it's usually about two or three foot high.

320
00:21:28,287 --> 00:21:30,087
But it's moving very fast.

321
00:21:30,087 --> 00:21:33,247
It moves at a speed
determined by the water depth.

322
00:21:33,247 --> 00:21:35,167
The deeper the water,
the faster it moves,

323
00:21:35,167 --> 00:21:40,767
so in the deep ocean, this wave
is moving at over 500 miles an hour.

324
00:21:40,767 --> 00:21:44,287
Deceptively, as a tsunami
speeds through deep water,

325
00:21:44,287 --> 00:21:48,439
it may appear completely harmless
and scarcely detectable.

326
00:21:49,767 --> 00:21:53,247
Close to shore, the wave
becomes a deadly killer.

327
00:21:53,247 --> 00:21:58,640
It is only then that a tsunami's
true power becomes clear.

328
00:22:00,087 --> 00:22:02,487
As the wave gets to shallower
and shallower water,

329
00:22:02,487 --> 00:22:05,687
as it approaches a coastline,
the wave slows down.

330
00:22:05,687 --> 00:22:08,847
The shallower the water, the slower
the wave, so it goes from 500, to 400,

331
00:22:08,847 --> 00:22:10,767
to 300, to 200, much, much slower.

332
00:22:10,767 --> 00:22:12,767
The back of the wave
is still going full speed,

333
00:22:12,767 --> 00:22:17,557
and so the whole thing piles up, and
that's why tsunamis are so destructive.

334
00:22:21,247 --> 00:22:25,847
It is this immense speed and power that
reveals how events here in Cascadia

335
00:22:25,847 --> 00:22:29,607
could devastate
a coastal village in Japan,

336
00:22:29,607 --> 00:22:34,007
how an earthquake in Chile
could decimate Hawaii,

337
00:22:34,007 --> 00:22:36,087
and how the Indian Ocean earthquake

338
00:22:36,087 --> 00:22:39,807
could kill almost
a quarter of a million people.

339
00:22:39,807 --> 00:22:43,687
If a quake like this
happened in Cascadia,

340
00:22:43,687 --> 00:22:47,847
the damage it would do
to the Pacific Northwest coastline

341
00:22:47,847 --> 00:22:49,599
would be catastrophic.

342
00:22:50,647 --> 00:22:53,167
But to be sure about the scale
of this threat,

343
00:22:53,167 --> 00:22:56,087
Brian Atwater has to be 100% certain

344
00:22:56,087 --> 00:23:00,167
that the dates of the two tsunamis
were the same.

345
00:23:00,167 --> 00:23:03,727
After fully exploring the estuary
of the Copalis river,

346
00:23:03,727 --> 00:23:08,047
he found one site that might hold
the information he was looking for -

347
00:23:08,047 --> 00:23:10,767
a ghost forest.

348
00:23:10,767 --> 00:23:15,127
This spruce root marks
the remains of a forest

349
00:23:15,127 --> 00:23:17,487
that includes the ghost forest
behind us,

350
00:23:17,487 --> 00:23:21,719
dropped down into tidewater
during the Cascadia earthquake.

351
00:23:24,527 --> 00:23:26,807
This ghost forest is made up

352
00:23:26,807 --> 00:23:30,167
of the standing dead trunks
of western red cedar,

353
00:23:30,167 --> 00:23:34,607
and they were killed on account
of the land here dropping,

354
00:23:34,607 --> 00:23:38,687
and then tides coming in
and surrounding these trees

355
00:23:38,687 --> 00:23:40,996
and bringing in saltwater.

356
00:23:42,007 --> 00:23:45,795
This area would once have been
covered with a dense forest.

357
00:23:47,207 --> 00:23:51,887
But today, only the bleached trunks
of the rot-resistant western red cedar

358
00:23:51,887 --> 00:23:54,247
remain in place.

359
00:23:54,247 --> 00:23:58,807
When Atwater and expert
tree ring specialists cut them open

360
00:23:58,807 --> 00:24:01,047
and studied the lines of growth inside,

361
00:24:01,047 --> 00:24:06,075
they finally cracked
the 300-year-old tsunami puzzle.

362
00:24:07,167 --> 00:24:10,127
The dates of the Japanese
and Cascadia events

363
00:24:10,127 --> 00:24:11,847
were exactly the same -

364
00:24:11,847 --> 00:24:14,407
January 1700.

365
00:24:14,407 --> 00:24:19,367
The Japanese orphan tsunami
finally had a parent.

366
00:24:19,367 --> 00:24:21,807
Maybe there's a certain
amount of justice to it

367
00:24:21,807 --> 00:24:25,527
that... that a place
that doesn't have written records

368
00:24:25,527 --> 00:24:28,887
has these outstanding
geological records.

369
00:24:28,887 --> 00:24:31,567
The link between the two events
made it certain

370
00:24:31,567 --> 00:24:36,807
that the Cascadia earthquake had been
at least an awesome magnitude nine.

371
00:24:36,807 --> 00:24:40,407
And ominously, it is almost
certainly not the only time

372
00:24:40,407 --> 00:24:43,080
that Cascadia has rocked this area.

373
00:24:44,767 --> 00:24:48,807
Atwater believes he has found proof
of a whole series of tsunamis

374
00:24:48,807 --> 00:24:51,765
stretching back 5,000 years.

375
00:24:52,847 --> 00:24:57,238
Each layer of sand in this sample
represents a separate tsunami.

376
00:24:59,207 --> 00:25:03,007
There are places at Cascadia
where I've seen nine stacked up

377
00:25:03,007 --> 00:25:06,407
in a column about 20 feet long.

378
00:25:06,407 --> 00:25:09,927
Uh, nine buried soils, some of
them coated with little sand sheets.

379
00:25:09,927 --> 00:25:11,807
And... and they, you know,
you... you say,

380
00:25:11,807 --> 00:25:16,358
"OK, it's... it's not a question of if,
but it's just a matter of when."

381
00:25:18,807 --> 00:25:22,007
Atwater's tireless detective work
alerted officials

382
00:25:22,007 --> 00:25:24,441
to the increased tsunami threat.

383
00:25:25,687 --> 00:25:29,447
As a result, the towns
along the Washington State coast

384
00:25:29,447 --> 00:25:32,598
have been able to prepare
for this potential catastrophe.

385
00:25:34,047 --> 00:25:38,167
If a Cascadia quake occurred,
the first waves could arrive here

386
00:25:38,167 --> 00:25:40,203
in just 25 minutes.

387
00:25:41,207 --> 00:25:45,967
Tsunami warning signs line the roads,
and sirens stand ready to warn

388
00:25:45,967 --> 00:25:48,407
of an approaching wave.

389
00:25:48,407 --> 00:25:54,607
The lives of thousands of people are
safer thanks to the work of Atwater,

390
00:25:54,607 --> 00:25:58,077
and to some 300-year-old
Japanese writings.

391
00:25:59,127 --> 00:26:04,087
This is a hazard that shows its face
often enough for us to take precautions,

392
00:26:04,087 --> 00:26:06,807
to fasten the seatbelt against it.

393
00:26:06,807 --> 00:26:11,447
By dating the ghost forest along
the Copalis River to precisely 1700,

394
00:26:11,447 --> 00:26:16,047
Atwater had the final proof that
Cascadia was capable of creating

395
00:26:16,047 --> 00:26:18,967
a Pacific-wide tsunami.

396
00:26:18,967 --> 00:26:22,887
Uncovering the multiple layers
of tsunami debris in the riverbank

397
00:26:22,887 --> 00:26:26,327
dating back 5,000 years
show that monster waves

398
00:26:26,327 --> 00:26:28,647
have struck here many times.

399
00:26:28,647 --> 00:26:31,241
This is an ongoing threat.

400
00:26:32,487 --> 00:26:35,007
Atwater knows that another
earthquake is due here,

401
00:26:35,007 --> 00:26:39,607
but he has no way of
knowing exactly when.

402
00:26:39,607 --> 00:26:41,647
Back in the Indian Ocean,

403
00:26:41,647 --> 00:26:45,527
the site of the world's most
lethal tsunami in 2004,

404
00:26:45,527 --> 00:26:50,367
one man has taken the investigation
of tsunamis to a new level.

405
00:26:50,367 --> 00:26:54,047
He believes that he has found a way
to make the Earth's fault lines

406
00:26:54,047 --> 00:26:58,327
give up their secrets and accurately
predict when the next deadly tsunami

407
00:26:58,327 --> 00:27:01,364
could be on its way.

408
00:27:05,087 --> 00:27:10,527
The idyllic looking Mentawai island chain
in Indonesia hides a violent secret,

409
00:27:10,527 --> 00:27:15,157
one that makes it today one of the
most dangerous places on Earth.

410
00:27:16,527 --> 00:27:20,127
These islands lie directly on top
of the Sunda Megathrust,

411
00:27:20,127 --> 00:27:22,927
south of where the enormous
Indian Ocean earthquake

412
00:27:22,927 --> 00:27:25,927
triggered the 2004 tsunami.

413
00:27:25,927 --> 00:27:30,407
The Sunda Megathrust is one of
the largest fault lines on the planet.

414
00:27:30,407 --> 00:27:33,887
Since it caused the 2004 earthquake,

415
00:27:33,887 --> 00:27:37,038
it has also become
one of the most notorious.

416
00:27:39,847 --> 00:27:41,927
Predicting earthquakes here is tricky,

417
00:27:41,927 --> 00:27:46,007
but Professor Kerry Sieh
has a good track record.

418
00:27:46,007 --> 00:27:51,365
He has successfully forecast two
along the Sunda Megathrust already.

419
00:27:53,127 --> 00:27:56,527
The key to successful tsunami
prediction is to forecast

420
00:27:56,527 --> 00:27:59,247
when and where
earthquakes will strike.

421
00:27:59,247 --> 00:28:03,927
And to do this,
scientists must look into the past.

422
00:28:03,927 --> 00:28:06,087
SIEH: If you want to answer
questions about earthquakes

423
00:28:06,087 --> 00:28:08,087
that only happen
every few hundred years

424
00:28:08,087 --> 00:28:09,887
or few thousand years,

425
00:28:09,887 --> 00:28:13,567
well, you've got to find some...
some geological instrument

426
00:28:13,567 --> 00:28:16,567
that allows you to see
those earthquakes.

427
00:28:16,567 --> 00:28:18,727
Professor Sieh has found
an unusual way

428
00:28:18,727 --> 00:28:23,967
to unlock the secrets of the Sunda
Megathrust's turbulent history.

429
00:28:23,967 --> 00:28:26,007
Corals.

430
00:28:26,007 --> 00:28:28,527
These coral atolls are built
from the limestone skeletons

431
00:28:28,527 --> 00:28:31,087
of millions of tiny creatures.

432
00:28:31,087 --> 00:28:35,367
Each generation builds
on the remains of the last.

433
00:28:35,367 --> 00:28:38,967
Over time, the atoll
gets bigger and bigger.

434
00:28:38,967 --> 00:28:42,687
As long as the corals
remain underwater, they flourish,

435
00:28:42,687 --> 00:28:46,047
but once they're above water, they die.

436
00:28:46,047 --> 00:28:50,447
Earthquakes are responsible
for killing all the coral stranded

437
00:28:50,447 --> 00:28:53,007
above water on this beach.

438
00:28:54,687 --> 00:28:57,767
This beach contains corals
of many different ages.

439
00:28:57,767 --> 00:29:01,607
Altogether, Professor Sieh has
nearly a thousand years of history

440
00:29:01,607 --> 00:29:03,807
at his fingertips.

441
00:29:03,807 --> 00:29:07,047
But to unlock the secret history
the corals contain,

442
00:29:07,047 --> 00:29:11,847
he and his team have to take
a less than delicate approach.

443
00:29:11,847 --> 00:29:16,007
We're looking at a sawcut that we
just made through a coral micro atoll.

444
00:29:16,007 --> 00:29:19,047
And the great thing about this head
is it records a sudden drop

445
00:29:19,047 --> 00:29:22,047
of about a foot and a half down to here.

446
00:29:22,047 --> 00:29:24,327
It died down to here,
because the island rose.

447
00:29:24,327 --> 00:29:26,087
The new low tide is way down here.

448
00:29:26,087 --> 00:29:29,284
Everything that was so bold
as to grow up this high dies.

449
00:29:31,247 --> 00:29:34,647
The shape of the coral records
the fall of the Mentawai islands

450
00:29:34,647 --> 00:29:38,879
as they are literally pulled down
by the Sunda Megathrust.

451
00:29:39,887 --> 00:29:43,567
But, crucially, the corals
also record the moments

452
00:29:43,567 --> 00:29:49,247
when the islands are thrust up out
of the water during an earthquake.

453
00:29:49,247 --> 00:29:53,287
Between quakes, the islands are
once again pulled down by the fault

454
00:29:53,287 --> 00:29:55,517
in a never-ending cycle.

455
00:29:57,727 --> 00:30:00,287
You have to imagine that
rocks actually are elastic.

456
00:30:00,287 --> 00:30:03,447
Take a diving board, the diver...
the diver walks out on the platform

457
00:30:03,447 --> 00:30:05,087
and it... it bends like this,

458
00:30:05,087 --> 00:30:07,887
and then he jumps and he springs up
and he jumps off.

459
00:30:07,887 --> 00:30:10,847
And when he jumps off,
the diving board doesn't stay here,

460
00:30:10,847 --> 00:30:13,167
it doesn't go like... it doesn't go like this,

461
00:30:13,167 --> 00:30:16,087
you know, the diving board
springs back up, it's elastic.

462
00:30:16,087 --> 00:30:18,767
Well, rocks are the same,
rocks are elastic too,

463
00:30:18,767 --> 00:30:23,287
so when the Indian Plate goes down
it pulls the Sumatran section down too,

464
00:30:23,287 --> 00:30:25,527
and then later, it fails.

465
00:30:25,527 --> 00:30:27,836
So it just springs up like a diving board.

466
00:30:28,847 --> 00:30:31,527
By analysing corals all over this beach,

467
00:30:31,527 --> 00:30:35,805
Professor Sieh has discovered
a regular pattern to this cycle.

468
00:30:36,807 --> 00:30:41,517
A major earthquake rocks these islands
roughly every 200 years.

469
00:30:43,607 --> 00:30:47,927
What we have here in Sumatra with
the corals is what I call the Holy Grail

470
00:30:47,927 --> 00:30:51,047
of, uh... of earthquake science,
of... of palaeoseismology,

471
00:30:51,047 --> 00:30:54,767
and that is a long record
that has many cycles in it,

472
00:30:54,767 --> 00:30:58,047
a thousand-year-long history
of earthquakes.

473
00:30:58,047 --> 00:31:00,647
But when the geologist
looked even closer,

474
00:31:00,647 --> 00:31:03,366
he saw that the cycle
was more complex.

475
00:31:04,727 --> 00:31:07,687
When we cut a slab, we can see it
in much more exquisite detail

476
00:31:07,687 --> 00:31:09,807
because we can see
what we call the stratigraphy,

477
00:31:09,807 --> 00:31:11,607
or the... the... the layering

478
00:31:11,607 --> 00:31:14,687
and how the layering relates
to the changes of the tide,

479
00:31:14,687 --> 00:31:19,127
so what we can see over here, then, is
the annual bands of growth, right here,

480
00:31:19,127 --> 00:31:24,599
so there's about ten years between
this earthquake and this earthquake.

481
00:31:26,487 --> 00:31:29,887
Professor Sieh
had discovered a major clue.

482
00:31:29,887 --> 00:31:34,687
The corals record that, not only does
a major earthquake and tsunami hit here

483
00:31:34,687 --> 00:31:37,847
every 200 years, but that
they are always accompanied

484
00:31:37,847 --> 00:31:41,127
by a number of smaller quakes.

485
00:31:41,127 --> 00:31:45,757
This is a cycle within a cycle,
a supercycle.

486
00:31:47,047 --> 00:31:49,847
And by counting back the layers
of growth within the coral,

487
00:31:49,847 --> 00:31:54,367
the geologists can put an exact date
on all of these earthquakes.

488
00:31:54,367 --> 00:31:56,807
We know there's a sequence
in the 1350s, 1370s,

489
00:31:56,807 --> 00:32:01,367
we know there's a sequence
in the 1560s, 1600s... 1600,

490
00:32:01,367 --> 00:32:05,127
we know there's a sequence
1797, 1833.

491
00:32:05,127 --> 00:32:08,961
Those sequences are about 200,
to 200... yeah, 230 years apart.

492
00:32:10,367 --> 00:32:15,047
This is crucial information
for the people of the Mentawai islands,

493
00:32:15,047 --> 00:32:17,327
who have no written history.

494
00:32:17,327 --> 00:32:19,927
But Professor Sieh's work
doesn't stop here.

495
00:32:19,927 --> 00:32:23,367
By uncovering their history
in the corals,

496
00:32:23,367 --> 00:32:27,155
he believes that he can now predict
the future for these islands.

497
00:32:28,487 --> 00:32:31,407
And he's already had some success.

498
00:32:31,407 --> 00:32:35,047
Professor Sieh began his work here
in 1993,

499
00:32:35,047 --> 00:32:38,527
and soon realised an earthquake
was imminent.

500
00:32:38,527 --> 00:32:43,317
The Mentawai islands were about
to start their next deadly supercycle.

501
00:32:44,687 --> 00:32:47,207
MAN: OK! Experienced
an earthquake!

502
00:32:47,207 --> 00:32:50,487
In September 2007, he was proved right,

503
00:32:50,487 --> 00:32:54,727
when an earthquake shook the islands
just enough to generate a small tsunami

504
00:32:54,727 --> 00:32:57,321
that wrecked homes and schools.

505
00:33:00,207 --> 00:33:04,166
History is repeating itself,
exactly as he predicted it would.

506
00:33:05,447 --> 00:33:07,567
A much bigger earthquake

507
00:33:07,567 --> 00:33:11,765
and more dangerous tsunami
could be due any day.

508
00:33:12,847 --> 00:33:15,607
SIEH: One section
hasn't failed since 1797,

509
00:33:15,607 --> 00:33:19,487
so, since George Washington
was President of the United States.

510
00:33:19,487 --> 00:33:22,207
We know we're now in a sequence
of at least three giant earthquakes,

511
00:33:22,207 --> 00:33:23,847
we're expecting another one.

512
00:33:23,847 --> 00:33:25,847
The question is whether
the earthquake and tsunami

513
00:33:25,847 --> 00:33:28,759
will be in the next 30 minutes
or the next 30 years.

514
00:33:29,967 --> 00:33:32,287
Thanks to Sieh's research,

515
00:33:32,287 --> 00:33:35,247
the people of these islands
have had time to prepare.

516
00:33:35,247 --> 00:33:38,487
When the wave comes,
they will be ready.

517
00:33:38,487 --> 00:33:41,047
Earthquakes
are forecastable.

518
00:33:41,047 --> 00:33:43,927
If you... if you have enough information
about how they've behaved

519
00:33:43,927 --> 00:33:47,087
over the last thousand years,
or two or three or four cycles,

520
00:33:47,087 --> 00:33:49,207
you can really make
a significant forecast

521
00:33:49,207 --> 00:33:52,085
that people living in the area
actually can do something about.

522
00:33:54,047 --> 00:33:56,767
Education is key.

523
00:33:56,767 --> 00:33:58,447
Children here are now taught

524
00:33:58,447 --> 00:34:01,367
that as soon as they feel
the shaking of an earthquake,

525
00:34:01,367 --> 00:34:03,358
they should run for higher ground.

526
00:34:05,727 --> 00:34:10,327
Newly built roads snake up
steep hills from waterside villages

527
00:34:10,327 --> 00:34:13,046
to allow rapid escape
from the deadly waves.

528
00:34:14,167 --> 00:34:18,367
I'll bet that young children alive today,
if they... certainly if they live to be 60,

529
00:34:18,367 --> 00:34:20,167
they're gonna see that earthquake.

530
00:34:20,167 --> 00:34:23,367
In fact, I think there's a better than
50% chance that it'll happen in...

531
00:34:23,367 --> 00:34:24,847
...within the next 30 years.

532
00:34:24,847 --> 00:34:28,607
By analysing the shape of the corals
on the Mentawai islands,

533
00:34:28,607 --> 00:34:34,127
Sieh has proved that a major tsunami
cycle starts here every 200 years.

534
00:34:34,127 --> 00:34:38,887
By dating the lines within the coral,
he can be even more exact.

535
00:34:38,887 --> 00:34:43,677
They show that these cycles contain not
just one, but several deadly tsunamis.

536
00:34:44,807 --> 00:34:48,800
The Sunda Megathrust
is the clear culprit for tsunamis here.

537
00:34:49,807 --> 00:34:53,567
But not every tsunami is generated
by an earthquake.

538
00:34:53,567 --> 00:34:59,517
A rarer, different type of wave
is out there - a megatsunami.

539
00:35:04,487 --> 00:35:08,567
Although earthquakes are by far
the most common cause of tsunamis,

540
00:35:08,567 --> 00:35:13,807
there is another source
for these deadly waves - landslides.

541
00:35:13,807 --> 00:35:17,287
And these tsunamis
have the potential to be so big

542
00:35:17,287 --> 00:35:20,916
that they have been called
megatsunamis.

543
00:35:22,167 --> 00:35:26,527
Scientists had long suspected that
waves could be generated in this way,

544
00:35:26,527 --> 00:35:32,284
but conclusive photographic proof
wasn't available until 1958.

545
00:35:33,607 --> 00:35:37,447
A landslide into Lituya Bay
in Alaska triggered a wave

546
00:35:37,447 --> 00:35:40,883
that reached heights
of several thousand feet.

547
00:35:42,207 --> 00:35:45,247
This footage,
shot just after the tsunami struck,

548
00:35:45,247 --> 00:35:47,967
shows the wave's enormous power.

549
00:35:47,967 --> 00:35:52,527
The trees here once stretched all
the way down to the shores of the bay,

550
00:35:52,527 --> 00:35:55,767
but were ripped off the slopes
by a wall of water,

551
00:35:55,767 --> 00:35:59,316
leaving nothing but bare exposed rock.

552
00:36:00,887 --> 00:36:04,247
The tsunami was generated
when a relatively small earthquake

553
00:36:04,247 --> 00:36:06,487
triggered a single enormous landslide

554
00:36:06,487 --> 00:36:09,559
of rocks and debris into the bay.

555
00:36:11,447 --> 00:36:14,967
The resulting wave was higher
than the Empire State Building

556
00:36:14,967 --> 00:36:18,807
and stunned scientists
around the world.

557
00:36:18,807 --> 00:36:22,766
Tsunamis on this scale
are incredibly rare.

558
00:36:24,847 --> 00:36:26,647
But another megatsunami,

559
00:36:26,647 --> 00:36:30,927
triggered by a rockfall 10,000
times bigger than Lituya Bay,

560
00:36:30,927 --> 00:36:36,240
could be on its way from a small island
across the Atlantic Ocean.

561
00:36:37,767 --> 00:36:39,807
The Canary Islands,
off the coast of Africa,

562
00:36:39,807 --> 00:36:43,004
are formed from a series of volcanoes.

563
00:36:45,167 --> 00:36:47,847
The youngest is the island
of La Palma.

564
00:36:47,847 --> 00:36:50,927
It is formed from two volcanic ridges.

565
00:36:50,927 --> 00:36:56,367
The first is the extinct Cumbre Nueva
to the north of the island.

566
00:36:56,367 --> 00:37:01,202
The younger, active Cumbre Vieja
lies to the south.

567
00:37:02,607 --> 00:37:05,997
It erupted as recently as 1971.

568
00:37:09,127 --> 00:37:12,727
Geologist Dr Simon Day's
research was crucial

569
00:37:12,727 --> 00:37:15,527
in developing the La Palma
megatsunami theory.

570
00:37:15,527 --> 00:37:18,287
It began with an unusual rift

571
00:37:18,287 --> 00:37:22,963
that had opened up during
a major volcanic eruption in 1949.

572
00:37:25,367 --> 00:37:31,367
We're standing here in the fault
and it runs way down to the south

573
00:37:31,367 --> 00:37:34,207
along the crest of the volcano
for two and a half miles,

574
00:37:34,207 --> 00:37:36,926
so it's one
continuous long structure.

575
00:37:38,047 --> 00:37:42,487
Day believes this fault is evidence
of a geological time bomb,

576
00:37:42,487 --> 00:37:45,923
the beginning of a giant landslide.

577
00:37:47,367 --> 00:37:50,887
What we see here to my right
are layers of... of volcanic rocks,

578
00:37:50,887 --> 00:37:54,007
volcanic blocks here
and layers of volcanic ash.

579
00:37:54,007 --> 00:37:57,567
And on the west of the fault,
we see the same layers of blocks

580
00:37:57,567 --> 00:38:00,847
and ash and those, before
the fault moved, were joined up

581
00:38:00,847 --> 00:38:03,087
and then when the fault moved,
they were separated

582
00:38:03,087 --> 00:38:06,847
and the rocks to my left
moved down and to the west.

583
00:38:06,847 --> 00:38:10,727
What we think will happen
in some future eruption

584
00:38:10,727 --> 00:38:13,767
is that this fault will have gotten bigger

585
00:38:13,767 --> 00:38:19,487
and the whole of this western side
will slide away in a giant landslide

586
00:38:19,487 --> 00:38:21,921
into the ocean to create the tsunami.

587
00:38:23,607 --> 00:38:28,407
This landslide would send the entire
southwest section of La Palma,

588
00:38:28,407 --> 00:38:32,687
one sixth of the island's total mass,
crashing into the Atlantic Ocean

589
00:38:32,687 --> 00:38:35,887
in a single giant landslide.

590
00:38:35,887 --> 00:38:38,567
What we envisage
is the whole of this coastline

591
00:38:38,567 --> 00:38:42,127
and the slope extending up all the way
to the crest of the volcano

592
00:38:42,127 --> 00:38:45,927
that is now in the clouds, all of
that mass of rock would slide away

593
00:38:45,927 --> 00:38:49,367
in a single massive landslide
into the ocean

594
00:38:49,367 --> 00:38:54,727
and pushing the water up in front
of it to create the tsunami wave.

595
00:38:54,727 --> 00:38:58,287
Initially, this wave would be
over 30 times bigger

596
00:38:58,287 --> 00:39:04,887
than the 2004 Indian Ocean tsunami,
more than 3,000 feet high.

597
00:39:04,887 --> 00:39:06,127
(EXPLOSION)

598
00:39:06,127 --> 00:39:10,727
The 1980 eruption of Mount St Helens
was proof that a volcano could collapse

599
00:39:10,727 --> 00:39:13,847
in this terrifying fashion.

600
00:39:13,847 --> 00:39:17,247
This was impressive, but the
collapse of the Cumbre Vieja

601
00:39:17,247 --> 00:39:21,206
would be 200 times the volume of this.

602
00:39:22,287 --> 00:39:23,607
(LOUD RUMBLING)

603
00:39:23,607 --> 00:39:30,683
1,200 billion tons of rock would hurtle
towards the ocean at top speed.

604
00:39:31,927 --> 00:39:36,287
The resulting wave would head
straight out into the Atlantic.

605
00:39:36,287 --> 00:39:38,447
DAY: That wave, of course,
would then spread out

606
00:39:38,447 --> 00:39:40,847
and separate out into smaller waves,

607
00:39:40,847 --> 00:39:46,967
but even so, after crossing the Atlantic
and piling up again on,

608
00:39:46,967 --> 00:39:50,007
for example, the eastern seaboard of
the United States or in the Caribbean

609
00:39:50,007 --> 00:39:53,767
or in northern Brazil,
the waves there, we predict,

610
00:39:53,767 --> 00:39:56,767
would still be between
30 and 100 feet high.

611
00:39:56,767 --> 00:40:00,887
So that's as large as, if not larger,

612
00:40:00,887 --> 00:40:05,005
than the tsunami
that struck Sumatra in 2004.

613
00:40:07,247 --> 00:40:08,805
Boston...

614
00:40:13,927 --> 00:40:15,485
New York...

615
00:40:19,087 --> 00:40:24,207
...and even Miami could all be
under threat from the giant waves.

616
00:40:29,967 --> 00:40:31,807
This was a bold prediction.

617
00:40:31,807 --> 00:40:35,567
Day needed more evidence
to back up his theory.

618
00:40:35,567 --> 00:40:39,927
As he was about to see,
the rift in La Palma's landscape

619
00:40:39,927 --> 00:40:43,167
was far worse than he expected.

620
00:40:43,167 --> 00:40:49,117
The 1949 eruption had left a different
type of geological scar on the island.

621
00:40:51,007 --> 00:40:53,887
Evidence of a more serious weakness
within La Palma

622
00:40:53,887 --> 00:40:58,165
came from a series of eerie-looking
lava flows dotted across the island.

623
00:41:00,927 --> 00:41:04,767
One of the characteristics of
the 1949 eruption that's unusual

624
00:41:04,767 --> 00:41:09,047
is that, instead of starting at one vent
and just continuing there,

625
00:41:09,047 --> 00:41:13,807
a series of volcanic vents opened up
in different parts of the island.

626
00:41:13,807 --> 00:41:16,167
When Day plotted these
weaknesses on a map,

627
00:41:16,167 --> 00:41:18,767
he came to a frightening conclusion.

628
00:41:18,767 --> 00:41:22,521
The rift was far bigger
than he had first suspected.

629
00:41:23,567 --> 00:41:27,727
The area that's potentially affected
is very much greater

630
00:41:27,727 --> 00:41:31,647
than the length of the fault at
the crest of the volcano would indicate,

631
00:41:31,647 --> 00:41:36,323
extending out, um, 10 or 15 miles
from the crest out to sea.

632
00:41:37,567 --> 00:41:39,407
This growing body
of evidence proved

633
00:41:39,407 --> 00:41:43,847
that the rift wasn't just a mere crack
in the surface of La Palma,

634
00:41:43,847 --> 00:41:46,567
but a deep fissure
that reached hundreds of feet

635
00:41:46,567 --> 00:41:49,367
down into the island's foundations.

636
00:41:49,367 --> 00:41:54,282
It is La Palma's volcanic heritage
that is the key to this tsunami threat.

637
00:41:55,527 --> 00:41:58,087
The big hazard here
isn't the eruptions themselves,

638
00:41:58,087 --> 00:42:00,967
it's the fact that the volcano is
building up and building up over time

639
00:42:00,967 --> 00:42:05,438
and becoming more and more unstable,
so that will eventually lead to a collapse.

640
00:42:06,447 --> 00:42:10,407
And it seems that this is not
the first time a La Palma eruption

641
00:42:10,407 --> 00:42:12,967
may have triggered a giant landslide.

642
00:42:12,967 --> 00:42:17,567
Proof lies in the north of the island
in these sheer cliff faces,

643
00:42:17,567 --> 00:42:20,604
formed 65,000 years ago.

644
00:42:21,687 --> 00:42:26,607
What we see in the north of
La Palma is the landslide scar left

645
00:42:26,607 --> 00:42:30,127
when the old volcano
in the north of La Palma

646
00:42:30,127 --> 00:42:33,407
experienced a giant collapse

647
00:42:33,407 --> 00:42:36,683
and produced a giant landslide
off to the west.

648
00:42:38,367 --> 00:42:39,967
So that was a huge collapse -

649
00:42:39,967 --> 00:42:43,807
it removed as much as
100 cubic miles of rock

650
00:42:43,807 --> 00:42:47,247
and deposited it out into the ocean,
so it's the sort of event

651
00:42:47,247 --> 00:42:49,287
that we think is going to happen again

652
00:42:49,287 --> 00:42:51,847
in the future
at the... at the Cumbre Vieja.

653
00:42:53,247 --> 00:42:56,767
This ancient collapse of the
old Cumbre Nueva volcano

654
00:42:56,767 --> 00:43:01,397
is almost certain to have generated
a gigantic wave.

655
00:43:03,487 --> 00:43:07,567
And the next collapse
might not be that far away.

656
00:43:07,567 --> 00:43:10,400
This tsunami could strike in our lifetime.

657
00:43:15,647 --> 00:43:17,607
DAY: Even though
it seems so extraordinary

658
00:43:17,607 --> 00:43:19,327
when we consider it in human terms,

659
00:43:19,327 --> 00:43:22,567
and we talk about a tsunami striking
the east coast of North America

660
00:43:22,567 --> 00:43:26,727
and causing huge devastation
on the scale of the Sumatra tsunami,

661
00:43:26,727 --> 00:43:29,487
but this is what happens
in the geological record,

662
00:43:29,487 --> 00:43:32,684
this is what Earth does.

663
00:43:33,887 --> 00:43:37,687
Although tsunamis have been
documented for thousands of years,

664
00:43:37,687 --> 00:43:41,607
it is only in the last century that
geologists have been able to prove

665
00:43:41,607 --> 00:43:44,644
how they are connected
to the movements of the Earth.

666
00:43:46,647 --> 00:43:50,847
By analysing data from the great
Chilean earthquake of 1960,

667
00:43:50,847 --> 00:43:55,367
scientists were finally able to firmly link
earthquakes with tsunamis.

668
00:43:55,367 --> 00:43:58,487
Unearthing buried
Native American settlements

669
00:43:58,487 --> 00:44:02,607
proved that the Cascadia fault line
in the Pacific Northwest

670
00:44:02,607 --> 00:44:05,327
was an active tsunami threat.

671
00:44:05,327 --> 00:44:10,167
Corals in the Indian Ocean proved that
some earthquake-generated tsunamis

672
00:44:10,167 --> 00:44:15,247
follow a pattern, and strike the
same area with regular intervals.

673
00:44:15,247 --> 00:44:19,727
And the giant rift in La Palma's
landscape shows that tsunamis

674
00:44:19,727 --> 00:44:25,967
generated by landslides are also
a very real threat, megatsunamis,

675
00:44:25,967 --> 00:44:30,324
which could prove to be the biggest
waves that threaten our coastline.

676
00:44:31,327 --> 00:44:33,167
Tsunamis are an inevitable part

677
00:44:33,167 --> 00:44:35,727
of Earth's dynamic structure.

678
00:44:35,727 --> 00:44:38,007
Their capacity to destroy

679
00:44:38,007 --> 00:44:39,407
is awesome,

680
00:44:39,407 --> 00:44:40,807
but, as
scientists

681
00:44:40,807 --> 00:44:42,287
begin to understand more

682
00:44:42,287 --> 00:44:43,887
about the origins of tsunamis,

683
00:44:43,887 --> 00:44:46,407
they are coming closer to predicting

684
00:44:46,407 --> 00:44:49,524
where and when
these monsters may strike.

