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NARRATOR:
Volcanologists climb
into the inferno

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on two of the planet's
most active volcanos...

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TOM:
This is actually
a bit worrying.

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This is an impact
from an explosion.

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NARRATOR:
Where nature's raw power
lay at every turn...

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[Explosion]

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TOM:
It was so fast,
I couldn't even get scared.

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NARRATOR:
And see firsthand the elements
that are shaping this earth.

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TOM:
This volcano is capable
of producing

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very powerful explosions.

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TOM:
It's never a
safe place to be,

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on the rim
of an active crater.

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NARRATOR:
This is the realm of
nature's greatest spectacle.

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♪♪♪

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♪♪♪

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♪♪♪

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♪♪♪

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♪♪♪

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♪♪♪

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♪♪♪

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NARRATOR:
Indonesia is called
the land of fire.

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And for good reason.

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It has 147 active
volcanos.

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Two of them,
Dukono and Ibu,

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are considered to be among
the most active volcanoes

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on the planet.

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In spite of the intense
level of activity,

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they're rarely visited
or photographed.

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That's because of
their location:

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in a remote part
of a country

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that is made up of more
than 17,000 islands.

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NARRATOR:
Volcanologist and
photographer Tom Pfeiffer

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runs a tour company
and a news website:

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Volcano Discovery.

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The website is an important
resource on volcanic activity

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used by scientists
all over the world.

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NARRATOR:
Dukono and Ibu feature
frequently in his reports,

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but recently he's noticed
a steady upturn

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in their behavior.

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NARRATOR:
Every volcano has a cycle.

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There are times when
its activity is increasing

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and it's still possible
to get close enough

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to see the eruptions.

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If Tom is ever going to see
these two volcanoes,

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the time is now.

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The remote location makes
getting there difficult.

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Tom has a small group of
fellow photographers

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who have signed on
for the trip.

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The furthest they can fly is
to the Island of Ternate.

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It takes three flights
and several days.

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From there, Tom charters a
boat to get them to the

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island of Helmahera where
both volcanoes are located.

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NARRATOR:
They are met by
Andi Susanto.

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He's Tom's operations
manager in Indonesia,

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and an expert when it comes
to Indonesian volcanoes.

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It's arguable that Andi
has spent more time

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on active volcanos than
anyone else in the world.

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Andi is one of
the few people

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who has climbed
Dukono and Ibu.

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NARRATOR:
The boat trip from Ternate
to Halmahera takes one hour.

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The hope is they'll be able
to climb both volcanoes

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as they are erupting,
but there are no certainties.

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Every step of the way will be
carefully evaluated for risk.

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NARRATOR:
Tom and Andi's first step
will be to check in

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with local authorities to obtain
the proper permissions

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to climb.

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TOM:
We are here at the
volcano observatory

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for Mount Dukono.

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Each active volcano in
Indonesia has at least one

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local observatory.

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We hope we can talk to the
volcanologists to find out

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what the activity has been,
what to expect.

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Also to let them know
that we are climbing.

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ANDI:
And in here there are
three staff who work for

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the observatory post.

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In every observatory post
they have to report

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every evening
and in the mornings,

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to report the seismic activity
to the centre of the office

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of the Volcanological
Survey of Indonesia.

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NARRATOR:
The volcano is monitored by
a series of seismometers.

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These machines,
up on the volcano,

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record every
minute earthquake

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that indicates magma
moving through the system,

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or each explosion.

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Scientists can tell a lot
from these seismic signals.

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Here, the near-continuous
pattern indicates

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the constant venting of ash.

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Looking at the read-outs,
Tom and Andi can see

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that Dukono is now more active
than in the proceeding weeks.

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ANDI:
This is from 7 November;
it's yesterday.

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Therefore it's really active
with the ash plume

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and an ash eruption
from Dukono

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from the main vents.

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Two days ago is
also the same.

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This is 6.

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So almost every day
with ash explosions,

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with ash eruptions.

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NARRATOR:
Even though it's
more active,

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the current phase is more
predictable and less dangerous.

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That's good news.

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They get their permission
to climb.

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First up they hit
a local market

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to buy everything
they will need for the trip.

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NARRATOR:
At the foot of Dukono is the
small village of Tobelo.

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About 15,000 people
live and work here

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and keep a watchful eye
on the activity.

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ANDI:
She said two years ago
when Dukono was really active,

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she could hear about the
rumbling and ash also here

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and they were ready
to evacuate at the time.

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So actually the people here
are afraid about Dukono.

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NARRATOR:
Tom finds a stall
selling rocks and minerals.

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TOM:
A nicely cut piece of
black volcanic rock.

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I don't...
I'm not...

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I would guess
it's a volcanic rock.

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It's dense, glassy,
almost like obsidian,

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but it's probably
something else.

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NARRATOR:
For locals, trading in rocks
and semi-precious stones

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is a great way for
people to earn money.

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In a country prone to
earthquakes and eruptions

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geology is taught in depth
in the local schools.

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The subject covers rocks
and minerals

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as well as the volcanoes
around them.

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NARRATOR:
As the start of the hike
is a ways out,

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Andi has arranged for
transportation

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through a local
coconut plantation.

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TOM:
I think the biggest danger
right now

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will be hit by a branch
or something.

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I've had similar
situations sometimes.

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You look at something else

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and don't see a branch
coming, and bonk!

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NARRATOR:
You'd think with
an active volcano,

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people would completely
vacate the area.

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But Dukono has been
active since 1933

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and posed little threat
to the villages.

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People have grown used to
living in the shadow

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of this volcano.

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Here the coconut plantation
is still in operation.

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However, the roads that
extend into the danger zone

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are not used and have currently
fallen into disrepair

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during the rainy seasons.

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It makes getting to the
volcano's upper slopes

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challenging.

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[Indistinct chatter]

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[Indistinct chatter]

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[Indistinct chatter]

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NARRATOR:
The vehicle will need
a good run

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at the difficult sections,

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so to shed weight,
the group walks ahead.

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NARRATOR:
They are still a ways out.

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If the vehicle
has to turn back

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it will mean that
the moderate hike ahead

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will turn into a hard
full day's journey,

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something they won't be able
to make before night fall.

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♪♪♪

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♪♪♪

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TOM:
The truck's made it.

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So... time to continue.

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Glad it hadn't rained.

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When you have a lot of rain
you can't pass here.

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NARRATOR:
All along the way
they encounter new obstacles.

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The drivers don't give up.

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[Indistinct chatter]

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♪♪♪

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♪♪♪

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♪♪♪

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♪♪♪

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[Indistinct chatter]

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♪♪♪

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00:10:03,169 --> 00:10:07,440
♪♪♪

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NARRATOR:
They've reached the furthest
point the cars can go.

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TOM:
We've made it!
Or the car's made it.

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Now the last kilometers
is on foot.

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According to Andi,
it's about two to three hours,

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easy to moderate.

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ANDI:
So now we are in the altitude
of 350 meters above sea level.

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And we have to get packed
all the things,

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and then we'll proceed
to climb.

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NARRATOR:
They may be climbing
an active volcano,

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but at this point
it's pretty much

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like any other ascent.

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They plan to stay two days,
so a team of porters

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brings all the equipment
and tents needed.

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NARRATOR:
Part way up, they
run into a surprise.

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A university group
and their teacher

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are also heading up
to see the active crater.

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These students will be
the next generation

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of geologists in Indonesia.

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Some will go to work on
volcanoes around the country.

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Here they get first
real-world knowledge

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of an active volcano.

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NARRATOR:
As they get closer to
the active crater

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everything around them is
covered in a layer of ash.

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NARRATOR:
And finally their
first reward...

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A close up view of Dukono.

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They establish a camp at the
boundary of the danger zone.

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Beyond it, the risk of
being hit by falling rocks

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during a moderate eruption
increases.

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Hundreds of trips to volcanoes
has led Tom to believe

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that if you respect
the danger

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and pay heed to
the warning signs

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other elements of the trip
will actually pose

202
00:12:02,655 --> 00:12:07,427
a bigger danger
than the explosions.

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[Crashing]

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[Rumbling]

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NARRATOR:
A lightning strike
from a simple rain storm

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nearly hits the camp
just as the students arrive.

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00:12:26,479 --> 00:12:29,649
TOM:
We just had a lightning strike
out of the blue.

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00:12:29,649 --> 00:12:32,118
It was so fast I couldn't
even get scared.

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00:12:32,118 --> 00:12:36,689
And there was a big bang
right that second.

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It must've been less
than 100 meters.

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NARRATOR:
After the rain breaks,
and the camp is set,

212
00:12:50,236 --> 00:12:54,340
Tom has a look at the volcano
he has only read about.

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00:12:54,340 --> 00:12:56,275
It's a beautiful ash cone

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00:12:56,275 --> 00:12:58,511
and as the seismographs
predicted,

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it's constantly
emitting ash.

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00:13:01,748 --> 00:13:05,251
TOM:
Right now there is ash fall
in the downwind area

217
00:13:05,251 --> 00:13:06,686
of the plume.

218
00:13:06,686 --> 00:13:13,393
Sometimes you can see
vertical lines under the ash.

219
00:13:13,393 --> 00:13:16,129
It is a result of light
and shadow,

220
00:13:16,129 --> 00:13:19,732
but it's curtains of fine,
sandy material

221
00:13:19,732 --> 00:13:23,636
that is falling out
of the plume.

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00:13:23,636 --> 00:13:26,272
NARRATOR:
The ash here is washed
downstream,

223
00:13:26,272 --> 00:13:28,808
where it builds the lower
slopes of the volcano

224
00:13:28,808 --> 00:13:30,777
and provides the
nutrient-rich soils

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00:13:30,777 --> 00:13:33,646
of the village farmland.

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00:13:34,847 --> 00:13:37,083
TOM:
If you go from the top
to the bottom,

227
00:13:37,083 --> 00:13:39,485
you go back in history.

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00:13:39,485 --> 00:13:42,188
You can have an idea of what
a volcano has been doing

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in the past.

230
00:13:43,623 --> 00:13:46,693
The top black layer
would be the phase

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00:13:46,693 --> 00:13:48,828
of mildly explosive activity,

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00:13:48,828 --> 00:13:51,097
a bit like what
we're seeing now.

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00:13:51,097 --> 00:13:53,666
NARRATOR:
If you go from the top layer
to the bottom,

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00:13:53,666 --> 00:13:55,635
you can have an idea
of what a volcano

235
00:13:55,635 --> 00:13:58,204
has been doing in the past.

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TOM:
Here is also a little
pumice layer.

237
00:14:00,139 --> 00:14:02,475
During this activity
there must have been

238
00:14:02,475 --> 00:14:05,445
very powerful explosions...

239
00:14:05,445 --> 00:14:07,513
where fresh magma,
rich in gases,

240
00:14:07,513 --> 00:14:12,318
came out to erupt and become
pumice, especially here.

241
00:14:12,318 --> 00:14:14,520
And I don't know
how deep this goes

242
00:14:14,520 --> 00:14:18,658
but typically you find this
pumice as an oval-shaped deposit

243
00:14:18,658 --> 00:14:22,361
in the same direction
as the wind at the time.

244
00:14:22,361 --> 00:14:25,164
NARRATOR:
When they're putting together
the history of a volcano,

245
00:14:25,164 --> 00:14:29,135
volcanologists will sample
several locations around it.

246
00:14:29,135 --> 00:14:31,637
By determining the ash
and pumice thickness

247
00:14:31,637 --> 00:14:33,840
they can plot the
total area affected

248
00:14:33,840 --> 00:14:38,177
and calculate the volume
of the material deposited.

249
00:14:38,177 --> 00:14:40,780
From this they are able
to recreate the volcano's

250
00:14:40,780 --> 00:14:45,384
eruptive history dating back
thousands of years.

251
00:14:45,384 --> 00:14:48,721
Information like this can
help determine the danger

252
00:14:48,721 --> 00:14:53,760
and understand the far-reaching
effects of each volcano.

253
00:14:53,760 --> 00:14:57,130
They can also look for evidence
of cataclysmic eruptions

254
00:14:57,130 --> 00:14:59,398
and the phases
that preceded them.

255
00:14:59,398 --> 00:15:01,334
TOM:
It is important to know

256
00:15:01,334 --> 00:15:03,770
what the volcano has been
doing in the past

257
00:15:03,770 --> 00:15:06,572
to have an idea of what
it might do in the future.

258
00:15:06,572 --> 00:15:09,809
It might be doing something
like this for centuries

259
00:15:09,809 --> 00:15:13,146
but it doesn't mean that
it's always like this.

260
00:15:13,146 --> 00:15:15,515
NARRATOR:
The group will stay
in camp tonight,

261
00:15:15,515 --> 00:15:17,316
for safety's sake.

262
00:15:17,316 --> 00:15:19,118
Before they can do
any climbing,

263
00:15:19,118 --> 00:15:21,320
they will take time
to watch Dukono,

264
00:15:21,320 --> 00:15:22,789
and make sure
that its behavior

265
00:15:22,789 --> 00:15:26,292
is consistent with
the seismic data.

266
00:15:26,292 --> 00:15:28,694
It's absolutely necessary
to know what the recent

267
00:15:28,694 --> 00:15:30,730
seismic patterns are.

268
00:15:30,730 --> 00:15:34,133
But that's not a safety
guarantee.

269
00:15:34,133 --> 00:15:36,702
It is possible that
the volcano's activity

270
00:15:36,702 --> 00:15:39,505
will ramp up and become
dangerous with no warning.

271
00:15:42,441 --> 00:15:46,746
NARRATOR:
For the porters,
it is just another day.

272
00:15:46,746 --> 00:15:49,849
TOM:
If you choose to go up,
it should be based on

273
00:15:49,849 --> 00:15:53,219
a risk-benefit analysis.

274
00:15:53,219 --> 00:15:56,189
Dukono can certainly produce
very strong and powerful

275
00:15:56,189 --> 00:16:00,193
explosions that eject
bombs and rocks

276
00:16:00,193 --> 00:16:02,228
to the crater rim
and beyond.

277
00:16:02,228 --> 00:16:04,330
In which case,
if you're there,

278
00:16:04,330 --> 00:16:09,669
you are at risk to be hit
and lose your life.

279
00:16:09,669 --> 00:16:12,405
It is not a completely safe
thing to do.

280
00:16:12,405 --> 00:16:15,107
But on the other hand,
I believe that the risk

281
00:16:15,107 --> 00:16:17,376
if you stayed a couple
of hours is lower

282
00:16:17,376 --> 00:16:19,812
than the risk of
a car accident,

283
00:16:19,812 --> 00:16:23,049
especially after experiencing
how people drive here.

284
00:16:30,723 --> 00:16:32,725
NARRATOR:
The group will make
their climb to the crater

285
00:16:32,725 --> 00:16:35,261
in the early hours
of the morning.

286
00:16:35,261 --> 00:16:38,231
In the meantime,
they break for dinner.

287
00:16:38,231 --> 00:16:40,199
And their guide Andi
gets to show off

288
00:16:40,199 --> 00:16:42,668
some of his other skills.

289
00:16:42,668 --> 00:16:45,471
ANDI:
Now I'm cooking
we just call in Indonesia

290
00:16:45,471 --> 00:16:46,539
"Cah Kangkung."

291
00:16:46,539 --> 00:16:49,408
"Kangkung" means
"water spinach."

292
00:16:49,408 --> 00:16:52,211
So, the way is easy,

293
00:16:52,211 --> 00:16:55,381
but this is very
good flavor,

294
00:16:55,381 --> 00:16:58,017
and then delicious.

295
00:17:00,086 --> 00:17:07,293
[Speaking Indonesian]

296
00:17:07,293 --> 00:17:09,395
NARRATOR:
After dinner the group
takes time to relax

297
00:17:09,395 --> 00:17:11,063
before their climb.

298
00:17:11,063 --> 00:17:14,133
It will take less than
an hour.

299
00:17:14,133 --> 00:17:17,069
NARRATOR:
The climb begins
at the crack of dawn

300
00:17:17,069 --> 00:17:19,138
and members of Tom's group
make it to the rim

301
00:17:19,138 --> 00:17:22,441
before sunrise.

302
00:17:24,744 --> 00:17:27,647
[Rumbling]

303
00:17:27,647 --> 00:17:30,416
NARRATOR:
They're standing above
the active crater

304
00:17:30,416 --> 00:17:34,553
as it continues to erupt ash
in a constant plume.

305
00:17:34,553 --> 00:17:39,558
♪♪♪

306
00:17:39,558 --> 00:17:44,563
♪♪♪

307
00:17:44,563 --> 00:17:49,568
♪♪♪

308
00:17:49,568 --> 00:17:54,573
♪♪♪

309
00:17:54,573 --> 00:17:59,578
♪♪♪

310
00:17:59,578 --> 00:18:01,747
NARRATOR:
The volcano continues
to erupt ash,

311
00:18:01,747 --> 00:18:04,517
as it's been doing
for weeks.

312
00:18:04,517 --> 00:18:08,154
Inside you can hear the sounds
of the elemental processes

313
00:18:08,154 --> 00:18:10,423
of our earth at work.

314
00:18:10,423 --> 00:18:14,527
ANDI:
Now the ash plume looks
more active and intense.

315
00:18:14,527 --> 00:18:19,131
[Rumbling]

316
00:18:19,131 --> 00:18:23,269
ANDI:
The rumbling comes from
ash venting occurring,

317
00:18:23,269 --> 00:18:26,005
and then also with
the rock falls down there.

318
00:18:31,243 --> 00:18:33,713
TOM:
You can see it's
a very active volcano.

319
00:18:33,713 --> 00:18:37,616
It has been in continuous
eruptions for decades now.

320
00:18:37,616 --> 00:18:41,253
It almost sounds like hail,

321
00:18:41,253 --> 00:18:44,490
heavy hail during
a thunderstorm.

322
00:18:44,490 --> 00:18:48,127
I imagine there's a jet
coming out

323
00:18:48,127 --> 00:18:52,264
of gas, ash
and small rocks.

324
00:18:52,264 --> 00:18:56,202
We don't see them,
but we clearly hear

325
00:18:56,202 --> 00:19:00,172
these little rocks
falling back.

326
00:19:00,172 --> 00:19:03,376
And those sounds, these are
lightnings, not explosions.

327
00:19:03,376 --> 00:19:05,644
NARRATOR:
Scientists don't fully
understand why there's

328
00:19:05,644 --> 00:19:08,247
lightning in volcanos.

329
00:19:08,247 --> 00:19:11,117
It's believed to
be caused by ash particles

330
00:19:11,117 --> 00:19:15,087
that move against each other,
causing a static build up.

331
00:19:15,087 --> 00:19:17,490
As the plume rises,
the convection within

332
00:19:17,490 --> 00:19:22,795
pulls apart the two masses
with opposite charges.

333
00:19:22,795 --> 00:19:25,031
If the charge is
strong enough,

334
00:19:25,031 --> 00:19:27,033
it can create a path
of ionized air

335
00:19:27,033 --> 00:19:31,570
that conducts electricity
that forms a lightning bolt.

336
00:19:31,570 --> 00:19:35,641
Large ash plumes can generate
long bolts of lightning.

337
00:19:35,641 --> 00:19:37,810
Here it happens
on a smaller scale

338
00:19:37,810 --> 00:19:41,480
within the denser part
of the plume.

339
00:19:41,480 --> 00:19:44,784
Volcanic lightning
can be dangerous.

340
00:19:44,784 --> 00:19:48,454
During an eruption of
Paricutin Volcano in Mexico,

341
00:19:48,454 --> 00:19:50,456
three people were killed
by lightning

342
00:19:50,456 --> 00:19:54,226
that originated
from the ash cloud.

343
00:19:56,328 --> 00:19:58,497
NARRATOR:
The geology students arrive
at the rim

344
00:19:58,497 --> 00:20:02,668
to conduct their classes
on active volcanoes.

345
00:20:02,668 --> 00:20:05,471
Here they get a first-hand
look at the forces

346
00:20:05,471 --> 00:20:09,275
that are shaping
their country.

347
00:20:09,275 --> 00:20:14,280
♪♪♪

348
00:20:14,280 --> 00:20:19,285
♪♪♪

349
00:20:19,285 --> 00:20:22,288
♪♪♪

350
00:20:22,288 --> 00:20:24,623
TOM:
I think we're safe-ish here.

351
00:20:24,623 --> 00:20:27,660
It's not-- of course
it's never a safe place to be

352
00:20:27,660 --> 00:20:30,162
on the rim of
an active crater,

353
00:20:30,162 --> 00:20:33,365
but I haven't seen
any fresh impacts.

354
00:20:33,365 --> 00:20:37,269
In fact, I haven't seen
any impacts here in this part.

355
00:20:37,269 --> 00:20:39,538
So the likelihood
is very, very little

356
00:20:39,538 --> 00:20:42,508
that something
is being ejected here

357
00:20:42,508 --> 00:20:45,644
while we're here.

358
00:20:45,644 --> 00:20:48,214
However, this volcano
is capable of producing

359
00:20:48,214 --> 00:20:51,584
very powerful explosions
called vulcanian explosions.

360
00:20:51,584 --> 00:20:52,485
Throughout the past years,
every now and then

361
00:20:52,485 --> 00:20:55,254
you get reports of
very tall ash plumes

362
00:20:55,254 --> 00:20:57,456
rising several kilometers.

363
00:20:57,456 --> 00:21:01,327
That means you have
an explosive activity

364
00:21:01,327 --> 00:21:02,795
ten times more powerful
than this,

365
00:21:02,795 --> 00:21:05,631
and probably more as
an isolated explosion.

366
00:21:05,631 --> 00:21:07,633
When the plug
forms at the vent,

367
00:21:07,633 --> 00:21:09,401
which now seems to be
more or less open,

368
00:21:09,401 --> 00:21:10,703
but when there is
a plug that forms,

369
00:21:10,703 --> 00:21:13,272
it blocks it
and pressure can build up

370
00:21:13,272 --> 00:21:15,407
and then release it
in a sudden, powerful,

371
00:21:15,407 --> 00:21:18,511
so-called vulcanian type
explosion...

372
00:21:18,511 --> 00:21:21,280
then you'd be
in trouble here.

373
00:21:24,517 --> 00:21:29,188
NARRATOR:
Standing on the rim, the view
of Dukono is spectacular.

374
00:21:29,188 --> 00:21:31,123
But looking downhill
from the crater

375
00:21:31,123 --> 00:21:34,260
is also an impressive sight.

376
00:21:34,260 --> 00:21:39,064
This cone is mostly built
from loose ash deposits.

377
00:21:44,870 --> 00:21:47,439
NARRATOR:
When it rains,
this material is eroded,

378
00:21:47,439 --> 00:21:50,042
creating an other-worldly
landscape.

379
00:21:51,710 --> 00:21:54,246
NARRATOR:
This mountain-building process
is testament

380
00:21:54,246 --> 00:21:56,415
to Dukono's high activity.

381
00:21:56,415 --> 00:21:59,552
TOM:
I would count Dukono as
one of the four or five

382
00:21:59,552 --> 00:22:01,754
most active volcanos
in Indonesia.

383
00:22:01,754 --> 00:22:03,289
And Indonesia is
a heavyweight

384
00:22:03,289 --> 00:22:04,557
when it comes to volcanos.

385
00:22:04,557 --> 00:22:06,358
It is number one
when it comes to the number

386
00:22:06,358 --> 00:22:08,127
of active volcanos.

387
00:22:08,127 --> 00:22:12,164
And this is one out of the
top four or five of Indonesia.

388
00:22:12,164 --> 00:22:17,670
And on a global scale it's one
out of the top 20, I'd say.

389
00:22:17,670 --> 00:22:19,672
NARRATOR:
There are many factors
that determine

390
00:22:19,672 --> 00:22:21,440
how a volcano erupts.

391
00:22:21,440 --> 00:22:23,676
Three of those are:

392
00:22:23,676 --> 00:22:27,846
the amount of magma in its
reserves below the volcano,

393
00:22:27,846 --> 00:22:31,483
the amount of volatile gases
contained in the magma,

394
00:22:31,483 --> 00:22:34,620
and the type of magma.

395
00:22:36,722 --> 00:22:40,159
NARRATOR:
Some types of magma flow out
in gently glowing rivers

396
00:22:40,159 --> 00:22:42,561
that cover the land...

397
00:22:42,561 --> 00:22:45,397
while others explode
suddenly with force,

398
00:22:45,397 --> 00:22:50,436
throwing ash and lava blocks
into the air.

399
00:22:50,436 --> 00:22:53,539
For the past 80 or more years,
Dukono has produced

400
00:22:53,539 --> 00:22:55,774
mostly consistent
ash eruptions

401
00:22:55,774 --> 00:22:59,278
mixed with the
occasional lava flow.

402
00:22:59,278 --> 00:23:02,248
So, while it is one of
the most active volcanoes

403
00:23:02,248 --> 00:23:04,483
on the planet, its activity
has had little impact

404
00:23:04,483 --> 00:23:07,253
on the people
living around it,

405
00:23:07,253 --> 00:23:11,390
and for the time being
is not threatening.

406
00:23:11,390 --> 00:23:13,592
Dukono's neighbor
Mount Ibu,

407
00:23:13,592 --> 00:23:17,663
an hour's drive to the west,
is a different story.

408
00:23:17,663 --> 00:23:20,466
It is a small volcano with
an explosive personality.

409
00:23:23,702 --> 00:23:27,473
NARRATOR:
It erupts magma
known as andisite,

410
00:23:27,473 --> 00:23:30,109
which is very sticky
and collects at the summit

411
00:23:30,109 --> 00:23:32,411
in what's called
a lava dome.

412
00:23:32,411 --> 00:23:35,748
Lava domes can build up to the
point where they collapse,

413
00:23:35,748 --> 00:23:38,517
causing a burning hot avalanche
called a pyroclastic flow.

414
00:23:40,619 --> 00:23:46,191
NARRATOR:
Here, the volcano sits above
the small town of Talen.

415
00:23:46,191 --> 00:23:48,427
TOM:
The first thing
we'll do now

416
00:23:48,427 --> 00:23:50,529
is to visit the local
observatory

417
00:23:50,529 --> 00:23:52,831
to get informed about
the activity.

418
00:23:52,831 --> 00:23:57,303
Also to tell them that we
have an intention to climb.

419
00:23:57,303 --> 00:23:59,638
They expect everybody
to register so they know

420
00:23:59,638 --> 00:24:04,376
and hopefully give us
sort of a permit.

421
00:24:04,376 --> 00:24:06,545
[Speaking Indonesian]

422
00:24:08,814 --> 00:24:12,351
TOM:
The observatories are
usually at the same time

423
00:24:12,351 --> 00:24:14,753
equipped with a kitchen,
bedrooms,

424
00:24:14,753 --> 00:24:17,623
because they are manned
24 hours.

425
00:24:19,358 --> 00:24:22,628
TOM:
Up there at the crater
you have inside the lava dome,

426
00:24:22,628 --> 00:24:24,797
which has been growing
over the past years.

427
00:24:24,797 --> 00:24:27,399
It could easily generate
pyroclastic flows

428
00:24:27,399 --> 00:24:31,603
that come down here
and threaten this village.

429
00:24:31,603 --> 00:24:34,306
NARRATOR:
Tom and Andi want to look at
the seismic charts

430
00:24:34,306 --> 00:24:38,477
to see Ibu's most recent
eruptive behavior.

431
00:24:38,477 --> 00:24:43,282
ANDI:
So he said that since 2012
that actually Ibu volcano

432
00:24:43,282 --> 00:24:46,819
has been erupting,
being active.

433
00:24:46,819 --> 00:24:50,155
And also the status now
is level 2.

434
00:24:50,155 --> 00:24:52,391
NARRATOR:
Level 2 means activity
is present

435
00:24:52,391 --> 00:24:56,328
but continuing at
a constant level.

436
00:24:56,328 --> 00:24:59,264
If a volcano shows signs
of increased activity

437
00:24:59,264 --> 00:25:01,500
that may lead to
a larger eruption,

438
00:25:01,500 --> 00:25:03,802
it will be categorized
as level 3

439
00:25:03,802 --> 00:25:07,039
and evacuations will begin.

440
00:25:07,039 --> 00:25:11,710
Each mark on the seismograph
represents an eruption.

441
00:25:11,710 --> 00:25:14,213
What they can tell
from these charts

442
00:25:14,213 --> 00:25:17,516
is this is a
very active volcano.

443
00:25:17,516 --> 00:25:21,553
Today alone there have have
been more then 50 eruptions.

444
00:25:21,553 --> 00:25:25,357
ANDI:
There are explosions
and sometimes the pumice

445
00:25:25,357 --> 00:25:28,293
is ejected until
900 meters.

446
00:25:28,293 --> 00:25:30,662
NARRATOR:
Where they plan to go
will put them right inside

447
00:25:30,662 --> 00:25:33,265
the active crater.

448
00:25:33,265 --> 00:25:37,336
ANDI:
Yeah, we'll still climb

449
00:25:37,336 --> 00:25:39,805
but let's see if that
is too dangerous.

450
00:25:39,805 --> 00:25:43,108
Yeah, we will see that,
so...

451
00:25:43,108 --> 00:25:44,443
NARRATOR:
As they're standing,

452
00:25:44,443 --> 00:25:47,846
the seismograph registers
an eruption.

453
00:25:47,846 --> 00:25:49,548
TOM:
You can see an explosion
that occurred right now.

454
00:25:49,548 --> 00:25:51,650
See the ash plume?

455
00:25:51,650 --> 00:25:56,855
Yeah, that's quite
an explosion.

456
00:25:56,855 --> 00:26:01,593
If you're close this would
be quite something.

457
00:26:03,228 --> 00:26:05,664
That's why the guys are
here to observe it

458
00:26:05,664 --> 00:26:08,300
and if the situation changes
at some point,

459
00:26:08,300 --> 00:26:11,637
maybe in the future
the government

460
00:26:11,637 --> 00:26:14,239
will have to take measures,
I guess.

461
00:26:14,239 --> 00:26:18,043
But it could be
in 100 years,

462
00:26:18,043 --> 00:26:22,047
it could be next year,
it could be in 1,000 years.

463
00:26:22,047 --> 00:26:25,818
But as it is now,
life goes on.

464
00:26:25,818 --> 00:26:28,187
NARRATOR:
Duono village is
a 30-minute drive

465
00:26:28,187 --> 00:26:29,822
from the observatory.

466
00:26:29,822 --> 00:26:32,124
It is the gateway to Ibu.

467
00:26:32,124 --> 00:26:34,326
It is also the place
most in danger

468
00:26:34,326 --> 00:26:37,296
if there is
a major eruption.

469
00:26:37,296 --> 00:26:39,731
The town sits at the opening
of a giant breach

470
00:26:39,731 --> 00:26:42,267
in Ibu's cone.

471
00:26:42,267 --> 00:26:44,336
Any eruptive flow
from the volcano

472
00:26:44,336 --> 00:26:47,806
would come straight down
to the village.

473
00:26:47,806 --> 00:26:50,342
About two years ago
when Ibu woke up

474
00:26:50,342 --> 00:26:54,379
after a short slumber,
the village was evacuated.

475
00:26:54,379 --> 00:26:56,782
But as the volcano's
activity stabilized,

476
00:26:56,782 --> 00:26:59,852
people have moved back.

477
00:26:59,852 --> 00:27:03,188
But still, outsiders
rarely come here.

478
00:27:03,188 --> 00:27:07,092
Duono doesn't even
have a hotel.

479
00:27:07,092 --> 00:27:09,294
TOM:
I think they haven't seen
many visitors here.

480
00:27:09,294 --> 00:27:11,330
It's so remote hardly
anybody comes in,

481
00:27:11,330 --> 00:27:15,200
maybe a few Westerners
per year,

482
00:27:15,200 --> 00:27:18,537
and that would be a lot,
I guess.

483
00:27:18,537 --> 00:27:20,672
NARRATOR:
Without any tourism
in the area,

484
00:27:20,672 --> 00:27:24,042
Andi is forced to improvise
for accommodations.

485
00:27:24,042 --> 00:27:25,644
ANDI:
This is actually the house
of the Kardesh.

486
00:27:25,644 --> 00:27:27,746
"Kardesh" means the chief
of the village.

487
00:27:27,746 --> 00:27:29,448
So that's very
important to us.

488
00:27:29,448 --> 00:27:32,818
We're going to stay here
for camp tonight.

489
00:27:32,818 --> 00:27:35,254
So we just sleep
in the floor.

490
00:27:35,254 --> 00:27:37,489
And then we're going to
start climbing Ibu

491
00:27:37,489 --> 00:27:40,826
tomorrow morning then
from here.

492
00:27:40,826 --> 00:27:43,262
NARRATOR:
With rain continuing
into the night,

493
00:27:43,262 --> 00:27:46,465
the group won't be able to
see any eruptions.

494
00:27:46,465 --> 00:27:48,534
Tom had hoped to see
if the eruptions

495
00:27:48,534 --> 00:27:51,103
were ejecting lava rocks
called bombs

496
00:27:51,103 --> 00:27:54,339
as far as the crater rim.

497
00:27:54,339 --> 00:27:58,777
At night these bombs
are visible.

498
00:28:02,414 --> 00:28:05,684
NARRATOR:
The following morning
it's still raining,

499
00:28:05,684 --> 00:28:09,354
and the forecast says rain
will continue most of the day.

500
00:28:12,491 --> 00:28:16,395
TOM:
We are actually not 100% sure
if we can go

501
00:28:16,395 --> 00:28:18,030
all the way to the rim.

502
00:28:18,030 --> 00:28:22,501
It will depend on
the activity.

503
00:28:22,501 --> 00:28:27,439
The lava dome has been
producing frequent explosions.

504
00:28:27,439 --> 00:28:31,376
We'll have to see if...

505
00:28:31,376 --> 00:28:35,247
and how fresh any impacts are
in the upper areas.

506
00:28:35,247 --> 00:28:37,749
If we find too many
fresh bombs impacts

507
00:28:37,749 --> 00:28:41,687
obviously it wouldn't be
a good idea to go.

508
00:28:41,687 --> 00:28:45,324
NARRATOR:
Tom's also worried
about the cloud cover.

509
00:28:45,324 --> 00:28:47,593
TOM:
If there is no visibility
there is no real point

510
00:28:47,593 --> 00:28:50,228
in staying at
the crater rim.

511
00:28:50,228 --> 00:28:52,197
It also increases
the hazard,

512
00:28:52,197 --> 00:28:54,633
the risk of being caught
in an explosion

513
00:28:54,633 --> 00:28:57,636
because you can't
see anything.

514
00:28:57,636 --> 00:29:00,272
There is no value
of being there.

515
00:29:00,272 --> 00:29:03,175
So we should only go
to the rim

516
00:29:03,175 --> 00:29:05,143
if there is also
good visibility.

517
00:29:05,143 --> 00:29:06,745
NARRATOR:
In spite of the weather,

518
00:29:06,745 --> 00:29:09,748
Tom and Andi decide
to go ahead with the climb

519
00:29:09,748 --> 00:29:11,717
in the hope that
weather breaks

520
00:29:11,717 --> 00:29:15,754
by the time they reach
the crater rim.

521
00:29:15,754 --> 00:29:19,024
NARRATOR:
Although the group managed
to get the necessary permission,

522
00:29:19,024 --> 00:29:22,127
officials were hesitant
to let Andi's group climb

523
00:29:22,127 --> 00:29:25,530
because of Ibu's increase
in eruptive activity.

524
00:29:25,530 --> 00:29:29,568
They agreed because of Tom's
status and experience.

525
00:29:29,568 --> 00:29:32,137
But the officials require
that the group be accompanied

526
00:29:32,137 --> 00:29:36,308
by Arnold who is the spiritual
guardian of the volcano.

527
00:29:36,308 --> 00:29:39,511
This is considered
a high honor.

528
00:29:39,511 --> 00:29:42,114
One thing Tom's experience
has taught him

529
00:29:42,114 --> 00:29:44,650
on volcanoes all
over the world

530
00:29:44,650 --> 00:29:47,719
is the importance of having
a local guide.

531
00:29:47,719 --> 00:29:49,554
TOM:
He's the chief
of the volcano.

532
00:29:49,554 --> 00:29:56,561
The most experienced man around
who knows Mount Ibu volcano.

533
00:29:56,561 --> 00:30:00,198
I just got the idea
a stick would be handy,

534
00:30:00,198 --> 00:30:01,400
and I ask him...

535
00:30:01,400 --> 00:30:05,003
I think this makes it cool.
Everybody now will want one.

536
00:30:13,078 --> 00:30:16,415
TOM:
It seems this trail
hasn't been walked recently,

537
00:30:16,415 --> 00:30:21,753
so Arnold, our head guide,
has to use his machete a lot

538
00:30:21,753 --> 00:30:24,122
to clear the path.

539
00:30:30,696 --> 00:30:34,332
NARRATOR:
It's likely Andi was the last
person to climb the volcano,

540
00:30:34,332 --> 00:30:37,335
six months ago.

541
00:30:37,335 --> 00:30:41,673
He came to check out its
potential for guiding.

542
00:30:41,673 --> 00:30:44,476
Tom will rely heavily
on his experience,

543
00:30:44,476 --> 00:30:47,679
and Arnold's too.

544
00:30:47,679 --> 00:30:51,116
ANDI:
Phew!
Challenging!

545
00:30:53,285 --> 00:30:56,188
TOM:
Okay, yeah,
that's volcanic ash.

546
00:30:56,188 --> 00:30:59,357
Occasionally when the wind
is going this way

547
00:30:59,357 --> 00:31:02,594
and there is an explosion

548
00:31:02,594 --> 00:31:04,763
you will have ash fall
on this part.

549
00:31:04,763 --> 00:31:07,299
In the dry season the ash
will cover the leaves.

550
00:31:07,299 --> 00:31:10,836
With the first rain
the forest washes itself.

551
00:31:10,836 --> 00:31:14,139
That happened tonight,
but you see remnants.

552
00:31:14,139 --> 00:31:19,077
So I suppose the closer
we get to the rim,

553
00:31:19,077 --> 00:31:20,679
the more of this
we will see.

554
00:31:20,679 --> 00:31:23,548
NARRATOR:
They also have come upon
the seismograph station

555
00:31:23,548 --> 00:31:25,484
that relays
earthquake info

556
00:31:25,484 --> 00:31:28,153
back to the volcanic
observatory.

557
00:31:28,153 --> 00:31:30,188
TOM:
So probably right now
they'll have some noise

558
00:31:30,188 --> 00:31:31,556
as we're walking by.

559
00:31:31,556 --> 00:31:35,761
Our steps will be recorded
by the instrument.

560
00:31:35,761 --> 00:31:39,331
NARRATOR:
Now they're entering
the high danger zone.

561
00:31:39,331 --> 00:31:41,566
Fragments of rocks
thrown from the crater

562
00:31:41,566 --> 00:31:47,606
during large explosions
are visible.

563
00:31:47,606 --> 00:31:49,775
TOM:
This is actually
a bit worrying.

564
00:31:49,775 --> 00:31:53,745
This is an impact from
an explosion at the summit.

565
00:31:53,745 --> 00:31:55,547
This is one of
the larger fragments.

566
00:31:55,547 --> 00:31:57,816
But they're all around,
I guess.

567
00:31:57,816 --> 00:32:00,719
You know, they fall
at great speed,

568
00:32:00,719 --> 00:32:04,489
a hundred meters a second.

569
00:32:04,489 --> 00:32:05,657
There's so much energy.

570
00:32:05,657 --> 00:32:08,226
When they fall
and the soil is soft

571
00:32:08,226 --> 00:32:10,529
it makes these
sort of craters.

572
00:32:10,529 --> 00:32:12,564
GIAN:
This one could
slice you, man.

573
00:32:12,564 --> 00:32:14,800
TOM:
We are one kilometer
horizontal distance

574
00:32:14,800 --> 00:32:17,135
from the crater,

575
00:32:17,135 --> 00:32:21,106
so this is entirely
within the range

576
00:32:21,106 --> 00:32:24,342
of moderately sized
explosions.

577
00:32:24,342 --> 00:32:26,845
Nothing unusual.

578
00:32:26,845 --> 00:32:30,448
So one shouldn't be deceived
by the lush vegetation.

579
00:32:30,448 --> 00:32:35,487
We are in
a high-risk zone

580
00:32:35,487 --> 00:32:36,855
of an active volcano.

581
00:32:36,855 --> 00:32:39,724
NARRATOR:
Arnold their guide
tells Tom that impact

582
00:32:39,724 --> 00:32:42,093
was from two years ago.

583
00:32:42,093 --> 00:32:44,629
If it were more recent fresh
fragments would be found

584
00:32:44,629 --> 00:32:49,301
on top of the vegetation.

585
00:32:49,301 --> 00:32:51,670
They're thirty minutes
from the crater rim,

586
00:32:51,670 --> 00:32:55,473
and should begin to see
a lot more of this.

587
00:33:00,645 --> 00:33:03,448
TOM:
Here's another bomb,
right on the trail.

588
00:33:07,118 --> 00:33:11,189
TOM:
Obviously the higher
we come,

589
00:33:11,189 --> 00:33:13,491
the closer we get
to the dome,

590
00:33:13,491 --> 00:33:18,730
the more of these guys
we can expect.

591
00:33:18,730 --> 00:33:22,267
Just hope they're
not very recent.

592
00:33:22,267 --> 00:33:27,272
♪♪♪

593
00:33:27,272 --> 00:33:29,074
♪♪♪

594
00:33:29,074 --> 00:33:31,443
TOM:
It didn't impact right here.

595
00:33:31,443 --> 00:33:34,045
It may be somewhere,
but it's difficult to see.

596
00:33:36,615 --> 00:33:39,651
TOM:
This could be the same one
or another one.

597
00:33:39,651 --> 00:33:42,320
It could be--
likely it's the same.

598
00:33:42,320 --> 00:33:44,623
Maybe it impacted here.

599
00:33:44,623 --> 00:33:51,129
This one sits in the soil.

600
00:33:51,129 --> 00:33:55,333
We're definitely getting
close to the crater.

601
00:33:55,333 --> 00:33:57,869
ANDI:
According to my
experience, my opinion,

602
00:33:57,869 --> 00:34:00,171
even now we are,
if we continue to the rim

603
00:34:00,171 --> 00:34:03,608
it's still safe.

604
00:34:03,608 --> 00:34:08,146
From what I saw from
the seismograph.

605
00:34:10,215 --> 00:34:12,384
TOM:
I've never been on
this volcano,

606
00:34:12,384 --> 00:34:16,588
but as a general rule,

607
00:34:16,588 --> 00:34:19,291
you should approach it
slowly.

608
00:34:19,291 --> 00:34:22,327
We've been climbing fast,

609
00:34:22,327 --> 00:34:26,231
and to me it looks the rim
is in mist at the moment

610
00:34:26,231 --> 00:34:28,700
so we have no added
value to be at the rim

611
00:34:28,700 --> 00:34:31,369
but increase our risk.

612
00:34:31,369 --> 00:34:34,139
I'm sorry to talk about risk
and these things,

613
00:34:34,139 --> 00:34:38,343
but from here we have
much more safety margin.

614
00:34:38,343 --> 00:34:43,348
If we stay here half an hour,
relax and maybe listen.

615
00:34:43,348 --> 00:34:46,551
Down there I could hear the
weak sound of an explosion.

616
00:34:46,551 --> 00:34:49,721
If we stay here
for half an hour,

617
00:34:49,721 --> 00:34:52,157
maybe hear another
explosion

618
00:34:52,157 --> 00:34:54,659
and get a better feeling
for the mountain,

619
00:34:54,659 --> 00:35:00,765
that it's maybe not
too active.

620
00:35:00,765 --> 00:35:03,401
One thing I would hate
is we arrive at the rim

621
00:35:03,401 --> 00:35:05,337
and we just hear
a very loud explosion

622
00:35:05,337 --> 00:35:07,672
and we don't know
what's happening.

623
00:35:07,672 --> 00:35:11,042
NARRATOR:
Both the volcano chief
and Andi disagree with Tom,

624
00:35:11,042 --> 00:35:12,811
but he overrules them.

625
00:35:12,811 --> 00:35:16,147
The crater rim sits just
over a football field away

626
00:35:16,147 --> 00:35:18,249
from the active crater.

627
00:35:18,249 --> 00:35:21,353
There's no room for error
on this volcano.

628
00:35:23,521 --> 00:35:26,358
NARRATOR:
After 30 minutes
and no eruption,

629
00:35:26,358 --> 00:35:28,693
they decide to continue on.

630
00:35:28,693 --> 00:35:30,595
[Explosion]

631
00:35:31,396 --> 00:35:34,366
TOM:
There was an explosion,
the sound of...

632
00:35:41,139 --> 00:35:46,211
TOM:
Uh, no bombs.
That's a good sign.

633
00:35:46,211 --> 00:35:47,746
But we are getting close.

634
00:35:47,746 --> 00:35:50,215
I think we are 100,
maybe 150 meters

635
00:35:50,215 --> 00:35:51,649
below the crater rim.

636
00:35:51,649 --> 00:35:58,323
So... yeah.

637
00:35:58,323 --> 00:36:00,325
This will be interesting.

638
00:36:03,361 --> 00:36:05,730
NARRATOR:
Tom makes it to
the volcano rim.

639
00:36:05,730 --> 00:36:08,600
The cloud cover is so thick
that they can't see how far

640
00:36:08,600 --> 00:36:11,403
they are from
the active vents.

641
00:36:11,403 --> 00:36:14,072
They'll wait for the
next eruption and listen

642
00:36:14,072 --> 00:36:18,576
to hear where the bombs
are falling.

643
00:36:18,576 --> 00:36:23,148
TOM:
This must be the active flow
that goes down this way.

644
00:36:23,148 --> 00:36:25,683
I try to go a little bit
further there

645
00:36:25,683 --> 00:36:28,520
to see how far it goes.

646
00:36:29,454 --> 00:36:31,756
NARRATOR:
The porters begin
to set up camp

647
00:36:31,756 --> 00:36:35,427
as the rest of Tom's group
makes it onto the rim.

648
00:36:35,427 --> 00:36:37,829
In the mist they hear
the sounds of the volcano

649
00:36:37,829 --> 00:36:39,831
violently degassing...

650
00:36:39,831 --> 00:36:44,102
[Hissing]

651
00:36:44,102 --> 00:36:46,704
NARRATOR:
...followed by an eruption.

652
00:36:46,704 --> 00:36:50,275
[Explosion]

653
00:36:59,150 --> 00:37:01,286
NARRATOR:
From the sounds
they can tell that the bombs

654
00:37:01,286 --> 00:37:04,155
are not flying
towards their camp.

655
00:37:04,155 --> 00:37:07,092
That means they're
in a good location.

656
00:37:07,092 --> 00:37:09,160
The porters get back to
building a shelter

657
00:37:09,160 --> 00:37:11,763
in case the rain
starts again.

658
00:37:11,763 --> 00:37:14,699
Tom retrieves a couple of
dead trees to use as poles

659
00:37:14,699 --> 00:37:17,602
for a makeshift shelter.

660
00:37:26,678 --> 00:37:30,615
NARRATOR:
After a while the clouds
begin to break.

661
00:37:30,615 --> 00:37:32,817
They get their first look
at the active vents

662
00:37:32,817 --> 00:37:34,686
within the crater.

663
00:37:34,686 --> 00:37:37,355
It's unnervingly close.

664
00:37:37,355 --> 00:37:42,460
This volcano is not for
the faint of heart.

665
00:37:46,464 --> 00:37:53,138
TOM:
This is Ibu volcano's crater,
and the recent lava dome,

666
00:37:53,138 --> 00:37:57,208
this black-greyish mass
of lava that occupies

667
00:37:57,208 --> 00:37:58,476
most of the crater.

668
00:37:58,476 --> 00:38:01,146
At its centre,
a small cindercone,

669
00:38:01,146 --> 00:38:03,615
which is currently active.

670
00:38:09,354 --> 00:38:14,526
[Explosion]

671
00:38:17,061 --> 00:38:22,233
NARRATOR:
It's a small eruption
from the furthest crater.

672
00:38:22,233 --> 00:38:27,238
This eruption only produces
ash mixed with steam.

673
00:38:27,238 --> 00:38:32,477
It's not from the vent
that ejected bombs.

674
00:38:32,477 --> 00:38:34,512
Each vent will erupt
differently,

675
00:38:34,512 --> 00:38:36,114
so they will have to see
an eruption

676
00:38:36,114 --> 00:38:39,217
from the other two
to know if it's safe.

677
00:38:40,485 --> 00:38:42,787
TOM:
Right now it seems
it is, however,

678
00:38:42,787 --> 00:38:48,560
in a phase of more frequent
but smaller eruptions.

679
00:38:48,560 --> 00:38:55,066
That's why I think we're
reasonably safe here...

680
00:38:55,066 --> 00:38:58,269
for a limited time,
of course.

681
00:38:58,269 --> 00:39:00,305
But you can see all the trees
have been stripped

682
00:39:00,305 --> 00:39:02,307
of their smaller branches.

683
00:39:02,307 --> 00:39:06,644
Trees all died as a result of
frequent impacts,

684
00:39:06,644 --> 00:39:10,381
leaving just the trunks
and the major branches intact.

685
00:39:12,250 --> 00:39:14,352
TOM:
These volcanoes
in subduction zones

686
00:39:14,352 --> 00:39:16,221
typically produce
a kind of lava

687
00:39:16,221 --> 00:39:19,257
that is relatively
rich in silica,

688
00:39:19,257 --> 00:39:21,459
so it is rather
viscous.

689
00:39:21,459 --> 00:39:24,662
It doesn't flow; it doesn't
behave like a lava

690
00:39:24,662 --> 00:39:26,431
on volcanoes like Hawaii,
which is fluid

691
00:39:26,431 --> 00:39:28,466
and can form channels
and can actually

692
00:39:28,466 --> 00:39:31,469
behave visually
like a liquid.

693
00:39:31,469 --> 00:39:35,106
No, the lava that the
volcano has been erupting

694
00:39:35,106 --> 00:39:39,043
over the past years
accumulates above the vent

695
00:39:39,043 --> 00:39:44,449
to form a broad, cake-like
structure called a lava dome.

696
00:39:44,449 --> 00:39:47,418
It's too stiff
to actually flow,

697
00:39:47,418 --> 00:39:52,590
so it'd rather accumulates
as a huge pile of blocking mass.

698
00:39:52,590 --> 00:39:58,463
These type of eruptions
are potentially very dangerous

699
00:39:58,463 --> 00:40:02,400
because the high viscosity
of the lava

700
00:40:02,400 --> 00:40:06,371
also traps gases inside,

701
00:40:06,371 --> 00:40:11,442
which can lead to
sometimes big explosions.

702
00:40:12,810 --> 00:40:16,114
NARRATOR:
This is footage
Andi shot on Semeru Volcano

703
00:40:16,114 --> 00:40:18,216
on the Island of Java.

704
00:40:18,216 --> 00:40:21,352
It shows an active lava dome
in action.

705
00:40:21,352 --> 00:40:23,621
As the pressure
builds up inside

706
00:40:23,621 --> 00:40:27,558
the entire structure lifts
and the dome inflates.

707
00:40:27,558 --> 00:40:29,427
If too much pressure
builds up,

708
00:40:29,427 --> 00:40:35,199
the dome can
suddenly explode.

709
00:40:35,199 --> 00:40:37,669
NARRATOR:
Back on Ibu,
suddenly the left vent

710
00:40:37,669 --> 00:40:40,204
begins to vigorously de-gas.

711
00:40:40,204 --> 00:40:45,209
[Hissing]

712
00:40:45,209 --> 00:40:49,614
[Hissing]

713
00:40:49,614 --> 00:40:51,716
NARRATOR:
The sound is similar
to the group heard

714
00:40:51,716 --> 00:40:54,452
when they first arrived
on the crater rim,

715
00:40:54,452 --> 00:40:59,123
just before
the first explosion.

716
00:40:59,123 --> 00:41:03,561
The gas indicates that this
is a small lava dome.

717
00:41:03,561 --> 00:41:06,364
As on Semeru, the
gas is trapped under

718
00:41:06,364 --> 00:41:09,334
the crusted-over magma.

719
00:41:09,334 --> 00:41:12,370
When the pressure builds up
and the vent explodes

720
00:41:12,370 --> 00:41:17,241
it will likely throw bombs
into the air.

721
00:41:27,585 --> 00:41:32,423
[Explosion]

722
00:41:32,423 --> 00:41:36,294
[Rumbling]

723
00:41:36,294 --> 00:41:39,764
NARRATOR:
This shoots jets of ash.

724
00:41:44,836 --> 00:41:49,841
[Rumbling]

725
00:41:49,841 --> 00:41:54,779
[Rumbling]

726
00:41:59,650 --> 00:42:02,453
TOM:
So I think the vent on
our right side is having

727
00:42:02,453 --> 00:42:04,789
so-called phreatomagmatic
eruptions,

728
00:42:04,789 --> 00:42:08,326
where ground water
interacts with magma

729
00:42:08,326 --> 00:42:11,229
and produces an explosion.

730
00:42:11,229 --> 00:42:14,532
NARRATOR:
As it flashes to steam,
the instantaneous expansion

731
00:42:14,532 --> 00:42:18,503
of the gas is enough
to blast through the rock,

732
00:42:18,503 --> 00:42:21,539
fragmenting it into
small pieces.

733
00:42:21,539 --> 00:42:23,608
The pieces fall
around the crater,

734
00:42:23,608 --> 00:42:26,277
building up its small cone.

735
00:42:53,571 --> 00:43:01,512
NARRATOR:
Now they wait for
the third crater to erupt.

736
00:43:01,512 --> 00:43:08,219
[Explosion]

737
00:43:08,219 --> 00:43:12,256
[Explosion]

738
00:43:26,471 --> 00:43:30,641
NARRATOR:
We get to see the eruption
in detail.

739
00:43:30,641 --> 00:43:32,710
The explosion
shatters the dome,

740
00:43:32,710 --> 00:43:36,380
sending chunks of lava
away at supersonic speeds.

741
00:43:36,380 --> 00:43:39,817
Thankfully, in a direction
away from the group.

742
00:43:39,817 --> 00:43:44,388
The inner crater is bombarded
with rock fragments.

743
00:43:44,388 --> 00:43:47,124
It was these types
of explosions,

744
00:43:47,124 --> 00:43:48,826
yet on a much
larger scale,

745
00:43:48,826 --> 00:43:50,828
that produced the impact site
that Tom found

746
00:43:50,828 --> 00:43:53,231
on the way up.

747
00:43:55,466 --> 00:43:59,470
TOM:
Volcanoes are always
good for surprises.

748
00:43:59,470 --> 00:44:03,274
I didn't expect at all this type
of strombolian activity

749
00:44:03,274 --> 00:44:05,409
and the classical,
beautiful explosions

750
00:44:05,409 --> 00:44:08,579
where lots of incandescent bombs
are thrown up to

751
00:44:08,579 --> 00:44:10,481
maybe 100, 200,
meters.

752
00:44:10,481 --> 00:44:15,219
Accompanied by loud bangs
that resound

753
00:44:15,219 --> 00:44:17,388
at the crater walls;
you have wonderful echoes.

754
00:44:17,388 --> 00:44:22,059
It's an absolutely
eerie atmosphere.

755
00:44:27,665 --> 00:44:29,734
TOM:
So you see the blueish gas
is an indication

756
00:44:29,734 --> 00:44:33,538
of fresh magma underneath.

757
00:44:33,538 --> 00:44:37,375
The same vent is probably
feeding a bit the lava flow,

758
00:44:37,375 --> 00:44:39,577
which has a slightly
brown color.

759
00:44:39,577 --> 00:44:42,747
[Rumbling]

760
00:44:42,747 --> 00:44:45,550
NARRATOR:
As the sun dips behind
the horizon,

761
00:44:45,550 --> 00:44:51,088
the faint glow of lava
can start to be seen.

762
00:44:51,088 --> 00:44:56,093
♪♪♪

763
00:44:56,093 --> 00:44:57,395
♪♪♪

764
00:44:57,395 --> 00:45:01,465
NARRATOR:
At night, the eruptions
look completely different.

765
00:45:01,465 --> 00:45:03,501
Glowing, incandescent
lava blocks

766
00:45:03,501 --> 00:45:05,469
are thrown from
the craters.

767
00:45:07,572 --> 00:45:12,577
[Explosion]

768
00:45:12,577 --> 00:45:18,583
♪♪♪

769
00:45:18,583 --> 00:45:25,656
♪♪♪

770
00:45:25,656 --> 00:45:29,627
[Explosion]

771
00:45:29,627 --> 00:45:34,632
♪♪♪

772
00:45:34,632 --> 00:45:39,637
♪♪♪

773
00:45:39,637 --> 00:45:44,108
♪♪♪

774
00:45:44,108 --> 00:45:47,545
[Explosion]

775
00:45:47,545 --> 00:45:52,550
♪♪♪

776
00:45:52,550 --> 00:45:53,584
♪♪♪

777
00:45:53,584 --> 00:45:56,420
TOM:
So I think we've had
a great experience

778
00:45:56,420 --> 00:45:58,689
and we saw another one
of the top five

779
00:45:58,689 --> 00:46:02,226
most active volcanoes
in all of Indonesia.

780
00:46:02,226 --> 00:46:04,161
Each volcano has
its own personality.

781
00:46:04,161 --> 00:46:06,397
It's completely different
from what we saw at Dukono,

782
00:46:06,397 --> 00:46:09,600
but it's great as well.

783
00:46:09,600 --> 00:46:14,038
For me this ranks
so far number one

784
00:46:14,038 --> 00:46:18,376
in terms of scenery,
experience.

785
00:46:18,376 --> 00:46:21,646
Also, the climb here
is a relatively long

786
00:46:21,646 --> 00:46:23,414
strenuous climb,

787
00:46:23,414 --> 00:46:27,418
but you are rewarded
with a magnificent view.

788
00:46:27,418 --> 00:46:30,621
NARRATOR:
It's been another
great adventure for Tom,

789
00:46:30,621 --> 00:46:33,157
but getting this close to
Ibu's crater

790
00:46:33,157 --> 00:46:38,129
is something very few people
will experience.

791
00:46:38,129 --> 00:46:40,831
Its remote location
makes it tough to get to,

792
00:46:40,831 --> 00:46:43,501
and the chance that the volcano
could suddenly generate

793
00:46:43,501 --> 00:46:47,304
a large eruption
keeps people away.

794
00:46:47,304 --> 00:46:48,773
But for Tom,

795
00:46:48,773 --> 00:46:51,842
getting to experience
both Ibu and Dukono

796
00:46:51,842 --> 00:46:54,845
and read the geological
records they've left

797
00:46:54,845 --> 00:46:59,817
is an important part of
his work as a volcanologist.

798
00:46:59,817 --> 00:47:03,120
Both Ibu and Dukono
are in the elite,

799
00:47:03,120 --> 00:47:07,491
the top twenty of the most
active volcanoes on earth.

800
00:47:07,491 --> 00:47:10,494
They are the surface layer
of the elemental forces

801
00:47:10,494 --> 00:47:13,330
that continue to shape
and reshape

802
00:47:13,330 --> 00:47:15,566
Indonesia's volcanic islands.

803
00:47:15,566 --> 00:47:21,172
♪♪♪

804
00:47:22,239 --> 00:47:27,244
♪♪♪

805
00:47:27,244 --> 00:47:32,249
♪♪♪

806
00:47:32,249 --> 00:47:37,254
♪♪♪

807
00:47:37,254 --> 00:47:42,259
♪♪♪

808
00:47:42,259 --> 00:47:47,264
♪♪♪

809
00:47:47,264 --> 00:47:51,736
♪♪♪


