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Hidden in the heart of Africa, | 0:00:06 | 0:00:10 | |
deep in the Congo, | 0:00:10 | 0:00:12 | |
is one of the most spectacular volcanoes on Earth. | 0:00:12 | 0:00:15 | |
Nyiragongo. | 0:00:19 | 0:00:20 | |
It is also one of the most deadly. | 0:00:22 | 0:00:24 | |
It's ferocious. | 0:00:25 | 0:00:26 | |
It feels very alive. | 0:00:26 | 0:00:28 | |
It last erupted in 2002... | 0:00:29 | 0:00:31 | |
..devastating the nearby city of Goma. | 0:00:34 | 0:00:36 | |
The Earth's molten core enveloping an African town. | 0:00:38 | 0:00:42 | |
There are few places on Earth | 0:00:44 | 0:00:46 | |
where an active volcano threatens so many people, | 0:00:46 | 0:00:50 | |
in a country already shattered by decades of violence. | 0:00:50 | 0:00:53 | |
Now there's an uneasy peace, | 0:00:57 | 0:01:00 | |
so a team of international and local scientists are on a mission | 0:01:00 | 0:01:03 | |
to explore this rarely visited volcano... | 0:01:03 | 0:01:05 | |
..to try and predict when it will next erupt. | 0:01:08 | 0:01:10 | |
This is some of this really fast moving lava. | 0:01:12 | 0:01:15 | |
30, 40, even more miles per hour. | 0:01:15 | 0:01:18 | |
The team are also investigating the surprising ways this volcano affects | 0:01:18 | 0:01:22 | |
all aspects of life here. | 0:01:22 | 0:01:24 | |
Their search for answers will take them deep inside the crater... | 0:01:32 | 0:01:36 | |
I've just come over the edge. | 0:01:36 | 0:01:38 | |
..and into great danger. | 0:01:38 | 0:01:41 | |
If any of this rock goes here, that's it for both of us. | 0:01:41 | 0:01:44 | |
On a remote jungle road, | 0:02:05 | 0:02:07 | |
the team of scientists is heading towards a highly active volcano... | 0:02:07 | 0:02:10 | |
..Nyiragongo. | 0:02:12 | 0:02:14 | |
It lies on the Democratic Republic of Congo's | 0:02:16 | 0:02:19 | |
eastern border with Rwanda. | 0:02:19 | 0:02:21 | |
To the south, just seven miles away, is Goma, | 0:02:21 | 0:02:25 | |
a city of almost a million people. | 0:02:25 | 0:02:27 | |
Last time Nyiragongo erupted, Goma was taken by surprise. | 0:02:33 | 0:02:36 | |
The expedition hopes to find new ways of predicting the next eruption | 0:02:38 | 0:02:42 | |
so the city has enough warning to evacuate. | 0:02:42 | 0:02:45 | |
The team have brought an array of equipment to investigate this | 0:02:48 | 0:02:51 | |
volcano like never before. | 0:02:51 | 0:02:52 | |
-Just take care that the men take the heavy bag. -Yes. | 0:02:56 | 0:02:59 | |
Leading the science team is Belgian volcanologist Benoit Smets. | 0:02:59 | 0:03:03 | |
Actually, that's the one I'm worried about. | 0:03:05 | 0:03:07 | |
-The seismometer? -I don't want someone to drop it. | 0:03:07 | 0:03:10 | |
Americans Professor Jeff Johnson and Dr Kayla Iacovino | 0:03:10 | 0:03:13 | |
have brought specialist kit | 0:03:13 | 0:03:15 | |
that can identify warning signs of an impending eruption. | 0:03:15 | 0:03:19 | |
I think it'll be good. | 0:03:19 | 0:03:21 | |
Is this like normal fieldwork? | 0:03:21 | 0:03:23 | |
Is this what you always bring? | 0:03:23 | 0:03:25 | |
I think, for me, this kind of | 0:03:25 | 0:03:27 | |
highlights the range of things we do in geology, right? | 0:03:27 | 0:03:31 | |
Joining them are two British scientists, | 0:03:31 | 0:03:34 | |
humanitarian Dr Xand van Tulleken | 0:03:34 | 0:03:36 | |
and geologist Professor Chris Jackson. | 0:03:36 | 0:03:39 | |
For me, I'd literally have a notebook and a pencil, a compass. | 0:03:40 | 0:03:44 | |
-A little hammer? -A little hammer! | 0:03:44 | 0:03:46 | |
Sun's out down here. Did you have a good night last night? | 0:03:52 | 0:03:55 | |
Absolutely hammered it down. | 0:03:55 | 0:03:57 | |
Really come down. Big, big... | 0:03:57 | 0:03:59 | |
Former Royal Marine Aldo Kane is in charge of getting everyone and | 0:03:59 | 0:04:02 | |
everything to the top of the volcano, | 0:04:02 | 0:04:06 | |
and he's hired in 140 local porters to help. | 0:04:06 | 0:04:10 | |
So we've got science kit, expedition kit, rigging kit, food, water. | 0:04:10 | 0:04:15 | |
Nearly four tonnes of kit that's going up the hill today. | 0:04:15 | 0:04:18 | |
Nyiragongo's crater rim is 2,000 vertical metres above the jungle | 0:04:29 | 0:04:34 | |
and only accessible on foot. | 0:04:34 | 0:04:36 | |
But Chris and Xand both know | 0:04:39 | 0:04:41 | |
how important getting the expedition to the top is... | 0:04:41 | 0:04:43 | |
..because yesterday they travelled | 0:04:46 | 0:04:48 | |
in through the city that lies at the foot of this volcano. | 0:04:48 | 0:04:51 | |
Goma is little known outside the Congo, | 0:04:57 | 0:05:01 | |
but it's an extraordinary city | 0:05:01 | 0:05:03 | |
that owes its very existence to Nyiragongo. | 0:05:03 | 0:05:05 | |
It's all made of lava, isn't it? | 0:05:12 | 0:05:14 | |
Yeah, this is all lava rock directly from Nyiragongo, | 0:05:14 | 0:05:19 | |
the volcano we're going to go and visit. | 0:05:19 | 0:05:21 | |
It's amazing to think that there's such a threat posed by that volcano, | 0:05:21 | 0:05:25 | |
yet because of that volcano | 0:05:25 | 0:05:27 | |
you can build houses and some sort of infrastructure, | 0:05:27 | 0:05:29 | |
so there's a gift and a curse, really, there with the volcano. | 0:05:29 | 0:05:33 | |
I guess I was expecting one thing | 0:05:33 | 0:05:35 | |
-and it's actually quite a lively town, isn't it? -Yeah. | 0:05:35 | 0:05:39 | |
Today, Goma is growing rapidly, | 0:05:40 | 0:05:43 | |
but it has been rebuilt, literally from ashes, | 0:05:43 | 0:05:47 | |
because in 2002 it was shattered by the eruption of Nyiragongo. | 0:05:47 | 0:05:51 | |
-NEWS CORRESPONDENT: -The red river keeps flowing, | 0:05:56 | 0:05:58 | |
pouring out of the volcano and down towards Goma. | 0:05:58 | 0:06:01 | |
With little warning, the city was overrun by lava. | 0:06:04 | 0:06:07 | |
Daylight and some of the first pictures reveal a black blanket of | 0:06:07 | 0:06:12 | |
lava covering entire neighbourhoods. | 0:06:12 | 0:06:14 | |
SIREN | 0:06:14 | 0:06:16 | |
Nyiragongo impacts life here in many unexpected ways... | 0:06:22 | 0:06:25 | |
..and it's this that Xand will be investigating. | 0:06:28 | 0:06:30 | |
I'm a doctor and I have a particular interest in humanitarian medicine. | 0:06:33 | 0:06:37 | |
I'm fascinated by this relationship to the volcano, | 0:06:37 | 0:06:40 | |
how the volcano affects every aspect of daily life here, | 0:06:40 | 0:06:44 | |
how people here cope with the constant threat of eruption, | 0:06:44 | 0:06:47 | |
and what another eruption would do to the people living here. | 0:06:47 | 0:06:50 | |
Nyiragongo has erupted twice within the last 40 years. | 0:06:52 | 0:06:56 | |
There's little doubt it will again, | 0:06:58 | 0:07:01 | |
with the same catastrophic consequences. | 0:07:01 | 0:07:03 | |
Chris has studied volcanic landscapes across the world. | 0:07:05 | 0:07:09 | |
For him, predicting eruptions is | 0:07:09 | 0:07:12 | |
both a scientific and humanitarian challenge. | 0:07:12 | 0:07:16 | |
For a geologist, this is incredibly exciting, | 0:07:16 | 0:07:18 | |
to be joining an expedition like this to do cutting-edge, | 0:07:18 | 0:07:22 | |
critical science for the people | 0:07:22 | 0:07:24 | |
living in the shadow of this giant volcano. | 0:07:24 | 0:07:26 | |
After six hours, the team are | 0:07:38 | 0:07:40 | |
reaching the upper slopes of Nyiragongo. | 0:07:40 | 0:07:42 | |
The weather's closed in and it's cold. | 0:07:49 | 0:07:52 | |
But their reward is a view of one of Earth's great natural wonders. | 0:07:56 | 0:08:01 | |
HE LAUGHS | 0:08:06 | 0:08:09 | |
Oh, my goodness. | 0:08:11 | 0:08:13 | |
So, this is the coolest thing I've ever seen, but you all seem pretty | 0:08:21 | 0:08:24 | |
psyched as well and, like, this is for you another day in the office, | 0:08:24 | 0:08:27 | |
isn't it? You're like, "Yeah, another day, another volcano." | 0:08:27 | 0:08:30 | |
No? | 0:08:30 | 0:08:31 | |
I think this might be the coolest thing I've ever seen. | 0:08:31 | 0:08:34 | |
-Really? -There's literally | 0:08:34 | 0:08:36 | |
nothing like this in the world. | 0:08:36 | 0:08:38 | |
There are six lava lakes, permanent lava lakes, on Earth. | 0:08:44 | 0:08:47 | |
You are standing looking into one of those six. | 0:08:47 | 0:08:49 | |
Of those six lava lakes, they are all babies compared to... | 0:08:49 | 0:08:52 | |
Yeah, they are. | 0:08:52 | 0:08:53 | |
All other global lava lakes could fit into this lava lake | 0:08:53 | 0:08:57 | |
with tons of room left over. | 0:08:57 | 0:08:58 | |
This lava lake is enormous. | 0:08:58 | 0:09:00 | |
The sheer size of it, I think, is just hard to even fathom. | 0:09:00 | 0:09:03 | |
The crater rim is a vast | 0:09:09 | 0:09:10 | |
1.2 kilometres in diameter. | 0:09:10 | 0:09:14 | |
Inside is a permanent cauldron of molten rock | 0:09:14 | 0:09:17 | |
that is 260 metres across, | 0:09:17 | 0:09:20 | |
more than twice the length of a football pitch... | 0:09:20 | 0:09:22 | |
..and it constantly churns at over 1,000 degrees. | 0:09:27 | 0:09:31 | |
It's ferocious. | 0:09:36 | 0:09:38 | |
It feels very alive. | 0:09:38 | 0:09:39 | |
And even when we're silent, | 0:09:41 | 0:09:43 | |
there's that constant roar. | 0:09:43 | 0:09:45 | |
It just doesn't let up at all. | 0:09:45 | 0:09:47 | |
As a structural geologist, we're | 0:09:48 | 0:09:50 | |
often left with what's at the Earth's surface, so we're looking at | 0:09:50 | 0:09:52 | |
rocks, we're describing the rocks, we're measuring the rocks, | 0:09:52 | 0:09:55 | |
we're mapping the rocks, and we may then use also some other geophysical | 0:09:55 | 0:09:59 | |
techniques to look down into the Earth, | 0:09:59 | 0:10:03 | |
but we don't need to kind of image it. | 0:10:03 | 0:10:05 | |
We're actually seeing right down into the lava lake. | 0:10:05 | 0:10:07 | |
But the team haven't come this far just to admire the view. | 0:10:11 | 0:10:14 | |
Tomorrow, they plan to abseil into the crater | 0:10:19 | 0:10:22 | |
to study the lava lake up close. | 0:10:22 | 0:10:24 | |
From where we are here, to get down there is over 400 metres. | 0:10:29 | 0:10:32 | |
So that's, what, four times Big Ben? | 0:10:32 | 0:10:34 | |
That is full-on. | 0:10:36 | 0:10:38 | |
That's where we hope to camp, down there on that second level. | 0:10:41 | 0:10:44 | |
Are you all like, "Yeah, I can't wait," | 0:10:47 | 0:10:49 | |
first light, you're going to be down there? | 0:10:49 | 0:10:51 | |
You are super-psyched to get down there? | 0:10:51 | 0:10:52 | |
Well, I don't know. This is terrifying. | 0:10:52 | 0:10:55 | |
That, to me... When I look at the lava lake, I don't see danger | 0:10:55 | 0:10:58 | |
so much. It's an amazement. It's not a fear. | 0:10:58 | 0:11:01 | |
I'm afraid of the getting down there. | 0:11:01 | 0:11:03 | |
That's terrifying. That is absolutely terrifying. | 0:11:03 | 0:11:06 | |
Understanding the lava lake's behaviour is crucial, | 0:11:17 | 0:11:21 | |
because it could be linked to forces deep inside the volcano... | 0:11:21 | 0:11:24 | |
..and may provide warning signs of an eruption. | 0:11:27 | 0:11:30 | |
But as Chris and Xand bed down for the night, | 0:11:34 | 0:11:37 | |
it's the descent into the crater, rather than volcano science, | 0:11:37 | 0:11:40 | |
that's playing on their minds. | 0:11:40 | 0:11:43 | |
Whether it's going to be the physical aspect or the mental aspect | 0:11:43 | 0:11:46 | |
that's most challenging, that's probably what I'm going to have | 0:11:46 | 0:11:49 | |
the most sleeplessness about tonight. | 0:11:49 | 0:11:52 | |
There's a lot of risk there that you can't modify. | 0:11:52 | 0:11:54 | |
-Yeah. -You can wear a helmet and stuff, | 0:11:54 | 0:11:56 | |
but if you're going to get hit by a big rock, | 0:11:56 | 0:11:58 | |
-it's going to be bad. -That's it. | 0:11:58 | 0:12:00 | |
Hello. Sorry, were you doing a video diary? | 0:12:00 | 0:12:02 | |
We're doing a big diary sesh. Now we've got the man himself. | 0:12:02 | 0:12:04 | |
Now, we've been talking about risk, Aldo. | 0:12:04 | 0:12:07 | |
When is something too risky to not do it? | 0:12:07 | 0:12:10 | |
We've done as much as we can | 0:12:10 | 0:12:11 | |
to mitigate all of the known risks that we can mitigate against, | 0:12:11 | 0:12:15 | |
and then the rest of it is just risky. | 0:12:15 | 0:12:18 | |
LAUGHTER | 0:12:18 | 0:12:20 | |
You were really doing well there. | 0:12:21 | 0:12:23 | |
It was really convincing until you said that. | 0:12:23 | 0:12:26 | |
For Xand, this is only a brief visit to the crater. | 0:12:26 | 0:12:28 | |
Now he's seen the volcano, | 0:12:31 | 0:12:33 | |
he's heading back down | 0:12:33 | 0:12:34 | |
to investigate the complex ways it impacts life in Goma. | 0:12:34 | 0:12:38 | |
First light on the crater rim. | 0:12:43 | 0:12:45 | |
The priority is to get down to the lava lake as soon as possible. | 0:12:47 | 0:12:50 | |
Even though the current weather conditions are miserable, | 0:12:53 | 0:12:56 | |
at this altitude it can get a lot worse. | 0:12:56 | 0:12:59 | |
The temperature is slightly warmer in there, | 0:12:59 | 0:13:01 | |
but it can change like that, | 0:13:01 | 0:13:03 | |
and it can go down to freezing. | 0:13:03 | 0:13:05 | |
My team were down there yesterday and were caught out in a hailstorm. | 0:13:05 | 0:13:08 | |
OK, it's just started with the heaviest hail. | 0:13:10 | 0:13:14 | |
Torrents streamed down the loose crater wall, | 0:13:19 | 0:13:23 | |
creating the climber's enemy - rock fall. | 0:13:23 | 0:13:26 | |
OK, there are waterfalls coming all down the side of the volcano. | 0:13:26 | 0:13:32 | |
And the waterfalls are knocking massive rocks | 0:13:32 | 0:13:35 | |
coming flying towards us. | 0:13:35 | 0:13:37 | |
For Aldo, the risk of bad weather means a change of plan. | 0:13:38 | 0:13:42 | |
What we want to do is cut the amount of people that are going down into | 0:13:43 | 0:13:47 | |
the volcano to essentials only. | 0:13:47 | 0:13:50 | |
And, Kayla, I was speaking to you earlier on and you mentioned you can | 0:13:50 | 0:13:53 | |
do a lot of your stuff up on the top here, | 0:13:53 | 0:13:56 | |
so I'm happy to keep you up here | 0:13:56 | 0:13:58 | |
and not take you down there because of that. | 0:13:58 | 0:14:00 | |
I can do all of the work that I need to do, basically, on the rim. | 0:14:00 | 0:14:04 | |
There are definitely some mixed emotions behind | 0:14:09 | 0:14:12 | |
me not being able to go down. | 0:14:12 | 0:14:13 | |
There's a bit of relief because it is so dangerous to do | 0:14:13 | 0:14:19 | |
and there's also a bit of disappointment because, you know, | 0:14:19 | 0:14:23 | |
what an amazing experience | 0:14:23 | 0:14:24 | |
to spend a couple of nights in the crater next to the lava lake. | 0:14:24 | 0:14:27 | |
It's something I could never have dreamed of being able to ever do. | 0:14:27 | 0:14:30 | |
Later, the weather clears, | 0:14:32 | 0:14:34 | |
and Aldo decides to get the team down. | 0:14:34 | 0:14:36 | |
I can feel my heart rate going up just putting the harness on. | 0:14:38 | 0:14:41 | |
-Wait till you look over the edge. -Yeah. | 0:14:41 | 0:14:44 | |
Last bit before we go down, kicking rocks off, | 0:14:44 | 0:14:46 | |
if you do kick a rock off, big shout, "Rock!" | 0:14:46 | 0:14:49 | |
-OK. -If one of these rocks hits someone on the head, | 0:14:49 | 0:14:52 | |
it'll kill them, even with these helmets on. | 0:14:52 | 0:14:54 | |
OK. I think I'm ready. | 0:14:54 | 0:14:56 | |
You should enjoy the view first before we go over, | 0:14:56 | 0:14:58 | |
-because after that you're going to be fairly busy. -OK. | 0:14:58 | 0:15:01 | |
Nyiragongo's crater has three levels. | 0:15:04 | 0:15:07 | |
Tier one is a small outcrop around 250 metres below the rim. | 0:15:09 | 0:15:13 | |
A sheer 80-metre drop below is tier two, | 0:15:15 | 0:15:18 | |
where the team will be camping. | 0:15:18 | 0:15:21 | |
And finally, tier three, the bottom level that surrounds the lava lake. | 0:15:21 | 0:15:25 | |
-How are you feeling? -A blend of excitement and nerves, | 0:15:25 | 0:15:28 | |
I'll be honest with you, yeah. | 0:15:28 | 0:15:30 | |
Climbing down is the most dangerous part of the expedition. | 0:15:33 | 0:15:36 | |
Doubly so for Chris... | 0:15:39 | 0:15:41 | |
Nice and gently, Chris. | 0:15:41 | 0:15:43 | |
..because he's not an experienced climber. | 0:15:43 | 0:15:45 | |
How does it feel? | 0:15:49 | 0:15:51 | |
Better now. I've just come over the edge. | 0:15:51 | 0:15:53 | |
And in such a remote location, if anything goes wrong, | 0:15:53 | 0:15:58 | |
there are no rescue teams. | 0:15:58 | 0:15:59 | |
-Sorry. -Try not to do that because there are sections, if you do that, | 0:16:03 | 0:16:06 | |
that the whole slope will go. | 0:16:06 | 0:16:08 | |
-Yeah. -All of this is just waiting to fall. | 0:16:08 | 0:16:11 | |
That wind's just picked up. | 0:16:15 | 0:16:17 | |
Yeah, yeah, I can feel it. | 0:16:17 | 0:16:18 | |
Be careful not to kick anything. | 0:16:22 | 0:16:23 | |
If you kick anything, it's coming down on my head. | 0:16:23 | 0:16:26 | |
Yeah, OK. | 0:16:31 | 0:16:34 | |
Everything's moving. | 0:16:34 | 0:16:35 | |
Nothing is stable. | 0:16:37 | 0:16:38 | |
Rock! | 0:16:41 | 0:16:43 | |
Oh, Jesus. | 0:16:46 | 0:16:48 | |
Sorry. | 0:16:50 | 0:16:52 | |
Have a look back up. | 0:16:52 | 0:16:54 | |
Oh, yeah. | 0:16:54 | 0:16:56 | |
Yeah. | 0:16:56 | 0:16:57 | |
Yeah, that's good, that's good. | 0:17:01 | 0:17:03 | |
-Ow. -You OK? -Yeah. | 0:17:06 | 0:17:07 | |
As the weather holds, the rest of the team also start the descent. | 0:17:11 | 0:17:15 | |
Just watch your feet coming down. | 0:17:17 | 0:17:19 | |
Halfway down, Aldo spots a small but potentially deadly problem. | 0:17:20 | 0:17:24 | |
Super sharp rock. | 0:17:26 | 0:17:28 | |
-You see that? -Wow. | 0:17:29 | 0:17:31 | |
What's happened there? | 0:17:31 | 0:17:32 | |
That's where the rock fall has come down and chopped this rope. | 0:17:32 | 0:17:36 | |
Has it gone through the fabric to the core? | 0:17:36 | 0:17:38 | |
It's not chopped it completely. | 0:17:38 | 0:17:40 | |
The inner core still looks like it's usable, | 0:17:40 | 0:17:43 | |
but it will have lost a lot of its strength. | 0:17:43 | 0:17:45 | |
I'm going to change over onto this, | 0:17:45 | 0:17:47 | |
and then we'll put a backup on this. | 0:17:47 | 0:17:49 | |
After three hours on the ropes, | 0:17:52 | 0:17:54 | |
Chris has almost reached tier one. | 0:17:54 | 0:17:56 | |
That's where we are heading to, to the base camp down there. | 0:17:56 | 0:17:59 | |
-OK. -OK? | 0:17:59 | 0:18:00 | |
But he needs to get to tier two | 0:18:05 | 0:18:07 | |
if he's going to have a bed for the night. | 0:18:07 | 0:18:09 | |
Goma isn't totally unprepared for Nyiragongo's next eruption. | 0:18:19 | 0:18:22 | |
The city does have a volcano observatory. | 0:18:24 | 0:18:27 | |
Its job is to keep an eye on volcanic activity... | 0:18:29 | 0:18:32 | |
..and warn people about the dangers of living in this landscape. | 0:18:34 | 0:18:37 | |
Xand is on his way to a small village just outside the city | 0:18:41 | 0:18:46 | |
to meet with two scientists... | 0:18:46 | 0:18:48 | |
..Dario Tedesco and Mathieu Yalire, | 0:18:50 | 0:18:54 | |
who work there. | 0:18:54 | 0:18:55 | |
This region comes with its own unique threats, | 0:18:57 | 0:19:00 | |
and the scientists are warning the villagers about one of them. | 0:19:00 | 0:19:03 | |
We've assembled the whole village around an area that, to me, | 0:19:08 | 0:19:11 | |
looks completely normal, but is apparently extremely dangerous, | 0:19:11 | 0:19:13 | |
and then we're going to do a demonstration. | 0:19:13 | 0:19:16 | |
EQUIPMENT BEEPS | 0:19:16 | 0:19:18 | |
Seeping from the ground is an invisible but lethal gas, | 0:19:18 | 0:19:22 | |
so the observatory scientists use goats to warn local people, | 0:19:22 | 0:19:25 | |
especially children, about its presence. | 0:19:25 | 0:19:28 | |
The animal is led into an innocuous-looking patch of ground. | 0:19:31 | 0:19:35 | |
At first, nothing happens, | 0:19:38 | 0:19:40 | |
and the goat appears fine. | 0:19:40 | 0:19:42 | |
But then, it collapses. | 0:19:47 | 0:19:49 | |
Bring him up. | 0:19:52 | 0:19:54 | |
-Bring him up. -With bottled oxygen to hand, | 0:19:54 | 0:19:57 | |
it's a simple job to bring the animal round. | 0:19:57 | 0:20:00 | |
There we go. | 0:20:01 | 0:20:04 | |
OK, OK. There we go. | 0:20:04 | 0:20:06 | |
How's he doing? Oh, he's good, he's back. | 0:20:06 | 0:20:08 | |
Good job. Good job, young man. | 0:20:08 | 0:20:11 | |
There you go. | 0:20:11 | 0:20:13 | |
Well, my first goat resus. | 0:20:13 | 0:20:15 | |
That is a very happy ending. Lovely. | 0:20:15 | 0:20:18 | |
Although it looks traumatic, the goat makes a full recovery. | 0:20:18 | 0:20:22 | |
It collapsed because it was | 0:20:22 | 0:20:23 | |
suffocated by the invisible, odourless gas, carbon dioxide. | 0:20:23 | 0:20:27 | |
This gas seeps up slowly through cracks in the rocks. | 0:20:30 | 0:20:34 | |
It comes from the volcanic system that underlies this whole area. | 0:20:34 | 0:20:37 | |
Because carbon dioxide is heavier than air, | 0:20:39 | 0:20:42 | |
it forms deadly pools in thousands | 0:20:42 | 0:20:43 | |
of shallow depressions that litter this region... | 0:20:43 | 0:20:46 | |
..making them a particular hazard for children. | 0:20:48 | 0:20:51 | |
This seems like an incredibly dangerous thing | 0:21:06 | 0:21:10 | |
to have near a village. | 0:21:10 | 0:21:11 | |
We call these areas mazuku. | 0:21:11 | 0:21:15 | |
Mazuku? | 0:21:15 | 0:21:16 | |
Mazuku means | 0:21:16 | 0:21:19 | |
-evil wind. -Evil wind? | 0:21:19 | 0:21:21 | |
Evil wind, yeah. | 0:21:21 | 0:21:23 | |
I mean, it's one thing to have your parents say, | 0:21:23 | 0:21:25 | |
"Don't go and play in the hole," | 0:21:25 | 0:21:27 | |
but it's another thing to see the goat pass out in the hole | 0:21:27 | 0:21:29 | |
and realise how dangerous it is, I think. | 0:21:29 | 0:21:32 | |
I started with a very clear idea that volcanoes are dangerous | 0:21:33 | 0:21:36 | |
because they're boiling hot and they throw out rocks and lava, | 0:21:36 | 0:21:39 | |
and actually this is a much more dangerous threat. | 0:21:39 | 0:21:41 | |
It's not evident. It's secret. | 0:21:41 | 0:21:43 | |
And because it's so un-obvious, | 0:21:43 | 0:21:45 | |
it gets the most vulnerable people in the community. | 0:21:45 | 0:21:47 | |
Back on the rock face, Chris is still descending. | 0:22:04 | 0:22:08 | |
Just ready for first. It's going to be Chris, over. | 0:22:08 | 0:22:11 | |
Make yourself comfy. | 0:22:13 | 0:22:15 | |
He's about to be lowered by Aldo and his team | 0:22:17 | 0:22:20 | |
down a final 80-metre free-hanging drop to the campsite below. | 0:22:20 | 0:22:24 | |
Clear now. | 0:22:29 | 0:22:30 | |
-Thank you. -Rock! | 0:22:32 | 0:22:34 | |
Steady. | 0:22:53 | 0:22:54 | |
-OK. -Chris is down. | 0:22:54 | 0:22:56 | |
-Thanks. Cheers, man. -Spot on. | 0:22:56 | 0:22:58 | |
-That is very good. -Oh, too intense. | 0:22:58 | 0:23:01 | |
-Don't look back. -Don't look back. | 0:23:01 | 0:23:03 | |
Don't look back. | 0:23:03 | 0:23:04 | |
So, I've made it down to tier two. | 0:23:20 | 0:23:22 | |
Daz is just sorting out the ropes to be sent back up for the next victim. | 0:23:22 | 0:23:27 | |
The first thing I noticed as soon as I come down to this level, | 0:23:27 | 0:23:30 | |
these giant chasms, | 0:23:30 | 0:23:32 | |
maybe a metre, maybe two metres wide. | 0:23:32 | 0:23:35 | |
You can see in the distance the campsite that's been set up. | 0:23:37 | 0:23:40 | |
The tents are pitched between two potentially fatal hazards. | 0:23:41 | 0:23:45 | |
The vertical drop down to the lava lake is less than 30 metres away. | 0:23:47 | 0:23:50 | |
Just behind the tents | 0:23:52 | 0:23:53 | |
lies a field of fallen rocks from the crater wall. | 0:23:53 | 0:23:56 | |
Despite the danger, for Chris, it is out of this world. | 0:24:00 | 0:24:04 | |
If I was to compare this environment anywhere else, I'd say Mars. | 0:24:05 | 0:24:10 | |
There's just blacks and whites and reds - | 0:24:10 | 0:24:12 | |
very simple colours everywhere. | 0:24:12 | 0:24:14 | |
There is no vegetation whatsoever. | 0:24:18 | 0:24:20 | |
There doesn't seem to be anything living down here. | 0:24:20 | 0:24:23 | |
One of the reasons is actually what I'm smelling. It's sulphur. | 0:24:23 | 0:24:27 | |
And all around us | 0:24:27 | 0:24:28 | |
there's these vents which are spewing out sulphur into the air. | 0:24:28 | 0:24:32 | |
As evening falls, the rest of the team descend... | 0:24:46 | 0:24:49 | |
..with Aldo the last... | 0:24:58 | 0:24:59 | |
..chancing his luck in complete darkness. | 0:25:03 | 0:25:06 | |
Tomorrow, the science can begin. | 0:25:09 | 0:25:11 | |
The next morning, down on tier two... | 0:25:18 | 0:25:20 | |
..Benoit is up first, sorting out his experiment. | 0:25:22 | 0:25:25 | |
Nyiragongo is very important for me | 0:25:28 | 0:25:30 | |
because this volcano is very dangerous. | 0:25:30 | 0:25:32 | |
It threatens a lot of people. | 0:25:32 | 0:25:34 | |
Everything we do to understand this volcano is very important to avoid | 0:25:34 | 0:25:39 | |
another disaster like in 2002. | 0:25:39 | 0:25:42 | |
Benoit wants to monitor the lava lake level | 0:25:45 | 0:25:48 | |
throughout the time in the crater. | 0:25:48 | 0:25:50 | |
He wants to work out what's going on inside Nyiragongo. | 0:25:50 | 0:25:53 | |
Unlike most volcanoes, Nyiragongo erupts from fissures in its flanks. | 0:25:55 | 0:25:59 | |
But like all volcanoes, | 0:26:01 | 0:26:02 | |
it erupts when pressure builds in its magma chamber. | 0:26:02 | 0:26:05 | |
If the team could measure that pressure, | 0:26:09 | 0:26:11 | |
it would provide a warning signal of an eruption. | 0:26:11 | 0:26:14 | |
The problem is the magma chamber is over a kilometre underground, | 0:26:14 | 0:26:19 | |
so it's impossible to measure pressure changes directly. | 0:26:19 | 0:26:21 | |
But Benoit suspects | 0:26:24 | 0:26:26 | |
those pressure changes may affect the behaviour of the lava lake. | 0:26:26 | 0:26:30 | |
Here, we have the chance to have this big lava lake, | 0:26:31 | 0:26:35 | |
and you can see the lava lake as a magmatic chamber at ground surface. | 0:26:35 | 0:26:38 | |
The plan is to use time-lapse photography | 0:26:41 | 0:26:44 | |
to record any changes in the lake level. | 0:26:44 | 0:26:47 | |
But when it spends half its time hidden by clouds of gas, | 0:26:47 | 0:26:50 | |
it's tricky to see, | 0:26:50 | 0:26:53 | |
so Benoit has built his own infrared cameras to overcome this problem. | 0:26:53 | 0:26:56 | |
I made these boxes myself. | 0:27:01 | 0:27:04 | |
My box is made of a microcomputer | 0:27:04 | 0:27:07 | |
that will control everything, | 0:27:07 | 0:27:09 | |
a real-time clock | 0:27:09 | 0:27:10 | |
to have an accurate time, | 0:27:10 | 0:27:12 | |
and a camera. | 0:27:12 | 0:27:14 | |
It's a small camera like you have in your smartphone. | 0:27:14 | 0:27:18 | |
And it'll take every ten seconds, | 0:27:18 | 0:27:20 | |
and by comparing these pictures | 0:27:20 | 0:27:22 | |
I will be able to see the variations of the lava lake level. | 0:27:22 | 0:27:25 | |
The next day, Benoit returns to his cameras to see if they've worked, | 0:27:31 | 0:27:36 | |
and, more importantly, | 0:27:36 | 0:27:37 | |
whether they can reveal anything about pressure in the magma chamber. | 0:27:37 | 0:27:41 | |
Whoa. | 0:27:41 | 0:27:43 | |
We've got a beautiful lava lake level drop compared to yesterday | 0:27:43 | 0:27:47 | |
at the same time. It's great. | 0:27:47 | 0:27:49 | |
So we recorded something special. | 0:27:49 | 0:27:51 | |
The home-made technology works. | 0:27:53 | 0:27:55 | |
Over the last 24 hours, | 0:27:55 | 0:27:57 | |
the cameras recorded a small drop in the lake level. | 0:27:57 | 0:28:00 | |
This suggests pressure in the magma chamber does affect the lava lake. | 0:28:00 | 0:28:05 | |
It's not about having the lava lake level high or low, | 0:28:05 | 0:28:08 | |
it's understanding these movements to predict | 0:28:08 | 0:28:12 | |
big events like a flank eruption. | 0:28:12 | 0:28:16 | |
We have the opportunity to measure the pressure change | 0:28:16 | 0:28:19 | |
by looking at the lava lake level. | 0:28:19 | 0:28:20 | |
At the moment, the volcano is stable, | 0:28:23 | 0:28:26 | |
so there are only small changes in pressure. | 0:28:26 | 0:28:29 | |
If the volcano was building towards an eruption, | 0:28:29 | 0:28:32 | |
Benoit would expect to see huge variations in level, | 0:28:32 | 0:28:35 | |
40 metres or more. | 0:28:35 | 0:28:36 | |
His cameras can spot these changes, | 0:28:39 | 0:28:42 | |
but they're not designed to be left in the crater... | 0:28:42 | 0:28:44 | |
..so the team need to find a way to permanently monitor the lake level | 0:28:46 | 0:28:50 | |
to provide Goma with a warning. | 0:28:50 | 0:28:52 | |
Despite the threat of a volcanic eruption, Goma is a growing city. | 0:29:00 | 0:29:05 | |
Each new house is built on old lava flows. | 0:29:06 | 0:29:09 | |
This brings with it a potentially fatal health problem. | 0:29:09 | 0:29:12 | |
I didn't... I didn't bring any safety goggles, | 0:29:24 | 0:29:27 | |
so I've got my sun specs instead. | 0:29:27 | 0:29:29 | |
Every house starts with a stonemason | 0:29:30 | 0:29:33 | |
like Heritier, chiselling out a long drop toilet. | 0:29:33 | 0:29:37 | |
Problem is, cooled lava is an incredibly hard rock. | 0:29:37 | 0:29:41 | |
I've been doing this for about 30 seconds and I'm winded. | 0:29:41 | 0:29:45 | |
Heritier's job is tough but necessary, | 0:29:52 | 0:29:55 | |
because without toilets, | 0:29:55 | 0:29:57 | |
there's a deadly side-effect of living on lava. | 0:29:57 | 0:29:59 | |
Long drop toilets work really well if you have a long drop toilet. | 0:30:00 | 0:30:04 | |
And the problem here is that there have been loads and loads of things | 0:30:04 | 0:30:07 | |
in Goma that have moved people out of Goma or moved people into them | 0:30:07 | 0:30:09 | |
where they don't have toilets. | 0:30:09 | 0:30:11 | |
We have refugee movement, violent conflict, and volcanic eruptions. | 0:30:11 | 0:30:15 | |
And so if you have people without access to toilets, | 0:30:15 | 0:30:18 | |
what you have is massive spread of infectious diarrhoeal illness, | 0:30:18 | 0:30:23 | |
particularly cholera. | 0:30:23 | 0:30:24 | |
This is one of the world hotspots for cholera. | 0:30:24 | 0:30:27 | |
An estimated 13,000 refugees have died in the last week, | 0:30:29 | 0:30:33 | |
mostly from cholera, and the bodies line the streets. | 0:30:33 | 0:30:37 | |
In 1994, more than a million people crossed the border, | 0:30:37 | 0:30:41 | |
which is just a few miles in that direction, | 0:30:41 | 0:30:43 | |
from Rwanda, Rwandan refugees, | 0:30:43 | 0:30:45 | |
and they stopped in Goma and in the surrounding countryside. | 0:30:45 | 0:30:49 | |
A team of nurses are desperately trying to save the dying. | 0:30:50 | 0:30:54 | |
There's a scramble to set up drips of rehydration fluids and salts. | 0:30:54 | 0:30:57 | |
I've worked in cholera epidemics, | 0:30:59 | 0:31:00 | |
and it's almost impossible to | 0:31:00 | 0:31:02 | |
describe the amount of diarrhoea that's produced. | 0:31:02 | 0:31:05 | |
So in a cholera treatment centre, | 0:31:05 | 0:31:06 | |
you have sloping floors and you have beds with holes in them, | 0:31:06 | 0:31:09 | |
so people go to the toilet directly onto the floor | 0:31:09 | 0:31:11 | |
and you're just washing it into a central gutter. | 0:31:11 | 0:31:14 | |
It's unbelievable, the quantities of fluid that you need to replace. | 0:31:14 | 0:31:18 | |
We are talking about 20 litres, | 0:31:18 | 0:31:20 | |
sometimes more, per day, of diarrhoea. | 0:31:20 | 0:31:23 | |
So it can kill you within hours. | 0:31:23 | 0:31:25 | |
The added layer of tragedy on top of that number of deaths | 0:31:27 | 0:31:31 | |
is that, in this region, digging graves is virtually impossible, | 0:31:31 | 0:31:34 | |
as you can see. Very, very hard to do. | 0:31:34 | 0:31:37 | |
The cholera outbreak in 1994 | 0:31:38 | 0:31:40 | |
was caused by a mass movement of people | 0:31:40 | 0:31:43 | |
with no access to decent sanitation, | 0:31:43 | 0:31:46 | |
so human waste polluted Goma's main water source. | 0:31:46 | 0:31:49 | |
Goma's population has now grown to almost a million people, | 0:32:15 | 0:32:19 | |
so when Nyiragongo next erupts | 0:32:19 | 0:32:21 | |
there will be a mass evacuation | 0:32:21 | 0:32:23 | |
in numbers that haven't been seen since 1994. | 0:32:23 | 0:32:26 | |
SIREN | 0:32:27 | 0:32:29 | |
Practice drills have recently been introduced to test the response of | 0:32:33 | 0:32:37 | |
police, charities, and medical aid to an eruption. | 0:32:37 | 0:32:40 | |
But the danger is that hundreds of thousands of people | 0:32:47 | 0:32:50 | |
fleeing their homes | 0:32:50 | 0:32:52 | |
will find themselves without access to a toilet, | 0:32:52 | 0:32:54 | |
leading to another epidemic. | 0:32:54 | 0:32:56 | |
This town, Goma, | 0:32:57 | 0:32:59 | |
is one of the first places I ever heard about when I started studying | 0:32:59 | 0:33:02 | |
tropical medicine. I guess I thought that I knew a fair bit, | 0:33:02 | 0:33:06 | |
and what I really love, and what's been very interesting and amazing, | 0:33:06 | 0:33:11 | |
is that I really didn't understand anything at all. | 0:33:11 | 0:33:14 | |
I guess you wouldn't think that | 0:33:14 | 0:33:17 | |
a bacteria getting inside you and giving you diarrhoea | 0:33:17 | 0:33:19 | |
would be determined by a volcano. | 0:33:19 | 0:33:21 | |
Up on the volcano rim, Kayla is starting her investigation. | 0:33:26 | 0:33:29 | |
She's studying the gases | 0:33:31 | 0:33:32 | |
that constantly vent from the lake's surface... | 0:33:32 | 0:33:35 | |
..because they can provide another way | 0:33:38 | 0:33:39 | |
to tell what's happening in the magma chamber. | 0:33:39 | 0:33:42 | |
The real power in gas measurements is that it can tell us about | 0:33:44 | 0:33:47 | |
the entire system miles and miles beneath your feet. | 0:33:47 | 0:33:49 | |
So that's where the action is. That is the driving force of volcanism. | 0:33:49 | 0:33:53 | |
It's controlled deep down in the guts of the volcano. | 0:33:53 | 0:33:57 | |
All lava contains gases, | 0:33:59 | 0:34:02 | |
but when an eruption is building, those gases change. | 0:34:02 | 0:34:05 | |
The one that alarms volcanologists is sulphur dioxide, | 0:34:07 | 0:34:11 | |
because it often signals that lava is moving up towards the surface. | 0:34:11 | 0:34:15 | |
With a simple device called a gas box, Kayla can detect its presence. | 0:34:18 | 0:34:23 | |
Sulphur dioxide is the kind of gas that bubbles out of the magma | 0:34:23 | 0:34:26 | |
in the really shallow part of the system, | 0:34:26 | 0:34:28 | |
so just beneath the lava lake. | 0:34:28 | 0:34:30 | |
If we see, all of a sudden, | 0:34:30 | 0:34:31 | |
a huge spike in the amount of sulphur dioxide | 0:34:31 | 0:34:34 | |
that's coming out of the crater, | 0:34:34 | 0:34:35 | |
that could be something that happens before an eruption. | 0:34:35 | 0:34:38 | |
After 12 hours, Kayla returns to find out what's been recorded. | 0:34:42 | 0:34:46 | |
So, I'm just looking at the data now, and I'm pretty happy. | 0:34:52 | 0:34:54 | |
So, these are sulphur dioxide. We're getting some readings there. | 0:34:54 | 0:34:58 | |
Less than one part per million, but there is some reading there. | 0:34:58 | 0:35:01 | |
So maybe not an immediate eruption. | 0:35:01 | 0:35:03 | |
This low sulphur dioxide reading | 0:35:04 | 0:35:06 | |
means no new magma is rising up through the volcano. | 0:35:06 | 0:35:09 | |
For the moment, Goma is safe. | 0:35:10 | 0:35:13 | |
The problem is, gases on their own are an unreliable warning indicator. | 0:35:15 | 0:35:19 | |
Sampling them depends on weather conditions and wind direction. | 0:35:19 | 0:35:23 | |
But the team are hoping to test another piece of technology | 0:35:23 | 0:35:26 | |
that could provide a better way to warn of an eruption. | 0:35:26 | 0:35:29 | |
When Nyiragongo erupted in 2002, lava flows split the city in three, | 0:35:40 | 0:35:46 | |
killing around 100 people | 0:35:46 | 0:35:47 | |
as the rest of the city fled for their lives. | 0:35:47 | 0:35:50 | |
So is that where the lava got to? | 0:35:53 | 0:35:55 | |
Yeah, exactly. The lava came and stopped... | 0:35:55 | 0:35:58 | |
Xand's meeting local journalist Caleb Kabanda | 0:35:58 | 0:36:01 | |
to find out what it was like | 0:36:01 | 0:36:03 | |
and if there are any lessons to be learned. | 0:36:03 | 0:36:05 | |
You couldn't get to, like, the top of a big building? | 0:36:08 | 0:36:11 | |
The lava has been flowing for two days now. | 0:36:40 | 0:36:43 | |
It shows no sign of stopping. | 0:36:43 | 0:36:45 | |
So you come back that morning, and what does the city look like? | 0:36:48 | 0:36:51 | |
As if the people of Goma had not suffered enough, | 0:37:22 | 0:37:25 | |
this was a day that brought them more death, more tragedy. | 0:37:25 | 0:37:29 | |
Fireballs filled the sky after a petrol station here exploded. | 0:37:29 | 0:37:33 | |
Fuel cans leapt into the air. | 0:37:33 | 0:37:36 | |
Walking through Goma, having heard Caleb's story, | 0:37:45 | 0:37:48 | |
it's hard to think back to 2002 and imagine lava flowing through these | 0:37:48 | 0:37:52 | |
streets, knocking buildings down, destroying everything. | 0:37:52 | 0:37:56 | |
But what's even harder to imagine is how little time it took for the city | 0:37:57 | 0:38:01 | |
to be inundated, how it seemed to be caught unawares. | 0:38:01 | 0:38:05 | |
No matter how much warning the science team can provide, | 0:38:09 | 0:38:12 | |
Goma's residents still need to know how much time they have to evacuate | 0:38:12 | 0:38:17 | |
once the lava starts flowing from the volcano. | 0:38:17 | 0:38:19 | |
Back in the crater, the team are now focusing on how quickly | 0:38:27 | 0:38:29 | |
the lava could reach Goma. | 0:38:29 | 0:38:32 | |
That's down to how fast it will flow during the next eruption. | 0:38:32 | 0:38:35 | |
To find out, they'd ideally study | 0:38:41 | 0:38:43 | |
the chemical composition of lava from the lake. | 0:38:43 | 0:38:46 | |
But collecting samples is simply too dangerous. | 0:38:46 | 0:38:50 | |
There is, though, another possibility. | 0:38:50 | 0:38:52 | |
During preparations for filming, | 0:38:55 | 0:38:57 | |
Aldo witnessed a new vent opening up | 0:38:57 | 0:38:59 | |
that sent rivers of lava running across tier three, | 0:38:59 | 0:39:02 | |
the crater floor. | 0:39:02 | 0:39:05 | |
We were supposed to be heading down, | 0:39:05 | 0:39:07 | |
but this aggressive vent here is | 0:39:07 | 0:39:11 | |
constantly boiling and the, er... | 0:39:11 | 0:39:14 | |
You can see there the lava bombs that are getting blown out of there | 0:39:15 | 0:39:18 | |
are probably 40, 50 metres into the air. | 0:39:18 | 0:39:20 | |
For Aldo, it was terrifying. | 0:39:23 | 0:39:25 | |
Just so many... | 0:39:31 | 0:39:33 | |
Now the vent is simply smoking. | 0:39:42 | 0:39:43 | |
But the lava flows it left are just a few months old. | 0:39:45 | 0:39:49 | |
They could be what the scientists need. | 0:39:49 | 0:39:52 | |
So the plan is to descend to tier three. | 0:39:52 | 0:39:55 | |
First, they need to check if the lava is cool enough to walk on. | 0:39:56 | 0:39:59 | |
We're about to launch a thermal camera fitted to a drone | 0:40:01 | 0:40:07 | |
that the Belgian science team have brought along, and it's going to be | 0:40:07 | 0:40:10 | |
flown over T3, the lowermost level next to the lava lake, | 0:40:10 | 0:40:15 | |
specifically to look at where there may be hot rocks or magma | 0:40:15 | 0:40:20 | |
underneath a thin crust. | 0:40:20 | 0:40:22 | |
So if we go over the fumaroles, we know they are about 60 degrees. | 0:40:22 | 0:40:25 | |
So this would be, like, something we can use for... | 0:40:25 | 0:40:27 | |
What's its max? | 0:40:27 | 0:40:29 | |
-500. -500. -Yeah. | 0:40:29 | 0:40:31 | |
-Don't go over the lake! -No! | 0:40:31 | 0:40:32 | |
It's flying back this way. | 0:40:38 | 0:40:41 | |
Yeah, there's something really hot there. | 0:40:42 | 0:40:45 | |
It could be this vent. | 0:40:45 | 0:40:46 | |
I have a problem with the drone. | 0:40:46 | 0:40:48 | |
I cannot control it. | 0:40:48 | 0:40:49 | |
Is the drone... Have you got control? | 0:40:49 | 0:40:51 | |
-No. -Maybe you can move, try to keep the signal. | 0:40:51 | 0:40:54 | |
Yeah, I think here. | 0:40:54 | 0:40:56 | |
Just watch the... | 0:40:56 | 0:40:58 | |
So we're, kind of, almost over | 0:40:58 | 0:41:00 | |
the area that we'll be running the ropes in and abseiling down. | 0:41:00 | 0:41:03 | |
Was that safe enough for tomorrow? | 0:41:03 | 0:41:05 | |
I think that's fine as long as we don't go too close to the vent, | 0:41:05 | 0:41:08 | |
which was really hot, but everything else was OK. | 0:41:08 | 0:41:10 | |
I'm coming back, because I cannot control the drone. | 0:41:10 | 0:41:13 | |
The wind is too strong. | 0:41:13 | 0:41:15 | |
I've got visual. | 0:41:15 | 0:41:16 | |
The crater floor is just about safe enough to walk on. | 0:41:23 | 0:41:26 | |
But, by chance, Chris has discovered | 0:41:30 | 0:41:32 | |
that it's not just the bottom of the crater that's warm beneath the feet. | 0:41:32 | 0:41:36 | |
I've walked only ten metres away from the camp to take a pee, | 0:41:37 | 0:41:40 | |
which is the minimum distance we have all agreed we should go | 0:41:40 | 0:41:43 | |
before we actually use the toilet, and I've found out | 0:41:43 | 0:41:46 | |
something remarkable about the rocks just around us. | 0:41:46 | 0:41:48 | |
I'm going to pour some water on here in a live experiment | 0:41:48 | 0:41:51 | |
to show you just how changeable and hostile this environment is. | 0:41:51 | 0:41:54 | |
The water boils straightaway | 0:41:59 | 0:42:02 | |
as it hits the rocks here, | 0:42:02 | 0:42:04 | |
produces this horrible sulphuric acid smell or sulphur smell which | 0:42:04 | 0:42:09 | |
has gone straight in my nostrils, | 0:42:09 | 0:42:10 | |
so I think this isn't going to be my toilet place of choice any more. | 0:42:10 | 0:42:13 | |
While Chris heads off to find a new location, | 0:42:15 | 0:42:18 | |
at the edge of the cliff face | 0:42:18 | 0:42:19 | |
Aldo is preparing the climb down to tier three | 0:42:19 | 0:42:22 | |
for petrologist Olivier Namur. | 0:42:22 | 0:42:25 | |
He thinks samples from the recent lava flow will reveal | 0:42:25 | 0:42:28 | |
if the next eruption will be fast flowing or slow moving lava. | 0:42:28 | 0:42:32 | |
I'm interested in the composition of the lavas | 0:42:34 | 0:42:36 | |
and the evolution through time, | 0:42:36 | 0:42:38 | |
so I've been sampling old lavas in the last couple of days | 0:42:38 | 0:42:41 | |
and I will be sampling this very young lava | 0:42:41 | 0:42:43 | |
that erupted last year on tier three. | 0:42:43 | 0:42:46 | |
I think it's about 100 metres, so, that's... | 0:42:46 | 0:42:48 | |
I think where we are now is about the height | 0:42:48 | 0:42:51 | |
of the white cliffs of Dover. | 0:42:51 | 0:42:52 | |
Yeah, thereabouts. | 0:42:52 | 0:42:54 | |
I've never been down here before. | 0:42:54 | 0:42:56 | |
This is going to be my first time. | 0:42:57 | 0:42:59 | |
The descent isn't straightforward. | 0:43:03 | 0:43:05 | |
There's an initial short abseil, | 0:43:05 | 0:43:07 | |
then a sloping field of fallen boulders where the crater wall has | 0:43:07 | 0:43:11 | |
collapsed, followed by a final | 0:43:11 | 0:43:13 | |
vertical drop down to the crater floor. | 0:43:13 | 0:43:16 | |
It all has to be rigged safely, | 0:43:16 | 0:43:19 | |
so Aldo goes first. | 0:43:19 | 0:43:21 | |
So brittle. | 0:43:21 | 0:43:23 | |
-RADIO: -Go ahead. | 0:43:25 | 0:43:26 | |
That's both Daz and I on boulder field, over. | 0:43:26 | 0:43:28 | |
Whoa, there's some big chunks of rock there, mate. | 0:43:35 | 0:43:40 | |
About 150 metres away from the lava lake at the minute, but... | 0:43:40 | 0:43:43 | |
I reckon, Daz, about 80 metres? | 0:43:44 | 0:43:47 | |
So it's about 80 metres straight down there. | 0:43:47 | 0:43:49 | |
At the foot of the cliff, | 0:43:52 | 0:43:53 | |
recent rock fall is clear evidence of its fragility. | 0:43:53 | 0:43:57 | |
Oh, man, look at these rocks. | 0:43:57 | 0:44:00 | |
Just precariously balanced. | 0:44:00 | 0:44:02 | |
If any of these rocks decide to go... | 0:44:02 | 0:44:04 | |
..then that's it. | 0:44:09 | 0:44:10 | |
As Aldo drops over the edge, | 0:44:15 | 0:44:17 | |
Daz, his climbing buddy, keeps an eye on him. | 0:44:17 | 0:44:20 | |
Any false move could create a lethal rock fall. | 0:44:32 | 0:44:35 | |
Even up on the camping level, Benoit can see the risk Aldo is taking. | 0:44:45 | 0:44:50 | |
Mate, right here. | 0:45:01 | 0:45:03 | |
So, I've just arrived on tier three. | 0:45:05 | 0:45:07 | |
The lava lake is about 100 meters that way | 0:45:09 | 0:45:12 | |
and that is the route I've just abseiled down. | 0:45:12 | 0:45:16 | |
It is... | 0:45:16 | 0:45:17 | |
..without doubt, | 0:45:18 | 0:45:20 | |
one of the most dangerous things I've ever done. | 0:45:20 | 0:45:23 | |
My mouth is dry... | 0:45:24 | 0:45:26 | |
..and my heart rate is up. | 0:45:28 | 0:45:29 | |
All the classic signs of... | 0:45:32 | 0:45:34 | |
..100% pure, unadulterated fear. | 0:45:37 | 0:45:40 | |
Time to get out. | 0:45:49 | 0:45:50 | |
It is super sketchy. | 0:46:01 | 0:46:03 | |
I think it's the most sketchiest thing that | 0:46:03 | 0:46:06 | |
I've seen since being in here. | 0:46:06 | 0:46:09 | |
I don't know what you're used to, but... | 0:46:09 | 0:46:11 | |
..not entirely sure I would go back down there. | 0:46:13 | 0:46:16 | |
If you think it's not a good idea, we'll not take the risk. | 0:46:16 | 0:46:20 | |
I mean, we are here to do good science | 0:46:20 | 0:46:22 | |
and collect exceptional data, but not taking stupid risks. | 0:46:22 | 0:46:27 | |
I know you well enough to know | 0:46:27 | 0:46:30 | |
that if that situation down there is... | 0:46:30 | 0:46:34 | |
..you're fearful of that, then... | 0:46:34 | 0:46:37 | |
No, it's too dangerous. | 0:46:37 | 0:46:39 | |
Let's forget about going to tier three. | 0:46:39 | 0:46:41 | |
The team abandon the planned descent to the crater floor, | 0:46:45 | 0:46:49 | |
but there is still a possible source of fresh lava. | 0:46:49 | 0:46:51 | |
During the recent eruption, the vent threw out lava bombs, | 0:46:53 | 0:46:57 | |
and some may have landed on the boulder field | 0:46:57 | 0:47:00 | |
halfway down to tier three. | 0:47:00 | 0:47:02 | |
If they can find any, Olivier will have his sample of lava. | 0:47:02 | 0:47:05 | |
For the rock samples, we can have some spatters. | 0:47:08 | 0:47:11 | |
-Yeah, but only... -..coming from the vent in the boulder field. | 0:47:11 | 0:47:14 | |
It's not ideal. | 0:47:14 | 0:47:16 | |
It's not ideal but it's better than nothing. | 0:47:16 | 0:47:19 | |
The team quickly get to work. | 0:47:24 | 0:47:27 | |
No-one wants to hang around here too long. | 0:47:27 | 0:47:29 | |
I mean, you're standing hammering a cliff | 0:47:33 | 0:47:36 | |
which is clearly already unstable. | 0:47:36 | 0:47:39 | |
Yeah, this is true but this is the only way to get these samples. | 0:47:39 | 0:47:44 | |
Olivier soon finds what he was looking for - new lava bombs. | 0:47:44 | 0:47:48 | |
What have you got? | 0:47:49 | 0:47:50 | |
It's a very fine grained lava. | 0:47:50 | 0:47:53 | |
This should be enough. | 0:47:53 | 0:47:55 | |
It's quite fresh. I think that will tell us quite a lot about | 0:47:55 | 0:47:58 | |
the recent activity of the volcano. | 0:47:58 | 0:48:00 | |
They are quite nice. | 0:48:02 | 0:48:03 | |
After one happily uneventful hour, | 0:48:05 | 0:48:08 | |
he has enough samples | 0:48:08 | 0:48:10 | |
and, for an experienced geologist, | 0:48:10 | 0:48:12 | |
they contain an unmistakable message, | 0:48:12 | 0:48:14 | |
but it's not good news. | 0:48:14 | 0:48:16 | |
Let me show you one of the samples that I collected | 0:48:16 | 0:48:19 | |
from the active vent. | 0:48:19 | 0:48:20 | |
We can see that these samples are a glassy black matrix. | 0:48:23 | 0:48:27 | |
We can see a lot of bubbles here around, | 0:48:27 | 0:48:30 | |
and a few tiny white crystals. | 0:48:30 | 0:48:32 | |
We know that the composition of these volcanoes are low in silica, | 0:48:32 | 0:48:36 | |
very low, below 40%. | 0:48:36 | 0:48:38 | |
This makes this lava very fluid, so they have low viscosity, | 0:48:38 | 0:48:42 | |
they will be flowing like water | 0:48:42 | 0:48:43 | |
along the flanks of the volcano, rather than mud. | 0:48:43 | 0:48:47 | |
And on top of that, because they have only a few crystals, | 0:48:47 | 0:48:49 | |
that decreases again the viscosity of this lava. | 0:48:49 | 0:48:52 | |
Because they have only a few crystals, they are very fluid. | 0:48:52 | 0:48:56 | |
So I suspect that if there is a new eruption, with this composition, | 0:48:56 | 0:48:59 | |
it might be flowing even faster than during 2002. | 0:48:59 | 0:49:02 | |
In 2002, lava flowed into Goma | 0:49:07 | 0:49:10 | |
at reported speeds of up to 40 kilometres per hour, | 0:49:10 | 0:49:14 | |
reaching its centre in fewer than ten hours. | 0:49:14 | 0:49:17 | |
Olivier's samples have revealed that next time, it could be even faster, | 0:49:18 | 0:49:22 | |
so the city may have even less time to evacuate. | 0:49:22 | 0:49:25 | |
That makes the need for an effective warning system more pressing. | 0:49:26 | 0:49:29 | |
Tomorrow, the team have the last piece of kit to test. | 0:49:31 | 0:49:35 | |
Nyiragongo creates a unique set of problems for | 0:49:44 | 0:49:47 | |
the people who live in its shadow. | 0:49:47 | 0:49:49 | |
But there's another side to this city - | 0:49:49 | 0:49:52 | |
the character that's defined by the volcano. | 0:49:52 | 0:49:54 | |
It's symbolised by a local invention | 0:49:56 | 0:49:58 | |
that is found nowhere else in Africa - | 0:49:58 | 0:50:01 | |
a deceptively simple wooden scooter called a chukudu. | 0:50:01 | 0:50:06 | |
Xand wants to find out the story behind them. | 0:50:06 | 0:50:08 | |
Since I arrived in Goma, I've seen hundreds of these things. | 0:50:12 | 0:50:15 | |
They're all over the place. | 0:50:15 | 0:50:16 | |
They're usually carrying massive, massive loads. | 0:50:16 | 0:50:19 | |
They're real feature of the landscape here. | 0:50:19 | 0:50:22 | |
But seeing them up close, I mean, | 0:50:25 | 0:50:27 | |
carving a perfectly circular wheel out of hardwood with a machete is... | 0:50:27 | 0:50:33 | |
I don't think it looks easy, but it's a lot harder than it looks. | 0:50:35 | 0:50:38 | |
Can I try? OK. | 0:50:41 | 0:50:44 | |
Like that? OK. | 0:50:44 | 0:50:46 | |
I'm not very good at this. | 0:50:46 | 0:50:48 | |
You made it look... You made it look very easy. | 0:50:49 | 0:50:51 | |
I got a little bit off there. | 0:50:57 | 0:50:58 | |
How did you learn to do this? | 0:51:00 | 0:51:02 | |
How much weight could this chukudu carry? | 0:51:09 | 0:51:11 | |
You don't have a tape measure. | 0:51:15 | 0:51:16 | |
What colour can I get it in? | 0:51:27 | 0:51:30 | |
The chukudus tell... | 0:51:30 | 0:51:32 | |
..almost tell the story of the whole region | 0:51:32 | 0:51:34 | |
just captured in this one thing. | 0:51:34 | 0:51:35 | |
You have people doing a kind of extraordinary job | 0:51:37 | 0:51:41 | |
under unbelievably difficult circumstances. | 0:51:41 | 0:51:44 | |
You don't find these anywhere else | 0:51:44 | 0:51:46 | |
and that's because this is a totally unique place. | 0:51:46 | 0:51:48 | |
There isn't really another landscape like it. | 0:51:48 | 0:51:51 | |
It's very difficult to farm. It's very difficult to move stuff around. | 0:51:53 | 0:51:56 | |
You do see this extraordinary | 0:51:58 | 0:52:00 | |
level of work and resilience and willingness to try and imagine | 0:52:00 | 0:52:05 | |
a better future and work towards it. | 0:52:05 | 0:52:07 | |
This is almost a symbol of resistance | 0:52:08 | 0:52:10 | |
and a very, very big part of people's identity here. | 0:52:10 | 0:52:13 | |
Back inside the crater, the team return to their main challenge... | 0:52:20 | 0:52:24 | |
..detecting signs of an impending eruption. | 0:52:25 | 0:52:29 | |
Earlier, Benoit established | 0:52:29 | 0:52:31 | |
that sudden, erratic changes in the lava lake level | 0:52:31 | 0:52:34 | |
usually happen before an eruption, | 0:52:34 | 0:52:37 | |
so the key to an early warning system is monitoring that level. | 0:52:37 | 0:52:40 | |
American volcanologist Jeff Johnson thinks he can do this by listening | 0:52:43 | 0:52:48 | |
to the sounds Nyiragongo produces. | 0:52:48 | 0:52:50 | |
But not just any sounds. | 0:52:51 | 0:52:52 | |
This is a custom-built microphone, | 0:52:55 | 0:52:57 | |
and it's capable of recording sounds | 0:52:57 | 0:52:59 | |
beyond the threshold of human hearing. | 0:52:59 | 0:53:03 | |
Jeff's microphone is designed to pick up very low-frequency sound, | 0:53:03 | 0:53:07 | |
what's known as infrasound. | 0:53:07 | 0:53:09 | |
Volcanoes speak at low frequencies. | 0:53:09 | 0:53:12 | |
They generate sound that we can hear, | 0:53:12 | 0:53:14 | |
but they also generate this world of infrasound... | 0:53:14 | 0:53:17 | |
..a unique voice print that we want to recognise and understand | 0:53:19 | 0:53:24 | |
so that when that tone changes in the future, | 0:53:24 | 0:53:26 | |
we will be able to understand what's going on. | 0:53:26 | 0:53:29 | |
The theory is that, like a sliding trombone, | 0:53:32 | 0:53:36 | |
as the level of the lava lake rises and falls, | 0:53:36 | 0:53:39 | |
the infrasound tone changes. | 0:53:39 | 0:53:40 | |
Using infrasound is at the cutting edge of volcano science, | 0:53:44 | 0:53:48 | |
and Chris is keen to see how it works. | 0:53:48 | 0:53:50 | |
So we're listening to sounds coming from the lava lake, is that right? | 0:53:57 | 0:54:01 | |
We're trying to hear the lava lake with these sensors? | 0:54:01 | 0:54:03 | |
The infrasound is detecting motions | 0:54:03 | 0:54:05 | |
that occur both at the lava lake surface | 0:54:05 | 0:54:07 | |
and also inside this bowl, that can be vibrating. | 0:54:07 | 0:54:10 | |
You don't think of a caldera this big as being an air mass | 0:54:13 | 0:54:16 | |
-that may be going up and down. -No. | 0:54:16 | 0:54:18 | |
But that's what we have discovered, | 0:54:18 | 0:54:20 | |
the crater actually acts as a musical instrument. | 0:54:20 | 0:54:23 | |
First, the microphones need to be installed. | 0:54:24 | 0:54:27 | |
To detect the infra sound tone, | 0:54:28 | 0:54:30 | |
Jeff and Chris place groups of them | 0:54:30 | 0:54:32 | |
at several locations around the crater, | 0:54:32 | 0:54:35 | |
as close to the edge as they dare. | 0:54:35 | 0:54:37 | |
Go from here to there. | 0:54:37 | 0:54:39 | |
-Yeah. -And from here to there. | 0:54:39 | 0:54:41 | |
OK. | 0:54:41 | 0:54:42 | |
It's not long before they are producing results. | 0:54:49 | 0:54:52 | |
So we've collected some data. | 0:54:53 | 0:54:55 | |
It looks like a bunch of wiggles on a screen to me. | 0:54:55 | 0:54:57 | |
What noise is the volcano making? | 0:54:57 | 0:55:00 | |
Right, so, we can't hear infrasound, | 0:55:00 | 0:55:02 | |
but we can speed it up and we can make it audible. | 0:55:02 | 0:55:04 | |
Here's an example of the infrasound being sped up... | 0:55:04 | 0:55:06 | |
-RATTLING -..by a factor of 40. | 0:55:06 | 0:55:10 | |
This, to me, is exciting. | 0:55:10 | 0:55:11 | |
I see the data, it's good, good quality, and I am happy. | 0:55:11 | 0:55:15 | |
Different infrasound tones | 0:55:16 | 0:55:18 | |
correlate with different levels of the lava lake. | 0:55:18 | 0:55:21 | |
Installing a network of microphones within the crater would mean | 0:55:21 | 0:55:24 | |
the level can be monitored remotely, | 0:55:24 | 0:55:26 | |
and any dramatic changes in the lake level used as a warning. | 0:55:26 | 0:55:30 | |
So it would be fair to say that infrasound could help better | 0:55:30 | 0:55:33 | |
protect the people of Goma from a volcanic eruption? | 0:55:33 | 0:55:35 | |
So, I'm a scientist and I'm naturally cagey about | 0:55:35 | 0:55:38 | |
answering a question like that but, yes, I do believe | 0:55:38 | 0:55:40 | |
that infrasound is a fundamental tool for volcano monitoring | 0:55:40 | 0:55:44 | |
and, not too far down the road, we will be able to use | 0:55:44 | 0:55:47 | |
infrasound monitoring here to better forecast Nyiragongo's next eruption. | 0:55:47 | 0:55:51 | |
The science team are packing up, ready to head out of the crater. | 0:55:56 | 0:55:59 | |
It's a time to reflect on what's been achieved. | 0:56:03 | 0:56:06 | |
The volcanoes can live for millions of years and we're here for a couple | 0:56:12 | 0:56:15 | |
of weeks, but we're getting the beginnings of an idea of what | 0:56:15 | 0:56:18 | |
this volcano is capable of doing. | 0:56:18 | 0:56:20 | |
Their work has revealed that, for the moment, Nyiragongo is quiet, | 0:56:24 | 0:56:29 | |
but when it does next erupt, | 0:56:29 | 0:56:30 | |
the lava is likely to reach Goma faster than ever. | 0:56:30 | 0:56:33 | |
They've also established that infrasound could be a way | 0:56:36 | 0:56:39 | |
to remotely monitor the lake level, | 0:56:39 | 0:56:42 | |
a key warning sign of an eruption. | 0:56:42 | 0:56:44 | |
Nyiragongo is not an easy volcano to study. | 0:56:48 | 0:56:50 | |
It is a massive headache in terms of getting people and equipment here. | 0:56:50 | 0:56:54 | |
The motivation for it is very clear. | 0:56:54 | 0:56:56 | |
There are a million people living very close to this volcano | 0:56:56 | 0:56:59 | |
so, despite all the problems, it's worth it. | 0:56:59 | 0:57:01 | |
The expedition has also worked with a local volcano observatory | 0:57:04 | 0:57:07 | |
to help prepare the people of Goma for the dangers of living | 0:57:07 | 0:57:11 | |
in this highly volcanic landscape. | 0:57:11 | 0:57:13 | |
I've been thinking more and more | 0:57:15 | 0:57:16 | |
about how people here can manage to do the impossible thing | 0:57:16 | 0:57:20 | |
of living with this volcano that is such a constant threat to this city. | 0:57:20 | 0:57:24 | |
On the one hand, the volcano | 0:57:24 | 0:57:26 | |
is deeply connected to deadly epidemics, | 0:57:26 | 0:57:29 | |
to the destruction of houses, the destruction of communities. | 0:57:29 | 0:57:32 | |
And, of course, you can't quite live with that idea. | 0:57:32 | 0:57:36 | |
It's hard to hold it in your head. | 0:57:36 | 0:57:38 | |
But the work the scientists are doing in predicting the eruption | 0:57:38 | 0:57:41 | |
will give people time, maybe to not save their property or their houses, | 0:57:41 | 0:57:44 | |
maybe not to save their land, but at least to save themselves, | 0:57:44 | 0:57:48 | |
and that does give you a hope of rebuilding. | 0:57:48 | 0:57:50 | |
Next time, the team move on | 0:57:56 | 0:57:58 | |
to an even bigger and more violent volcano... | 0:57:58 | 0:58:01 | |
..and discover how these volcanoes affect every aspect of life here, | 0:58:03 | 0:58:07 | |
from endangered wildlife to the conflicts this region has suffered. | 0:58:07 | 0:58:12 |