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This week on Fierce Earth we explore the power of ice. | 0:00:03 | 0:00:06 | |
And where better to start than here. | 0:00:08 | 0:00:10 | |
Welcome to Iceland. | 0:00:11 | 0:00:13 | |
Iceland is one of the least populated countries in Europe. | 0:00:13 | 0:00:17 | |
There may not be many people here | 0:00:17 | 0:00:19 | |
but there are loads of mountains, volcanoes and glaciers. | 0:00:19 | 0:00:22 | |
And it's those glaciers that have brought us here | 0:00:25 | 0:00:27 | |
because on today's Fierce Earth... | 0:00:27 | 0:00:29 | |
The big chill sets in, as we get to grips with ice. | 0:00:29 | 0:00:32 | |
We're going to show you the awesome power of ice as carves its way | 0:00:34 | 0:00:37 | |
through mountains. | 0:00:37 | 0:00:39 | |
Mike will be there as a terrifying winter storm | 0:00:39 | 0:00:43 | |
strikes North America. | 0:00:43 | 0:00:45 | |
Just look at this! This is insane! | 0:00:45 | 0:00:47 | |
And we'll see Leo shoot across ice at super-high speeds. | 0:00:47 | 0:00:51 | |
And we're going to see how this seemingly innocent substance | 0:00:52 | 0:00:56 | |
can be so destructive and dangerous. | 0:00:56 | 0:00:58 | |
What happens when the ground shakes, the seas rise up | 0:01:01 | 0:01:05 | |
and the air tears itself apart? | 0:01:05 | 0:01:08 | |
The Fierce Earth team move in, | 0:01:08 | 0:01:09 | |
taking on the most powerful forces on the planet. | 0:01:09 | 0:01:12 | |
Get ready for Fierce Earth - the Earth and how to survive it. | 0:01:30 | 0:01:34 | |
Ice makes up about 10% of our planet. | 0:01:38 | 0:01:41 | |
There's enough of this frozen substance on Earth to cover | 0:01:41 | 0:01:45 | |
the whole of Britain over 65 times. | 0:01:45 | 0:01:47 | |
Ice takes all kinds of different forms. | 0:01:52 | 0:01:54 | |
It can be glacial ice which forms on land. | 0:01:55 | 0:01:59 | |
Ice sheets which float on the sea. | 0:01:59 | 0:02:02 | |
Or polar ice which forms a frozen desert at the top | 0:02:02 | 0:02:05 | |
and bottom of our planet. | 0:02:05 | 0:02:06 | |
But where does this ice actually come from? | 0:02:07 | 0:02:10 | |
We've travelled all the way to the country of Iceland to show you. | 0:02:11 | 0:02:15 | |
To understand how ice forms, | 0:02:16 | 0:02:18 | |
I'm coming face to face with a gigantic lump of the stuff. | 0:02:18 | 0:02:23 | |
It's called the Svinafellsjokull glacier. | 0:02:23 | 0:02:26 | |
When water gets to about zero degrees centigrade, | 0:02:26 | 0:02:30 | |
it can freeze rapidly and turn to ice. | 0:02:30 | 0:02:32 | |
But that isn't how most of the ice on Earth is created. | 0:02:32 | 0:02:36 | |
Some of the most powerful ice on our planet | 0:02:36 | 0:02:38 | |
starts off as the humble snowflake. | 0:02:38 | 0:02:42 | |
Now it's hard to imagine how simple, | 0:02:42 | 0:02:44 | |
fluffy snowflakes that fall from the sky, can actually become this. | 0:02:44 | 0:02:49 | |
But if you collect enough of them, and you compact them over time, | 0:02:49 | 0:02:53 | |
you can form some of the most powerful ice rivers on the planet. | 0:02:53 | 0:02:57 | |
And the way that the snowflakes are crushed together, | 0:02:58 | 0:03:01 | |
helps scientists like me actually study the ice. | 0:03:01 | 0:03:04 | |
Iceland has some fantastic glacial formations. | 0:03:06 | 0:03:09 | |
When you see them in cross-section, | 0:03:09 | 0:03:12 | |
they tell you the age of the ice, step by step, year by year. | 0:03:12 | 0:03:16 | |
You can pick out dark and light layers. | 0:03:16 | 0:03:19 | |
The light layers represent snowfall in winter. | 0:03:19 | 0:03:22 | |
The dark layers represent dust blown over the ice in the summer. | 0:03:22 | 0:03:27 | |
It's like the rings of a tree. | 0:03:27 | 0:03:29 | |
Winter after winter, new layers of snow fall | 0:03:29 | 0:03:32 | |
and the weight from each layer weighs heavily on the previous one. | 0:03:32 | 0:03:36 | |
The layers get thinner and thinner, making them more dense. | 0:03:36 | 0:03:39 | |
The pretty snowflake shape we know is crushed | 0:03:39 | 0:03:43 | |
and all of the air squeezed out, | 0:03:43 | 0:03:45 | |
until you get to see the dark blue dense ice that we see around us. | 0:03:45 | 0:03:49 | |
And that is how the ice that covers over 10% of our planet is formed. | 0:03:50 | 0:03:55 | |
But as you can see from these speeded up pictures | 0:03:55 | 0:03:58 | |
once it's been created, | 0:03:58 | 0:03:59 | |
the ice in these glaciers doesn't just sit there. | 0:03:59 | 0:04:02 | |
It moves, | 0:04:02 | 0:04:03 | |
and that movement is responsible for the way the land around us looks. | 0:04:03 | 0:04:08 | |
I'm fascinated by how ice has shaped our planet for thousands, | 0:04:08 | 0:04:12 | |
if not millions, of years. | 0:04:12 | 0:04:14 | |
Glaciers are ever-changing. | 0:04:14 | 0:04:17 | |
These huge lumps of ice that move | 0:04:17 | 0:04:19 | |
and gouge out the sides of the mountains to create the valleys. | 0:04:19 | 0:04:23 | |
Glaciers move because of the huge weight | 0:04:23 | 0:04:25 | |
pushing down from the snow and ice at the top of mountain. | 0:04:25 | 0:04:29 | |
Slowly but surely, this huge beast moves forward, | 0:04:29 | 0:04:33 | |
sweeping away everything in front of it. | 0:04:33 | 0:04:36 | |
Thousands of years ago glaciers like this covered Britain too, | 0:04:36 | 0:04:40 | |
and it's their movement, pushing rock and soil in front of them, | 0:04:40 | 0:04:44 | |
that shaped our country as well. | 0:04:44 | 0:04:45 | |
Glaciers are really fascinating powerhouses of our planet. | 0:04:46 | 0:04:50 | |
They represent Mother Earth's bulldozer, | 0:04:51 | 0:04:54 | |
carving the mountains and valleys that we see around us. | 0:04:54 | 0:04:58 | |
From California in the USA to the Lake District in the UK, | 0:04:58 | 0:05:03 | |
the power of ice has helped shape the whole planet. | 0:05:03 | 0:05:06 | |
When it comes to rocks and ice there's only one winner. | 0:05:07 | 0:05:10 | |
And that's ice. | 0:05:10 | 0:05:12 | |
Up on mountains isn't the only place you'll find ice. | 0:05:15 | 0:05:19 | |
You'll also find it floating in the water as icebergs. | 0:05:19 | 0:05:22 | |
How do icebergs get into the sea and what could they mean for our planet? | 0:05:24 | 0:05:29 | |
I've travelled to the south east coast of Iceland to find out. | 0:05:30 | 0:05:34 | |
This is the Jokulsarlon lagoon. | 0:05:34 | 0:05:37 | |
It is filled with icebergs. | 0:05:37 | 0:05:39 | |
The glacier is just up there and that's where the icebergs come from. | 0:05:39 | 0:05:42 | |
They break off or carve and float very slowly down towards the coast. | 0:05:42 | 0:05:46 | |
The lagoon is a brilliant example of how | 0:05:47 | 0:05:50 | |
icebergs are created from melting or retreating glaciers. | 0:05:50 | 0:05:54 | |
80 years ago, this was solid ice | 0:05:54 | 0:05:56 | |
but, since then, the glaciers have slowly retreated. | 0:05:56 | 0:05:59 | |
In doing so, the sea has flowed in, | 0:05:59 | 0:06:01 | |
but the glacier continues to feed the icebergs. | 0:06:01 | 0:06:05 | |
It is an incredible sight. | 0:06:05 | 0:06:06 | |
Icebergs cover the lagoon, there are hundreds of them. | 0:06:08 | 0:06:11 | |
But there's a lot more to be seen under the surface. | 0:06:11 | 0:06:15 | |
To investigate what's going on below the water line, | 0:06:15 | 0:06:17 | |
I've got a little camera here. | 0:06:17 | 0:06:19 | |
It shows me | 0:06:21 | 0:06:22 | |
that almost 90% of the icebergs are actually below the water. | 0:06:22 | 0:06:26 | |
And that means the more you can see of an iceberg above, | 0:06:26 | 0:06:29 | |
the more there is below. | 0:06:29 | 0:06:30 | |
Hence the phrase "tip of the iceberg". | 0:06:31 | 0:06:34 | |
And that's the reason they can cause so many problems for ships. | 0:06:34 | 0:06:38 | |
The largest icebergs could sink even the biggest and strongest of ships. | 0:06:39 | 0:06:44 | |
The one that sank Titanic was over a mile long, now that's a lot of ice. | 0:06:45 | 0:06:52 | |
But big chunks of ice don't just pose a danger to ships. | 0:06:52 | 0:06:56 | |
Ice sheets, that can be as much as 100 miles across, | 0:06:56 | 0:06:58 | |
could have a worldwide effect when they fall in to the oceans. | 0:06:58 | 0:07:02 | |
When water freezes, it expands. | 0:07:04 | 0:07:06 | |
Ice takes up more space than water, | 0:07:06 | 0:07:09 | |
so when a big chunk breaks off an ice shelf the sea level rises. | 0:07:09 | 0:07:13 | |
Although we're only talking about a small rise in levels, | 0:07:13 | 0:07:17 | |
when you combine melting ice with other factors that lead to | 0:07:17 | 0:07:20 | |
an increase in sea levels, it could be serious. | 0:07:20 | 0:07:23 | |
If the sea rises by just 7m, | 0:07:24 | 0:07:26 | |
both London and Los Angeles would be under water. | 0:07:26 | 0:07:29 | |
We don't need to panic...yet. | 0:07:30 | 0:07:33 | |
Melting polar ice and rising sea levels happens over decades | 0:07:33 | 0:07:37 | |
and, by fighting global warming, we can still help to reduce it. | 0:07:37 | 0:07:42 | |
But here in Iceland, something very unusual can happen | 0:07:44 | 0:07:47 | |
that the Icelanders DO need to worry about. | 0:07:47 | 0:07:50 | |
There are fierce volcanoes here that can make huge amounts of ice | 0:07:54 | 0:07:58 | |
melt in a matter of seconds. | 0:07:58 | 0:08:00 | |
To show you what happens when ice meets fire, | 0:08:02 | 0:08:06 | |
I need to get right on top of the ice cap. | 0:08:06 | 0:08:08 | |
Now, that's several miles in that direction, | 0:08:08 | 0:08:11 | |
but I'm going to go in style. | 0:08:11 | 0:08:12 | |
I'm travelling in one of these babies | 0:08:12 | 0:08:14 | |
This bad boy is fully loaded with... | 0:08:14 | 0:08:17 | |
Massive tyres to get us over the snow and ice. | 0:08:17 | 0:08:20 | |
A whopping great engine to get us up the steep slopes. | 0:08:21 | 0:08:24 | |
And a driver that knows the terrain like the back of his hand. | 0:08:24 | 0:08:29 | |
I think we're good to go. | 0:08:29 | 0:08:30 | |
Here we go. You can't really see it outside but on the GPS | 0:08:40 | 0:08:44 | |
You can see this blue line | 0:08:44 | 0:08:46 | |
and that marks the point that we're actually going onto the ice cap. | 0:08:46 | 0:08:51 | |
So although it's a whiteout outside, | 0:08:51 | 0:08:54 | |
the car is now driving on ice. Below us. | 0:08:54 | 0:08:57 | |
This is one of the biggest single chunks of ice | 0:09:02 | 0:09:04 | |
in the whole of Europe. | 0:09:04 | 0:09:05 | |
It's fierce, cold, and a blizzard is blowing. | 0:09:06 | 0:09:09 | |
So we've driven up on top of the ice cap now. | 0:09:10 | 0:09:14 | |
I'm standing on snow | 0:09:14 | 0:09:15 | |
and there's a blizzard around me | 0:09:15 | 0:09:18 | |
but beneath the snow is hundreds of metres of ice | 0:09:18 | 0:09:21 | |
and beneath that is a volcano, Katla. A live active volcano. | 0:09:21 | 0:09:25 | |
And when that volcano erupts it brings hot magma, | 0:09:25 | 0:09:29 | |
hundreds of degrees centigrade, almost 1,000 degrees centigrade, | 0:09:29 | 0:09:34 | |
in contact with that cold ice and it starts to melt, | 0:09:34 | 0:09:38 | |
producing millions and millions of tonnes of meltwater | 0:09:38 | 0:09:41 | |
and when that meltwater is released it is called a jokulhlaup. | 0:09:41 | 0:09:45 | |
And that is what we're here to find out about. | 0:09:45 | 0:09:47 | |
Time to get out of the blizzard. | 0:09:47 | 0:09:50 | |
I've travelled into the heart of the glacier to create | 0:09:52 | 0:09:55 | |
an experiment that will show you what happens when fire meets ice. | 0:09:55 | 0:09:59 | |
So here we are, we've actually come under the ice. | 0:10:01 | 0:10:05 | |
You can see the blue light shining through the ice. | 0:10:05 | 0:10:08 | |
We're actually in an ice cave. | 0:10:08 | 0:10:11 | |
So we're going to do a little experiment. | 0:10:11 | 0:10:13 | |
What we've got here is a couple of holes that we've drilled | 0:10:13 | 0:10:16 | |
into the ice and we've put a little water reservoir in there | 0:10:16 | 0:10:20 | |
and I'm going to start up my volcano here. There we go. | 0:10:20 | 0:10:24 | |
So my little meltwater pocket is trapped. | 0:10:24 | 0:10:27 | |
There we go. There. It's all flooding out now. | 0:10:30 | 0:10:34 | |
This is a very small-scale operation. | 0:10:34 | 0:10:37 | |
You imagine millions and millions of tonnes of water | 0:10:37 | 0:10:41 | |
filling up in a cave just like what we've got around us now. | 0:10:41 | 0:10:45 | |
And then all of a sudden the volcano comes knocking at the door | 0:10:45 | 0:10:49 | |
and - whoosh! - the whole lot comes rushing out in one go, | 0:10:49 | 0:10:53 | |
rocks, ice and debris, all in one big massive flood. | 0:10:53 | 0:10:56 | |
You've got yourself a massive jokulhlaup. | 0:10:56 | 0:10:58 | |
This is a jokulhlaup that hit Iceland recently | 0:11:01 | 0:11:04 | |
and, believe it or not, this is just a small one. | 0:11:04 | 0:11:06 | |
Luckily no-one lived in the area the water flowed through and I'm | 0:11:08 | 0:11:12 | |
now standing right in the middle of where all that melted ice travelled. | 0:11:12 | 0:11:16 | |
This devastated land that you can see all around me | 0:11:17 | 0:11:20 | |
is the result of one of these flooding events | 0:11:20 | 0:11:23 | |
that hit here two years ago. | 0:11:23 | 0:11:25 | |
It's covered an area the size of a small city. | 0:11:25 | 0:11:28 | |
There is no vegetation for miles. | 0:11:28 | 0:11:30 | |
A flash flood, cutting through everything, bringing in debris | 0:11:30 | 0:11:35 | |
and creating, essentially, a moonscape. | 0:11:35 | 0:11:37 | |
There's absolutely nothing left. | 0:11:37 | 0:11:39 | |
If you're here when this jokulhlaup hits, | 0:11:39 | 0:11:42 | |
there's no surviving it. | 0:11:42 | 0:11:44 | |
Like weather forecasters, volcano experts like me | 0:11:45 | 0:11:48 | |
can roughly predict when a volcano is likely to erupt. | 0:11:48 | 0:11:52 | |
And the bad news for the people of Iceland is that the one underneath | 0:11:52 | 0:11:56 | |
the huge glacier I travelled across is expected to blow. | 0:11:56 | 0:12:00 | |
Soon. | 0:12:00 | 0:12:01 | |
When it does, the ice will melt | 0:12:01 | 0:12:03 | |
and unleash a flood with more water than there is in all of Britain's | 0:12:03 | 0:12:07 | |
rivers combined with the Amazon, the Nile and the mighty Mississippi. | 0:12:07 | 0:12:12 | |
But there is hope. | 0:12:12 | 0:12:13 | |
Now the key to survival in one of these flooding events, | 0:12:15 | 0:12:17 | |
is prediction and warning. | 0:12:17 | 0:12:19 | |
If Katla starts erupting, | 0:12:20 | 0:12:22 | |
signals from this station will get sent to Reykjavik. | 0:12:22 | 0:12:25 | |
They can understand those signals | 0:12:25 | 0:12:27 | |
and tell people in surrounding areas that the volcano is becoming alive. | 0:12:27 | 0:12:33 | |
It's that chain of connection | 0:12:33 | 0:12:35 | |
and those chains of events that will help save lives | 0:12:35 | 0:12:38 | |
and allow people to prepare, | 0:12:38 | 0:12:39 | |
ultimately, for a massive flooding event. | 0:12:39 | 0:12:42 | |
The place most at risk | 0:12:45 | 0:12:46 | |
from the flood of icy water is a small town called Vik. | 0:12:46 | 0:12:49 | |
When the warning is sent out, every person who lives here has to | 0:12:51 | 0:12:54 | |
get ready to evacuate. | 0:12:54 | 0:12:55 | |
This is Throan, he's the man in charge of making sure | 0:12:58 | 0:13:01 | |
the town of Vik is empty when Katla erupts and the ice melts. | 0:13:01 | 0:13:05 | |
He'll receive the signal that the volcano is coming to life | 0:13:05 | 0:13:08 | |
and sound the alarm. | 0:13:08 | 0:13:10 | |
When Katla erupts, the amount of water comes down from the glacier. | 0:13:11 | 0:13:14 | |
The flooding, it would take out most of the houses in the lower village | 0:13:14 | 0:13:19 | |
so we have to evacuate the lower part of the village. | 0:13:19 | 0:13:23 | |
We sent directly text messages to all phones in that area to tell | 0:13:23 | 0:13:28 | |
people where to go, what is happening and to try to find a safe place. | 0:13:28 | 0:13:32 | |
After the text message is sent we have to | 0:13:32 | 0:13:35 | |
make sure that everyone has left. | 0:13:35 | 0:13:37 | |
When the alarm rings out across Vik, the clock will be ticking | 0:13:37 | 0:13:41 | |
because the villagers now have just 45 minutes to get out. | 0:13:41 | 0:13:44 | |
This satellite image shows the huge section of land | 0:13:46 | 0:13:49 | |
the glacial flood would threaten. | 0:13:49 | 0:13:52 | |
When they receive the alert, | 0:13:52 | 0:13:53 | |
everyone in Vik must get out of that danger zone. | 0:13:53 | 0:13:56 | |
The risk of Katla erupting and the ice melting is so high that | 0:13:57 | 0:14:01 | |
even the youngest of villagers has to be educated about the dangers. | 0:14:01 | 0:14:06 | |
If we stay here, it could be very dangerous | 0:14:06 | 0:14:09 | |
because the volcano is going to...explode. | 0:14:09 | 0:14:15 | |
Then we have to go high up because there is more safe. | 0:14:18 | 0:14:23 | |
Knowing what to do when Katla erupts could be a matter of life and death. | 0:14:23 | 0:14:27 | |
That's why every few months the kids practise this evacuation drill. | 0:14:27 | 0:14:31 | |
First they're taken to an evacuation centre at the top of a hill, | 0:14:33 | 0:14:37 | |
And from there they are taken even further out of the danger zone. | 0:14:37 | 0:14:42 | |
Only when they have travelled 45 minutes | 0:14:42 | 0:14:44 | |
out of town are the children safe. | 0:14:44 | 0:14:47 | |
I know what to do then. That's why I'm not worried. | 0:14:47 | 0:14:51 | |
It's good to know there's a plan like this in place | 0:14:51 | 0:14:53 | |
and that the kids are ready | 0:14:53 | 0:14:55 | |
because, when fire meets ice here, it spells trouble. | 0:14:55 | 0:14:59 | |
Get ready to buckle up, because later on Fierce Earth, | 0:15:02 | 0:15:05 | |
Leo is shooting across the ice at super-high speed. | 0:15:05 | 0:15:08 | |
But first, you've seen the destructive power of ice on water, | 0:15:11 | 0:15:16 | |
on the ground, as it carves its way through mountains... | 0:15:16 | 0:15:20 | |
..and now it's time to see the power of ice when it forms in the air. | 0:15:23 | 0:15:28 | |
I witnessed its awesome power | 0:15:29 | 0:15:31 | |
when I travelled to Boston in the northeast United States | 0:15:31 | 0:15:35 | |
and found myself in one of the biggest winter storms ever. | 0:15:35 | 0:15:39 | |
Man, we're getting nailed by this blizzard right now. | 0:15:41 | 0:15:44 | |
Just look at this! This is insane! | 0:15:44 | 0:15:46 | |
'It was a scary night.' | 0:15:46 | 0:15:48 | |
You need things like this just to hold on to | 0:15:48 | 0:15:50 | |
because you'll get blown down the road. | 0:15:50 | 0:15:52 | |
'And the heavy snowfall was one part of a winter storm | 0:15:52 | 0:15:55 | |
'I never want to see again, | 0:15:55 | 0:15:57 | |
'but it's what I saw the next morning that really blew me away... | 0:15:57 | 0:16:01 | |
'..cars wrapped in ice... | 0:16:04 | 0:16:05 | |
'..entire rows of houses covered with a layer | 0:16:08 | 0:16:11 | |
'of thick, frozen water.' | 0:16:11 | 0:16:13 | |
Just look at this ice. It's rock-solid. | 0:16:14 | 0:16:17 | |
'I couldn't believe the damage the storm had done to trees, | 0:16:18 | 0:16:21 | |
'houses, and even electrical cables.' | 0:16:21 | 0:16:25 | |
The weight of the ice has taken these power lines | 0:16:25 | 0:16:28 | |
and pulled them down to the ground. | 0:16:28 | 0:16:30 | |
'What were the conditions that made this different to just snowfall?' | 0:16:30 | 0:16:34 | |
To find out, Leo is visiting a special testing facility | 0:16:38 | 0:16:42 | |
in the UK, where normally they run cold-weather tests on cars. | 0:16:42 | 0:16:47 | |
But there's no cars today, just me, | 0:16:47 | 0:16:50 | |
a cold chamber and a couple of bottles of water. | 0:16:50 | 0:16:52 | |
This cold room is about minus ten, similar to a nasty winter storm. | 0:16:55 | 0:16:59 | |
Watch this. Looks like an ordinary bottle of water, right? | 0:17:01 | 0:17:04 | |
Wrong. I'm going to show you a trick. Check this out. | 0:17:04 | 0:17:07 | |
Bang. Turns to rock-hard ice. | 0:17:09 | 0:17:11 | |
In very special circumstances, water like this | 0:17:14 | 0:17:17 | |
can exist as a liquid below zero degrees centigrade. | 0:17:17 | 0:17:20 | |
It's called supercooled water. | 0:17:20 | 0:17:22 | |
And when that water is given something to crystallise around, | 0:17:22 | 0:17:26 | |
like air bubbles when the bottle is slapped, | 0:17:26 | 0:17:29 | |
the ice crystals quickly spread and form solid ice. | 0:17:29 | 0:17:32 | |
I'm about to show you how water like this | 0:17:32 | 0:17:35 | |
can be responsible for devastating ice storms like the one Mike saw. | 0:17:35 | 0:17:38 | |
Now, remember, this is just cold water, supercooled water. | 0:17:42 | 0:17:46 | |
Watch what happens when I pour it on these freezing surfaces. | 0:17:46 | 0:17:49 | |
Here you can see my house, | 0:17:49 | 0:17:50 | |
my dumper truck, just like the one I drive at home, | 0:17:50 | 0:17:53 | |
and I'm going to show you what happens in an ice storm. | 0:17:53 | 0:17:56 | |
Look at that. It turns to ice | 0:17:56 | 0:17:58 | |
immediately, and it stays as ice. And you can see it's layering up | 0:17:58 | 0:18:02 | |
and getting heavier and heavier. | 0:18:02 | 0:18:05 | |
When the supercooled water hits an object like a tree, car | 0:18:06 | 0:18:10 | |
or house that's already cold, it turns to ice. | 0:18:10 | 0:18:13 | |
Imagine if that's the roof of your house, there. | 0:18:13 | 0:18:16 | |
It's starting to get a massive amount of weight on it. | 0:18:16 | 0:18:19 | |
When this happens for real, it can have devastating consequences. | 0:18:19 | 0:18:23 | |
And that build-up of frozen water is exactly what happens | 0:18:23 | 0:18:27 | |
during an ice storm - supercooled water falls through the air | 0:18:27 | 0:18:30 | |
and hits cold objects on the ground, like tree branches. | 0:18:30 | 0:18:34 | |
Layers of heavy ice build up and cause devastating damage. | 0:18:34 | 0:18:38 | |
Some of the most damaging and expensive storms | 0:18:39 | 0:18:42 | |
in North America have been ice storms. | 0:18:42 | 0:18:44 | |
This ice storm that hit Canada in 1998 | 0:18:44 | 0:18:47 | |
caused over 1 billion worth of damage, destroyed trees and houses, | 0:18:47 | 0:18:51 | |
and left some people living without power for a whole month. | 0:18:51 | 0:18:55 | |
All that devastation from something as simple as cold water. | 0:18:56 | 0:19:00 | |
That is the power of ice. | 0:19:00 | 0:19:02 | |
CLARE: We're back in the land of fire and ice, Iceland. | 0:19:05 | 0:19:08 | |
As you've seen, ice can be dangerous stuff, | 0:19:08 | 0:19:11 | |
and that's especially true of these things - glaciers. | 0:19:11 | 0:19:15 | |
You can understand why people would want to come here | 0:19:15 | 0:19:17 | |
and experience this most amazing sight, but when an adventurer's hike | 0:19:17 | 0:19:21 | |
becomes the stuff of nightmares, who do you call? | 0:19:21 | 0:19:24 | |
The answer is Iceland's rescue service - ICESAR. | 0:19:27 | 0:19:30 | |
Ice is such a big deal here that these guys specialise | 0:19:33 | 0:19:36 | |
in saving people when they get into trouble on its frozen surface. | 0:19:36 | 0:19:40 | |
There are 18,000 volunteer members of ICESAR, | 0:19:40 | 0:19:43 | |
and they are highly skilled in ice rescue. | 0:19:43 | 0:19:46 | |
They can move like lightning across ice, | 0:19:48 | 0:19:50 | |
using crampons that give them extra grip, ice axes that allow them | 0:19:50 | 0:19:55 | |
to safely climb up and down, | 0:19:55 | 0:19:56 | |
and special rope and ice anchor systems that allow them | 0:19:56 | 0:20:00 | |
to pull people to safety on this treacherous surface. | 0:20:00 | 0:20:04 | |
Today, they're on a training exercise for something they're called out to | 0:20:05 | 0:20:09 | |
most often - crevasse rescue. | 0:20:09 | 0:20:11 | |
Glaciers move on a daily basis, | 0:20:12 | 0:20:15 | |
and as they move, deep cracks in the ice appear. | 0:20:15 | 0:20:18 | |
These cracks are called crevasses, | 0:20:18 | 0:20:21 | |
and its when people fall into them that ICESAR are called out. | 0:20:21 | 0:20:25 | |
So the training that you're doing today | 0:20:25 | 0:20:28 | |
is so essential for saving lives? | 0:20:28 | 0:20:30 | |
Yes, it is. | 0:20:30 | 0:20:31 | |
We have accidents on glaciers and we have to keep updated - | 0:20:31 | 0:20:35 | |
we have to do this over and over again, to increase our efficiency. | 0:20:35 | 0:20:40 | |
Living in Iceland, you... Well, you have to love ice. | 0:20:40 | 0:20:42 | |
OK. Put me into a crevasse. Let's go. | 0:20:42 | 0:20:45 | |
The team are going to do a simple rescue exercise where they lower me | 0:20:47 | 0:20:50 | |
into and out of a crevasse. | 0:20:50 | 0:20:53 | |
It's one of the first lessons they give to new team members. | 0:20:53 | 0:20:57 | |
It's a great chance for me to safely see what it's like inside a glacier, | 0:20:57 | 0:21:02 | |
but I'm still a bit nervous. | 0:21:02 | 0:21:03 | |
That's it, yeah. OK. | 0:21:05 | 0:21:06 | |
On ice, anything can happen. | 0:21:06 | 0:21:09 | |
Oh. Hang on. Hold it tight. That's it. | 0:21:09 | 0:21:11 | |
This is putting science really into action. | 0:21:13 | 0:21:16 | |
I'm going down to a part of the glacier that probably no-one's ever | 0:21:17 | 0:21:21 | |
seen before, and may never see again, because the thing about glaciers - | 0:21:21 | 0:21:25 | |
they're for ever moving. | 0:21:25 | 0:21:27 | |
Oh, it's really deep down there! | 0:21:27 | 0:21:29 | |
The thing is now, it's getting very narrow down here. | 0:21:29 | 0:21:32 | |
-Um... Hang on a sec. -Stop. | 0:21:32 | 0:21:36 | |
Even though I'm safely attached to a rope, | 0:21:38 | 0:21:41 | |
it's an eerie feeling, being surrounded by ice, | 0:21:41 | 0:21:44 | |
and looking down, I can see how dangerous a crevasse is. | 0:21:44 | 0:21:48 | |
So if you were ever to find yourself on a glacier, | 0:21:48 | 0:21:51 | |
here is the ICESAR survival guide. | 0:21:51 | 0:21:53 | |
First up, never go onto a glacier without a professional guide. | 0:21:55 | 0:21:59 | |
Glaciers change all the time, and crevasses can be hidden | 0:21:59 | 0:22:03 | |
and even covered with snow. | 0:22:03 | 0:22:05 | |
The second survival tip is not to fall into a crevasse | 0:22:05 | 0:22:08 | |
in the first place! | 0:22:08 | 0:22:10 | |
Travel slowly, carefully, | 0:22:10 | 0:22:11 | |
and experienced mountaineers even travel linked together by a rope. | 0:22:11 | 0:22:15 | |
Crevasses can be up to 50m deep. | 0:22:15 | 0:22:18 | |
That's enough of a fall to cause serious injury. | 0:22:19 | 0:22:23 | |
If you are lucky enough to fall onto a flat ledge, stay calm, | 0:22:23 | 0:22:26 | |
stay still and wait for rescue. | 0:22:26 | 0:22:30 | |
You don't want to fall any further. | 0:22:30 | 0:22:32 | |
'Back to my crevasse, | 0:22:36 | 0:22:38 | |
'and I've reached the bottom, and being surrounded by this dark ice | 0:22:38 | 0:22:41 | |
'is enough to make anyone nervous, so I'm not hanging around.' | 0:22:41 | 0:22:46 | |
OK, I think I'm ready to come up now! | 0:22:46 | 0:22:48 | |
I'd be very scared indeed, fearful for my life, | 0:22:51 | 0:22:55 | |
if I fell down one of these crevasses, | 0:22:55 | 0:22:57 | |
but that's why these sort of practice runs are so essential. | 0:22:57 | 0:23:00 | |
Nice and slowly. Hand over hand. | 0:23:01 | 0:23:04 | |
'With one last heave, I'm out. Safety at last.' | 0:23:06 | 0:23:09 | |
Thank you. Thank you. | 0:23:15 | 0:23:17 | |
That's good. On the top of the ice again. | 0:23:17 | 0:23:20 | |
It's the movement of ice that creates crevasses | 0:23:23 | 0:23:26 | |
and the need for many ICESAR rescues, | 0:23:26 | 0:23:28 | |
so, next, Leo's travelled to Switzerland in the European Alps | 0:23:28 | 0:23:32 | |
to find out what it is about ice that makes this slippery customer move, | 0:23:32 | 0:23:37 | |
and how we humans have used the slippery properties of ice | 0:23:37 | 0:23:40 | |
to create super-speed winter sports. | 0:23:40 | 0:23:43 | |
But how do you reach these speeds travelling on ice? | 0:23:44 | 0:23:47 | |
Well, I'm here in Switzerland to show you. | 0:23:47 | 0:23:49 | |
Hidden in a peaceful forest near the town of St Moritz, | 0:23:53 | 0:23:55 | |
this is one of the most famous and feared sports venues in the world. | 0:23:55 | 0:23:59 | |
We're at the famous Olympia bobsleigh track. | 0:24:02 | 0:24:05 | |
This is where the sport of bobsleighing was born. | 0:24:09 | 0:24:12 | |
It's the only track like it on the planet, | 0:24:15 | 0:24:17 | |
and it's only here for a few icy months of the year. | 0:24:17 | 0:24:20 | |
It is the perfect place to demonstrate why ice can appear | 0:24:22 | 0:24:25 | |
to be so slippery when, in fact, it isn't. I'll show you why. | 0:24:25 | 0:24:28 | |
If I take these two chunks of ice and rub them together, | 0:24:28 | 0:24:32 | |
they stick and grate and slide. Look at that. | 0:24:32 | 0:24:35 | |
Nothing slippery about that at all. They're totally stuck together. | 0:24:35 | 0:24:38 | |
But watch what happens now, | 0:24:38 | 0:24:39 | |
when I move this knife blade | 0:24:39 | 0:24:41 | |
over the surface of the ice. | 0:24:41 | 0:24:42 | |
You can see it slides easily. The ice has become a slippery surface. | 0:24:42 | 0:24:47 | |
That's because the thin edge of the blade puts a lot of pressure on it. | 0:24:47 | 0:24:51 | |
Pressure creates heat, melts the ice, and the blade slides over | 0:24:51 | 0:24:55 | |
the water, just like when you slip on a wet floor. | 0:24:55 | 0:24:58 | |
Think about it - that's why the things that move fastest on ice | 0:24:58 | 0:25:01 | |
have really sharp blades, like ice skates or bobsleds. | 0:25:01 | 0:25:04 | |
The sharper the blades, the more heat is created | 0:25:06 | 0:25:09 | |
and the quicker the object moves. | 0:25:09 | 0:25:10 | |
'And today I'm getting to grips with this shiny beauty. | 0:25:12 | 0:25:16 | |
'But first, I need to get some expert advice.' | 0:25:16 | 0:25:19 | |
So what do you think is the top speed I can get out of this thing, | 0:25:20 | 0:25:23 | |
-on this run? -When you start from the top, then you reach about 125, | 0:25:23 | 0:25:28 | |
226, top-speed. | 0:25:28 | 0:25:30 | |
It feels like a rocket. | 0:25:30 | 0:25:31 | |
Wow - speed into three figures. I'd better get my racing threads on. | 0:25:33 | 0:25:38 | |
Skintight Lycra, nice and aerodynamic so I can go even faster. | 0:25:38 | 0:25:42 | |
This is one of the fastest tracks in the world. | 0:25:42 | 0:25:46 | |
And that horseshoe corner looks terrifying. | 0:25:46 | 0:25:48 | |
And all this in the name of showing you the slippery properties of ice. | 0:25:49 | 0:25:53 | |
-I'm ready! -OK. Let's go. -Wahey! | 0:25:53 | 0:25:56 | |
It's a slow start before gravity and the ice start to do their work, | 0:25:58 | 0:26:02 | |
increasing my speed. | 0:26:02 | 0:26:03 | |
And here comes that horseshoe corner. | 0:26:06 | 0:26:08 | |
At this speed, it's difficult to keep control. | 0:26:11 | 0:26:14 | |
And then there's a disaster. | 0:26:14 | 0:26:16 | |
MAN SPEAKS IN GERMAN | 0:26:20 | 0:26:22 | |
Don't worry - it was just one of the cameras! | 0:26:26 | 0:26:28 | |
I've covered 800m in just 15 seconds. | 0:26:30 | 0:26:33 | |
I'm just centimetres off the ground, | 0:26:33 | 0:26:35 | |
and travelling faster than your parents' car on the motorway. | 0:26:35 | 0:26:38 | |
The blades are cutting into the ice, generating heat | 0:26:40 | 0:26:42 | |
and shooting me down this track at over 100km an hour! | 0:26:42 | 0:26:46 | |
This is ice at its most slippery! | 0:26:47 | 0:26:49 | |
That was brilliant. My goodness. You come down so quick, | 0:26:57 | 0:27:01 | |
flying round the corners. there's so little friction on the ice, you're | 0:27:01 | 0:27:05 | |
just whizzing down. Zoom, zoom, zoom. Absolutely amazing. | 0:27:05 | 0:27:08 | |
It's not as violent as I thought it was going to be. You're actually | 0:27:08 | 0:27:11 | |
quite smooth when you're in the bottom, but... | 0:27:11 | 0:27:13 | |
That's so much fun. Can we do it again? | 0:27:13 | 0:27:15 | |
Afraid not, Leo, because our expedition | 0:27:15 | 0:27:17 | |
through the land of ice is over. | 0:27:17 | 0:27:19 | |
On this journey, | 0:27:19 | 0:27:21 | |
we've seen how tiny snowflakes can create mighty glaciers, | 0:27:21 | 0:27:26 | |
how ice storms can bring whole cities to a standstill, | 0:27:26 | 0:27:30 | |
and we've found out what it's like to fall into a crevasse. | 0:27:30 | 0:27:34 | |
Next time on Fierce Earth, get ready for the heavens to open... | 0:27:35 | 0:27:41 | |
It's pouring it down! | 0:27:41 | 0:27:42 | |
..because we're on a soaking journey to the rainiest place on the planet. | 0:27:44 | 0:27:48 | |
-It's going to be wet.. -..and wild! | 0:27:48 | 0:27:51 |