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Our planet is unique. | 0:00:17 | 0:00:20 | |
An extraordinary piece of engineering, | 0:00:20 | 0:00:23 | |
over four and a half billion years old. | 0:00:23 | 0:00:26 | |
And to show you how it works, we've created something rather special. | 0:00:28 | 0:00:33 | |
We've collected the latest information | 0:00:36 | 0:00:38 | |
from scientists around the world. | 0:00:38 | 0:00:40 | |
We've added satellite maps, sonar and radar images | 0:00:40 | 0:00:42 | |
and we've brought it all together to make this. | 0:00:42 | 0:00:45 | |
We've created a virtual planet earth. | 0:00:47 | 0:00:50 | |
In here we can dismantle the earth's machinery piece by piece, | 0:00:52 | 0:00:59 | |
and see how an enormous energy source, | 0:00:59 | 0:01:03 | |
buried deep within the planet, shapes our world, | 0:01:03 | 0:01:06 | |
up here on the surface. | 0:01:06 | 0:01:09 | |
Many of the most powerful effects happen on the ocean floor. | 0:01:10 | 0:01:15 | |
And it was the movement of the sea bed 80 miles off the coast of Japan | 0:01:19 | 0:01:23 | |
that triggered the tsunami in March 2011. | 0:01:23 | 0:01:27 | |
So to reveal how the earth machine works, | 0:01:28 | 0:01:32 | |
we need to drain the oceans. | 0:01:32 | 0:01:35 | |
Every now and then, we get a glimpse of what's below the surface. | 0:01:48 | 0:01:52 | |
We can shine a light or we can go down in a sub. | 0:01:55 | 0:01:59 | |
But it's hard to get the whole picture. | 0:02:00 | 0:02:03 | |
The more I think about the sea beneath me, | 0:02:03 | 0:02:07 | |
the more questions I have. | 0:02:07 | 0:02:08 | |
What if we could drain the oceans? | 0:02:08 | 0:02:11 | |
What would we see? What surprises are down there? | 0:02:14 | 0:02:16 | |
And what dangers lurk? | 0:02:16 | 0:02:18 | |
-Have you ever had anybody panic completely? -Yes. | 0:02:20 | 0:02:23 | |
Why does more volcanic activity take place underwater than on land? | 0:02:25 | 0:02:29 | |
Seeing as I'm already dressed... | 0:02:29 | 0:02:31 | |
What's one of the biggest underwater threats to the Internet... | 0:02:31 | 0:02:35 | |
-If that phone goes...? -If that phone goes, I'll get all... | 0:02:35 | 0:02:39 | |
..and our lives? | 0:02:39 | 0:02:42 | |
How can chimneys spout gold | 0:02:46 | 0:02:49 | |
and be home to snails made of metal? | 0:02:49 | 0:02:51 | |
And why have more men been to the moon | 0:02:51 | 0:02:55 | |
than to the deepest point in our oceans? | 0:02:55 | 0:02:59 | |
We've combined the latest scientific data | 0:02:59 | 0:03:03 | |
with some very clever computer software | 0:03:03 | 0:03:06 | |
to show you the wonders of the deep ocean. | 0:03:06 | 0:03:09 | |
Wonders created by a machine hidden beneath the sea floor. | 0:03:09 | 0:03:14 | |
A machine so powerful, it not only affects all our lives, | 0:03:14 | 0:03:18 | |
it drives the planet. | 0:03:18 | 0:03:20 | |
We're going to take you on a journey to the bottom of the sea | 0:03:20 | 0:03:23 | |
and beyond even that. | 0:03:23 | 0:03:26 | |
On Friday 11th March, 2011... | 0:03:50 | 0:03:53 | |
..a devastating tsunami crashed into the coast of Japan. | 0:03:58 | 0:04:02 | |
In some places, the waves reached 98 feet high. | 0:04:05 | 0:04:09 | |
It was caused by a powerful earthquake | 0:04:13 | 0:04:16 | |
that measured nine on the Richter scale. | 0:04:16 | 0:04:18 | |
This was the worst earthquake to hit Japan for over 100 years. | 0:04:39 | 0:04:44 | |
The death toll was at least 25,000. | 0:04:46 | 0:04:50 | |
This was the earth machine in action on an awesome scale. | 0:04:54 | 0:04:58 | |
The source of this devastation was 80 miles offshore | 0:05:00 | 0:05:04 | |
and deep below the surface of the ocean. | 0:05:04 | 0:05:07 | |
Oh, yeah, that's me. I'm doing that. | 0:05:18 | 0:05:20 | |
I did that then. | 0:05:23 | 0:05:24 | |
In order to show you how the earth machine works | 0:05:26 | 0:05:29 | |
and see how it affects us, we need first to get down to the ocean floor. | 0:05:29 | 0:05:34 | |
And we start, I'm delighted to say, down there. | 0:05:34 | 0:05:38 | |
The English Channel. | 0:05:38 | 0:05:40 | |
I know it may not be the most obvious place | 0:05:40 | 0:05:44 | |
to start a journey to the bottom of the sea, but bear with me. | 0:05:44 | 0:05:47 | |
The waters between Dover and Calais are about 40 metres deep, | 0:05:50 | 0:05:55 | |
which, in sea terms, is pretty shallow. | 0:05:55 | 0:05:58 | |
That's because this part of the seabed is just flooded land. | 0:06:03 | 0:06:07 | |
9,000 years ago you could walk - | 0:06:07 | 0:06:08 | |
give or take the odd river - from England to France. | 0:06:08 | 0:06:12 | |
Now we can reveal what that looks like today. | 0:06:17 | 0:06:20 | |
So, let's drain it and have a look. | 0:06:22 | 0:06:24 | |
With a bit of computer technology, we can do in seconds | 0:06:39 | 0:06:42 | |
what it takes the earth machine thousands of years to do. | 0:06:42 | 0:06:46 | |
And, well, frankly, the English Channel is a bit of a mess. | 0:06:57 | 0:07:03 | |
From up here, it looks like a scrap yard. | 0:07:03 | 0:07:05 | |
There are over 8,000 shipwrecks in this stretch of water alone. | 0:07:07 | 0:07:13 | |
What the Channel does show us is that, over time, | 0:07:18 | 0:07:21 | |
the boundaries of the land we live on can change. | 0:07:21 | 0:07:25 | |
The earth machine has such power | 0:07:25 | 0:07:28 | |
that it continually changes the surface of the earth. | 0:07:28 | 0:07:31 | |
The earth's surface is made up of a series of giant tectonic plates | 0:07:48 | 0:07:52 | |
which are constantly on the move. | 0:07:52 | 0:07:54 | |
Over time, as the continents have shifted | 0:07:58 | 0:08:01 | |
and sea levels rise and fall, | 0:08:01 | 0:08:03 | |
what was once land has sunk underwater. | 0:08:03 | 0:08:06 | |
As we begin to drain the ocean, the first thing we see | 0:08:15 | 0:08:18 | |
is that the continents we live on extend far out from the shore. | 0:08:18 | 0:08:22 | |
In some places, hundreds of miles. | 0:08:29 | 0:08:31 | |
This submerged land makes up the continental shelf. | 0:08:35 | 0:08:40 | |
The continental shelf has become one of the most valuable places on earth. | 0:08:51 | 0:08:55 | |
And there's a very good reason for this. | 0:08:55 | 0:08:58 | |
If we plot all the oil and gas platforms found out at sea, | 0:08:58 | 0:09:02 | |
it becomes clear that almost all of these | 0:09:02 | 0:09:05 | |
are concentrated on the continental shelf. | 0:09:05 | 0:09:08 | |
For millions of years, dead sea creatures | 0:09:14 | 0:09:17 | |
and sediment from the land have rained down on the sea bed. | 0:09:17 | 0:09:21 | |
With time, pressure and heat, this debris turns into oil | 0:09:22 | 0:09:27 | |
and this has made the shelf immensely valuable. | 0:09:27 | 0:09:30 | |
Today, these large oil and gas fields | 0:09:32 | 0:09:35 | |
help fuel our cars... | 0:09:35 | 0:09:37 | |
..boats... | 0:09:39 | 0:09:41 | |
and jets. | 0:09:41 | 0:09:43 | |
As we drain the water from the seas and leave the shore far behind, | 0:09:52 | 0:09:56 | |
we come to the edge of the continental land mass, | 0:09:56 | 0:09:59 | |
where the sea bed slopes steeply down to the ocean floor. | 0:09:59 | 0:10:03 | |
The edge of the continental shelf is often unstable and easily eroded. | 0:10:07 | 0:10:12 | |
It's here that we find some of the shelf's biggest features. | 0:10:12 | 0:10:15 | |
Deep canyons. | 0:10:20 | 0:10:22 | |
To get an idea of the scale of these underwater canyons, | 0:10:46 | 0:10:49 | |
think the Grand Canyon in the USA. | 0:10:49 | 0:10:54 | |
It's one mile deep, 18 miles wide and 277 miles long. | 0:10:54 | 0:11:00 | |
Yet the canyons on the continental shelf can be even larger. | 0:11:03 | 0:11:08 | |
Anyone can visit the Grand Canyon. I've done it myself. | 0:11:11 | 0:11:14 | |
But to see these underwater canyons is a much more serious challenge. | 0:11:14 | 0:11:19 | |
This is Monterey Bay, California, | 0:11:31 | 0:11:33 | |
and just out there is one of the wonders of the ocean. | 0:11:33 | 0:11:38 | |
To show you it, I need a pretty specialised vehicle. This. | 0:11:38 | 0:11:43 | |
Oh, yeah. | 0:11:50 | 0:11:52 | |
'It may look like a glass bubble but this little baby | 0:11:52 | 0:11:54 | |
'is actually a two-man sub that can dive nearly one mile beneath the surface. | 0:11:54 | 0:12:01 | |
'It's one of the world's most technologically advanced glass bubbles. | 0:12:01 | 0:12:06 | |
'And it needs to be, | 0:12:08 | 0:12:09 | |
'because to get to the bottom of an undersea canyon is a deep, dark | 0:12:09 | 0:12:14 | |
'and potentially dangerous dive.' | 0:12:14 | 0:12:16 | |
You've got the fire extinguisher, mask, oxygen system. And that's it. | 0:12:18 | 0:12:23 | |
Our visibility is good. | 0:12:24 | 0:12:27 | |
'Now, which way is the ocean?' | 0:12:29 | 0:12:31 | |
'Luckily, I'm in the capable hands of pilot Mike Caplehorn.' | 0:12:33 | 0:12:37 | |
'Monterey Bay Canyon begins just a few hundred metres off the shore, | 0:12:43 | 0:12:49 | |
'so we don't have to go out too far.' | 0:12:49 | 0:12:51 | |
I'm steering 203, south. | 0:12:53 | 0:12:56 | |
Roger, stand by. | 0:12:56 | 0:12:57 | |
'The support diver unhooks us from the boat | 0:13:01 | 0:13:04 | |
'and we'll then head down into the abyss.' | 0:13:04 | 0:13:07 | |
This is where it's going to come up the window | 0:13:07 | 0:13:09 | |
and, I presume, feel pretty unnerving. | 0:13:09 | 0:13:13 | |
-Mike, have you ever had anyone panic completely? -Yes. | 0:13:13 | 0:13:16 | |
OK... | 0:13:18 | 0:13:19 | |
'I wasn't scared, I was just sweating...cos it's warm in there.' | 0:13:19 | 0:13:23 | |
My main vents are about to be closed. | 0:13:23 | 0:13:26 | |
'High speed with four wheels on land, | 0:13:26 | 0:13:29 | |
'not usually a problem for me. But trapped in here, | 0:13:29 | 0:13:32 | |
'heading vertically down, it was a BIT scary.' | 0:13:32 | 0:13:37 | |
There goes the sun. | 0:13:37 | 0:13:39 | |
-That's it. We are now, just, officially underwater. -Yeah. | 0:13:45 | 0:13:49 | |
I'm trying very hard to be cool about this, but arrrhhh! | 0:13:50 | 0:13:55 | |
OK, we're commencing our descent. | 0:13:56 | 0:13:58 | |
Comm is good and we are tracking you. | 0:14:01 | 0:14:03 | |
O2 is 19.2... | 0:14:03 | 0:14:06 | |
'The Monterey Canyon is deep. | 0:14:06 | 0:14:10 | |
'From the surface of the ocean to the bottom of the canyon, it's over two miles.' | 0:14:10 | 0:14:14 | |
Yeah, Deep Sea, Deep Sea... | 0:14:14 | 0:14:16 | |
Heading 160. | 0:14:16 | 0:14:18 | |
'We're now more than 300 feet down, | 0:14:26 | 0:14:28 | |
'rapidly descending into the mouth of the canyon.' | 0:14:28 | 0:14:32 | |
There's the monster. | 0:14:34 | 0:14:37 | |
Two miles deep from the surface of the sea | 0:14:37 | 0:14:39 | |
down to the bottom of the deepest part. | 0:14:39 | 0:14:42 | |
That's 3km that way. | 0:14:42 | 0:14:45 | |
'You'd think the water down here would be crystal clear, | 0:14:50 | 0:14:54 | |
'but it's like a snow storm. | 0:14:54 | 0:14:56 | |
'Much of this sediment has been washed off the land | 0:14:56 | 0:14:59 | |
'and funnelled into the deep, | 0:14:59 | 0:15:01 | |
'a process that helps carve out the canyon.' | 0:15:01 | 0:15:04 | |
-Look at the jellyfish. See them? -Where, where? Oh, God! | 0:15:12 | 0:15:15 | |
-That is enormous! -It is very big. | 0:15:15 | 0:15:19 | |
OK, I'm going a little bit deeper, see if we can get more vertical. | 0:15:27 | 0:15:31 | |
'The sun's rays can't penetrate this far down. | 0:15:33 | 0:15:37 | |
'We're now 700 feet down and can only see as far as our lights can shine. | 0:15:37 | 0:15:43 | |
'It's cold, dark and just a bit intimidating. | 0:15:46 | 0:15:51 | |
'This is where creatures glow in the dark. | 0:15:53 | 0:15:56 | |
'I'm in the realm of aliens.' | 0:16:00 | 0:16:03 | |
That one flashed neon when it hit the light. | 0:16:03 | 0:16:05 | |
Lit up. | 0:16:05 | 0:16:07 | |
'So far, so good, | 0:16:12 | 0:16:14 | |
'and I was just about getting used to this deep ocean business, | 0:16:14 | 0:16:17 | |
-'when, all of a sudden...' -CRACK | 0:16:17 | 0:16:20 | |
What was that? | 0:16:20 | 0:16:22 | |
That was just a crack in the glass, nothing to worry about. | 0:16:22 | 0:16:25 | |
That's not a sound I want to hear! Don't ever say that to me again! | 0:16:25 | 0:16:29 | |
OK, we'll turn around and head for the wall. | 0:16:29 | 0:16:32 | |
'Yeah, I hope Mike's a better pilot that he is comedian. | 0:16:34 | 0:16:39 | |
'Because somewhere up in front of us is the wall of the canyon. | 0:16:39 | 0:16:43 | |
'The visibility is getting worse. | 0:16:43 | 0:16:45 | |
'This is where it gets tense.' | 0:16:45 | 0:16:48 | |
If you go forward 200 south, 200 south. | 0:16:48 | 0:16:53 | |
-That is it. -That's the wall? -That's the wall. | 0:17:03 | 0:17:06 | |
Look at that. That really is the walls of a canyon. | 0:17:06 | 0:17:10 | |
Mike, well done! | 0:17:14 | 0:17:17 | |
'Mike tells me the walls extend for hundreds of feet below | 0:17:28 | 0:17:31 | |
'and for miles either side but with the poor visibility | 0:17:31 | 0:17:35 | |
'and the fact we can't go any deeper, | 0:17:35 | 0:17:37 | |
'it's time to head back to the surface.' | 0:17:37 | 0:17:39 | |
Oh, land! It's there. | 0:17:49 | 0:17:52 | |
It might not be the most original thought | 0:17:56 | 0:17:58 | |
but that really is another world down there. | 0:17:58 | 0:18:01 | |
And bobbing about back up on the surface, waiting to be picked up, | 0:18:01 | 0:18:04 | |
again, it's not the most original thought, | 0:18:04 | 0:18:07 | |
but I felt like we were two returning astronauts in our capsule, all sealed in. | 0:18:07 | 0:18:12 | |
I need a cup of tea more than anything else in the whole world. | 0:18:12 | 0:18:16 | |
I've been lucky to get a glimpse of the canyon | 0:18:17 | 0:18:20 | |
but there's only one way to see the whole thing. | 0:18:20 | 0:18:23 | |
With our virtual earth, we can drain all the water from Monterey Bay Canyon. | 0:18:26 | 0:18:30 | |
It took around ten million years to carve this canyon | 0:18:37 | 0:18:41 | |
into the side of the continental shelf. | 0:18:41 | 0:18:45 | |
But if you think THAT's big, just hold on. | 0:18:45 | 0:18:48 | |
A few thousand miles northwest of California, | 0:18:48 | 0:18:51 | |
just off the coast of Russia, | 0:18:51 | 0:18:53 | |
there's a canyon that makes Monterey look like a teacup. | 0:18:53 | 0:18:57 | |
The largest canyon on the planet is the Zhemchug. | 0:19:17 | 0:19:20 | |
It's nearly two miles deep at its deepest point | 0:19:20 | 0:19:24 | |
and 144 miles long and 62 miles wide. | 0:19:24 | 0:19:29 | |
Of course, it's normally hidden by the Pacific Ocean | 0:19:29 | 0:19:32 | |
but the Zhemchug is so wide it's impossible to see from one side to the other | 0:19:32 | 0:19:37 | |
unless you are above the curvature of the Earth. | 0:19:37 | 0:19:40 | |
So far on our journey to the bottom of the sea, | 0:20:09 | 0:20:12 | |
we've drained the water from the beaches to the edge of the continental shelf. | 0:20:12 | 0:20:16 | |
We've drained the water from the cliffs and canyons | 0:20:16 | 0:20:19 | |
and now we've reached the floor of the deep ocean. | 0:20:19 | 0:20:22 | |
For the first time, we can see direct evidence | 0:20:22 | 0:20:24 | |
of the earth machine and how it affects this part of the sea floor. | 0:20:24 | 0:20:29 | |
It's called the abyssal plain | 0:20:29 | 0:20:32 | |
and it covers over half the planet's surface. | 0:20:32 | 0:20:35 | |
For years, it was thought to be flat and lifeless, | 0:20:36 | 0:20:40 | |
but in the middle of the Atlantic, you find one of the biggest geological features on the planet. | 0:20:40 | 0:20:45 | |
It is one of the most important parts of the earth machine. | 0:20:49 | 0:20:53 | |
This huge mountain range is called the Mid-Atlantic Ridge | 0:20:53 | 0:20:58 | |
and it's one of the largest and most active geological structures | 0:20:58 | 0:21:03 | |
in the entire solar system. | 0:21:03 | 0:21:05 | |
It's part of a vast tear in the planet's surface - | 0:21:08 | 0:21:13 | |
a single line of underwater mountains and volcanoes | 0:21:13 | 0:21:17 | |
that runs for over 40,000 miles around the planet. | 0:21:17 | 0:21:22 | |
At the mid-ocean ridge, lava forces its way up from below. | 0:21:25 | 0:21:29 | |
It's supplied by the mantle, a searing-hot layer below the crust. | 0:21:32 | 0:21:36 | |
This tear in the crust shows the power | 0:21:40 | 0:21:44 | |
of the machine that drives planet earth. | 0:21:44 | 0:21:47 | |
As the lava flows out, | 0:21:50 | 0:21:52 | |
it spreads away from the centre of the ridge and cools. | 0:21:52 | 0:21:56 | |
This pushes the whole sea floor ahead of it | 0:22:00 | 0:22:03 | |
and creates incredible stresses and strains. | 0:22:03 | 0:22:07 | |
This pressure triggers earthquakes and landslides, | 0:22:09 | 0:22:13 | |
makes deep valleys and huge undersea mountains. | 0:22:13 | 0:22:17 | |
This continuous process produces a square mile of new rock every year. | 0:22:20 | 0:22:27 | |
If we travel north, up here we come to a place | 0:22:31 | 0:22:34 | |
where the vast volcano range rises out of the water, | 0:22:34 | 0:22:37 | |
creating an island like no other. | 0:22:37 | 0:22:40 | |
Iceland. | 0:22:54 | 0:22:56 | |
Iceland is the only place in the world where the mid-ocean ridge | 0:23:02 | 0:23:06 | |
rises above the waves, exposing over 100 active volcanoes. | 0:23:06 | 0:23:11 | |
At one time, this whole landscape would have been underwater. | 0:23:18 | 0:23:23 | |
It's the closest I'll get to the ocean floor. | 0:23:23 | 0:23:25 | |
Iceland gives me the chance to take a look | 0:23:32 | 0:23:34 | |
at the mid-ocean ridge from the inside. | 0:23:34 | 0:23:37 | |
That is Lake Thingvellir | 0:23:41 | 0:23:43 | |
and this crack is part of the Mid-Atlantic Ridge. | 0:23:43 | 0:23:46 | |
It's known locally as Silfra and it's considered | 0:23:46 | 0:23:49 | |
one of the most beautiful and spectacular dives in the world. | 0:23:49 | 0:23:53 | |
And seeing as I'm already dressed... | 0:23:53 | 0:23:56 | |
'You can swim through the gap | 0:24:08 | 0:24:11 | |
'between the two halves of the mid-ocean ridge. | 0:24:11 | 0:24:14 | |
'They're moving apart by about an inch a year.' | 0:24:14 | 0:24:18 | |
On this side, the United States. | 0:24:18 | 0:24:21 | |
On that side, Europe. | 0:24:21 | 0:24:25 | |
And they're just metres apart. | 0:24:25 | 0:24:27 | |
'A couple of million years ago, there would have been lava pouring up through this crack. | 0:24:27 | 0:24:32 | |
'Now it's cooled and solidified, it's left an incredible opportunity | 0:24:32 | 0:24:36 | |
'for us to see inside the mid-ocean ridge.' | 0:24:36 | 0:24:40 | |
Because the ground in Iceland is very thin - | 0:24:52 | 0:24:55 | |
in some places only a few miles deep - | 0:24:55 | 0:24:58 | |
you can see other effects caused by the volcanic machine below. | 0:24:58 | 0:25:03 | |
The thermal power of the earth is evident everywhere here. | 0:25:10 | 0:25:14 | |
This is one of Iceland's many famous geysers, | 0:25:14 | 0:25:16 | |
and the way it works is actually pretty simple. | 0:25:16 | 0:25:19 | |
It's like switching on a giant, instantly boiling kettle every few minutes. | 0:25:19 | 0:25:23 | |
The rocks down there are at about 200 degrees centigrade. | 0:25:23 | 0:25:26 | |
When water enters an underground chamber about 60 feet down, | 0:25:26 | 0:25:30 | |
it's boiled instantly, so it expands hugely, | 0:25:30 | 0:25:33 | |
it explodes into steam and fires out of the hole, | 0:25:33 | 0:25:36 | |
creating this magnificent spectacle. | 0:25:36 | 0:25:38 | |
Surprisingly, geysers exist all along the mid-ocean ridge. | 0:26:01 | 0:26:05 | |
One mile down, on the ocean floor, they look like this. | 0:26:18 | 0:26:22 | |
They're called black smokers | 0:26:22 | 0:26:24 | |
and they were only discovered about 30 years ago. | 0:26:24 | 0:26:27 | |
Superheated water laced with precious minerals - | 0:26:40 | 0:26:44 | |
gold, silver and iron - races up from the volcanic rocks below. | 0:26:44 | 0:26:48 | |
As they hit the cold sea water, the minerals turn black. | 0:26:51 | 0:26:55 | |
They then solidify into chimneys that can grow up to 180 feet high. | 0:26:55 | 0:27:01 | |
The chimneys would be worth a fortune | 0:27:05 | 0:27:07 | |
but right now they're just too difficult to mine. | 0:27:07 | 0:27:11 | |
But scientists have recently discovered a little chap | 0:27:13 | 0:27:17 | |
who's been mining the black smokers for years. | 0:27:17 | 0:27:19 | |
A metal snail. | 0:27:26 | 0:27:29 | |
This snail makes its shell and the scales on its foot | 0:27:31 | 0:27:34 | |
from the metals in the water around it. | 0:27:34 | 0:27:38 | |
The scaly-foot is the most extraordinary thing I've found. | 0:27:38 | 0:27:41 | |
These scaly-foot snails were discovered nearly two miles down | 0:27:42 | 0:27:46 | |
in the ocean by Professor Cindy Van Dover. | 0:27:46 | 0:27:49 | |
We were sampling the large common snails, | 0:27:52 | 0:27:55 | |
and in the handful of snails that we brought to the surface, | 0:27:55 | 0:27:58 | |
we discovered these small, scaly-foot snails. | 0:27:58 | 0:28:02 | |
We wondered for a couple of weeks, what could they be? We didn't know. | 0:28:02 | 0:28:06 | |
There is no other known snail that has a metal-fortified shell. | 0:28:08 | 0:28:12 | |
Even in the animal kingdom, we don't know of anything else that has a metal-fortified shell. | 0:28:14 | 0:28:20 | |
The animals have spent evolutionary time | 0:28:20 | 0:28:23 | |
honing the composition of their shell | 0:28:23 | 0:28:25 | |
to make it deflect predators, to make it strong. | 0:28:25 | 0:28:28 | |
So, it's like having armour. | 0:28:28 | 0:28:30 | |
What a weird little fellow. | 0:28:34 | 0:28:37 | |
Each time scientists visit these volcanic worlds, | 0:28:37 | 0:28:40 | |
over half the animals they find are unknown to science. | 0:28:40 | 0:28:45 | |
Here's this little animal that sits in this warm water that's coming out, | 0:28:45 | 0:28:48 | |
that's metal-rich, and it's sitting there mining these metals. | 0:28:48 | 0:28:52 | |
That is extraordinary. | 0:28:52 | 0:28:53 | |
Super snails and precious metals are just a tiny part of the riches | 0:29:02 | 0:29:07 | |
produced by the volcanic machine below. | 0:29:07 | 0:29:10 | |
A machine that has a much more destructive side. | 0:29:10 | 0:29:14 | |
When the new sea floor spreads out from the mid-ocean ridge, | 0:29:17 | 0:29:21 | |
the sea floor buckles, and causes massive undersea movements and landslides. | 0:29:21 | 0:29:26 | |
Although these happen miles beneath the ocean, they can affect us all. | 0:29:34 | 0:29:39 | |
You might not know this, but pretty much all Internet traffic | 0:29:47 | 0:29:50 | |
is carried between the continents by undersea cables. | 0:29:50 | 0:29:53 | |
In December 2006, nine fibre optic cables | 0:29:53 | 0:29:58 | |
between Taiwan and the Philippines suddenly went dead. | 0:29:58 | 0:30:01 | |
Computers across Asia crashed. | 0:30:01 | 0:30:03 | |
Engineers soon discovered that the cables had been severed. | 0:30:03 | 0:30:07 | |
But...by what? | 0:30:07 | 0:30:10 | |
Let's take a look beneath the waves. | 0:30:12 | 0:30:15 | |
Sediment collects in huge quantities | 0:30:20 | 0:30:23 | |
on the edge of underwater ledges and canyons. | 0:30:23 | 0:30:26 | |
Earthquakes then trigger underwater landslides. | 0:30:36 | 0:30:40 | |
On this occasion, just off the coast of Taiwan, | 0:30:45 | 0:30:47 | |
thousands of tonnes of rock and debris were dislodged. | 0:30:47 | 0:30:50 | |
The Internet cables were out of action for weeks. | 0:31:00 | 0:31:03 | |
It was an economic disaster. | 0:31:03 | 0:31:05 | |
The cables didn't stand a chance. | 0:31:08 | 0:31:11 | |
Help is at hand, but it needs a serious bit of kit. | 0:31:14 | 0:31:18 | |
Underwater landslides happen all the time. | 0:31:20 | 0:31:25 | |
The problem is, it's all too common for them to sever the cables | 0:31:25 | 0:31:28 | |
that support the Internet. | 0:31:28 | 0:31:29 | |
And that means someone's got to go around fixing them. | 0:31:29 | 0:31:33 | |
And that's these chaps here. | 0:31:33 | 0:31:35 | |
I'm on board the Wave Sentinel. | 0:31:46 | 0:31:49 | |
It's one of a fleet of high-tech vessels | 0:31:49 | 0:31:51 | |
whose job it is to keep the world connected. | 0:31:51 | 0:31:54 | |
The hot phone. That rings, we start running. | 0:31:58 | 0:32:00 | |
-That's it? -That's it. | 0:32:00 | 0:32:02 | |
-Seriously? Is it on now? -Yeah, it's on. | 0:32:02 | 0:32:05 | |
-So, if that phone goes... -If that phone goes, I'll get all... | 0:32:05 | 0:32:09 | |
So this whole thing is on permanent standby, | 0:32:09 | 0:32:12 | |
-this whole operation? -Permanent standby. | 0:32:12 | 0:32:14 | |
MOBILE RINGS Excuse me. | 0:32:14 | 0:32:16 | |
Wave Sentinel captain. | 0:32:16 | 0:32:17 | |
Contract at 24 hours' notice. | 0:32:19 | 0:32:22 | |
We're fuelled up, water, provisions, we're ready to go. | 0:32:23 | 0:32:28 | |
You get that phone call, all of a sudden everyone's in a hurry. | 0:32:28 | 0:32:31 | |
We get as much information as fast as we can and make a plan. | 0:32:39 | 0:32:43 | |
And the plan involves heading to the most remote parts of the ocean | 0:32:44 | 0:32:49 | |
and risking life and limb to fix the cables quickly. | 0:32:49 | 0:32:53 | |
99% of all Internet business and communication | 0:32:55 | 0:33:00 | |
that flows between the continents passes through ocean-floor cables. | 0:33:00 | 0:33:03 | |
They search for the broken cables at depths of up to three miles | 0:33:05 | 0:33:09 | |
with high-tech, remote-operated vehicles. | 0:33:09 | 0:33:11 | |
-RADIO: -Back to normal speed. Keep it nice and slow. | 0:33:13 | 0:33:18 | |
When they find the cable, it's brought back on deck | 0:33:20 | 0:33:24 | |
and taken to a state-of-the-art operating theatre. | 0:33:24 | 0:33:28 | |
-So that's what's in there, inside all that cladding, doing the job? -Yes. | 0:33:45 | 0:33:50 | |
Everything this is about - you, all of your time, the ship, | 0:33:50 | 0:33:54 | |
the seas, the struggle, the toil - it's in there | 0:33:54 | 0:33:59 | |
and it's a fraction a thickness of a hair and that's it? | 0:33:59 | 0:34:02 | |
That's correct. | 0:34:02 | 0:34:04 | |
How much information is flowing along those? | 0:34:04 | 0:34:08 | |
Each fibre comes in a pair | 0:34:08 | 0:34:10 | |
and each fibre pair, at a conservative estimate, | 0:34:10 | 0:34:13 | |
can transmit 150 million simultaneous phone calls. | 0:34:13 | 0:34:16 | |
All at the same time. | 0:34:16 | 0:34:18 | |
It must get very crowded in there. | 0:34:18 | 0:34:21 | |
It's a very delicate-looking thing to send to the bottom of the sea. | 0:34:21 | 0:34:25 | |
It's a very fiddly job. | 0:34:35 | 0:34:37 | |
How the hell do you do this on a moving ship? | 0:34:39 | 0:34:42 | |
With a great deal of difficulty. | 0:34:43 | 0:34:46 | |
We're trained professionals. | 0:34:46 | 0:34:48 | |
Each repair can cost half a million pounds. | 0:34:50 | 0:34:53 | |
All the big global telecoms companies have these guys on speed dial. | 0:34:53 | 0:34:58 | |
There are hundreds of landslides each year in the Atlantic. | 0:35:04 | 0:35:08 | |
It's ships like the Wave Sentinel that keep the World Wide Web connected. | 0:35:08 | 0:35:12 | |
Having seen a tiny bit of the sea floor myself, | 0:35:14 | 0:35:19 | |
I now realise just how vast it is, | 0:35:19 | 0:35:21 | |
yet the only sign of human activity | 0:35:21 | 0:35:23 | |
is the odd deep-sea sub and some cables. | 0:35:23 | 0:35:26 | |
Strange how we still think we dominate our planet. | 0:35:26 | 0:35:30 | |
But of course, the planet is really dominated by the earth machine. | 0:35:33 | 0:35:39 | |
And that means volcanoes. | 0:35:39 | 0:35:40 | |
80% of Earth's volcanic activity is hidden underwater | 0:35:41 | 0:35:45 | |
and some of the volcanoes on the sea floor are big. Very big. | 0:35:45 | 0:35:51 | |
We think of Everest as the world's tallest mountain. | 0:35:51 | 0:35:54 | |
But strictly speaking, that accolade belongs to a mountain in the middle of the Pacific Ocean. | 0:35:54 | 0:35:59 | |
The summit of Mauna Kea volcano on Hawaii | 0:36:05 | 0:36:08 | |
has grown over two and a half miles above sea level. | 0:36:08 | 0:36:12 | |
But it's another three and a half miles down to the sea floor. | 0:36:12 | 0:36:17 | |
And it doesn't stop there. | 0:36:17 | 0:36:19 | |
Because the island is so heavy, it's sunk into in the sea floor. | 0:36:19 | 0:36:23 | |
And that means the true base is another five miles further down. | 0:36:25 | 0:36:29 | |
From top to bottom, Mauna Kea is over 11 miles high. | 0:36:32 | 0:36:36 | |
That's twice the height of Mount Everest. | 0:36:36 | 0:36:39 | |
Now we're going to go from the tallest mountain | 0:36:40 | 0:36:44 | |
to the deepest place on earth. | 0:36:44 | 0:36:46 | |
So far, we've drained down the oceans down to about three miles, | 0:36:49 | 0:36:52 | |
which has revealed most of the sea floor. | 0:36:52 | 0:36:55 | |
But surprisingly, there is more to drain - another four miles, in fact. | 0:36:59 | 0:37:05 | |
We're about to go to the deepest point on the surface of the earth. | 0:37:05 | 0:37:09 | |
Normally hidden by water, there is a huge ravine in the earth's crust, | 0:37:11 | 0:37:16 | |
where two tectonic plates meet. | 0:37:16 | 0:37:18 | |
And this is it, the Mariana Trench in the western Pacific. | 0:37:22 | 0:37:26 | |
This baby reaches down nearly seven miles deep. | 0:37:26 | 0:37:30 | |
At 1,500 miles long and 40 miles wide, | 0:37:43 | 0:37:46 | |
this massive trench contains the deepest point on earth... | 0:37:46 | 0:37:50 | |
..the Challenger Deep. | 0:37:55 | 0:37:57 | |
What's it like down there, nearly seven miles below the surface? | 0:38:19 | 0:38:23 | |
And why would anyone go there? | 0:38:23 | 0:38:26 | |
There is a man who knows, first-hand. | 0:38:26 | 0:38:30 | |
12 men have stood on the moon, | 0:38:30 | 0:38:31 | |
but only two have been to the deepest place on earth. | 0:38:31 | 0:38:35 | |
One of them is Don Walsh | 0:38:36 | 0:38:38 | |
and he's here in San Diego, where it all began. | 0:38:38 | 0:38:42 | |
Don, then a Navy Lieutenant | 0:38:48 | 0:38:50 | |
set sail with Swiss oceanographer Jacques Piccard, | 0:38:50 | 0:38:53 | |
on secret US Navy mission. | 0:38:53 | 0:38:56 | |
At 6am on 23rd January 1960, | 0:38:59 | 0:39:03 | |
they climbed into the confined space of the research submarine, Trieste. | 0:39:03 | 0:39:08 | |
The space inside the cabin was about 35, 38 cubic feet. | 0:39:13 | 0:39:19 | |
The average household refrigerator has about that same capacity. | 0:39:19 | 0:39:24 | |
The temperature inside wasn't much different. | 0:39:24 | 0:39:26 | |
To get an idea, climb into your refrigerator | 0:39:26 | 0:39:28 | |
for a beer with a six-foot tall friend, | 0:39:28 | 0:39:31 | |
-close the door and spend nine hours in there? -Nine hours. -Right. | 0:39:31 | 0:39:34 | |
The Trieste had five-inch-thick walls, | 0:39:34 | 0:39:37 | |
and the 13-tonne pressure sphere hung under a massive tank | 0:39:37 | 0:39:41 | |
filled with 22,500 gallons of gasoline for buoyancy. | 0:39:41 | 0:39:46 | |
The pressure is eight tons per square inch, | 0:39:49 | 0:39:51 | |
so in an area that size, you'd have eight tons pushing down. | 0:39:51 | 0:39:55 | |
Total pressure on the cabin was 200,000 tons, | 0:39:55 | 0:40:00 | |
like 100 WW2 Navy destroyers piled on top of you. | 0:40:00 | 0:40:06 | |
You will have thought of this, Don, | 0:40:06 | 0:40:08 | |
if something had gone wrong, what happened? | 0:40:08 | 0:40:11 | |
It was over. | 0:40:11 | 0:40:12 | |
The great danger to the mission was the tremendous pressure at these depths. | 0:40:13 | 0:40:18 | |
At 31,000 feet on our way down, we had a huge bang. | 0:40:18 | 0:40:22 | |
BANG | 0:40:22 | 0:40:25 | |
There's a window in the hatch and that had cracked. | 0:40:25 | 0:40:27 | |
The descent took nearly five hours. | 0:40:30 | 0:40:33 | |
They'd reached the bottom of the Mariana Trench, | 0:40:37 | 0:40:40 | |
seven miles below the surface. | 0:40:40 | 0:40:42 | |
We were in a space ship. It was like visiting another planet. | 0:40:44 | 0:40:47 | |
Once we'd disconnected from the surface, it was like going through a void of space | 0:40:47 | 0:40:51 | |
and then landing on an alien planet, it was very much like that. | 0:40:51 | 0:40:55 | |
After we surfaced, Jacques and I were sitting there, | 0:40:55 | 0:40:58 | |
waiting for the boats to come fetch us. | 0:40:58 | 0:41:01 | |
We're talking about this, "When do you think somebody will be back next?" | 0:41:01 | 0:41:05 | |
We kind of agreed, between one and two years. | 0:41:05 | 0:41:07 | |
That was a half century ago. | 0:41:13 | 0:41:15 | |
No-one's been back. | 0:41:17 | 0:41:19 | |
Don is now the only living man to have been to the deepest place on earth. | 0:41:27 | 0:41:33 | |
On my little trip into Monterey Bay, I went down a few hundred feet. | 0:41:33 | 0:41:36 | |
It's extraordinary to think he went down a further six and a half miles. | 0:41:36 | 0:41:42 | |
Those early glimpses of the deep ocean floor | 0:41:42 | 0:41:45 | |
suggested very little happened down there. | 0:41:45 | 0:41:49 | |
But that couldn't have been more wrong. | 0:41:49 | 0:41:51 | |
We've got to the bottom of the ocean but it's not the end of the journey. | 0:41:51 | 0:41:56 | |
Because the power of the earth machine beneath the sea floor | 0:41:58 | 0:42:01 | |
affects the lives of millions of people. | 0:42:01 | 0:42:05 | |
As the sea floor spreads out from the mid-ocean ridge, | 0:42:08 | 0:42:12 | |
it eventually collides with the land. | 0:42:12 | 0:42:14 | |
Massive pressure builds up... | 0:42:18 | 0:42:20 | |
..until suddenly... | 0:42:25 | 0:42:27 | |
EXPLOSION | 0:42:28 | 0:42:30 | |
..it gives. | 0:42:30 | 0:42:31 | |
This is what happened off the coast of Japan in March 2011. | 0:42:50 | 0:42:54 | |
An earthquake beneath the sea floor created the devastating tsunami that hit Japan. | 0:43:01 | 0:43:07 | |
It was a horribly powerful reminder that the whole of the Pacific region | 0:43:22 | 0:43:27 | |
is very unstable, and earthquakes are frequent. | 0:43:27 | 0:43:31 | |
Seven years earlier, there was an even bigger earthquake | 0:43:31 | 0:43:35 | |
and an even more destructive tsunami. | 0:43:35 | 0:43:37 | |
On 26th December 2004, Indonesia was hit by a devastating earthquake | 0:43:39 | 0:43:44 | |
that came from beneath the sea floor. | 0:43:44 | 0:43:47 | |
Just off the coast of Indonesia, the sea bed was ripped open. | 0:43:56 | 0:44:01 | |
In just six seconds, part of the ocean floor shot up by as much as 20 metres. | 0:44:04 | 0:44:10 | |
This quake created a powerful tsunami. | 0:44:52 | 0:44:54 | |
Around South East Asia, more than 200,000 people died. | 0:44:54 | 0:45:00 | |
The earthquake was so powerful, it shifted the earth on its axis, | 0:45:17 | 0:45:21 | |
and shortened our days by 2.8 microseconds. | 0:45:21 | 0:45:25 | |
The quake also moved the North Pole nearly an inch to the east. | 0:45:28 | 0:45:32 | |
Fortunately, most undersea quakes go unnoticed by you and me. | 0:45:42 | 0:45:47 | |
But scientists always record the effect they have on earth. | 0:45:47 | 0:45:51 | |
Normally we can't hear them, but thanks to a clever bit of technology, | 0:45:51 | 0:45:55 | |
we can hear what the Indonesian undersea earthquake sounded like. | 0:45:55 | 0:46:01 | |
DISTANT RUMBLING | 0:46:01 | 0:46:04 | |
The Earth literally rang like a bell for weeks. | 0:46:09 | 0:46:13 | |
The enormous power of the devastating Indonesian earthquake | 0:46:18 | 0:46:23 | |
is evidence of a much bigger process that starts on the ocean floor. | 0:46:23 | 0:46:28 | |
As the heavier rock of the sea floor bumps up against the land, | 0:46:29 | 0:46:34 | |
it has nowhere to go but down. | 0:46:34 | 0:46:38 | |
It's a process called subduction. | 0:46:47 | 0:46:50 | |
This collision between the sea floor and the land creates enormous pressure. | 0:46:52 | 0:46:57 | |
As it falls, the rock begins to melt. | 0:46:59 | 0:47:04 | |
The heat and pressure is so great that some of this molten rock | 0:47:04 | 0:47:07 | |
escapes upwards through cracks in the land above. | 0:47:07 | 0:47:11 | |
When the lava reaches the surface, the results are spectacular. | 0:47:11 | 0:47:16 | |
This is engineering on a truly global scale. | 0:47:16 | 0:47:22 | |
As the sea floor is pushed under the land, | 0:47:24 | 0:47:26 | |
the melting rock has created a chain of over 200 volcanoes | 0:47:26 | 0:47:30 | |
along the west coast of South America... | 0:47:30 | 0:47:33 | |
..and another 50 active volcanoes further up the coast to the USA and Alaska. | 0:47:34 | 0:47:40 | |
Across and down around the coast of Russia, Japan and China, | 0:47:45 | 0:47:49 | |
there are hundreds more. | 0:47:49 | 0:47:50 | |
From back here, they look like rivets holding the planet together. | 0:47:53 | 0:47:59 | |
This line of coastal volcanoes is known as the Pacific Ring of Fire. | 0:48:05 | 0:48:11 | |
These volcanoes mark the zone where the sea floor has been pushed down beneath the land. | 0:48:29 | 0:48:34 | |
When it melts, the searing heat and build-up of pressure | 0:48:34 | 0:48:38 | |
causes some of the most destructive eruptions ever seen. | 0:48:38 | 0:48:42 | |
The most volcanically active of these islands is Java in Indonesia, | 0:48:48 | 0:48:53 | |
with 42 volcanoes in a row. | 0:48:53 | 0:48:57 | |
I've always thought of volcanoes as purely destructive, | 0:48:58 | 0:49:01 | |
but, in fact, they bring valuable minerals | 0:49:01 | 0:49:03 | |
and vital gases to the surface. | 0:49:03 | 0:49:06 | |
At the Kawah Ijen volcano in Indonesia, | 0:49:06 | 0:49:09 | |
you can witness one of the most extraordinary sights created by the earth's machine. | 0:49:09 | 0:49:13 | |
This haunting spectacle is liquid sulphur burning within the crater of the volcano. | 0:49:34 | 0:49:40 | |
Sulphur is one of the most important chemicals for industry, | 0:50:04 | 0:50:08 | |
but it's also is one of the key minerals needed | 0:50:08 | 0:50:10 | |
for all life on earth. | 0:50:10 | 0:50:12 | |
These liquid rivers of burning sulphur are fed by the sea floor | 0:50:14 | 0:50:18 | |
melting 60 miles below the land. | 0:50:18 | 0:50:23 | |
In Kawah Ijen, we can see first-hand how the earth's machine | 0:50:39 | 0:50:44 | |
produces these valuable chemicals. | 0:50:44 | 0:50:46 | |
In the craters of volcanoes like this, we can get our hands on raw sulphur. | 0:50:48 | 0:50:54 | |
The poisonous gases sulphur gives off make this place | 0:50:54 | 0:50:58 | |
one of the most toxic environments on the planet. | 0:50:58 | 0:51:02 | |
Every day, hundreds of miners descend into these fumes | 0:51:13 | 0:51:17 | |
to bring out solid sulphur by hand. | 0:51:17 | 0:51:20 | |
These gases are so corrosive that the men can only spend | 0:51:30 | 0:51:34 | |
-a brief time in the crater. -MEN COUGH | 0:51:34 | 0:51:37 | |
No wonder they have a short life expectancy. | 0:51:37 | 0:51:40 | |
Liquid sulphur pours out of the ground at 600 degrees centigrade... | 0:52:07 | 0:52:12 | |
..then solidifies. | 0:52:17 | 0:52:19 | |
Every day, the miners bring out tonnes of the yellow sulphur... | 0:52:24 | 0:52:28 | |
the hard way! | 0:52:28 | 0:52:31 | |
Sulphur is used in everything from medicines to fertilisers, | 0:52:41 | 0:52:45 | |
vulcanising rubber and even for making your sugar that perfect white. | 0:52:45 | 0:52:49 | |
Volcanoes bring other vital minerals to the surface | 0:53:00 | 0:53:05 | |
that enrich the soil and release gases that help create the air we breathe. | 0:53:05 | 0:53:10 | |
Volcanoes are an essential part of the earth's machine. | 0:53:14 | 0:53:18 | |
But our journey isn't over yet. | 0:53:26 | 0:53:28 | |
We're about to find out what happens to the sea floor | 0:53:28 | 0:53:30 | |
when it plunges under the land. | 0:53:30 | 0:53:32 | |
Having been forced down under the land, | 0:53:35 | 0:53:38 | |
some of the slabs of melting sea floor continue to fall, | 0:53:38 | 0:53:42 | |
their weight pulling more sea floor behind them. | 0:53:42 | 0:53:45 | |
Beneath the mantle is the core. | 0:53:47 | 0:53:49 | |
The core is the energy source that drives the earth's machine. | 0:53:52 | 0:53:57 | |
The core is even hotter than the mantle | 0:54:01 | 0:54:03 | |
and, as the descending sea floor reaches its outer surface, | 0:54:03 | 0:54:06 | |
it's superheated and rises back up | 0:54:06 | 0:54:09 | |
in vast plumes towards the surface. | 0:54:09 | 0:54:12 | |
It's one continuous cycle - | 0:54:17 | 0:54:20 | |
one that takes millions of years. | 0:54:20 | 0:54:22 | |
It really is the most amazing piece of engineering. | 0:54:22 | 0:54:26 | |
And it's all driven by the core of the earth machine. | 0:54:29 | 0:54:33 | |
So far we've drained the ocean from the coast to the deepest point on earth. | 0:54:37 | 0:54:42 | |
We've followed the journey of the sea bed | 0:54:42 | 0:54:45 | |
from its birth at the mid-ocean ridge to where it collides with the land. | 0:54:45 | 0:54:49 | |
We've seen the enormous forces | 0:54:49 | 0:54:51 | |
that drive the whole cycle of the sea floor, | 0:54:51 | 0:54:54 | |
yet we've overlooked the water itself. | 0:54:54 | 0:54:57 | |
Without it, there would be no life on earth. | 0:54:59 | 0:55:05 | |
So what would happen if the earth really did lose all its oceans? | 0:55:19 | 0:55:25 | |
Seriously scary things would happen, that's what! | 0:55:25 | 0:55:30 | |
Without the weight of the oceans, the mid-ocean ridge | 0:55:31 | 0:55:34 | |
would erupt violently, the planet would unzip | 0:55:34 | 0:55:37 | |
around the mid-ocean ridge. | 0:55:37 | 0:55:40 | |
Vast sheets of lava would explode into the sky. | 0:55:43 | 0:55:48 | |
Without the weight of water to support their sides, | 0:55:50 | 0:55:54 | |
the continental shelves would collapse. | 0:55:54 | 0:55:56 | |
Mud slides and dirt avalanches bigger than anything seen before | 0:56:00 | 0:56:04 | |
would be unleashed. | 0:56:04 | 0:56:07 | |
Massive pockets of methane gas would explode. | 0:56:10 | 0:56:13 | |
All this would cause hundreds of devastating earthquakes. | 0:56:16 | 0:56:20 | |
And with no water, there would be no weather, | 0:56:25 | 0:56:28 | |
no rain. | 0:56:28 | 0:56:30 | |
The entire planet would become a desert. | 0:56:30 | 0:56:33 | |
There would be nothing left alive. | 0:56:33 | 0:56:37 | |
Luckily, that's not going to happen. | 0:56:45 | 0:56:47 | |
So let's put it all back again. | 0:56:47 | 0:56:50 | |
We've seen how the earth works. | 0:56:54 | 0:56:56 | |
How the machine beneath the sea floor creates | 0:56:56 | 0:56:59 | |
the biggest geological features on the planet | 0:56:59 | 0:57:02 | |
and also drives the movement of the sea floor | 0:57:02 | 0:57:05 | |
to release minerals and gases so vital to life on earth. | 0:57:05 | 0:57:10 | |
The oceans are one of the most beautiful sights on our planet. | 0:57:20 | 0:57:25 | |
Hidden beneath the waves are some extraordinary processes | 0:57:25 | 0:57:28 | |
without which life on earth simply could not exist. | 0:57:28 | 0:57:33 | |
Subtitles by Red Bee Media Ltd | 0:58:09 | 0:58:11 | |
E-mail [email protected] | 0:58:11 | 0:58:13 |