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There are many moons in the solar system, but none like ours. | 0:00:06 | 0:00:11 | |
It exerts an extraordinary influence on Planet Earth, | 0:00:13 | 0:00:19 | |
keeping our world in balance. | 0:00:19 | 0:00:23 | |
But why is it so powerful? | 0:00:25 | 0:00:30 | |
I want to explore the relationship we have with our closest neighbour, | 0:00:30 | 0:00:34 | |
to see how the Moon has sculpted our planet and shaped our evolution. | 0:00:34 | 0:00:39 | |
Without the Moon, would we even be here? | 0:00:39 | 0:00:43 | |
'I'm Maggie Aderin-Pocock. | 0:00:43 | 0:00:47 | |
'I'm a space scientist and a lunar fanatic. | 0:00:47 | 0:00:51 | |
'I've always been mad about the Moon, | 0:00:51 | 0:00:55 | |
'convinced it plays a huge role in our lives.' | 0:00:55 | 0:00:59 | |
But I've always taken for granted that it is where it is | 0:00:59 | 0:01:04 | |
in the night sky, a quarter of a million miles away. | 0:01:04 | 0:01:08 | |
In this film I'm taking nothing for granted. | 0:01:08 | 0:01:12 | |
I'm going to find out what would happen if the Moon wasn't where it is now. | 0:01:12 | 0:01:19 | |
What if the Moon was in a different position, | 0:01:19 | 0:01:22 | |
closer or further away? | 0:01:22 | 0:01:26 | |
How different would our world be? | 0:01:26 | 0:01:28 | |
The Moon is a ball of rock out in space, | 0:01:56 | 0:01:59 | |
but it has the power to create great tides here on Earth. | 0:01:59 | 0:02:05 | |
This is Loch Etive on the west coast of Scotland. | 0:02:06 | 0:02:12 | |
Twice a day, the Moon drags 66 million tonnes of sea water through this loch. | 0:02:13 | 0:02:20 | |
The result, white water rapids. | 0:02:22 | 0:02:26 | |
The head of the loch is like a bottleneck. | 0:02:29 | 0:02:33 | |
Water is funnelled through a very narrow channel. | 0:02:33 | 0:02:36 | |
And for an hour or two, this becomes one of the wildest, wettest rides in the world. | 0:02:36 | 0:02:42 | |
These are the Falls of Lora. | 0:02:48 | 0:02:51 | |
That's what the locals call them. | 0:02:51 | 0:02:53 | |
In Gaelic, "Lora" means "noisy" | 0:02:53 | 0:02:56 | |
because as the tidal waters rush out of the loch, it gets very, very loud! | 0:02:56 | 0:03:01 | |
Kayakers come from all across the world to take the challenge of these waters. | 0:03:09 | 0:03:14 | |
But they have to paddle like mad just to keep up. | 0:03:14 | 0:03:17 | |
Even our outboard engine is struggling with the flow. | 0:03:17 | 0:03:20 | |
This is what the power of the Moon looks like up close. | 0:03:20 | 0:03:24 | |
My love affair with the Moon began as a child. | 0:03:29 | 0:03:33 | |
# I wish I was a spaceman | 0:03:33 | 0:03:36 | |
# The fastest guy alive... # | 0:03:36 | 0:03:39 | |
I was born in 1968, in the age of Apollo. | 0:03:39 | 0:03:43 | |
I took my first steps as Neil Armstrong took his giant leap. | 0:03:43 | 0:03:49 | |
Of course I was too young to know what was going on. | 0:03:53 | 0:03:55 | |
But the images became seared in my mind. | 0:03:55 | 0:04:00 | |
From an early age, I wanted to go to the Moon. | 0:04:00 | 0:04:04 | |
At school I struggled because I'm dyslexic. | 0:04:05 | 0:04:11 | |
But then I discovered science, and something clicked. | 0:04:11 | 0:04:16 | |
I wanted to become a scientist. | 0:04:16 | 0:04:20 | |
And sure enough, today I build satellites. | 0:04:21 | 0:04:26 | |
It's a mix of engineering and physics and I love it. | 0:04:26 | 0:04:30 | |
But now that I'm a space scientist, hardly anyone is talking about the Moon any more. | 0:04:30 | 0:04:37 | |
It used to be the new frontier, | 0:04:39 | 0:04:41 | |
our future. | 0:04:41 | 0:04:43 | |
Now it's seen as quaint, old-fashioned, irrelevant. | 0:04:43 | 0:04:49 | |
I think that's wrong, | 0:04:49 | 0:04:52 | |
completely wrong. | 0:04:52 | 0:04:55 | |
I'm still mad about the Moon, | 0:04:55 | 0:04:57 | |
not just because I want to be an astronaut and go there one day. | 0:04:57 | 0:05:01 | |
No. | 0:05:01 | 0:05:02 | |
I'm mad about the Moon because the more I find out about it, | 0:05:02 | 0:05:05 | |
the more extraordinary it seems. | 0:05:05 | 0:05:08 | |
The way its presence can conjure up this torrent of water, | 0:05:10 | 0:05:15 | |
and these waves. | 0:05:15 | 0:05:16 | |
And how does it do this? | 0:05:18 | 0:05:20 | |
With the help of gravity. | 0:05:20 | 0:05:23 | |
Gravity is a great universal force of attraction. | 0:05:25 | 0:05:29 | |
It keeps us firmly in our place on Earth | 0:05:29 | 0:05:32 | |
and keeps the Moon in orbit around us. | 0:05:32 | 0:05:35 | |
But while the Earth is attracting the Moon, | 0:05:38 | 0:05:41 | |
the Moon is also attracting the Earth, | 0:05:41 | 0:05:44 | |
pulling at our oceans. | 0:05:44 | 0:05:46 | |
So I have a set of scales, a metal block and a powerful little magnet. | 0:05:48 | 0:05:53 | |
You see, the force of gravity is very similar to magnetism. | 0:05:53 | 0:05:57 | |
They're both forces of attraction. | 0:05:57 | 0:05:59 | |
If I put the metal block on the scales, | 0:05:59 | 0:06:01 | |
you can see it weighs 1.3 kg. | 0:06:01 | 0:06:05 | |
When I put the magnet in and nudge it closer, | 0:06:05 | 0:06:09 | |
the block appears to weigh less. | 0:06:09 | 0:06:12 | |
You can see the needle moving. | 0:06:12 | 0:06:16 | |
That's because the magnet is attracting the metal towards it, | 0:06:16 | 0:06:20 | |
pulling it upwards, off the scales. | 0:06:20 | 0:06:23 | |
And that's what the Moon's doing. | 0:06:23 | 0:06:25 | |
It's pulling on the oceans, moving them upwards, away from the surface of the Earth. | 0:06:25 | 0:06:31 | |
The gravitational force of the Moon causes the oceans to bulge slightly. | 0:06:32 | 0:06:38 | |
And as the Earth spins, | 0:06:40 | 0:06:42 | |
this bulging produces high and low tides. | 0:06:42 | 0:06:45 | |
The size of the tides | 0:06:49 | 0:06:50 | |
depends on the distance between the Earth and the Moon. | 0:06:50 | 0:06:53 | |
The laws of physics are very clear about this. | 0:06:59 | 0:07:03 | |
The closer two things are, the more they attract each other, | 0:07:03 | 0:07:07 | |
the greater the gravitational force. | 0:07:07 | 0:07:10 | |
So we get the tides we do because the Moon is where it is, nearly a quarter of a million miles away. | 0:07:10 | 0:07:17 | |
But what if the Moon were closer? | 0:07:17 | 0:07:20 | |
If the Moon were a just a little closer than it is today | 0:07:22 | 0:07:27 | |
the tidal bulge would grow. | 0:07:27 | 0:07:30 | |
Low tides would be lower, | 0:07:31 | 0:07:33 | |
high tides would be higher. | 0:07:33 | 0:07:35 | |
And any low-lying coastline would be flooded. | 0:07:35 | 0:07:41 | |
But what if the Moon were much closer? | 0:07:41 | 0:07:44 | |
Five times, 10 times, 20 times closer than it is today. | 0:07:44 | 0:07:50 | |
How would that affect the tides and life here on Earth? | 0:07:50 | 0:07:54 | |
Another rush hour in London. | 0:08:00 | 0:08:03 | |
But this evening, as the sun sets, | 0:08:03 | 0:08:06 | |
a huge Moon rises,... | 0:08:06 | 0:08:09 | |
..20 times closer than normal. | 0:08:11 | 0:08:14 | |
This super-sized Moon exerts a super-sized gravitational force,... | 0:08:21 | 0:08:27 | |
..400 times stronger than we're used to. | 0:08:29 | 0:08:32 | |
And it creates a mighty tidal bulge. | 0:08:34 | 0:08:38 | |
Sea water pours across the British Isles, | 0:08:41 | 0:08:45 | |
London is flooded. | 0:08:46 | 0:08:49 | |
Hours later, the same tidal bulge hits the east coast of America. | 0:08:56 | 0:09:00 | |
And the story is the same. | 0:09:01 | 0:09:04 | |
It's New York's turn to disappear underwater. | 0:09:06 | 0:09:09 | |
A city submerged,... | 0:09:12 | 0:09:15 | |
..and all the work of the Moon. | 0:09:17 | 0:09:19 | |
Eventually, of course, the tide subsides. | 0:09:29 | 0:09:32 | |
And the waters retreat. | 0:09:34 | 0:09:37 | |
This scenario may seem rather far-fetched, like the plot of some disaster movie. | 0:09:44 | 0:09:51 | |
But something similar has happened. | 0:09:51 | 0:09:54 | |
Once upon a time, when the Moon was newly formed, | 0:09:54 | 0:09:58 | |
it really was so close, and it really was so powerful. | 0:09:58 | 0:10:03 | |
Let me take you back to the earliest days of our planet, | 0:10:05 | 0:10:10 | |
4.5 billion years ago. | 0:10:10 | 0:10:13 | |
At this time, the Earth had no Moon, | 0:10:15 | 0:10:18 | |
it was orbiting the Sun alone | 0:10:18 | 0:10:21 | |
and it was being assaulted by rocks and comets. | 0:10:21 | 0:10:24 | |
Today, there are no scars left from this cosmic pinball. | 0:10:29 | 0:10:34 | |
But to get a sense of the damage that was done, | 0:10:34 | 0:10:38 | |
I've come to the Arizona Desert,... | 0:10:38 | 0:10:41 | |
..to a great hole in the ground. | 0:10:43 | 0:10:46 | |
This is a beautiful crater, | 0:10:47 | 0:10:50 | |
a near perfect circle a mile in diameter. | 0:10:50 | 0:10:54 | |
It was formed when a meteorite crashed into the Earth a mere 50,000 years ago. | 0:10:54 | 0:10:59 | |
That's nothing on the timescale we're talking about, | 0:10:59 | 0:11:02 | |
but it's amazing how much damage that one passing rock can cause. | 0:11:02 | 0:11:06 | |
The early Earth was bombarded with rocks. It must have been mayhem. | 0:11:06 | 0:11:11 | |
And then along came something much, much bigger. | 0:11:11 | 0:11:15 | |
Another planet the size of Mars, drifted into the path of Earth. | 0:11:16 | 0:11:21 | |
It was on a collision course. | 0:11:23 | 0:11:25 | |
It hit the young Earth with a glancing blow. | 0:11:30 | 0:11:33 | |
Imagine the power released by such a collision. | 0:11:33 | 0:11:36 | |
The impact sent a mass of liquid rock into orbit. | 0:11:40 | 0:11:44 | |
This debris coalesced into a ball. | 0:11:48 | 0:11:52 | |
And the Moon was formed, | 0:11:55 | 0:11:58 | |
just 14,000 miles away from the early Earth. | 0:11:58 | 0:12:02 | |
This was the closest point it could have been. | 0:12:04 | 0:12:09 | |
Any closer, and gravity would have pulled the debris crashing back to Earth, | 0:12:10 | 0:12:16 | |
and our moon wouldn't exist. | 0:12:16 | 0:12:18 | |
Today the Moon is just a rock reflecting the sun's light, | 0:12:22 | 0:12:26 | |
but back then it was a molten sphere, burning brightly. | 0:12:26 | 0:12:31 | |
It must have looked amazing, an enormous orange disc in the sky. | 0:12:31 | 0:12:37 | |
Imagine the scene. | 0:12:39 | 0:12:42 | |
The first moonrise over the early Earth. | 0:12:42 | 0:12:46 | |
Our world was no longer alone. | 0:12:48 | 0:12:51 | |
It had a huge, powerful neighbour. | 0:12:51 | 0:12:54 | |
And ever since, this has been a very different type of planet. | 0:13:01 | 0:13:06 | |
The collision that created the Moon reset the basic chemistry of Earth. | 0:13:11 | 0:13:16 | |
And Earth Mk II was a place on which life could begin. | 0:13:19 | 0:13:25 | |
The collision released huge quantities of metal from the Earth's core, | 0:13:26 | 0:13:32 | |
one particular metal that would help change the atmosphere of our planet. | 0:13:32 | 0:13:38 | |
I'm talking about iron. | 0:13:41 | 0:13:44 | |
Iron is incredibly reactive. | 0:13:46 | 0:13:48 | |
Leave some out in the garden and it will rust. | 0:13:48 | 0:13:51 | |
It also combines with other chemicals to release gases | 0:13:51 | 0:13:54 | |
such as methane, carbon monoxide and hydrogen. | 0:13:54 | 0:13:57 | |
Today we see these gases as toxic and rather unpleasant. | 0:13:57 | 0:14:03 | |
But in the early Earth this was the very stuff of life. | 0:14:03 | 0:14:07 | |
In the 1950s, American chemist Stanley Miller did a classic experiment. | 0:14:11 | 0:14:19 | |
He took a cocktail of these gases and tried to simulate conditions on the early Earth, | 0:14:20 | 0:14:25 | |
adding electricity to mimic the power of lightning. | 0:14:26 | 0:14:31 | |
And what emerged, to everyone's surprise, was a flask of slime, | 0:14:32 | 0:14:38 | |
which turned out to be full of amino acids. | 0:14:38 | 0:14:42 | |
Like iron, amino acids are essential for life. | 0:14:44 | 0:14:48 | |
They are the raw material from which proteins are made. | 0:14:48 | 0:14:52 | |
And this great chemist was able to produce them using gases that were available on the early Earth. | 0:14:52 | 0:14:59 | |
The collision that formed the Moon helped set the scene for life to begin. | 0:15:00 | 0:15:06 | |
But there was still a way to go. | 0:15:08 | 0:15:10 | |
Life didn't start immediately after the collision. | 0:15:13 | 0:15:18 | |
It took up to 700 million years for the first living cells to emerge. | 0:15:18 | 0:15:24 | |
During this time, the Earth was cooling down. | 0:15:32 | 0:15:36 | |
It formed a rocky surface, water vapour condensed to form oceans. | 0:15:36 | 0:15:42 | |
And these oceans were being tugged by the Moon. | 0:15:45 | 0:15:49 | |
They were becoming tidal. | 0:15:51 | 0:15:53 | |
According to the latest theory from one leading chemist, | 0:15:55 | 0:15:59 | |
these early tides may have been the trigger | 0:15:59 | 0:16:03 | |
that kick-started life into action. | 0:16:03 | 0:16:06 | |
This seems like a very odd place to do some chemistry. | 0:16:09 | 0:16:12 | |
-Why are we here? -On the beach? | 0:16:12 | 0:16:14 | |
To investigate the effect of tides on chemistry taking place on the very early Earth, billions of years ago. | 0:16:14 | 0:16:21 | |
'Professor John Sutherland believes the ebb and flow of the tides | 0:16:21 | 0:16:24 | |
'may have played a crucial role in the origin of life. | 0:16:24 | 0:16:27 | |
'And he's going to show me how it could have happened. | 0:16:27 | 0:16:30 | |
We have to do some chemistry here. | 0:16:30 | 0:16:32 | |
'He's mixing up the sort of basic chemicals found in the first oceans and adding water. | 0:16:32 | 0:16:38 | |
'He's reproducing a tidal pool in his flask.' | 0:16:38 | 0:16:42 | |
And that's your starting tidal pool at high tide. | 0:16:42 | 0:16:46 | |
Then the tide goes out, the sun shines on the pool and starts drying it out. | 0:16:46 | 0:16:50 | |
And rather than wait for that to happen here, because that would take | 0:16:50 | 0:16:54 | |
a long time, I'm going to speed it up by using a burner here. | 0:16:54 | 0:16:57 | |
So what are we trying to mimic? | 0:16:57 | 0:16:58 | |
We're trying to mimic here the,... | 0:16:58 | 0:17:00 | |
the power of the Moon in chemistry on Earth. | 0:17:00 | 0:17:03 | |
So the Moon is responsible for the tides, the tides are filling these | 0:17:03 | 0:17:06 | |
ponds up and then, when the tide goes down, the sun shines, dries it up. | 0:17:06 | 0:17:11 | |
It's an inexorable process of wetting and drying and warming | 0:17:11 | 0:17:16 | |
and that is driven by the Moon. | 0:17:16 | 0:17:19 | |
Having created a soup of chemicals, washed and dried them, there's still one thing missing. | 0:17:20 | 0:17:27 | |
I'm going to now transfer this into | 0:17:27 | 0:17:30 | |
this other reaction vessel. | 0:17:30 | 0:17:32 | |
He exposes the chemicals to a blue lamp | 0:17:32 | 0:17:37 | |
that radiates ultraviolet energy | 0:17:37 | 0:17:41 | |
simulating the sun's light shining on the early Earth. | 0:17:41 | 0:17:45 | |
And as a result, he's changing the very structure of the chemicals,... | 0:17:47 | 0:17:53 | |
..creating, as if from nothing, elements of RNA, ribonucleic acid, | 0:17:54 | 0:18:02 | |
an essential component of all living cells. | 0:18:02 | 0:18:05 | |
So we are, in this setup, making some of the building blocks of life? | 0:18:07 | 0:18:12 | |
Yes! Just from simple tidal conditions and simple organic chemistry. | 0:18:12 | 0:18:17 | |
-But it's all driven by the Moon? -It's ultimately all driven by the Moon. | 0:18:17 | 0:18:21 | |
Life on Earth driven by the Moon. | 0:18:21 | 0:18:23 | |
140 years ago, Charles Darwin wrote a letter to a friend suggesting that | 0:18:28 | 0:18:33 | |
life probably began in what he called a "warm little pond". | 0:18:33 | 0:18:39 | |
At the time, it was mere speculation. | 0:18:39 | 0:18:41 | |
But now we think he might be right. | 0:18:41 | 0:18:43 | |
These tidal pools represent Darwin's warm little ponds. | 0:18:43 | 0:18:47 | |
Primordial chemistry labs where the raw materials of life can come together. | 0:18:50 | 0:18:55 | |
And all beautifully orchestrated by the tidal power of the Moon. | 0:18:55 | 0:19:00 | |
Once the first creatures had emerged in the oceans 3.8 billion years ago, | 0:19:02 | 0:19:08 | |
evolution was in full flow. | 0:19:08 | 0:19:11 | |
And ever since, the Moon has continued watching over us,... | 0:19:13 | 0:19:17 | |
..casting a protective veil. | 0:19:20 | 0:19:23 | |
When I was a teenager, I wanted a telescope so badly, | 0:19:25 | 0:19:30 | |
mainly to look at the Moon, but I couldn't afford a decent one, | 0:19:30 | 0:19:34 | |
so at the age of 14, I went to an evening class and I learnt to make my own. | 0:19:34 | 0:19:39 | |
Now my telescope worked on a similar principle to this one, using a mirror to reflect the light. | 0:19:39 | 0:19:46 | |
It took months to grind and polish those mirrors, but it was so worth it. | 0:19:46 | 0:19:51 | |
I remember the first night when I pointed the telescope up at the Moon | 0:19:51 | 0:19:54 | |
and I could see the craters in amazing detail. | 0:19:54 | 0:19:57 | |
And the first thing you notice is you're always looking at the same craters. | 0:20:03 | 0:20:10 | |
This is because the Moon spins very slowly, one rotation every 29 days, | 0:20:10 | 0:20:17 | |
and that's exactly the same speed as the Moon orbits the Earth. | 0:20:17 | 0:20:21 | |
So as the Moon travels around us, it's always showing us the same face. | 0:20:21 | 0:20:26 | |
So we never see the far side, or the so-called dark side of the Moon. | 0:20:26 | 0:20:30 | |
If we could, we'd see that it's riddled with craters. | 0:20:35 | 0:20:40 | |
In fact, we now know there are more craters on the far side of the Moon than the nearside | 0:20:40 | 0:20:46 | |
which is bit of a relief | 0:20:46 | 0:20:48 | |
because each of them was formed by an asteroid impact | 0:20:48 | 0:20:52 | |
that could otherwise have crashed into Earth | 0:20:52 | 0:20:55 | |
and stopped life in its tracks. | 0:20:55 | 0:20:57 | |
The Moon, which helped start life, may also have preserved it. | 0:21:01 | 0:21:06 | |
Our guardian angel. | 0:21:06 | 0:21:08 | |
This idea, that the Moon looks after us, is ancient. | 0:21:14 | 0:21:19 | |
5,000 years ago, people on the Outer Hebrides shaped these rocks into megaliths | 0:21:21 | 0:21:28 | |
and placed them in a great circle. | 0:21:28 | 0:21:32 | |
They didn't have metal tools, | 0:21:33 | 0:21:37 | |
let alone cranes. | 0:21:37 | 0:21:40 | |
It was a remarkable thing to do. | 0:21:40 | 0:21:42 | |
It's been suggested that they were building a sort of observatory | 0:21:42 | 0:21:47 | |
to mark a rare lunar event. | 0:21:47 | 0:21:50 | |
Every 18.5 years, the Moon drops in the sky for a couple of weeks, and barely makes it above the horizon. | 0:21:52 | 0:22:00 | |
It's known as a lunar standstill and it last happened in 2006, and it won't happen again until 2024. | 0:22:00 | 0:22:07 | |
Bizarrely, the people who built Callanish | 0:22:07 | 0:22:10 | |
probably knew about the lunar standstill | 0:22:10 | 0:22:12 | |
and they aligned their stones to witness it. | 0:22:12 | 0:22:14 | |
From this angle you can see the Moon rise above those hills over there and drop between those stones. | 0:22:16 | 0:22:24 | |
It must look spectacular. | 0:22:24 | 0:22:27 | |
To line up the stones accurately, | 0:22:29 | 0:22:32 | |
they could only check their position every 18.5 years, | 0:22:32 | 0:22:35 | |
at the next lunar standstill. | 0:22:35 | 0:22:38 | |
It seems incredibly complex, so why do it? | 0:22:39 | 0:22:44 | |
Across the ancient world, people revered the Moon | 0:22:47 | 0:22:51 | |
and made up stories about the mysterious power of this disc in the night sky. | 0:22:51 | 0:22:57 | |
Some stories have survived the test of time. | 0:23:01 | 0:23:06 | |
Think of the classic werewolf movie. | 0:23:06 | 0:23:09 | |
MAN SHOUTS, CREATURE GROWLS | 0:23:09 | 0:23:12 | |
It's all about the strange, terrible magic of the Moon. | 0:23:13 | 0:23:17 | |
Even today, it is often said that the full Moon casts a spell over us. | 0:23:23 | 0:23:29 | |
# I see a bad moon rising... # | 0:23:29 | 0:23:32 | |
It sends us a bit crazy. | 0:23:32 | 0:23:35 | |
It's Friday night and I'm out with the police. | 0:23:35 | 0:23:39 | |
It's always a busy time with people partying in clubs and bars. | 0:23:39 | 0:23:43 | |
But tonight is also a full Moon. | 0:23:43 | 0:23:45 | |
Does that make any difference? | 0:23:45 | 0:23:47 | |
Over the years, there have been many studies. | 0:23:52 | 0:23:55 | |
Some claim to show a link between the crime rate and a full Moon. | 0:23:55 | 0:24:00 | |
They suggest that people become wilder and more violent when the Moon is full. | 0:24:00 | 0:24:06 | |
It's called the Transylvania Effect. | 0:24:06 | 0:24:09 | |
One police force in the south of England | 0:24:12 | 0:24:14 | |
was so convinced, they put extra officers on the beat at a full Moon, | 0:24:14 | 0:24:18 | |
just in case. | 0:24:18 | 0:24:21 | |
But is it true? Does the Moon really change our behaviour? | 0:24:23 | 0:24:27 | |
Well, sadly, I don't think so. | 0:24:30 | 0:24:33 | |
For every study claiming an effect, there are many more dismissing it. | 0:24:33 | 0:24:37 | |
The theory probably stems from the fact that when the Moon is full, the sky is much, much brighter. | 0:24:37 | 0:24:43 | |
In the past, before electric lights, people were more likely to go out on a bright night, | 0:24:44 | 0:24:51 | |
so there was more chance for trouble. | 0:24:51 | 0:24:54 | |
These days, alcohol is surely a far more important factor | 0:24:54 | 0:24:58 | |
than the light of a full Moon. | 0:24:58 | 0:25:00 | |
But even if the Transylvania Effect is a bit of a myth, | 0:25:02 | 0:25:07 | |
the Moon is still very powerful. | 0:25:07 | 0:25:10 | |
There are many animals which react instinctively to the light of the full Moon. | 0:25:12 | 0:25:18 | |
They become more active, more vocal, | 0:25:18 | 0:25:22 | |
more fertile. | 0:25:22 | 0:25:24 | |
Most remarkable of all are these tropical corals. | 0:25:26 | 0:25:31 | |
Every year they synchronise their reproductive cycle, | 0:25:38 | 0:25:43 | |
so on one night they all spawn together. | 0:25:43 | 0:25:46 | |
And for these corals, it's triggered by the full Moon. | 0:25:48 | 0:25:53 | |
The Sargasso Sea, off the coast of Bermuda. | 0:26:05 | 0:26:08 | |
Marine biologist Dr Anne Cohen is studying how the Moon affects the growth of corals. | 0:26:11 | 0:26:18 | |
She's looking for a species known as Diploria strigosa, | 0:26:22 | 0:26:26 | |
the brain coral. | 0:26:26 | 0:26:28 | |
Every 29 days, on a full Moon, | 0:26:31 | 0:26:34 | |
brain corals grow a new layer of skeleton on top of the old. | 0:26:34 | 0:26:40 | |
This growth spurt is dictated by the monthly orbit of the Moon. | 0:26:40 | 0:26:45 | |
It's like clockwork. | 0:26:45 | 0:26:47 | |
And the skeletal layers can be used as a lunar calendar,... | 0:26:49 | 0:26:53 | |
..a record of time passing. | 0:26:54 | 0:26:57 | |
So, this is the coral that we pulled out of the water today. | 0:27:04 | 0:27:09 | |
And if we look under the microscope, | 0:27:09 | 0:27:11 | |
you can see very fine ridges | 0:27:11 | 0:27:16 | |
and we know that these are formed on the lunar cycle, these are monthly bands. | 0:27:16 | 0:27:20 | |
-So it's a bit like the rings of a tree, you can use that to date it. -That's right. | 0:27:20 | 0:27:25 | |
And we can count about 65 monthly bands in this coral, | 0:27:25 | 0:27:31 | |
which makes it just over five years old. | 0:27:31 | 0:27:34 | |
That's pretty amazing! | 0:27:34 | 0:27:36 | |
'But some corals are even more revealing. | 0:27:36 | 0:27:39 | |
'They allow us to peer into the distant past | 0:27:39 | 0:27:43 | |
'and find out something extraordinary about the power of the Moon. | 0:27:43 | 0:27:49 | |
'This is a fossil coral from the Devonian era. | 0:27:49 | 0:27:53 | |
'It's 400 million years old | 0:27:53 | 0:27:57 | |
'but still beautifully preserved. | 0:27:57 | 0:28:01 | |
'As well as monthly growth bands, there are annual bands | 0:28:01 | 0:28:06 | |
'and even daily bands, a quarter of a millimetre apart.' | 0:28:06 | 0:28:12 | |
So this coral grew about a quarter of a millimetre every day 400 million years ago. | 0:28:12 | 0:28:18 | |
400 million years ago. | 0:28:18 | 0:28:20 | |
And if we took the time to count up all these daily growth bands, | 0:28:20 | 0:28:25 | |
within the year we'd find... | 0:28:25 | 0:28:30 | |
not 365 days | 0:28:30 | 0:28:33 | |
but in fact in this coral there are 400 bands every year. | 0:28:33 | 0:28:39 | |
400 days a year. | 0:28:39 | 0:28:41 | |
-400 bands? -Per year. | 0:28:41 | 0:28:43 | |
-So that means that there were an extra 35 days every year? -That's right. | 0:28:43 | 0:28:48 | |
That's quite mind-boggling. | 0:28:48 | 0:28:50 | |
'If there were really 400 days in the year back then, how long was each day?' | 0:28:50 | 0:28:57 | |
If you do the sums, and take the total number of hours in a year | 0:28:59 | 0:29:04 | |
and divide by 400 days, then you come to the conclusion | 0:29:04 | 0:29:07 | |
that in the Devonian period, when this fossil was alive, | 0:29:07 | 0:29:12 | |
a day actually lasted 21 hours and 55 minutes. | 0:29:12 | 0:29:17 | |
Now I must admit I find that really weird. | 0:29:17 | 0:29:20 | |
The fact that in the past, a day wasn't 24 hours. | 0:29:20 | 0:29:24 | |
The length of a day is simply the time it takes for the Earth to spin once | 0:29:26 | 0:29:32 | |
and go from one sunrise to the next. | 0:29:32 | 0:29:36 | |
If, in the past, days were shorter, | 0:29:39 | 0:29:41 | |
then the Earth must have been spinning faster. | 0:29:41 | 0:29:45 | |
In fact, back in time, back billions of years, | 0:29:47 | 0:29:51 | |
the planet was spinning so fast | 0:29:51 | 0:29:54 | |
that each day lasted just five hours. | 0:29:54 | 0:29:57 | |
But why should the spin of the Earth have changed over time? | 0:29:59 | 0:30:03 | |
Because of the Moon. | 0:30:03 | 0:30:05 | |
When the Moon formed, it was so close to the Earth, | 0:30:08 | 0:30:12 | |
and pulling so hard that it acted as a brake on our planet. | 0:30:12 | 0:30:18 | |
The gravitational pull of the Moon was slowing the Earth's spin | 0:30:18 | 0:30:23 | |
and it's still doing so. | 0:30:23 | 0:30:25 | |
As the Earth spins, | 0:30:25 | 0:30:28 | |
the effect of friction between the ocean bulge and ocean floor | 0:30:28 | 0:30:32 | |
causes the Earth's spin to slow down. | 0:30:32 | 0:30:35 | |
It means days have been getting longer. | 0:30:36 | 0:30:39 | |
What was once was five hours now lasts 24. | 0:30:41 | 0:30:45 | |
We humans have been around for such a short time, | 0:30:47 | 0:30:50 | |
about 200,000 years, | 0:30:50 | 0:30:53 | |
that we've only ever known 24 hour days. | 0:30:53 | 0:30:56 | |
Our body clocks are completely geared for that length of day. | 0:30:56 | 0:31:00 | |
And yet, we only have 24-hour days because of the Moon. | 0:31:00 | 0:31:05 | |
It's amazing to think that the very rhythms of our planet | 0:31:07 | 0:31:10 | |
have been set by this ball of rock out in space. | 0:31:10 | 0:31:15 | |
But what about the Moon itself? | 0:31:16 | 0:31:19 | |
How has it been affected by the spin of the Earth? | 0:31:19 | 0:31:22 | |
One of the first things you learn in physics is that for every action | 0:31:25 | 0:31:29 | |
there is an equal and opposite reaction. | 0:31:29 | 0:31:34 | |
As the Earth has been slowing down all these years, | 0:31:34 | 0:31:37 | |
something else has been accelerating, | 0:31:37 | 0:31:39 | |
and that's the Moon. | 0:31:39 | 0:31:43 | |
And to compensate for its acceleration, | 0:31:43 | 0:31:45 | |
something's been happening to its orbit at the same time. | 0:31:45 | 0:31:49 | |
Imagine the centre of this roundabout is the Earth, and I'm the Moon in orbit. | 0:31:49 | 0:31:54 | |
As we speed up, I get slung outwards, | 0:31:54 | 0:31:57 | |
and I feel as if my body wants to move into a wider orbit. | 0:31:57 | 0:32:00 | |
And that, more or less, | 0:32:02 | 0:32:04 | |
is what's been happening to the Moon. | 0:32:04 | 0:32:06 | |
To balance out its acceleration, it's been spiralling outwards, | 0:32:09 | 0:32:14 | |
into a wider and wider orbit. | 0:32:14 | 0:32:16 | |
But is it still spiralling away? | 0:32:18 | 0:32:22 | |
Or has it stopped? | 0:32:22 | 0:32:23 | |
There's one way to find out. | 0:32:26 | 0:32:28 | |
Apache Point Observatory in New Mexico... | 0:32:36 | 0:32:39 | |
..one of America's largest telescopes. | 0:32:41 | 0:32:45 | |
It's also one of the last outposts of the Apollo programme. | 0:32:45 | 0:32:51 | |
Besides having a lot of fun on the Moon, | 0:32:54 | 0:32:58 | |
the Apollo astronauts were running a series of scientific experiments. | 0:32:58 | 0:33:03 | |
And on three of the missions they left behind retro-reflector units, | 0:33:06 | 0:33:11 | |
packed with small mirrors. | 0:33:11 | 0:33:13 | |
This one is from Apollo 15. | 0:33:15 | 0:33:17 | |
And ever since, astronomers have been firing lasers at them | 0:33:22 | 0:33:27 | |
to keep track of exactly how far away the Moon is. | 0:33:27 | 0:33:32 | |
So once we're all centred up on Apollo 15, | 0:33:32 | 0:33:36 | |
I can open the shutter and we're ready to shine the laser. | 0:33:36 | 0:33:40 | |
Dr Russet McMillan carries out the laser ranging at Apache Point. | 0:33:40 | 0:33:45 | |
So you're now sending pulses of laser-light out towards the Moon. | 0:33:48 | 0:33:51 | |
That's right, they're going to travel to the Moon, | 0:33:51 | 0:33:54 | |
get reflected, come back, and get detected by our detector. | 0:33:54 | 0:33:57 | |
So how much of the light do we actually get back? | 0:33:57 | 0:34:00 | |
Well, we're sending out about 100 quadrillion photons with each pulse. | 0:34:00 | 0:34:07 | |
If we're lucky, for each pulse we might get back one photon. | 0:34:07 | 0:34:10 | |
One photon back? | 0:34:10 | 0:34:12 | |
One photon out of 100 quadrillion going out. | 0:34:12 | 0:34:17 | |
A photon is a tiny particle of light and 100 quadrillion is... | 0:34:17 | 0:34:24 | |
a phenomenally large number! | 0:34:24 | 0:34:28 | |
But by capturing just a few photons, | 0:34:28 | 0:34:31 | |
it's possible to measure | 0:34:31 | 0:34:33 | |
the distance between the Earth and the Moon | 0:34:33 | 0:34:35 | |
down to the last millimetre. | 0:34:35 | 0:34:37 | |
As of right now, the distance to the Moon | 0:34:44 | 0:34:48 | |
is 393,499km, | 0:34:48 | 0:34:53 | |
257m and 798mm... | 0:34:53 | 0:34:58 | |
precisely. | 0:34:58 | 0:35:00 | |
Astronomers have been using lasers to measure the Moon's distance for nearly 40 years now. | 0:35:02 | 0:35:08 | |
And what they're finding amongst all those photons is a very clear pattern. | 0:35:08 | 0:35:14 | |
The Moon, which has been drifting away from us for billions of years, | 0:35:14 | 0:35:18 | |
is still drifting, | 0:35:18 | 0:35:20 | |
at a speed of 3.78 cm a year. | 0:35:20 | 0:35:24 | |
In human terms, | 0:35:24 | 0:35:25 | |
that's about the same speed that our fingernails grow! | 0:35:25 | 0:35:29 | |
Does it matter that the Moon is drifting away from us? | 0:35:30 | 0:35:35 | |
Well, for one thing, | 0:35:36 | 0:35:38 | |
if it keeps going, we'll lose a great natural wonder. | 0:35:38 | 0:35:44 | |
One of the benefits of astronomy is you get to stay up very late. | 0:35:48 | 0:35:53 | |
And if you don't go to bed at all, you can catch the Moon setting | 0:35:57 | 0:36:02 | |
while the sun rises. | 0:36:02 | 0:36:04 | |
What an amazing sight. | 0:36:09 | 0:36:12 | |
There the rising sun, and opposite the setting Moon. | 0:36:12 | 0:36:17 | |
They both look exactly the same size, | 0:36:17 | 0:36:19 | |
but that's an optical illusion. | 0:36:19 | 0:36:21 | |
Let's take these two balls. | 0:36:23 | 0:36:25 | |
The golf ball is much smaller than the tennis ball | 0:36:25 | 0:36:28 | |
and you can tell that when they are side by side. | 0:36:28 | 0:36:30 | |
But if I move the golf ball towards you, | 0:36:30 | 0:36:32 | |
you can see it's getting bigger and at this point, | 0:36:32 | 0:36:35 | |
they look to be the same size. | 0:36:35 | 0:36:39 | |
Now, it's exactly the same with the Sun and the Moon. | 0:36:39 | 0:36:42 | |
The Moon is actually 400 times smaller than the Sun. | 0:36:42 | 0:36:45 | |
But it's also 400 times closer, | 0:36:45 | 0:36:48 | |
and so they appear to be the same size. | 0:36:48 | 0:36:52 | |
And that's what gives us the most mesmerising sight, | 0:36:52 | 0:36:58 | |
a total eclipse. | 0:36:58 | 0:37:00 | |
Because the Moon's disc is the same size as the Sun's, | 0:37:02 | 0:37:06 | |
they line up perfectly, | 0:37:06 | 0:37:09 | |
with just a halo of solar gases spilling out around the rim. | 0:37:09 | 0:37:16 | |
I always thought there must be some astronomical reason for this, | 0:37:21 | 0:37:24 | |
something in the physics to make it so. | 0:37:24 | 0:37:27 | |
But no, it's just a cosmic coincidence. | 0:37:27 | 0:37:32 | |
It happens because right now, | 0:37:33 | 0:37:36 | |
the Moon is just the right distance from Earth. | 0:37:36 | 0:37:40 | |
But in the future, as the Moon keeps drifting away, | 0:37:40 | 0:37:45 | |
its disc will be too small to cover the sun | 0:37:45 | 0:37:49 | |
and we'll lose the magic of the total eclipse. | 0:37:49 | 0:37:53 | |
And then what? | 0:37:55 | 0:37:57 | |
As the Moon moves away from us, how will life change here on Earth? | 0:37:57 | 0:38:01 | |
New York City. | 0:38:14 | 0:38:17 | |
The sun went down an hour ago, | 0:38:17 | 0:38:20 | |
and the Moon is rising. | 0:38:20 | 0:38:22 | |
It may look familiar enough | 0:38:24 | 0:38:26 | |
but this Moon is smaller than normal in the night sky. | 0:38:26 | 0:38:31 | |
That's because it's further away. | 0:38:31 | 0:38:34 | |
Not much, an extra 10%, | 0:38:34 | 0:38:38 | |
just 24,000 miles. | 0:38:38 | 0:38:41 | |
But that makes a big difference. | 0:38:41 | 0:38:44 | |
The spin of the Earth has slowed down | 0:38:46 | 0:38:50 | |
and days are getting longer. | 0:38:50 | 0:38:53 | |
The sun will not rise here for another 20 hours. | 0:38:53 | 0:38:58 | |
The entire Western hemisphere has to endure a very long night. | 0:39:01 | 0:39:07 | |
While on the other side of the world, | 0:39:07 | 0:39:10 | |
there's an extra-long day. | 0:39:10 | 0:39:12 | |
But things get worse. | 0:39:14 | 0:39:16 | |
If the Moon were to really move by that 10%, | 0:39:16 | 0:39:19 | |
then the very stability of the planet would be threatened. | 0:39:19 | 0:39:23 | |
You see, the Moon, | 0:39:26 | 0:39:28 | |
which controls our tides and the spin of the earth | 0:39:28 | 0:39:31 | |
serves another critical function. | 0:39:31 | 0:39:33 | |
It keeps us stable. | 0:39:33 | 0:39:37 | |
To understand why, meet hoop wizard Jack Ryan. | 0:39:37 | 0:39:43 | |
As Jack runs rings around me, look how he keeps that ball spinning. | 0:39:45 | 0:39:50 | |
-Jack, what's the secret? -Speed. | 0:39:50 | 0:39:52 | |
You got to keep it fast, it's got to be going fast. | 0:39:52 | 0:39:56 | |
-Would you like to try? -I'd love to. What do I do? | 0:39:56 | 0:39:59 | |
Just stay still. Let me see your finger. | 0:39:59 | 0:40:01 | |
There you go. | 0:40:03 | 0:40:04 | |
So the ball is just like planet Earth. | 0:40:04 | 0:40:08 | |
The faster it spins, the more stable it is. | 0:40:08 | 0:40:10 | |
-But what happens if it slows down? -Let's see. | 0:40:10 | 0:40:13 | |
That's lots of wobble and, ooh, I lose control. | 0:40:14 | 0:40:19 | |
So that's just like the Earth - | 0:40:19 | 0:40:20 | |
when it's spinning very fast, it's very stable, but as it slows down, | 0:40:20 | 0:40:25 | |
it loses stability and starts to wobble like crazy. | 0:40:25 | 0:40:28 | |
Ever since the great collision that formed the Moon, | 0:40:30 | 0:40:35 | |
the Earth has been tilted, | 0:40:35 | 0:40:37 | |
spinning at 23 degrees. | 0:40:37 | 0:40:39 | |
This tilt has played a crucial role in shaping our climate. | 0:40:43 | 0:40:49 | |
If the Earth wasn't tilted, if it were upright, | 0:40:49 | 0:40:53 | |
then the sun's light would shine evenly over the surface throughout the year. | 0:40:53 | 0:40:58 | |
Always overhead at the equator, | 0:40:58 | 0:41:00 | |
and barely reaching the North and South poles. | 0:41:00 | 0:41:03 | |
The temperature would be constant throughout the year, | 0:41:03 | 0:41:06 | |
there'd be no summer or winter. | 0:41:06 | 0:41:08 | |
No variation at all. | 0:41:08 | 0:41:10 | |
But because of that 23 degrees tilt, | 0:41:10 | 0:41:14 | |
the light hitting the Earth's surface varies throughout the year. | 0:41:14 | 0:41:18 | |
It's this variety of light that's so important. | 0:41:20 | 0:41:24 | |
It means that throughout the year, | 0:41:24 | 0:41:26 | |
conditions on the planet are always changing. | 0:41:26 | 0:41:30 | |
In our summer, the light favours the northern hemisphere, | 0:41:32 | 0:41:35 | |
giving us warmer temperatures and longer days. | 0:41:35 | 0:41:38 | |
But six months later, | 0:41:38 | 0:41:40 | |
as the Earth travels to the other side of the sun, | 0:41:40 | 0:41:43 | |
the light now favours the southern hemisphere, | 0:41:43 | 0:41:46 | |
leaving us in the cold and dark with shorter days and longer nights. | 0:41:46 | 0:41:51 | |
In other words, we have seasons. | 0:41:51 | 0:41:55 | |
The life cycle of so many animals and plants | 0:41:57 | 0:42:02 | |
is driven by the beat of the seasons. | 0:42:02 | 0:42:05 | |
A burst of life in spring. | 0:42:06 | 0:42:09 | |
Balmy days of summer. | 0:42:09 | 0:42:13 | |
Migration in autumn. | 0:42:13 | 0:42:16 | |
A fight for survival in winter. | 0:42:16 | 0:42:19 | |
But the Earth only stays at this 23 degree tilt | 0:42:21 | 0:42:24 | |
because of the Moon's stabilising effect. | 0:42:24 | 0:42:28 | |
As the Moon keeps drifting away, the angle of the tilt will change. | 0:42:30 | 0:42:35 | |
And over time, the Earth will wobble. | 0:42:36 | 0:42:41 | |
And what will happen then? | 0:42:41 | 0:42:44 | |
It's possible we'll go the same way as Mars. | 0:42:44 | 0:42:47 | |
Mars - our planetary neighbour. | 0:42:49 | 0:42:52 | |
Today, it spins at an angle of 25 degrees, | 0:42:52 | 0:42:56 | |
very similar to Earth. | 0:42:56 | 0:42:58 | |
But it used to spin at a very different angle, | 0:42:58 | 0:43:02 | |
anything up 60 degrees. | 0:43:02 | 0:43:04 | |
You see, unlike Earth, | 0:43:07 | 0:43:10 | |
Mars has no large moon to keep it stable | 0:43:10 | 0:43:14 | |
so it wobbles chaotically. | 0:43:14 | 0:43:17 | |
It could almost tip over onto its side. | 0:43:17 | 0:43:21 | |
We may suffer the same fate if our Moon moved just that 10% further away. | 0:43:23 | 0:43:28 | |
It makes me wonder what would our world be like? | 0:43:28 | 0:43:33 | |
Probably very wet. | 0:43:33 | 0:43:35 | |
If the Earth tipped over and spun on its side, | 0:43:38 | 0:43:42 | |
then for three months of every year the poles would be exposed | 0:43:42 | 0:43:48 | |
to direct unrelenting sunshine. | 0:43:48 | 0:43:51 | |
Pretty quickly, the ice caps would melt. | 0:43:51 | 0:43:54 | |
And a huge amount of fresh water would flood the world's oceans. | 0:43:56 | 0:44:01 | |
Sea levels would rise by more than 60 metres. | 0:44:01 | 0:44:05 | |
Every coastal city in the world would be gone. | 0:44:05 | 0:44:10 | |
And inland areas that survived would be transformed. | 0:44:11 | 0:44:15 | |
Las Vegas is dark | 0:44:18 | 0:44:20 | |
and very cold. | 0:44:20 | 0:44:23 | |
It's minus 20. | 0:44:23 | 0:44:25 | |
Because the sun is pointing at Antarctica, | 0:44:27 | 0:44:31 | |
Vegas is in the grip of a freezing winter. | 0:44:31 | 0:44:34 | |
But in the spring, the snow melts, | 0:44:38 | 0:44:42 | |
the sun rises higher and higher in the sky. | 0:44:42 | 0:44:45 | |
Over the summer, the sun never sets. | 0:44:47 | 0:44:50 | |
In autumn, it's high in the sky. | 0:44:51 | 0:44:54 | |
And then it drops below the horizon again. | 0:44:55 | 0:44:58 | |
And the freezing winter returns. | 0:45:01 | 0:45:04 | |
Could we survive? | 0:45:05 | 0:45:07 | |
Probably, with enough air conditioning and artificial light. | 0:45:07 | 0:45:12 | |
But what of other life forms? | 0:45:15 | 0:45:19 | |
Dr Lynn Rothschild is an astro-biologist working for NASA. | 0:45:21 | 0:45:26 | |
Death Valley is the hottest place in North America. | 0:45:26 | 0:45:30 | |
And it turns out that as the Moon recedes from the Earth, | 0:45:30 | 0:45:33 | |
as it goes away, | 0:45:33 | 0:45:34 | |
there are going to be times that the Earth | 0:45:34 | 0:45:37 | |
tips over further on its side, | 0:45:37 | 0:45:39 | |
and what's going to happen then is that there are going to be | 0:45:39 | 0:45:42 | |
parts of the Earth that become excruciatingly hot in the summer, | 0:45:42 | 0:45:46 | |
much hotter than Death Valley is today. | 0:45:46 | 0:45:48 | |
And in the winter these same places are going to be bitterly cold, | 0:45:50 | 0:45:54 | |
much colder than your freezer. | 0:45:54 | 0:45:56 | |
There are organisms that can survive at reasonably low temperatures, | 0:45:59 | 0:46:03 | |
think of penguins and whales, and so on. | 0:46:03 | 0:46:07 | |
But high temperature is extremely tricky. | 0:46:07 | 0:46:10 | |
When you get up at about 70 degrees centigrade which is hot, | 0:46:10 | 0:46:14 | |
but it's nowhere near the boiling temperature of water, chlorophyll breaks down | 0:46:14 | 0:46:18 | |
so all the greenery you see around you would be gone. | 0:46:18 | 0:46:20 | |
So that means no photosynthesis? | 0:46:20 | 0:46:22 | |
Absolutely, so no photosynthesis, and that's what drives life on Earth today, photosynthesis. | 0:46:22 | 0:46:27 | |
Now, as you go up even beyond that, | 0:46:27 | 0:46:30 | |
your nucleic acids end up breaking and unravelling, | 0:46:30 | 0:46:33 | |
and this is your very genetic material. | 0:46:33 | 0:46:35 | |
So, clearly, you cannot survive without these. | 0:46:35 | 0:46:37 | |
There are some microbes with a very unusual genetic structure | 0:46:39 | 0:46:43 | |
which can live in deep-sea vents and geysers | 0:46:43 | 0:46:47 | |
at temperatures over 100 degrees. | 0:46:47 | 0:46:50 | |
But they can't cope anywhere cooler. | 0:46:50 | 0:46:54 | |
And that's the problem. | 0:46:54 | 0:46:57 | |
If the Earth tips over, | 0:46:57 | 0:47:00 | |
the seasonal shifts will be too fast and too extreme | 0:47:00 | 0:47:05 | |
for evolution to keep pace. | 0:47:05 | 0:47:07 | |
Even though there are a few organisms that can adapt to living in | 0:47:09 | 0:47:13 | |
excruciatingly hot temperatures, | 0:47:13 | 0:47:16 | |
and there are plenty of organisms that can live in very cold temperatures, | 0:47:16 | 0:47:20 | |
much colder than your freezer at home, | 0:47:20 | 0:47:22 | |
to have the same organism being able to shift between these extremes | 0:47:22 | 0:47:25 | |
during the course of a single year is nearly impossible. | 0:47:25 | 0:47:29 | |
And I suspect we're never going to evolve one that could do that. | 0:47:29 | 0:47:34 | |
Let us be clear, | 0:47:34 | 0:47:36 | |
we are in no immediate danger. | 0:47:36 | 0:47:38 | |
It will take at least a billion years | 0:47:38 | 0:47:41 | |
for the Moon to drift far enough away for the Earth to tip over. | 0:47:41 | 0:47:45 | |
So we have a little time to prepare. | 0:47:45 | 0:47:48 | |
But all this speculation makes me realise how lucky we are | 0:47:48 | 0:47:53 | |
the Moon is where it is right now. | 0:47:53 | 0:47:55 | |
A tiny shift and life on Earth could be so different. | 0:47:55 | 0:48:00 | |
And what about life beyond Earth? | 0:48:03 | 0:48:07 | |
Are we alone? | 0:48:07 | 0:48:10 | |
Or are there other planets with lifeforms similar to ours? | 0:48:11 | 0:48:17 | |
These radio telescopes are scanning the heavens, looking for any clues. | 0:48:20 | 0:48:28 | |
But where do we look? | 0:48:28 | 0:48:30 | |
Even our own galaxy has 100 billion stars | 0:48:30 | 0:48:34 | |
and each one of those stars has who knows how many planets in orbit. | 0:48:34 | 0:48:39 | |
I reckon, given what we now know about the Moon, | 0:48:39 | 0:48:41 | |
how it's influenced life here on Earth, | 0:48:41 | 0:48:44 | |
we should focus any future searches on planets with moons like ours. | 0:48:44 | 0:48:49 | |
There are many moons in the solar system | 0:48:52 | 0:48:55 | |
but they're not like ours. | 0:48:55 | 0:48:57 | |
The moons of Jupiter are too small and far away | 0:48:57 | 0:49:02 | |
to influence their planet. | 0:49:02 | 0:49:04 | |
The same is true for the moons of Saturn, Neptune and Uranus. | 0:49:06 | 0:49:11 | |
Only our moon is big enough and close enough to affect us, | 0:49:12 | 0:49:18 | |
but not so big to make life here unbearable. | 0:49:18 | 0:49:21 | |
It's not too big and it's not too small. | 0:49:24 | 0:49:29 | |
Like Goldilocks and the porridge, it's just right. | 0:49:29 | 0:49:33 | |
One day, I'm confident we'll find other planets with moons like ours. | 0:49:36 | 0:49:42 | |
But will we ever visit them? | 0:49:42 | 0:49:45 | |
Will we ever boldly go out into space? | 0:49:45 | 0:49:49 | |
If so, then the Moon has a big role to play. | 0:49:50 | 0:49:54 | |
So far, only 12 people have ever been there. | 0:49:58 | 0:50:02 | |
And they brought back a very precious cargo. | 0:50:02 | 0:50:06 | |
'That's 20 pounds of rock!' | 0:50:08 | 0:50:10 | |
382kg of lunar rock. | 0:50:11 | 0:50:16 | |
'Oh, Tony, it's got some beautiful crystals in it! | 0:50:16 | 0:50:19 | |
'Good show.' | 0:50:19 | 0:50:21 | |
When geologists analysed these rocks, they learnt a great deal | 0:50:25 | 0:50:30 | |
about the composition of the Moon, | 0:50:30 | 0:50:33 | |
and the history of the solar system. | 0:50:33 | 0:50:36 | |
But they didn't find what they were looking for - | 0:50:36 | 0:50:39 | |
any sign of water. | 0:50:39 | 0:50:42 | |
The Moon, they declared, was bone dry. | 0:50:45 | 0:50:48 | |
But now, they're changing their minds. | 0:50:53 | 0:50:57 | |
The Moon rocks are stored in a clean room | 0:51:03 | 0:51:06 | |
at NASA's Johnson Space Centre in Houston. | 0:51:06 | 0:51:10 | |
Dr Gary Lofgren has the job of keeping them pristine, | 0:51:12 | 0:51:17 | |
as if they were still on the lunar surface. | 0:51:17 | 0:51:22 | |
So this is it, this is a piece of Moon rock? | 0:51:22 | 0:51:25 | |
Yes, this is a piece of lava from Apollo 17. | 0:51:25 | 0:51:28 | |
For me, this is a fantastic moment because I've always dreamed of | 0:51:28 | 0:51:31 | |
going to the Moon, and so to be this close to a piece of Moon rock, | 0:51:31 | 0:51:35 | |
this is brilliant. | 0:51:35 | 0:51:36 | |
This is spectacular. If you look, you can see all the shiny crystals reflecting back at you. | 0:51:36 | 0:51:41 | |
They're all very fresh. That's one of the unique things about Moon rocks. | 0:51:41 | 0:51:47 | |
I was expecting it to be quite dull, but it looks so shiny. | 0:51:47 | 0:51:50 | |
Yeah, shiny it is, it's because there's no water there to alter and weather the minerals. | 0:51:50 | 0:51:56 | |
-So no reactions? -There's no reactions going on, that's right. | 0:51:56 | 0:51:59 | |
So that gave us the idea the Moon was very dry, very inert. | 0:51:59 | 0:52:03 | |
And we thought that for 40 years, but within the last few years, | 0:52:03 | 0:52:07 | |
we discovered that there is a lot of water on the Moon, in fact. | 0:52:07 | 0:52:11 | |
-It's water that's trapped. Because it's cold, it's frozen as ice. -Yes. | 0:52:11 | 0:52:15 | |
Recently, | 0:52:18 | 0:52:19 | |
probes have analysed some of the darkest craters on the Moon, | 0:52:19 | 0:52:23 | |
at the lunar poles, | 0:52:23 | 0:52:25 | |
and have found that they're packed with ice - | 0:52:25 | 0:52:28 | |
frozen water that has come from comets crashing into the Moon over time. | 0:52:28 | 0:52:34 | |
It now seems there's at least 400 billion litres of water | 0:52:36 | 0:52:41 | |
in these craters. | 0:52:41 | 0:52:43 | |
Having water on the moon opens up a whole area of possibilities. | 0:52:43 | 0:52:47 | |
Oh, yes, it allows humans to survive. | 0:52:47 | 0:52:49 | |
We need water to drink and water to survive up there. | 0:52:49 | 0:52:52 | |
But just as importantly we can use that water | 0:52:52 | 0:52:54 | |
to make rocket fuel, because rocket fuel is gaseous hydrogen and oxygen, | 0:52:54 | 0:52:59 | |
and we can make that on the Moon. | 0:52:59 | 0:53:01 | |
The Saturn V rockets | 0:53:04 | 0:53:05 | |
used by Apollo | 0:53:05 | 0:53:07 | |
burnt 2,500 tonnes of rocket fuel to escape Earth's gravity | 0:53:07 | 0:53:13 | |
and get into space. | 0:53:13 | 0:53:15 | |
But if we could produce fuel from lunar water, | 0:53:20 | 0:53:24 | |
that would make all the difference. | 0:53:24 | 0:53:27 | |
It would be far more efficient to travel into deep space | 0:53:29 | 0:53:33 | |
by launching rockets from the Moon, not the Earth. | 0:53:33 | 0:53:37 | |
Perhaps, one day, | 0:53:40 | 0:53:43 | |
the Moon will become a springboard for exploring the solar system. | 0:53:43 | 0:53:47 | |
Spaceships will make the short hop from Earth and then re-fuel here | 0:53:50 | 0:53:54 | |
before setting off on the long journey ahead. | 0:53:54 | 0:53:57 | |
But if this seems a bit too futuristic, | 0:54:01 | 0:54:05 | |
then one man has more immediate plans for the Moon. | 0:54:05 | 0:54:09 | |
For 30 years, space scientist Dr David Criswell has had a dream - | 0:54:12 | 0:54:17 | |
to put thousands of solar panels on the Moon | 0:54:17 | 0:54:22 | |
and harness the energy of the Sun. | 0:54:22 | 0:54:25 | |
We can have solar panels on Earth, why take them to the Moon? | 0:54:25 | 0:54:28 | |
You want to take them to the Moon | 0:54:28 | 0:54:30 | |
because the sunlight on the Moon is absolutely predictable. | 0:54:30 | 0:54:33 | |
There's no air, there's no water, there's no mechanical vibrations, | 0:54:33 | 0:54:36 | |
so you don't have to build massive facilities like this. | 0:54:36 | 0:54:39 | |
On the Moon, you could replace these with solar arrays that are the thickness of tissue paper. | 0:54:39 | 0:54:45 | |
The plan is to build thin solar panels along the rim of the Moon | 0:54:47 | 0:54:53 | |
so they get almost constant sunlight. | 0:54:53 | 0:54:55 | |
The electricity would then be transmitted back to Earth using microwaves. | 0:54:55 | 0:55:01 | |
He believes he can produce enough energy to meet global demand. | 0:55:02 | 0:55:06 | |
The Moon receives 13,000 terawatts of power, | 0:55:08 | 0:55:12 | |
solar power that's going to waste. | 0:55:12 | 0:55:15 | |
By going to the Moon, we can collect that power at the cheapest cost | 0:55:15 | 0:55:18 | |
and send it back here to Earth. | 0:55:18 | 0:55:19 | |
He's hoping to create an unlimited supply of energy | 0:55:22 | 0:55:27 | |
with the least environmental impact. | 0:55:27 | 0:55:29 | |
You see, the plan is to make everything on the Moon itself | 0:55:32 | 0:55:36 | |
from what's already there on the lunar surface. | 0:55:36 | 0:55:39 | |
When you look at the Moon, basically what you see is dust. | 0:55:39 | 0:55:44 | |
It's very, very finely ground-up rock and glass. You can make it into fibreglass, | 0:55:45 | 0:55:52 | |
you can make into containers, you can make into rods and tubes and all of that sort of stuff. | 0:55:52 | 0:55:57 | |
You make it sound so straightforward, so why aren't we doing it? | 0:56:00 | 0:56:04 | |
Well, you've got to be on the Moon, we've got to go back to the Moon. | 0:56:04 | 0:56:07 | |
Somehow we've lost the will to do this commitment, | 0:56:07 | 0:56:12 | |
going back to the Moon and making it a permanent stay, rather than just a short visit. | 0:56:12 | 0:56:17 | |
Now, this grand scheme would cost at least half a trillion dollars. | 0:56:18 | 0:56:23 | |
But that's less than oil companies spend every two years | 0:56:25 | 0:56:30 | |
getting oil and gas out of the ground. | 0:56:30 | 0:56:32 | |
There's nothing to stop us building solar-powered bases | 0:56:33 | 0:56:39 | |
on the Moon right now. | 0:56:39 | 0:56:41 | |
And I, for one, can't wait for the day. | 0:56:41 | 0:56:44 | |
For a few years during the age of Apollo, | 0:56:50 | 0:56:54 | |
we were all mad about the Moon. | 0:56:54 | 0:56:57 | |
It was fun, | 0:57:02 | 0:57:04 | |
it was exciting, and for me at least, | 0:57:04 | 0:57:09 | |
it was love at first sight. | 0:57:09 | 0:57:11 | |
But then, all too quickly, we lost interest in the Moon. | 0:57:24 | 0:57:29 | |
We moved on. | 0:57:29 | 0:57:32 | |
I think that was a mistake. | 0:57:33 | 0:57:36 | |
The Moon is far more important | 0:57:36 | 0:57:39 | |
and far more useful than we ever realised. | 0:57:39 | 0:57:43 | |
For billions of years, it's gazed down on us... | 0:57:45 | 0:57:49 | |
..shaping and changing | 0:57:51 | 0:57:53 | |
the course of life here on Earth. | 0:57:53 | 0:57:56 | |
In so many ways, the Moon has been the making of us. | 0:57:56 | 0:58:02 | |
Surely, it's time to re-think our relationship with the Moon, | 0:58:03 | 0:58:08 | |
to stop taking it for granted, | 0:58:08 | 0:58:10 | |
to fall in love again. | 0:58:10 | 0:58:12 | |
Do we really need the Moon? | 0:58:12 | 0:58:14 | |
Of course we do. | 0:58:14 | 0:58:16 | |
Subtitles by Red Bee Media Ltd | 0:58:30 | 0:58:33 |