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Tonight is one of the most spectacular meteor showers | 0:00:02 | 0:00:04 | |
-of the year, the Perseids. -If it's clear, despite the moon, | 0:00:04 | 0:00:07 | |
you should be able to see a number of shooting stars streaking across | 0:00:07 | 0:00:10 | |
the night sky. And just think about this - | 0:00:10 | 0:00:13 | |
every time one vaporises in the atmosphere, | 0:00:13 | 0:00:16 | |
a small part of that meteor can fall to Earth as dust. | 0:00:16 | 0:00:19 | |
In fact, this all adds to the 40,000 tonnes of space debris and dust | 0:00:19 | 0:00:24 | |
that falls onto our planet every year. 40,000 tonnes! | 0:00:24 | 0:00:29 | |
And so tonight, from here at the Norman Lockyer Observatory in Devon, | 0:00:29 | 0:00:33 | |
we're going to investigate the strange stuff | 0:00:33 | 0:00:35 | |
that comes from outer space. | 0:00:35 | 0:00:38 | |
Just think about that 40,000 tonnes for a moment. | 0:01:04 | 0:01:08 | |
That means around 50 times more stuff falls from the sky every year | 0:01:08 | 0:01:13 | |
than fell from the cliff in this landslide | 0:01:13 | 0:01:15 | |
just down the road in Sidmouth. | 0:01:15 | 0:01:17 | |
That sounds alarming, but most of this space debris is nothing more | 0:01:19 | 0:01:23 | |
than dust, tiny particles that waft gently through the atmosphere, | 0:01:23 | 0:01:28 | |
each no larger than a sand grain. | 0:01:28 | 0:01:30 | |
Slightly larger particles burn up on the way in, | 0:01:30 | 0:01:33 | |
producing spectacular shooting stars, or meteors. | 0:01:33 | 0:01:38 | |
Tonight we'll find out how Earth's history has been shaped by | 0:01:38 | 0:01:42 | |
this space debris in surprising ways, | 0:01:42 | 0:01:45 | |
and how some of it can be found on every rooftop in the land. | 0:01:45 | 0:01:49 | |
One of the remarkable things about cosmic dust is, these tiny little | 0:01:49 | 0:01:53 | |
particles have the same composition as the solar system as a whole. | 0:01:53 | 0:01:58 | |
We'll see how scientists are working to make sure that we're prepared for | 0:01:58 | 0:02:02 | |
the threat of a rogue meteorite hitting the Earth. | 0:02:02 | 0:02:05 | |
Pete explains the best ways to see the Perseids, | 0:02:07 | 0:02:09 | |
and he meets an astronomer who's found a way to see these meteors | 0:02:09 | 0:02:13 | |
in the daytime. | 0:02:13 | 0:02:15 | |
Fortunately, large objects that make it down to the ground, | 0:02:17 | 0:02:20 | |
meteorites, are pretty rare. | 0:02:20 | 0:02:22 | |
There've only been a few recorded falls in British history. | 0:02:22 | 0:02:25 | |
But smaller objects are falling around us all the time, | 0:02:25 | 0:02:29 | |
bringing with them new and surprising information | 0:02:29 | 0:02:32 | |
about our solar system's past. | 0:02:32 | 0:02:35 | |
These are micrometeorites. | 0:02:35 | 0:02:37 | |
Nothing more than cosmic dust. | 0:02:37 | 0:02:39 | |
And this stuff is all around us all the time, in the air, | 0:02:39 | 0:02:42 | |
settling onto the ground, landing in our gardens and on our roads. | 0:02:42 | 0:02:47 | |
In search of this valuable dust, | 0:02:49 | 0:02:51 | |
Maggie climbed up onto the roof here at the Norman Lockyer Observatory | 0:02:51 | 0:02:55 | |
along with micrometeorite expert Matt Genge. | 0:02:55 | 0:02:59 | |
Matt, I do have to ask, what are we doing up here on the roof? | 0:02:59 | 0:03:02 | |
Well, we are up here to look for something quite incredible. | 0:03:02 | 0:03:05 | |
We're looking for cosmic dust. | 0:03:05 | 0:03:07 | |
And usually, I have to go to the Antarctic, | 0:03:07 | 0:03:11 | |
but we've actually discovered that because it falls all the time | 0:03:11 | 0:03:15 | |
everywhere, about one particle per square metre, | 0:03:15 | 0:03:18 | |
that roofs like this are perfect | 0:03:18 | 0:03:21 | |
little collection plates for cosmic dust, because they fall on the roof | 0:03:21 | 0:03:26 | |
and then they get concentrated by the rains in gutters. | 0:03:26 | 0:03:30 | |
-So should we see if you can find some? -We'll give it a go. | 0:03:30 | 0:03:33 | |
So there's a nice little gutter here. | 0:03:36 | 0:03:39 | |
-This is going to be highly technical. -Right, OK. | 0:03:40 | 0:03:42 | |
So I'm going to start off by using a spoon. | 0:03:42 | 0:03:45 | |
So it just looks like the sort of things you do find in the gutter. | 0:03:47 | 0:03:50 | |
Yeah, it's nothing special. A lot of it is going to be algae. | 0:03:50 | 0:03:52 | |
-Ah, yes. -There's going to be a lot of terrestrial, wind-blown dust. | 0:03:52 | 0:03:57 | |
Some of that will be natural. So, for example, you end up with | 0:03:57 | 0:04:01 | |
dust from the Sahara on the roofs in the UK. | 0:04:01 | 0:04:05 | |
But a lot of it's also going to be artificial. | 0:04:05 | 0:04:07 | |
So how will you be able to identify the cosmic dust out of all these | 0:04:07 | 0:04:11 | |
-different materials? -Well, the cosmic dust is heated as it comes | 0:04:11 | 0:04:15 | |
through the atmosphere, so it burns up as it comes through... | 0:04:15 | 0:04:18 | |
Like a shooting star. It sort of burns up in the atmosphere. | 0:04:18 | 0:04:20 | |
Absolutely. And they end up as tiny little magma droplets. | 0:04:20 | 0:04:24 | |
So they're perfect little spheres, | 0:04:24 | 0:04:26 | |
so we're going to be looking for that shape. | 0:04:26 | 0:04:28 | |
But more importantly, they contain magnetic minerals. | 0:04:28 | 0:04:32 | |
And that means we can use a magnet | 0:04:32 | 0:04:34 | |
to separate them from all the terrestrial debris. | 0:04:34 | 0:04:37 | |
-Fantastic. Well, let's get started. -Yep. | 0:04:37 | 0:04:42 | |
We'll return to Matt's experiment later when he's had time to process | 0:04:42 | 0:04:46 | |
his potential cosmic dust. | 0:04:46 | 0:04:48 | |
Meanwhile, more on the highlight of this week's night sky, the Perseids. | 0:04:55 | 0:05:01 | |
And Pete's here to show you how to get the most out of this glorious | 0:05:01 | 0:05:04 | |
meteor shower, and how to see it even in the daytime. | 0:05:04 | 0:05:07 | |
The Perseid meteor shower is one of the astronomical highlights | 0:05:09 | 0:05:12 | |
of the year. Activity starts about mid July, but reaches its peak | 0:05:12 | 0:05:16 | |
on the nights around the 12th, 13th of August. | 0:05:16 | 0:05:20 | |
This year we've got a bit of a moon, | 0:05:20 | 0:05:22 | |
which is going to mess up some of the display, and it'll knock out | 0:05:22 | 0:05:25 | |
some of the fainter meteors. | 0:05:25 | 0:05:27 | |
But if you go outside and it's nice and clear, | 0:05:27 | 0:05:29 | |
you should still be able to see the brighter ones - | 0:05:29 | 0:05:32 | |
and they can be pretty magnificent. | 0:05:32 | 0:05:33 | |
The Perseids all appear to emanate from a small area which starts south | 0:05:35 | 0:05:40 | |
of the constellation Cassiopeia | 0:05:40 | 0:05:42 | |
and shifts eastward over a few weeks into Camelopardalis. | 0:05:42 | 0:05:46 | |
Make sure you're in darkness for at least 20 to 30 minutes so your eyes | 0:05:49 | 0:05:53 | |
can properly dark adapt. Now, if you intend to use a torch, | 0:05:53 | 0:05:56 | |
a good tip is to use some red gel over it so that it looks red and it | 0:05:56 | 0:06:00 | |
doesn't destroy your dark adaption. | 0:06:00 | 0:06:02 | |
The best time to view is after 1:00am BST, | 0:06:02 | 0:06:06 | |
because after that time, the Earth will have turned, | 0:06:06 | 0:06:09 | |
so we're hitting the meteors head on, | 0:06:09 | 0:06:11 | |
the energy of impact is increased, and the meteors appear brighter. | 0:06:11 | 0:06:15 | |
The Perseids are actually the remnants of Comet 109P/Swift-Tuttle. | 0:06:17 | 0:06:22 | |
Each flash is caused by a tiny piece of rock called a meteoroid, | 0:06:22 | 0:06:26 | |
typically between the size of a grain of sand | 0:06:26 | 0:06:29 | |
up to about the size of a golf ball. | 0:06:29 | 0:06:31 | |
A meteoroid trail is actually the site of some interesting science, | 0:06:32 | 0:06:36 | |
because a meteoroid doesn't burn up in the atmosphere, it vaporises. | 0:06:36 | 0:06:41 | |
Now, as the meteoroid passes through the atmosphere, | 0:06:41 | 0:06:43 | |
it compresses the air ahead of it, and that creates a huge amount | 0:06:43 | 0:06:47 | |
of heat, which vaporises the front surface of the meteoroid. | 0:06:47 | 0:06:51 | |
You can see how this happens with this glass piston. | 0:06:51 | 0:06:55 | |
There's a little bit of lint in the bottom and the piston is sealed. | 0:06:55 | 0:06:59 | |
When I press the plunger down... | 0:06:59 | 0:07:01 | |
..we get a flame. | 0:07:03 | 0:07:05 | |
By compressing the air in the piston fast, | 0:07:05 | 0:07:08 | |
I've raised its temperature hundreds of degrees, | 0:07:08 | 0:07:11 | |
so hot that the lint spontaneously combusts. | 0:07:11 | 0:07:15 | |
As the meteor vaporises, | 0:07:18 | 0:07:20 | |
it sometimes leaves a trail of colour in its trail. | 0:07:20 | 0:07:24 | |
The colours depend on the make-up | 0:07:24 | 0:07:26 | |
of the meteoroid and the gases in the atmosphere. | 0:07:26 | 0:07:29 | |
Sometimes, when you get a really bright meteor trail streaking across | 0:07:32 | 0:07:35 | |
the sky, you get what looks like a smoke trail left behind it. | 0:07:35 | 0:07:39 | |
And that's known as the meteor train. | 0:07:39 | 0:07:41 | |
Now, it's not a smoke trail at all, it's a column of ionised gas. | 0:07:41 | 0:07:45 | |
And if it's there for long enough, | 0:07:45 | 0:07:47 | |
the high altitude atmospheric winds can blow it about. | 0:07:47 | 0:07:50 | |
So you can see it distort in the sky as you watch it. | 0:07:50 | 0:07:54 | |
There is another technique which can be used to see these incredible | 0:07:55 | 0:07:58 | |
events, a technique which amateurs can use to see hundreds more meteors | 0:07:58 | 0:08:03 | |
than they would normally, even during the day. | 0:08:03 | 0:08:06 | |
Amateur Mike Dennis is able to spot meteors from indoors. | 0:08:10 | 0:08:15 | |
He uses radio waves. | 0:08:17 | 0:08:19 | |
So this looks interesting. What's going on here? | 0:08:20 | 0:08:22 | |
-Well, we have a VHF signal that goes up into the sky. -Right. | 0:08:22 | 0:08:26 | |
And when a meteoroid enters the Earth atmosphere, | 0:08:26 | 0:08:30 | |
and as it's burning up, it generates an ionization | 0:08:30 | 0:08:34 | |
that we can reflect radio waves off of. | 0:08:34 | 0:08:37 | |
Right, OK. So you're detecting the trail left. | 0:08:37 | 0:08:40 | |
Yes. These are very short little pips. | 0:08:40 | 0:08:43 | |
So each one of these peaks is actually a meteor... | 0:08:43 | 0:08:45 | |
-Tiny specks of dust. You wouldn't see them visually. -Oh, there's one. | 0:08:45 | 0:08:48 | |
Oh, look at that! Yes! So that's, that's quite... | 0:08:48 | 0:08:51 | |
I guess you're going to say... You're going to bring me down now | 0:08:51 | 0:08:54 | |
-and say that's quite a small one. -That is quite a small one. | 0:08:54 | 0:08:56 | |
You wouldn't even see it, but that is a larger speck. About the size | 0:08:56 | 0:09:02 | |
of a grain of sand, probably even smaller. | 0:09:02 | 0:09:05 | |
That's a big one going off there. | 0:09:05 | 0:09:07 | |
Yeah. You can see now that this one was faster when it... | 0:09:07 | 0:09:10 | |
-Right. -Although it produced less energy, it actually came in faster. | 0:09:10 | 0:09:13 | |
OK. So when you get an event at night, | 0:09:13 | 0:09:15 | |
can you tie that up to what you see visually? | 0:09:15 | 0:09:18 | |
We certainly can, and I've got an example here. | 0:09:18 | 0:09:21 | |
And you can see, this is the meteor that's happening on this building. | 0:09:21 | 0:09:26 | |
That's first from our north camera, then from the east. | 0:09:26 | 0:09:29 | |
-And this is the radar screen event that happened. -Oh, I see. | 0:09:29 | 0:09:33 | |
This is the actual event that you just saw. | 0:09:33 | 0:09:36 | |
-This is another meteor that came after it. -OK. | 0:09:36 | 0:09:38 | |
So, with a shower like the Perseids, what would that actually look like? | 0:09:38 | 0:09:42 | |
The peak of the Perseids... This is last year's. | 0:09:42 | 0:09:46 | |
-Wow, OK. -It can get very, very busy. | 0:09:46 | 0:09:50 | |
So, if people wanted to set this up themselves, is it difficult to do? | 0:09:50 | 0:09:53 | |
To set this up as we've done it, it would be very difficult. | 0:09:53 | 0:09:57 | |
But if you just want to experiment with listening to meteors, | 0:09:57 | 0:10:02 | |
you can use even as something as simple as an FM broadcast radio, | 0:10:02 | 0:10:07 | |
during a busy meteor shower. | 0:10:07 | 0:10:09 | |
So long as there is an out of range radio station on that frequency, | 0:10:09 | 0:10:13 | |
when a meteor happens, | 0:10:13 | 0:10:15 | |
the radio wave will bounce off the meteor... | 0:10:15 | 0:10:17 | |
-Oh, right, OK. So you can hear it? -You'll hear for a brief moment, | 0:10:17 | 0:10:20 | |
you'll hear that for about half a second to a second. | 0:10:20 | 0:10:23 | |
-Sometimes longer. -That's actually brilliant because, I mean, | 0:10:23 | 0:10:27 | |
the thing which clobbers us all the time in the UK, of course, | 0:10:27 | 0:10:30 | |
is the cloud cover. So with that, | 0:10:30 | 0:10:31 | |
you can actually effectively hear a meteor shower throughout the day? | 0:10:31 | 0:10:36 | |
-Yes. -Fantastic! Well, thank you very much for your time. -Thank you. | 0:10:36 | 0:10:40 | |
We learn a lot about meteors from watching them in the sky. | 0:10:42 | 0:10:45 | |
But even more when they land on Earth. | 0:10:45 | 0:10:48 | |
Objects which do that are known not as meteors, but as meteorites. | 0:10:48 | 0:10:53 | |
Earlier this year, we had the chance to see one of the largest | 0:10:58 | 0:11:01 | |
collections of meteorites in the world. | 0:11:01 | 0:11:04 | |
Perhaps surprisingly, | 0:11:04 | 0:11:06 | |
that collection belongs to the Vatican Observatory. | 0:11:06 | 0:11:10 | |
Maggie saw some of the highlights guided by the collection's curator, | 0:11:10 | 0:11:14 | |
Brother Bob Macke. | 0:11:14 | 0:11:16 | |
So, Brother Macke, how big is the collection? | 0:11:16 | 0:11:19 | |
We have 1,200 specimens here, representing all of the different | 0:11:19 | 0:11:22 | |
meteorite types. The vast majority | 0:11:22 | 0:11:24 | |
of our collection are ordinary chondrites. | 0:11:24 | 0:11:28 | |
These form the majority of the meteorites that fall to the Earth. | 0:11:28 | 0:11:31 | |
These are primitive meteorites that are 1,000 million years old. | 0:11:31 | 0:11:35 | |
And so, they still contain tracers of the origin of our solar system. | 0:11:35 | 0:11:40 | |
They are older than any rock you'll find on the Earth. | 0:11:40 | 0:11:43 | |
This is an important historical sample right here. | 0:11:43 | 0:11:46 | |
This is a specimen of L'Aigle, which fell in 1803. | 0:11:46 | 0:11:51 | |
It fell in France. This was the first meteorite fall that was | 0:11:51 | 0:11:54 | |
well-documented by scientists of the era. | 0:11:54 | 0:11:58 | |
So, it represents the recognition among the scientific community | 0:11:58 | 0:12:04 | |
that meteorites actually are rocks that fall from space, | 0:12:04 | 0:12:07 | |
that they have an extra-terrestrial origin. | 0:12:07 | 0:12:09 | |
Oh, wow! And so you've got the chondrites, | 0:12:09 | 0:12:12 | |
these are the common chondrites, | 0:12:12 | 0:12:14 | |
-what other types do you have? -There are carbonaceous chondrites, | 0:12:14 | 0:12:17 | |
which are also very primitive | 0:12:17 | 0:12:19 | |
but formed in a different part of the solar system. This is a very | 0:12:19 | 0:12:23 | |
rare type of carbonaceous chondrite called Orgueil, | 0:12:23 | 0:12:27 | |
also fell in France in 1864. | 0:12:27 | 0:12:29 | |
And these have been very precisely dated | 0:12:29 | 0:12:32 | |
to 4.568 thousand million years in age. And this gives us the best | 0:12:32 | 0:12:38 | |
estimate we have for the age of our solar system. | 0:12:38 | 0:12:42 | |
This is an iron meteorite. | 0:12:42 | 0:12:45 | |
-Oh, yeah. -It is made of solid iron nickel. | 0:12:45 | 0:12:49 | |
You can see all the crystal structure. It's amazing. | 0:12:49 | 0:12:52 | |
Yes, it's called the Widmanstatten pattern. | 0:12:52 | 0:12:54 | |
And it's because there's two different alloys of iron and nickel, | 0:12:54 | 0:12:58 | |
one with a little more nickel, one with a little less nickel. | 0:12:58 | 0:13:00 | |
And they formed together. | 0:13:00 | 0:13:02 | |
-And they form this pattern. -Yes. Beautiful. | 0:13:02 | 0:13:06 | |
-What else have you got? -This is a specimen of Chelyabinsk. | 0:13:06 | 0:13:10 | |
-Oh! -Which fell over Russia in 2013. | 0:13:10 | 0:13:13 | |
When it exploded, it exploded into hundreds and hundreds of pieces. | 0:13:13 | 0:13:16 | |
So the original object would have been possibly perhaps as large as | 0:13:16 | 0:13:20 | |
this small room here. This closet. | 0:13:20 | 0:13:23 | |
So you have this amazing collection, what science do you do with them? | 0:13:23 | 0:13:26 | |
Here, we study meteorite physical properties - | 0:13:26 | 0:13:30 | |
density, porosity, which is the amount of pore space, | 0:13:30 | 0:13:32 | |
and heat capacity, which is the amount of energy it takes to change | 0:13:32 | 0:13:37 | |
the temperature of the meteorite. | 0:13:37 | 0:13:38 | |
It's a very important property for understanding the asteroids | 0:13:38 | 0:13:42 | |
that they came from, how they behave when they interact with each other | 0:13:42 | 0:13:46 | |
or interact with the sun. | 0:13:46 | 0:13:47 | |
For instance, an important effect is called the Yarkovsky effect, | 0:13:47 | 0:13:51 | |
which as the sunlight heats one side as that energy re-radiates, | 0:13:51 | 0:13:56 | |
as the asteroid rotates, | 0:13:56 | 0:13:58 | |
it can actually change the orbit, or the spin rate, of the asteroid. | 0:13:58 | 0:14:04 | |
Many people study that specific effect. But to understand it better, | 0:14:04 | 0:14:07 | |
they need to know what the heat capacity is. | 0:14:07 | 0:14:09 | |
-And that's what you measure here? -That's what we measure here. | 0:14:09 | 0:14:12 | |
Thank you. | 0:14:12 | 0:14:13 | |
Studying meteorites can tell us about the solar system. | 0:14:19 | 0:14:23 | |
But some scientists believe they can also tell us a lot about the Earth. | 0:14:24 | 0:14:28 | |
Scientists now believe that this steady rain of stuff from space | 0:14:30 | 0:14:34 | |
may have influenced our atmosphere, our geology and even our weather. | 0:14:34 | 0:14:38 | |
And possibly life itself. | 0:14:38 | 0:14:41 | |
Dr Penny Wozniakiewicz is at the heart of this new research into | 0:14:41 | 0:14:46 | |
the role larger meteorites have played in Earth's evolution. | 0:14:46 | 0:14:49 | |
Her team at the University of Kent have built a massive gun | 0:14:51 | 0:14:55 | |
and are using to model how meteorites could produce unique | 0:14:55 | 0:14:58 | |
compounds as they smash into the Earth itself. | 0:14:58 | 0:15:01 | |
So in the lab, we take an object that we know really well, | 0:15:07 | 0:15:09 | |
we accelerate it to high velocities | 0:15:09 | 0:15:11 | |
into any target that we are interested in. So, for example, | 0:15:11 | 0:15:14 | |
here we have an aluminium plate | 0:15:14 | 0:15:16 | |
that's been impacted by something only a few millimetres across. | 0:15:16 | 0:15:20 | |
-Wow! -But at 7km/s. And so you can see that | 0:15:20 | 0:15:23 | |
the impact crater that it's produced is much bigger. | 0:15:23 | 0:15:26 | |
And that's down to the sheer energy of the impact process. | 0:15:26 | 0:15:28 | |
It really does look like a crater. It looks like something you might | 0:15:28 | 0:15:31 | |
-see on the moon, with the rough edge to the crater there. -Yeah. | 0:15:31 | 0:15:34 | |
So what's going on with these impacts? What are the results? | 0:15:34 | 0:15:36 | |
After we impacted, we found that we had produced impact melt. | 0:15:36 | 0:15:40 | |
So, stuff that had solidified and, well, it quenched as a glass. | 0:15:40 | 0:15:44 | |
But we also found within that, | 0:15:44 | 0:15:45 | |
that we had crystals that seem to have kept the original composition, | 0:15:45 | 0:15:51 | |
but changed their structure. So their atomic form had changed under | 0:15:51 | 0:15:54 | |
-the pressure and temperature of the impact. -So these are quite profound, | 0:15:54 | 0:15:58 | |
detailed changes to the composition of these bodies. | 0:15:58 | 0:16:02 | |
Yeah, so you get the production of what we would see as exotic | 0:16:02 | 0:16:06 | |
materials during these impact events. | 0:16:06 | 0:16:08 | |
And so, if we think about what meteorites might bring to a planet, | 0:16:08 | 0:16:13 | |
particularly in the earlier days, it's not just about what's in the | 0:16:13 | 0:16:16 | |
-meteorite, it's about what can be produced when it hits. -Absolutely. | 0:16:16 | 0:16:18 | |
And there's been some very interesting research done recently | 0:16:18 | 0:16:21 | |
looking at whether you can actually produce more interesting organics. | 0:16:21 | 0:16:25 | |
So things that might be interesting for life. | 0:16:25 | 0:16:28 | |
-So, quite complex molecules? -Complex molecules, yes. | 0:16:28 | 0:16:30 | |
So, if that's the case, and these things happen on impact, we know | 0:16:30 | 0:16:34 | |
there was a time when Earth was hit by lots of these small bodies. | 0:16:34 | 0:16:37 | |
So could some of the stuff we see around us on Earth | 0:16:37 | 0:16:40 | |
-come from impacts? -Yeah, I think something could have been generated | 0:16:40 | 0:16:43 | |
by the impact event itself. | 0:16:43 | 0:16:45 | |
And some of it could have been brought by the impacting object. | 0:16:45 | 0:16:48 | |
It's a fascinating idea. Four billion years ago, | 0:16:49 | 0:16:53 | |
basic organic materials, the very stuff of life, | 0:16:53 | 0:16:57 | |
might have been created by the impacts of meteorites. | 0:16:57 | 0:17:01 | |
And those meteorites might have changed Earth's destiny | 0:17:01 | 0:17:04 | |
in other ways, too. | 0:17:04 | 0:17:06 | |
There are theories that some of the water on Earth actually accreted | 0:17:08 | 0:17:12 | |
as part of the original Earth. | 0:17:12 | 0:17:14 | |
Another thought is that water was also brought in at a later time | 0:17:14 | 0:17:18 | |
by comets and meteorites - sorry, asteroids. | 0:17:18 | 0:17:21 | |
You would have had to have had a lot of impacts, though, surely, | 0:17:21 | 0:17:24 | |
-to create enough water on the Earth. -Yeah, and there were a lot of | 0:17:24 | 0:17:28 | |
impacts in the early history of the solar system. So, yeah. | 0:17:28 | 0:17:32 | |
The water could've come from these objects. | 0:17:32 | 0:17:34 | |
So Earth's water might have come at least partly from asteroids | 0:17:34 | 0:17:37 | |
and comets. But what else might meteorites bring down to Earth? | 0:17:37 | 0:17:41 | |
So, meteorites can also bring things | 0:17:41 | 0:17:43 | |
like organics to the Earth's surface. So, a particular example | 0:17:43 | 0:17:46 | |
would be the carbonaceous-type chondrite meteorites. | 0:17:46 | 0:17:50 | |
These have quite a large proportion of organic materials within them. | 0:17:50 | 0:17:55 | |
A very notable example is the meteorite Murchison. | 0:17:55 | 0:17:57 | |
This one is often referred to as, if you smell it, you can smell | 0:17:57 | 0:18:01 | |
a solvent smell, because of the organics that it contains. | 0:18:01 | 0:18:04 | |
-You get smelly meteorites? -Smelly meteorites, yes. | 0:18:04 | 0:18:06 | |
And that's because of the complex chemistry that's inside? | 0:18:06 | 0:18:09 | |
Exactly. These can be a whole range of organic molecules within them. | 0:18:09 | 0:18:13 | |
So, including carboxylic acid, amino acids, amines, alcohol, sugars. | 0:18:13 | 0:18:18 | |
A whole range. So these are, I mean, you don't want to jump to this, | 0:18:18 | 0:18:21 | |
but they're the building blocks of life. | 0:18:21 | 0:18:23 | |
-They're the kind of things that biology uses. -Exactly, yeah. | 0:18:23 | 0:18:26 | |
They are the precursor chemistry that you need for life to thrive. | 0:18:26 | 0:18:31 | |
It's an amazing thought that the ingredients that produced life on | 0:18:31 | 0:18:34 | |
-Earth might have come from space. -Yeah. It's mind-blowing, really. | 0:18:34 | 0:18:37 | |
-It's fascinating stuff. -Yeah. -Thank you very much. -Thanks. | 0:18:37 | 0:18:41 | |
Meanwhile, in our makeshift laboratory, | 0:18:44 | 0:18:46 | |
Matt Genge has been preparing his sample from the rooftop. | 0:18:46 | 0:18:49 | |
Having dried it in an oven, | 0:18:51 | 0:18:53 | |
he sieves it and then passes a magnet over it, | 0:18:53 | 0:18:55 | |
pulling out anything magnetic. | 0:18:55 | 0:18:57 | |
He then places this material | 0:18:59 | 0:19:00 | |
on a slide and puts it into an electron microscope. | 0:19:00 | 0:19:04 | |
So we can see actually all these really dark things on here. | 0:19:06 | 0:19:10 | |
They're probably bits of algae with some windblown dust in. | 0:19:10 | 0:19:14 | |
What we're really interested in is the really bright stuff. | 0:19:14 | 0:19:17 | |
-Because that probably contains lots of iron. -There's one there. | 0:19:17 | 0:19:20 | |
But I guess that's a bit too irregular. | 0:19:20 | 0:19:22 | |
Yeah, this one's very angular. So, that's not melted. | 0:19:22 | 0:19:25 | |
I suspect if we look at some of these little bright spots. | 0:19:25 | 0:19:29 | |
Yeah. What's the probability of finding a cosmic particle? | 0:19:29 | 0:19:32 | |
-I'm afraid it's actually quite low. -So the odds are against us? | 0:19:32 | 0:19:34 | |
The odds are against us. But we will do our best. | 0:19:34 | 0:19:37 | |
-It does look as if we've got a few candidates. -There's a nice one here, | 0:19:37 | 0:19:40 | |
just below the middle. Let's try and get that one right into the middle. | 0:19:40 | 0:19:44 | |
And then I can increase the magnification. | 0:19:44 | 0:19:47 | |
-OK, so we are going up to sort of 150 times magnification now. -Yeah. | 0:19:47 | 0:19:50 | |
-200. -So, actually, it's not looking too bad. It's certainly... | 0:19:50 | 0:19:53 | |
Actually, it does look quite spherical. | 0:19:53 | 0:19:55 | |
It does look pretty spherical. | 0:19:55 | 0:19:56 | |
-Let's go right in. -OK, 1,000 times magnification now. | 0:19:56 | 0:20:00 | |
-This is amazing. -Actually, it's looking surprisingly good. | 0:20:00 | 0:20:04 | |
But it is a perfect little sphere. | 0:20:04 | 0:20:06 | |
-It is. Yeah, with sort of a small nodule on top. -Yeah. Actually, | 0:20:06 | 0:20:10 | |
the nodule's good, because many of the micrometeorites like this have | 0:20:10 | 0:20:13 | |
these little protrusions from the sides. | 0:20:13 | 0:20:16 | |
So... Actually, that's looking really good. | 0:20:16 | 0:20:18 | |
It's definitely a potential. We've got to be slightly careful because | 0:20:18 | 0:20:22 | |
there are molten droplets that we produce - artificial droplets. | 0:20:22 | 0:20:26 | |
So, how can we tell the difference? | 0:20:26 | 0:20:28 | |
Well, there's these wonderful little crystals on it. | 0:20:28 | 0:20:30 | |
Can you see these lines on the surface? | 0:20:30 | 0:20:33 | |
-Yes, like striations or something. -We called them dendrites. | 0:20:33 | 0:20:36 | |
And they tell us that this was molten. | 0:20:36 | 0:20:39 | |
So this was maybe a temperature of 1,500 degrees C. | 0:20:39 | 0:20:43 | |
And then cooled very rapidly. | 0:20:43 | 0:20:45 | |
And that's what happens to meteors during atmospheric entry. | 0:20:45 | 0:20:49 | |
-I see. -They burn up, and then they cool down really quickly. | 0:20:49 | 0:20:52 | |
So that all fits quite nicely. To be sure, though, | 0:20:52 | 0:20:55 | |
we'll do a chemical analysis on that. | 0:20:55 | 0:20:58 | |
-And we can do that...? -We can do that with this machine. | 0:20:58 | 0:21:01 | |
So what we're seeing here is there's lots of iron in the particle. | 0:21:01 | 0:21:06 | |
-Yes. -There's lots of oxygen over here. | 0:21:06 | 0:21:09 | |
So that means it's an iron oxide mineral. | 0:21:09 | 0:21:11 | |
There's some silicon and aluminium, but these particles tend to absorb | 0:21:11 | 0:21:15 | |
that when they're sitting around in all of this water and algae and... | 0:21:15 | 0:21:18 | |
-Yes, on the roof up there. -On the roof for a long time. | 0:21:18 | 0:21:22 | |
So, it's mainly iron oxide. And that's actually really good, | 0:21:22 | 0:21:25 | |
cos this isn't prepared at all, really. | 0:21:25 | 0:21:27 | |
It just comes straight off the roof, into an oven and then straight into | 0:21:27 | 0:21:30 | |
the microscope. So to have such an incredible image as this... | 0:21:30 | 0:21:34 | |
-It is. -..is actually really exciting. | 0:21:34 | 0:21:36 | |
I'm really quite sure that this... | 0:21:36 | 0:21:39 | |
This is a really good possible micrometeorite. | 0:21:39 | 0:21:42 | |
I'm 95% sure that this is a micrometeorite. | 0:21:42 | 0:21:46 | |
-And that's really against the odds. -It is really against the odds. | 0:21:46 | 0:21:49 | |
I am actually really excited by this. | 0:21:49 | 0:21:51 | |
Because I wasn't expecting to find anything on this roof at all. | 0:21:51 | 0:21:54 | |
Well, that's fantastic! So, what does this particle tell us | 0:21:54 | 0:21:57 | |
about the early solar system? | 0:21:57 | 0:21:59 | |
Grains like this, if this was one of those primordial grains, | 0:21:59 | 0:22:03 | |
they actually form in stars. | 0:22:03 | 0:22:06 | |
-Yes. -In the outflows from stars. | 0:22:06 | 0:22:08 | |
So we could be looking at, you know, a stellar dust particle | 0:22:08 | 0:22:13 | |
that has survived four and a half billion years | 0:22:13 | 0:22:16 | |
to be collected on a roof. | 0:22:16 | 0:22:18 | |
-In Devon. -In Devon. | 0:22:19 | 0:22:21 | |
Well, it's an amazing find and a wonderful story. | 0:22:21 | 0:22:24 | |
I wasn't expecting to see anything, so it's brilliant to find one. | 0:22:24 | 0:22:27 | |
It really is a remarkable find. | 0:22:30 | 0:22:32 | |
A genuine micrometeorite, possibly older than the solar system itself, | 0:22:32 | 0:22:37 | |
from the mud found on a rooftop. | 0:22:37 | 0:22:39 | |
And all the more amazing because of its size, | 0:22:41 | 0:22:43 | |
less than the width of a human hair. | 0:22:43 | 0:22:46 | |
Of course, space debris of this size is generally harmless. | 0:22:46 | 0:22:49 | |
It floats gently to the Earth. | 0:22:49 | 0:22:51 | |
But when the debris is larger, the outcome can be much more alarming. | 0:22:53 | 0:22:57 | |
To understand why, we need to think of the energy involved. | 0:23:00 | 0:23:04 | |
Your average Perseid is an object about this size | 0:23:04 | 0:23:07 | |
travelling at 30km/s - | 0:23:07 | 0:23:10 | |
far faster than a speeding bullet. | 0:23:10 | 0:23:12 | |
And if we scale it up to something the size of a brick, | 0:23:12 | 0:23:15 | |
when something this size hits the atmosphere, | 0:23:15 | 0:23:17 | |
it releases the equivalent of one tonne of TNT. | 0:23:17 | 0:23:21 | |
And many are much, much larger than bricks. | 0:23:23 | 0:23:26 | |
2013. A 300kg meteor explodes over Chelyabinsk in Russia. | 0:23:28 | 0:23:34 | |
The blast it produced was so powerful that it shattered windows | 0:23:35 | 0:23:39 | |
over several thousand square kilometres. | 0:23:39 | 0:23:42 | |
And there's plenty of evidence of even larger strikes, too. | 0:23:42 | 0:23:45 | |
In Siberia, trees were flattened for hundreds of square kilometres | 0:23:45 | 0:23:50 | |
after a meteor airburst in 1908. | 0:23:50 | 0:23:53 | |
This is the famous kilometre-wide | 0:23:53 | 0:23:55 | |
Barringer Meteorite Crater in Arizona. | 0:23:55 | 0:23:58 | |
And in the Yucatan Peninsula 66 million years ago, | 0:23:59 | 0:24:02 | |
scientists believed there was a super massive impact. | 0:24:02 | 0:24:06 | |
This radar image shows evidence of | 0:24:06 | 0:24:08 | |
a huge crater edge now buried deep underground. | 0:24:08 | 0:24:12 | |
This, of course, was the K-T impact. | 0:24:12 | 0:24:15 | |
The dinosaur killer. | 0:24:15 | 0:24:18 | |
Chris met asteroid expert Professor Alan Fitzsimmons | 0:24:18 | 0:24:21 | |
to gauge the real risks of a large meteorite impact. | 0:24:21 | 0:24:25 | |
How big a threat are asteroids to life on Earth? | 0:24:27 | 0:24:30 | |
Well, they're a threat, certainly. If we go back millions of years ago, | 0:24:30 | 0:24:35 | |
we know that mass extinctions | 0:24:35 | 0:24:36 | |
on Earth have been caused by asteroid impact, | 0:24:36 | 0:24:39 | |
and the famous one being the K-T impact, which helped at least | 0:24:39 | 0:24:42 | |
wipe out the dinosaurs. | 0:24:42 | 0:24:44 | |
So, how are we doing? Could there be a dinosaur killer out there? | 0:24:44 | 0:24:47 | |
Well, the good news is because the dinosaur killers, as we called them, | 0:24:47 | 0:24:50 | |
are so big, you're talking objects that are 10km across. | 0:24:50 | 0:24:54 | |
We can see those from a long way away and we believe | 0:24:54 | 0:24:58 | |
we've catalogued all of them. There are only a handful. | 0:24:58 | 0:25:00 | |
We know where they are. | 0:25:00 | 0:25:01 | |
They're not going to come anywhere near the Earth any time soon. | 0:25:01 | 0:25:04 | |
-OK, so any dinosaurs, they can relax. -They're fine. -Right. | 0:25:04 | 0:25:08 | |
-But we've seen you can get damaged from smaller objects. -Absolutely. | 0:25:08 | 0:25:11 | |
In fact, even if you go down to a 1km-diameter asteroid, | 0:25:11 | 0:25:14 | |
there's models that suggest that could still set off | 0:25:14 | 0:25:18 | |
significant casualties around the world | 0:25:18 | 0:25:20 | |
because of the environmental effects from the impact. | 0:25:20 | 0:25:22 | |
Up to perhaps 25% of the world's population dying from | 0:25:22 | 0:25:27 | |
starvation due to the failure of crops in farming around the world. | 0:25:27 | 0:25:31 | |
I hope the next line is, "I know where they all are." | 0:25:31 | 0:25:34 | |
We know where 90% of them are. | 0:25:34 | 0:25:37 | |
So we think there's roughly 1,000 of them, | 0:25:37 | 0:25:39 | |
and over 900 have been found. And, as the surveys continue, | 0:25:39 | 0:25:44 | |
we should sweep up most of the rest of those in the next | 0:25:44 | 0:25:47 | |
10 or 20 years. But we have a class of near-Earth asteroids we call | 0:25:47 | 0:25:50 | |
potentially hazardous asteroids. And these are asteroids that can | 0:25:50 | 0:25:54 | |
pass within seven 7.5 million km of the Earth's orbit. | 0:25:54 | 0:25:58 | |
So they come as close as that, or closer. | 0:25:58 | 0:26:01 | |
And we believe initially that they could be up to 140 metres | 0:26:01 | 0:26:05 | |
across or larger. And we have that size limit because we know that | 0:26:05 | 0:26:09 | |
no matter what the asteroid is, calculations show that if it enters | 0:26:09 | 0:26:13 | |
the Earth's atmosphere, it's going to make it to the ground. | 0:26:13 | 0:26:16 | |
OK, so that's the difference between a spectacular shooting star | 0:26:16 | 0:26:20 | |
and something we should worry about. | 0:26:20 | 0:26:22 | |
Absolutely, 140 metres across is when you worry, because you know, | 0:26:22 | 0:26:24 | |
no matter what it's made of, it's going to reach ground level | 0:26:24 | 0:26:27 | |
and it's going to make a crater and the effects will be multiplied. | 0:26:27 | 0:26:30 | |
So, what's next? We've found a potentially hazardous asteroid. | 0:26:30 | 0:26:33 | |
We think it's pretty big. We think it might be on a collision course. | 0:26:33 | 0:26:36 | |
We've got an initial orbit. | 0:26:36 | 0:26:38 | |
Does this get kept quiet, or do we announce immediately? | 0:26:38 | 0:26:41 | |
Well, the important thing to realise is that everything is public. | 0:26:41 | 0:26:44 | |
Everything is announced. And we need that because when you discover | 0:26:44 | 0:26:47 | |
a potentially hazardous asteroid, | 0:26:47 | 0:26:49 | |
you need everybody that can observe it to observe it, so we can pin down | 0:26:49 | 0:26:54 | |
the orbit better. And so everything is public. | 0:26:54 | 0:26:57 | |
And so, are you worried? | 0:26:57 | 0:26:59 | |
Are there objects that you know about that might hit us? | 0:26:59 | 0:27:02 | |
There are no significant worries at the moment. | 0:27:02 | 0:27:06 | |
But we've got to remember that if we go to the size range of potentially | 0:27:06 | 0:27:10 | |
hazardous objects - anything 140 metres across or larger - | 0:27:10 | 0:27:15 | |
then there's probably about 20-30,000 of those that exist | 0:27:15 | 0:27:18 | |
at the moment. We've only found 8,000 of them. | 0:27:18 | 0:27:21 | |
So, we've only got about 30% of that population. | 0:27:21 | 0:27:26 | |
And even when we do find them, | 0:27:26 | 0:27:28 | |
quite often, the orbits are uncertain. | 0:27:28 | 0:27:31 | |
If we go down to smaller sizes | 0:27:31 | 0:27:33 | |
such as the Chelyabinsk or Tunguska impacts, all bets are off. | 0:27:33 | 0:27:36 | |
These things are random. | 0:27:36 | 0:27:38 | |
They're like buses. Sometimes they won't turn up. | 0:27:38 | 0:27:41 | |
Sometimes, you can get two very closely arriving at the same time. | 0:27:41 | 0:27:45 | |
So, who knows? | 0:27:45 | 0:27:48 | |
We could be hit by one as people are watching this programme. | 0:27:48 | 0:27:51 | |
Well, there's a cheerful thought! | 0:27:51 | 0:27:53 | |
Alan, thank you very much. I hope you make it home safely. | 0:27:53 | 0:27:56 | |
Well, don't let that thought deter you - | 0:27:57 | 0:27:59 | |
do go out right now and try and see tonight's Perseid meteor shower. | 0:27:59 | 0:28:04 | |
It really is one of the astronomical highlights of the year. | 0:28:04 | 0:28:07 | |
Don't forget to watch us again next month, when we'll be | 0:28:09 | 0:28:12 | |
telling the incredible story of Cassini, | 0:28:12 | 0:28:15 | |
one of the most successful space explorations ever. | 0:28:15 | 0:28:18 | |
And as it reaches the end of its mission, | 0:28:18 | 0:28:20 | |
we'll be asking, what questions has it sent us for the future? | 0:28:20 | 0:28:23 | |
Meanwhile, don't forget to check out our website for more content | 0:28:23 | 0:28:26 | |
from this month's packed show, and for our star guide, | 0:28:26 | 0:28:30 | |
which includes information on how to spot asteroid Florence | 0:28:30 | 0:28:33 | |
as it skims past the Earth in September. | 0:28:33 | 0:28:36 | |
And, of course, get outside and get looking up. | 0:28:36 | 0:28:40 | |
-Especially if it's clear. Check out those Perseids. -Goodnight. | 0:28:40 | 0:28:44 |