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BOTH: Hello. | 0:00:28 | 0:00:29 | |
And welcome to the Royal Observatory in Greenwich here in London. | 0:00:29 | 0:00:33 | |
Tonight's programme is all about the moon | 0:00:33 | 0:00:35 | |
and we'll be finding out about the latest mission to go there | 0:00:35 | 0:00:38 | |
We'll also have the results from this summer's Moore Moon Marathon. | 0:00:38 | 0:00:42 | |
I know lots of you have taken part | 0:00:42 | 0:00:43 | |
and I'm really keen to find out how you got on. | 0:00:43 | 0:00:46 | |
Later this evening, we're hoping to catch a glimpse | 0:00:46 | 0:00:49 | |
of an intriguing lunar eclipse but, until then, | 0:00:49 | 0:00:52 | |
here's Pete Lawrence with what to see in November's night sky. | 0:00:52 | 0:00:55 | |
Astronomers are getting excited about comet ISON, | 0:01:02 | 0:01:04 | |
which is starting to produce a tail | 0:01:04 | 0:01:07 | |
as it nears and gets heated up by the sun. | 0:01:07 | 0:01:10 | |
At the start of November, the comet should be visible in the binoculars | 0:01:13 | 0:01:16 | |
close to the star Sigma Leonis which marks the rear paw of Leo | 0:01:16 | 0:01:20 | |
It passes very close to the stars Zavijava, or Beta Virginis, | 0:01:21 | 0:01:26 | |
on the morning of 7th November | 0:01:26 | 0:01:28 | |
and Porrima, or Gamma Virginis on the 13th. | 0:01:28 | 0:01:33 | |
On the 18th, ISON will be | 0:01:33 | 0:01:35 | |
very close to the star Spica, or Alpha Virginis. | 0:01:35 | 0:01:39 | |
The comet should be visible to the naked eye at this time. | 0:01:39 | 0:01:42 | |
With binoculars pointed at Spica, | 0:01:42 | 0:01:44 | |
you should be able to pick up the comet in the same field of view | 0:01:44 | 0:01:47 | |
As we head into the third week of November, the moon gets in the way | 0:01:49 | 0:01:53 | |
and the comet is only visible in the morning twilight. | 0:01:53 | 0:01:57 | |
One more thing for you to look at in November, the planet Jupiter, | 0:01:58 | 0:02:02 | |
which is in the eastern sky. | 0:02:02 | 0:02:04 | |
Throughout November it's located | 0:02:04 | 0:02:06 | |
close to the star Wasat in Gemini, the twins. | 0:02:06 | 0:02:09 | |
The charts to find the comet and Jupiter are on our website | 0:02:11 | 0:02:14 | |
This month's Sky At Night is from Greenwich | 0:02:23 | 0:02:26 | |
with astronomers converging on Blackheath Common. | 0:02:26 | 0:02:29 | |
Chris and I have been joined by Pete Lawrence | 0:02:30 | 0:02:32 | |
and Jon Culshaw to see the lunar eclipse. | 0:02:32 | 0:02:36 | |
What better time to announce the final of our Moore Moon Marathon? | 0:02:36 | 0:02:40 | |
Sir Patrick Moore, as a young astronomer, studied the moon. | 0:02:42 | 0:02:46 | |
I think the first explorers | 0:02:46 | 0:02:48 | |
may have some surprises | 0:02:48 | 0:02:49 | |
when they first step out of their craft | 0:02:49 | 0:02:52 | |
onto the barren, bleak moonscapes. | 0:02:52 | 0:02:54 | |
He spent thousands of hours building up lunar maps | 0:02:54 | 0:02:57 | |
which were later used by the Russians and Americans | 0:02:57 | 0:03:01 | |
when they went to the moon. | 0:03:01 | 0:03:03 | |
You can see the dark seas even without a telescope at all. | 0:03:03 | 0:03:06 | |
After all, the moon is by very much our nearest neighbour in space | 0:03:06 | 0:03:10 | |
Our nearest natural neighbour, that's to say. | 0:03:10 | 0:03:12 | |
Patrick always encouraged us | 0:03:12 | 0:03:14 | |
to look up and appreciate what's on our celestial doorstep. | 0:03:14 | 0:03:18 | |
We've tried to keep the spirit with our Moore Moon Marathon. | 0:03:19 | 0:03:23 | |
While Pete and I assemble our table of wares, | 0:03:25 | 0:03:27 | |
let's get the results from Chris and Jon. | 0:03:27 | 0:03:31 | |
Well, it has to be said, it's not the clearest of nights right now. | 0:03:31 | 0:03:34 | |
We've got plenty of astronomers | 0:03:34 | 0:03:36 | |
They're looking cheerful and enthusiastic and hopeful, so fingers crossed. | 0:03:36 | 0:03:39 | |
They certainly do, and one or two breaks in these clouds | 0:03:39 | 0:03:42 | |
which are giving us that sense of promise. | 0:03:42 | 0:03:45 | |
We might see a good view of that penumbral eclipse later | 0:03:45 | 0:03:48 | |
Let's hope so. | 0:03:48 | 0:03:49 | |
Before we get to that, let's talk about the Moore Moon Marathon. | 0:03:49 | 0:03:52 | |
We challenged you back at the start of the summer | 0:03:52 | 0:03:54 | |
to take a close look at the moon and thousands of you have taken part. | 0:03:54 | 0:03:58 | |
It's been wonderful to see people's enthusiasm. Terrific comments here. | 0:03:58 | 0:04:02 | |
Simon and Sarah Fisher from Worcestershire had a great deal of fun over the summer, | 0:04:02 | 0:04:06 | |
lots of clear nights. They had a really lucky run at it, actually, | 0:04:06 | 0:04:09 | |
and were able to go through all of their moon captures in great detail, | 0:04:09 | 0:04:12 | |
so a sense of the dedication there. | 0:04:12 | 0:04:13 | |
That's right. The waiting for clear skies is a bit of a theme. | 0:04:13 | 0:04:16 | |
Chris Goode from Devon says, "It took me over a few months to get | 0:04:16 | 0:04:20 | |
"all the information due to rubbish cloud cover," where he lives. | 0:04:20 | 0:04:24 | |
I sympathise with that. Dedication carried him through | 0:04:24 | 0:04:27 | |
Nice one here from David Winham in Newcastle. | 0:04:27 | 0:04:29 | |
"Looking at the moon, I had a feeling of intrigue and desolation, | 0:04:29 | 0:04:33 | |
"maybe magnificent desolation. Maybe I've become moonstruck." | 0:04:33 | 0:04:36 | |
I think you have, David, and we're glad of that. | 0:04:36 | 0:04:39 | |
Also moonstruck, Victor Suttle | 0:04:39 | 0:04:40 | |
who I think must be the youngest person so far. | 0:04:40 | 0:04:43 | |
He's five, in Essex, and he says, "I spotted the half moon and it was | 0:04:43 | 0:04:47 | |
"really tricky and it took me a long time." But well done for persevering. | 0:04:47 | 0:04:50 | |
Exactly. Half a moon is better than none at all, so well done for that. | 0:04:50 | 0:04:54 | |
Do you think so? I think so. Good. We'll settle for half a moon tonight. | 0:04:54 | 0:04:58 | |
Oh, there it is, through a little bit of hazy cloud. | 0:04:58 | 0:05:01 | |
These are the little glimpses that give us promise and hope. | 0:05:01 | 0:05:05 | |
It did vanish while you were saying that, Jon | 0:05:05 | 0:05:08 | |
Keith Moore from South Yorkshire enjoyed this, | 0:05:08 | 0:05:11 | |
"Very much enjoyed the MMM. | 0:05:11 | 0:05:13 | |
"Going to make it my quest to learn more about the moon, | 0:05:13 | 0:05:16 | |
"just like my namesake." | 0:05:16 | 0:05:18 | |
Well done to you. Well done, indeed. | 0:05:18 | 0:05:20 | |
And the Kilgore family from Glasgow took part in the MMM, | 0:05:20 | 0:05:23 | |
as I think we're going to call it from now on, in particular Alistair, | 0:05:23 | 0:05:27 | |
who enjoyed it so much he had a moon birthday cake. | 0:05:27 | 0:05:29 | |
So you can not only observe, but eat all of the features. | 0:05:29 | 0:05:33 | |
Well done, Alistair. A wonderful, award-winning cake, there. Indeed. | 0:05:33 | 0:05:36 | |
We'll come back to the Moore Moon Marathon in a moment | 0:05:36 | 0:05:38 | |
but, first, let's look at what's going to happen tonight | 0:05:38 | 0:05:41 | |
as Pete and Lucy explain the eclipse to us. It's gone again. | 0:05:41 | 0:05:44 | |
HE LAUGHS | 0:05:44 | 0:05:46 | |
Tonight's eclipse is slightly different, slightly unusual. | 0:05:48 | 0:05:51 | |
It comes down to the fact that there are two parts to the Earth's shadow. | 0:05:51 | 0:05:56 | |
You can illustrate that on the table, here. I'll have a go. | 0:05:56 | 0:05:59 | |
There we go. So, you've got the light passing over the Earth | 0:05:59 | 0:06:01 | |
and what I can see really clearly, | 0:06:01 | 0:06:03 | |
there's a dark centre to the shadow that we call the umbra | 0:06:03 | 0:06:06 | |
and then a slightly fainter shadow all the way around the edge | 0:06:06 | 0:06:10 | |
that we call the penumbra. | 0:06:10 | 0:06:11 | |
So, Pete, what is it that's happening tonight? | 0:06:11 | 0:06:13 | |
Tonight, the moon will be moving through the shadow, | 0:06:13 | 0:06:16 | |
but it's missing the main part in the middle | 0:06:16 | 0:06:19 | |
and it's moving through that outer fainter part, the penumbra, | 0:06:19 | 0:06:22 | |
so it's what is called a penumbral eclipse of the moon | 0:06:22 | 0:06:25 | |
So it's coming through here, is it? Yeah, that's right. | 0:06:25 | 0:06:28 | |
The best way to describe a penumbral eclipse | 0:06:28 | 0:06:31 | |
is to call it a subtle eclipse | 0:06:31 | 0:06:33 | |
If you were looking at it visually, you probably wouldn't see | 0:06:33 | 0:06:36 | |
much difference in the appearance of the full moon. | 0:06:36 | 0:06:39 | |
But if you take a photograph before the moon enters the penumbral shadow | 0:06:39 | 0:06:43 | |
and then another photograph of the moon when it's actually | 0:06:43 | 0:06:46 | |
in the penumbral shadow at the maximum part of the eclipse, | 0:06:46 | 0:06:49 | |
what you see is a very gentle shading close to the bit of the moon | 0:06:49 | 0:06:53 | |
which is closest to the darkest part of the shadow in space. | 0:06:53 | 0:06:57 | |
Still, it's a very special event | 0:06:57 | 0:06:58 | |
and it's one that I'm looking forward to seeing. | 0:06:58 | 0:07:01 | |
Our marathon has been divided into five sections | 0:07:05 | 0:07:08 | |
and the first is all about the lunar seas. | 0:07:08 | 0:07:12 | |
We've been joined on Blackheath Common by moon expert Katie Joy | 0:07:12 | 0:07:16 | |
Several people, including Pawel Kus from Poland | 0:07:17 | 0:07:21 | |
wanted to know about the seas, wanted to know how they formed | 0:07:21 | 0:07:24 | |
So, first of all, why do they look so different from the rest of the moon? | 0:07:24 | 0:07:27 | |
So on the moon we have two main rock types. These are my fake moon. | 0:07:27 | 0:07:30 | |
I'm not allowed to bring huge chunks of real moon out with me | 0:07:30 | 0:07:33 | |
It's a shame, really. It is a bit of a shame. | 0:07:33 | 0:07:35 | |
Essentially, we have two main rock types on the moon. | 0:07:35 | 0:07:37 | |
We have a white rock in the lunar highlands. | 0:07:37 | 0:07:39 | |
This is the very old rock. | 0:07:39 | 0:07:40 | |
And then we have lunar lava flows that were formed in volcanoes | 0:07:40 | 0:07:43 | |
and these are the material that formed those dark seas | 0:07:43 | 0:07:46 | |
that cover most of the nearside | 0:07:46 | 0:07:47 | |
that people have been spotting in the Moore Marathon. | 0:07:47 | 0:07:50 | |
So, this is the reason we have the seas - lava flows. | 0:07:50 | 0:07:52 | |
So, they're made of different stuff and so they're different colours? | 0:07:52 | 0:07:55 | |
Different colours, different chemistry, different minerals between the two. | 0:07:55 | 0:07:58 | |
The lunar seas appear to be a lot smoother as we look at the moon | 0:07:58 | 0:08:02 | |
is that true in reality? | 0:08:02 | 0:08:03 | |
The lunar seas are a lot younger, | 0:08:03 | 0:08:05 | |
so we have to go back to the origin of the moon | 0:08:05 | 0:08:07 | |
and talk about its early geology. | 0:08:07 | 0:08:09 | |
We think the moon formed about 4.5 billion years ago | 0:08:09 | 0:08:12 | |
in a giant impact event, | 0:08:12 | 0:08:13 | |
where a Mars-sized body crashed into the early Earth. | 0:08:13 | 0:08:17 | |
It spawns off a huge amount of material | 0:08:17 | 0:08:19 | |
and forms a magma body in space and then that magma body cools | 0:08:19 | 0:08:22 | |
and it forms an interior, a core, a mantle and a crust. | 0:08:22 | 0:08:26 | |
The crust that formed was made of this rock, | 0:08:26 | 0:08:29 | |
which is the very old highlands material. | 0:08:29 | 0:08:31 | |
Subsequently to that, | 0:08:31 | 0:08:32 | |
we had the lavas that were formed deep in the moon, | 0:08:32 | 0:08:35 | |
propagated through the crust | 0:08:35 | 0:08:36 | |
and erupted into large impact basins that are on the surface. | 0:08:36 | 0:08:39 | |
The reason they're so smooth is because the lavas were very runny. | 0:08:39 | 0:08:43 | |
They ran out and distributed very evenly | 0:08:43 | 0:08:45 | |
across some of these types of impact craters, making a smooth surface. | 0:08:45 | 0:08:48 | |
And they also haven't been heavily impact cratered like the highlands, | 0:08:48 | 0:08:52 | |
because they were a lot younger | 0:08:52 | 0:08:53 | |
It's kind of a twofold reason less impact craters | 0:08:53 | 0:08:56 | |
and smooth runny lava that made them. | 0:08:56 | 0:08:57 | |
Is this very different to the formation of | 0:08:57 | 0:08:59 | |
other moons in the solar system around Saturn and Jupiter? | 0:08:59 | 0:09:02 | |
Mars's moons, we hear, are captured asteroids, | 0:09:02 | 0:09:05 | |
so this sounds rather different It's a unique event, yeah. | 0:09:05 | 0:09:08 | |
Most of the other moons we think of are captured from bodies | 0:09:08 | 0:09:10 | |
moving in and then being gravitationally attracted | 0:09:10 | 0:09:12 | |
to their parent planets, but this is why the moon is so interesting, | 0:09:12 | 0:09:15 | |
it's a completely unique event and it tells us lots of information | 0:09:15 | 0:09:19 | |
about how the Earth formed and early terrestrial processes as well. | 0:09:19 | 0:09:23 | |
And also, because it's old, it's a | 0:09:23 | 0:09:25 | |
record of the early solar system as well. | 0:09:25 | 0:09:27 | |
There are some interesting results that come from counting craters | 0:09:27 | 0:09:30 | |
and looking at these older surfaces. | 0:09:30 | 0:09:32 | |
That's exactly why the moon is so important. | 0:09:32 | 0:09:34 | |
It's three days away, it is very easy to get to... Easy for you to say! | 0:09:34 | 0:09:37 | |
..it's accessible, it's 4.5 billion years old. | 0:09:37 | 0:09:39 | |
Well, if you've got a big spaceship, you can get there in three days | 0:09:39 | 0:09:42 | |
And it provides us with a record of the geological evolution | 0:09:42 | 0:09:45 | |
of the inner solar system over 4.5 billion years. | 0:09:45 | 0:09:48 | |
Much of that record has been lost on the Earth, | 0:09:48 | 0:09:50 | |
because we recycle our geology through plate tectonics | 0:09:50 | 0:09:52 | |
and other types of active geological processes, | 0:09:52 | 0:09:55 | |
but the moon is almost frozen in time. | 0:09:55 | 0:09:57 | |
The moon is really special for lots of reasons. | 0:09:57 | 0:10:00 | |
The lunar seas that we were talking about, | 0:10:00 | 0:10:02 | |
what a great starting point they were for the marathon, | 0:10:02 | 0:10:04 | |
great naked eye objects just to get you in there | 0:10:04 | 0:10:07 | |
and lead you on to the others. | 0:10:07 | 0:10:09 | |
Philip Jennings of York, | 0:10:09 | 0:10:10 | |
he was saying that the seas are a wonderful site with the telescope. | 0:10:10 | 0:10:13 | |
They certainly are, especially when rippled with wrinkled ridges | 0:10:13 | 0:10:16 | |
or crisscrossed with brighter crater rays at full moon. | 0:10:16 | 0:10:20 | |
A shame, then, that he locked himself out of his observatory | 0:10:20 | 0:10:23 | |
because he couldn't find the key. Oh, dear! | 0:10:23 | 0:10:25 | |
But this did remind him how wonderful the moon is to see | 0:10:25 | 0:10:28 | |
just with the naked eye, which is very true. | 0:10:28 | 0:10:30 | |
It is wonderful and there's no sign of it whatsoever, | 0:10:30 | 0:10:33 | |
so we're going to go to Pete and Lucy | 0:10:33 | 0:10:35 | |
to find out how some of the craters on the lunar surface formed. | 0:10:35 | 0:10:38 | |
Now, we're moving on to the second part of the Moore Moon Marathon | 0:10:41 | 0:10:44 | |
that looks at some of the features on the moon | 0:10:44 | 0:10:46 | |
that reflect its more violent history. | 0:10:46 | 0:10:48 | |
These are craters, bright and dark craters. | 0:10:48 | 0:10:51 | |
Pete, why did you choose these features? | 0:10:51 | 0:10:53 | |
Well, these are features which are easy to see | 0:10:53 | 0:10:55 | |
when the moon is fairly well illuminated. | 0:10:55 | 0:10:57 | |
I think they're pretty iconic, actually, on the moon's face. | 0:10:57 | 0:11:01 | |
There are very bright craters with very large rays coming off them and | 0:11:01 | 0:11:06 | |
also dark craters, which look like little lakes, if you like, of lava. | 0:11:06 | 0:11:11 | |
These are features that you perhaps need to have binoculars to see | 0:11:11 | 0:11:14 | |
so they're a little bit more challenging than the first | 0:11:14 | 0:11:16 | |
section of the Moore Moon Marathon. | 0:11:16 | 0:11:18 | |
Yeah, that's right. | 0:11:18 | 0:11:19 | |
Now, you mentioned rays, features of craters. We have a tray here | 0:11:19 | 0:11:23 | |
Now, you have a challenge because you can make a crater. | 0:11:24 | 0:11:28 | |
We've got flour underneath and cocoa powder | 0:11:28 | 0:11:31 | |
and chocolate on top and this is the asteroid. | 0:11:31 | 0:11:34 | |
To make this work, I've got to throw this hard into the tray, | 0:11:34 | 0:11:38 | |
so forgive me... I'm going to step back! OK. Go for it. | 0:11:38 | 0:11:41 | |
Oh, perfect! | 0:11:44 | 0:11:46 | |
Well, look at that. That is fantastic. | 0:11:47 | 0:11:49 | |
So, you've carved out the crater floor here, absolutely fantastic, | 0:11:49 | 0:11:53 | |
and all the bright material underneath has come into view. | 0:11:53 | 0:11:56 | |
So, it's gone across the dark floor of the sea there, | 0:11:56 | 0:12:00 | |
so this stands out as a ray crater. | 0:12:00 | 0:12:02 | |
So this would be a bright crater in a mare on the surface of the moon. | 0:12:02 | 0:12:05 | |
That's right, yes. Beautiful. And I can see the ejecta here. | 0:12:05 | 0:12:08 | |
And these would be the bright rays? That's right. | 0:12:08 | 0:12:11 | |
Tycho is a great example of that, of course, | 0:12:11 | 0:12:13 | |
in the southern part of the moon because it's got those bright rays | 0:12:13 | 0:12:16 | |
which extend right across the moon's face. | 0:12:16 | 0:12:18 | |
It's an iconic crater. And a lot of you really got excited by Tycho, | 0:12:18 | 0:12:22 | |
so I've got a comment from David Wenham from Newcastle. | 0:12:22 | 0:12:25 | |
And he says, "Tycho is spectacular to look at. | 0:12:25 | 0:12:28 | |
"The impact crater is so vast, which scars the moon." | 0:12:28 | 0:12:32 | |
And it really does, it spreads over a huge distance | 0:12:32 | 0:12:35 | |
I think that's my favourite crater to look at. | 0:12:35 | 0:12:37 | |
But this comment is lovely from Alan Fenner on the Wirral | 0:12:37 | 0:12:41 | |
He says, "If the moon was a giant fruit, Tycho would be the place | 0:12:41 | 0:12:45 | |
"where it hung from the tree." So this is a really lovely example. | 0:12:45 | 0:12:49 | |
You had bright and dark craters on your list. | 0:12:49 | 0:12:53 | |
So tell me a bit about how the dark craters form. | 0:12:53 | 0:12:56 | |
The dark craters, like Grimaldi which is a very distinctive marker | 0:12:56 | 0:13:01 | |
on the moon's face, is basically a crater where the floor of the crater | 0:13:01 | 0:13:06 | |
has become flooded with dark lava. | 0:13:06 | 0:13:09 | |
And they look very distinctive on the moon's face. | 0:13:09 | 0:13:13 | |
The craters you selected, they're all beautiful | 0:13:13 | 0:13:15 | |
but is there one that stands out as your favourite? | 0:13:15 | 0:13:18 | |
I think Copernicus, actually, because that's very well-defined crater | 0:13:18 | 0:13:22 | |
It's got great rays coming off from it. Just like this. | 0:13:22 | 0:13:25 | |
And it's got these beautiful terraced walls when you look at it. | 0:13:25 | 0:13:28 | |
They're sort of blocked down to the floor of the crater | 0:13:28 | 0:13:31 | |
And you can see that we have got that effect in our crater here | 0:13:31 | 0:13:34 | |
It does look like it. | 0:13:34 | 0:13:35 | |
Little terraces. | 0:13:35 | 0:13:36 | |
And that's formed as the lunar surface slumps back down again | 0:13:36 | 0:13:40 | |
Copernicus has got some fantastic mountains right in the centre. | 0:13:40 | 0:13:44 | |
So in the largest craters, | 0:13:44 | 0:13:45 | |
you get this central uplift as the rock becomes more plastic. | 0:13:45 | 0:13:49 | |
Yes, like a liquid. It comes back up and solidifies | 0:13:49 | 0:13:53 | |
I've got some more comments here that includes Copernicus. | 0:13:53 | 0:13:56 | |
It is a comment from David Scanlon in Hampshire and he says, | 0:13:56 | 0:14:00 | |
"Copernicus and Kepler, clearly obvious due to their size. | 0:14:00 | 0:14:04 | |
"Aristarchus, stunning, brightest lunar feature by far | 0:14:04 | 0:14:08 | |
"and awe-inspiring." Aristarchus is an interesting crater. It is. | 0:14:08 | 0:14:12 | |
It's a very young crater, very bright. | 0:14:12 | 0:14:14 | |
It's got those terraced walls again and very bright rays around it | 0:14:14 | 0:14:18 | |
So go to the website and find the location. | 0:14:18 | 0:14:21 | |
And we've got another comment here from Sammy Glastonbury. | 0:14:21 | 0:14:24 | |
"Kepler reminds me of a spider" OK. Do you see that? | 0:14:24 | 0:14:28 | |
It's never reminded me of a spider but it might do from now on. | 0:14:28 | 0:14:31 | |
Another comment here from Sarah and Simon Fisher from Worcestershire. | 0:14:31 | 0:14:35 | |
They said, "It was awesome to be able to use | 0:14:35 | 0:14:38 | |
"our own photos and name both the bright and the dark craters . | 0:14:38 | 0:14:41 | |
That's wonderful. Just wonderful. Really sums it up. | 0:14:41 | 0:14:44 | |
Now section 3 is craters in shadow. | 0:14:44 | 0:14:46 | |
We've got a demo here to illustrate how fantastic these craters look. | 0:14:46 | 0:14:51 | |
That's right. The reason I wanted to put these into the Moon Marathon | 0:14:51 | 0:14:54 | |
is that craters are really dramatic when they're very close | 0:14:54 | 0:14:57 | |
to the terminator, the line which marks the difference | 0:14:57 | 0:15:00 | |
between night and day on the moon. | 0:15:00 | 0:15:02 | |
And I can illustrate that with the sun again. The trusty sun. | 0:15:02 | 0:15:07 | |
And these fantastic models of craters. | 0:15:07 | 0:15:09 | |
In fact, if I illuminate this crater from above directly, | 0:15:09 | 0:15:13 | |
you don't get to see many of the relief features, | 0:15:13 | 0:15:16 | |
the features with the height on there. | 0:15:16 | 0:15:19 | |
But as the sun's angle starts to come down, | 0:15:19 | 0:15:21 | |
if you watch what happens inside it, | 0:15:21 | 0:15:24 | |
you can start to see the shadows growing in length. | 0:15:24 | 0:15:27 | |
Those craterlets have really become quite well defined. Yes. | 0:15:27 | 0:15:31 | |
You're absolutely right. I can suddenly see all the structure within the crater itself. | 0:15:31 | 0:15:35 | |
It's amazing. And look at the length of those shadows | 0:15:35 | 0:15:37 | |
as the sun starts to get lower and lower in the lunar sky. | 0:15:37 | 0:15:41 | |
Look at the central mountains there. Gosh. | 0:15:41 | 0:15:44 | |
Those mountains look enormous | 0:15:44 | 0:15:45 | |
because they have this huge triangular shadow. | 0:15:45 | 0:15:48 | |
There's suddenly huge drama to that crater. That's right. | 0:15:48 | 0:15:51 | |
And then suddenly it goes into complete darkness. | 0:15:51 | 0:15:55 | |
'Well, the eclipse is now well under way | 0:15:55 | 0:15:57 | |
and there are probably people who are enjoying a good sight of it. | 0:15:57 | 0:16:00 | |
If you could see the moon right now, | 0:16:00 | 0:16:02 | |
you would begin to notice a difference from an everyday moon. | 0:16:02 | 0:16:05 | |
We can't see anything. | 0:16:05 | 0:16:07 | |
Let's talk about the lunar surface again, | 0:16:07 | 0:16:09 | |
in particular David Scanlon from Hampshire talks about Clavius, | 0:16:09 | 0:16:14 | |
a wonderful myriad of younger craters over an older crater | 0:16:14 | 0:16:17 | |
which makes for superb exploration. | 0:16:17 | 0:16:20 | |
Yes, they really captured the imagination, the craters in shadow. | 0:16:20 | 0:16:23 | |
Tell us some more about Clavius, Katie. | 0:16:23 | 0:16:25 | |
There's a complex history here | 0:16:25 | 0:16:27 | |
Clavius is quite a large crater about 225km in diameter. | 0:16:27 | 0:16:31 | |
It has a rim around the edge that marks its exterior extent. | 0:16:31 | 0:16:35 | |
We don't know exactly when the crater formed | 0:16:35 | 0:16:38 | |
but we can count other craters that have been superimposed on top of it. | 0:16:38 | 0:16:41 | |
So we think that it's Nectarian in age | 0:16:41 | 0:16:43 | |
which is about 4 billion years ago. | 0:16:43 | 0:16:45 | |
Of course, we had other craters in shadow. What about Eratosthenes | 0:16:45 | 0:16:48 | |
I think that's...is that how you say it? Eratosthenes, is that it? | 0:16:48 | 0:16:52 | |
Yes, that's the elegant way of doing it. Very good. We'll let Jon say it. Eratosthenes. | 0:16:52 | 0:16:56 | |
Alan Fenner from the Wirral: "When I see Eratosthenes, | 0:16:56 | 0:16:59 | |
"I can't help but see..." ` I love these imaginative descriptions! | 0:16:59 | 0:17:03 | |
"I see the eye of a baby dinosaur | 0:17:03 | 0:17:05 | |
"with the Apennines as its neck and back". | 0:17:05 | 0:17:08 | |
Probably a young Polacanthus by that description. Yes, very good! | 0:17:08 | 0:17:12 | |
But, actually, that mention of the mountains | 0:17:12 | 0:17:14 | |
as the ridge of the dinosaur's back in that case | 0:17:14 | 0:17:17 | |
leads us on to Section 4, which was The Majestic Mountains. | 0:17:17 | 0:17:20 | |
And we had all sorts of comments. Keith Moore from South Yorkshire | 0:17:20 | 0:17:23 | |
just says, "Montes Jura on the terminator, wow!" | 0:17:23 | 0:17:27 | |
Quite simply, wow. Makes you think of future lunar mountaineers | 0:17:27 | 0:17:32 | |
who could probably climb the mountains rather easily | 0:17:32 | 0:17:34 | |
with that lower gravity, just floating up there. | 0:17:34 | 0:17:36 | |
And it wouldn't be quite so bad when you fell back down again. | 0:17:36 | 0:17:39 | |
It'd still be a long way down. But the mountains are spectacular. | 0:17:39 | 0:17:43 | |
They might not be as high as our mountains on Earth but they look wonderful | 0:17:43 | 0:17:46 | |
and Calum Kilgore saw the line of the Montes Jura disappearing | 0:17:46 | 0:17:50 | |
into space through binoculars and then later on | 0:17:50 | 0:17:52 | |
saw the whole semicircle of mountains through the telescope | 0:17:52 | 0:17:55 | |
thanks to his dad who got the telescope out in front of the neighbours. | 0:17:55 | 0:17:58 | |
So well done, Dad. I think that s the main takeaway from that one | 0:17:58 | 0:18:01 | |
Got the whole street talking! Indeed! | 0:18:01 | 0:18:04 | |
Over Blackheath in London, | 0:18:08 | 0:18:09 | |
the clouds have firmly set in | 0:18:09 | 0:18:11 | |
but, in Pennsylvania, they had clear skies. | 0:18:11 | 0:18:14 | |
The subtle shading in the bottom right of the moon | 0:18:14 | 0:18:17 | |
is the Earth's shadow. | 0:18:17 | 0:18:18 | |
In Massachusetts, a plane passed over the penumbral eclipse | 0:18:18 | 0:18:22 | |
and in Iran, you could see the Earth's shadow quite clearly. | 0:18:22 | 0:18:27 | |
There was a handy gap in the clouds over Stuttgart, | 0:18:27 | 0:18:29 | |
just enough for a glimpse of the moon. | 0:18:29 | 0:18:31 | |
Now it's a break from the moon and off to the planets | 0:18:33 | 0:18:35 | |
where we join Paul Abel, | 0:18:35 | 0:18:36 | |
who's been finding out about the latest research results. | 0:18:36 | 0:18:39 | |
Every year, astronomers who study the planets gather to share ideas and their research | 0:18:49 | 0:18:54 | |
It's the turn of London, | 0:18:55 | 0:18:57 | |
and University College London are the hosts. | 0:18:57 | 0:18:59 | |
Well, look at this. Isn't this stunning? | 0:19:04 | 0:19:06 | |
This is a beautiful panorama from Mars. | 0:19:06 | 0:19:10 | |
It's taken by the Mars Reconnaissance Orbiter spacecraft | 0:19:10 | 0:19:13 | |
and it shows the beautiful, majestic ravines | 0:19:13 | 0:19:15 | |
and the windswept sand dunes of the red planet | 0:19:15 | 0:19:18 | |
and it really is an incredible image. | 0:19:18 | 0:19:20 | |
Research is presented on posters | 0:19:25 | 0:19:27 | |
which are put up for everyone to look at. | 0:19:27 | 0:19:29 | |
Some of this is rather technical. | 0:19:30 | 0:19:32 | |
Look at this lovely poster. This is about an extrasolar planet. | 0:19:39 | 0:19:42 | |
And this is really a sign of the times | 0:19:42 | 0:19:44 | |
because we haven't just got results here from our own solar system | 0:19:44 | 0:19:47 | |
but we have data from other planetary systems as well. | 0:19:47 | 0:19:50 | |
News from our solar system is always exciting. | 0:19:53 | 0:19:55 | |
Mike Brown is here to talk about the latest from Jupiter's moon, Europa. | 0:19:57 | 0:20:01 | |
It seems the oceans of Europa have salts not unlike our own. | 0:20:01 | 0:20:05 | |
Mike is more famously known | 0:20:07 | 0:20:08 | |
for discovering lots of Kuiper Belt objects | 0:20:08 | 0:20:11 | |
such as Sedna, Makemake and Quaoar. | 0:20:11 | 0:20:15 | |
Their exotic names give an air of mystery to objects that lurk | 0:20:15 | 0:20:19 | |
in the farthest regions of our solar system, well beyond Neptune. | 0:20:19 | 0:20:22 | |
I shall introduce you to our viewers, | 0:20:24 | 0:20:27 | |
if you don't mind, as the man who killed off Pluto. | 0:20:27 | 0:20:29 | |
That's a fair thing to say, isn't it? I think that's OK. | 0:20:29 | 0:20:31 | |
Why did you do that? | 0:20:31 | 0:20:33 | |
You know, my usual response when people ask me | 0:20:33 | 0:20:36 | |
is because it had it coming, | 0:20:36 | 0:20:38 | |
but really I did it, | 0:20:38 | 0:20:40 | |
I killed off Pluto sort of by accident. | 0:20:40 | 0:20:43 | |
I was actually looking for something | 0:20:43 | 0:20:45 | |
that I would think would be a 1 th planet, something bigger than Pluto, | 0:20:45 | 0:20:49 | |
some substantially-sized object in the outer solar system. | 0:20:49 | 0:20:52 | |
And by looking, we surveyed the entire the outer solar system | 0:20:52 | 0:20:56 | |
and realised that not only is there nothing really substantially | 0:20:56 | 0:20:59 | |
bigger than Pluto but there are many things | 0:20:59 | 0:21:01 | |
that are just essentially the same size as Pluto, which really meant | 0:21:01 | 0:21:04 | |
that Pluto is not as special as we used to think it was | 0:21:04 | 0:21:07 | |
and it really never deserved to be called a planet. | 0:21:07 | 0:21:10 | |
So actually, you're completely unrepentant about killing of poor Pluto?! | 0:21:10 | 0:21:13 | |
I'm actually very happy about it. | 0:21:13 | 0:21:15 | |
These objects are what we would class as trans-Neptunian objects, | 0:21:15 | 0:21:19 | |
that's the general umbrella term. | 0:21:19 | 0:21:21 | |
In fact, we more often commonly call them Kuiper Belt objects. | 0:21:21 | 0:21:24 | |
They are the coldest, | 0:21:24 | 0:21:26 | |
least-processed objects in the solar system and by processed I mean | 0:21:26 | 0:21:31 | |
if you look around at the Earth or any other planet, | 0:21:31 | 0:21:35 | |
everything you see started out in the early solar system | 0:21:35 | 0:21:38 | |
and then has been heated up and crunched together and extruded | 0:21:38 | 0:21:41 | |
and split apart and so it's very difficult to figure out what | 0:21:41 | 0:21:46 | |
really things were like at the very beginning. | 0:21:46 | 0:21:48 | |
As you move further and further out of the solar system, | 0:21:48 | 0:21:50 | |
things have never heated up very much | 0:21:50 | 0:21:53 | |
and not only have they not heated up very much | 0:21:53 | 0:21:55 | |
they haven't been thrown around by the planets quite as much, | 0:21:55 | 0:21:58 | |
so we can try to use what they're made out of and where they are | 0:21:58 | 0:22:02 | |
to figure out not just what things were like | 0:22:02 | 0:22:05 | |
in the very earliest solar system but how things have rearranged | 0:22:05 | 0:22:09 | |
since the solar system was formed. | 0:22:09 | 0:22:10 | |
And that's really the promise of this region out beyond Neptune. | 0:22:10 | 0:22:14 | |
If you could pick up a piece of it, | 0:22:14 | 0:22:15 | |
you're almost getting a little slice of the original cake | 0:22:15 | 0:22:18 | |
of the solar system, which is what you'd like to do. That's quite a thought! | 0:22:18 | 0:22:21 | |
These distant worlds have volcanoes and water ice. | 0:22:24 | 0:22:28 | |
They are far from boring and bland. | 0:22:28 | 0:22:30 | |
They have geology and some of them are large. | 0:22:30 | 0:22:33 | |
Eris is about the same size as Pluto yet it was only discovered in 2 05. | 0:22:33 | 0:22:39 | |
Could it be that there is an even larger world | 0:22:39 | 0:22:42 | |
lurking in the icy depths of our solar system, the infamous Planet X? | 0:22:42 | 0:22:46 | |
There's always the possibility that out in the Oort Cloud, | 0:22:50 | 0:22:53 | |
people have always speculated about a brown dwarf | 0:22:53 | 0:22:56 | |
or a Jupiter-sized thing. | 0:22:56 | 0:22:57 | |
I think that these days it's harder to speculate about that | 0:22:57 | 0:23:01 | |
because we actually have data that suggests there's nothing out there. | 0:23:01 | 0:23:04 | |
But you can always hide them somewhere. | 0:23:04 | 0:23:06 | |
People will forever speculate about these Jupiter-sized things out there. I suspect it's not true | 0:23:06 | 0:23:11 | |
I think the biggest things that are still out there | 0:23:11 | 0:23:14 | |
are going to be Mercury or Mars-sized. | 0:23:14 | 0:23:16 | |
They're going to be very far away, very faint, hard to find and hard to study | 0:23:16 | 0:23:20 | |
But I bet they're out there. | 0:23:20 | 0:23:22 | |
We have discovered around 1,000 Kuiper Belt objects, | 0:23:25 | 0:23:29 | |
all in the past two decades. | 0:23:29 | 0:23:31 | |
The first was found in 1992 by Dave Jewitt and is called QB1. | 0:23:31 | 0:23:36 | |
Dave has come to London to talk about something new | 0:23:38 | 0:23:41 | |
and to solve an old mystery. | 0:23:41 | 0:23:43 | |
So asteroids have been known for 200 years or something like that | 0:23:44 | 0:23:47 | |
and I figured it's all over, | 0:23:47 | 0:23:49 | |
we know everything you ever want to know about asteroids. | 0:23:49 | 0:23:52 | |
It turns out there's this population that's been there all the time but it was only just discovered | 0:23:52 | 0:23:56 | |
They are asteroids by their orbits, | 0:23:56 | 0:23:58 | |
but they look like comets. Confusing! | 0:23:58 | 0:24:01 | |
And it's very freaky because an asteroid | 0:24:01 | 0:24:03 | |
you would think is a rock and a rock looks like a rock, | 0:24:03 | 0:24:05 | |
and nothing ever happens and it's kind of boring but they look like comets, | 0:24:05 | 0:24:09 | |
they release material, they eject dust. | 0:24:09 | 0:24:11 | |
And it's just very bizarre. So I'm trying to explore this population. | 0:24:11 | 0:24:14 | |
We don't have many. There's like 10 or 12 known at the present time. | 0:24:14 | 0:24:17 | |
But we're looking at these things, trying to understand what they are. | 0:24:17 | 0:24:21 | |
And they're part of this general phenomenon | 0:24:21 | 0:24:24 | |
that we call the active asteroid phenomenon. Wow. | 0:24:24 | 0:24:26 | |
By which an object that you think should just be a boring, inert rock | 0:24:26 | 0:24:30 | |
somehow is able to be active and eject material. | 0:24:30 | 0:24:33 | |
The Geminid meteor shower graces our winter skies every year. | 0:24:36 | 0:24:40 | |
And it's the asteroid Phaethon which creates them. | 0:24:40 | 0:24:43 | |
Phaethon, it seems, | 0:24:45 | 0:24:47 | |
is one of these new type of asteroids which acts like a comet. | 0:24:47 | 0:24:51 | |
Phaethon is in an elliptical orbit that goes all the way into 0.14 AU. | 0:24:51 | 0:24:58 | |
So that's quite close to the sun. | 0:24:58 | 0:24:59 | |
It goes seven times closer to the sun than we are. | 0:24:59 | 0:25:02 | |
So it gets 50 times more sunlight than we get, | 0:25:02 | 0:25:05 | |
so it gets really hot at the perihelion. | 0:25:05 | 0:25:07 | |
And in this particular case, | 0:25:07 | 0:25:08 | |
what I think is happening is that it gets so hot that it cracks, | 0:25:08 | 0:25:13 | |
it thermally fractures, just like if you take a glass of orange juice, | 0:25:13 | 0:25:18 | |
you drink the orange juice, you stick it in the sink to wash it, | 0:25:18 | 0:25:20 | |
you hit it with hot water and the glass will crack | 0:25:20 | 0:25:23 | |
because of thermal expansion of the glass. | 0:25:23 | 0:25:26 | |
Probably that happens to the surface of this body. | 0:25:26 | 0:25:29 | |
So it gets really hot and this material just flows out and this, | 0:25:29 | 0:25:32 | |
we think, is responsible for our Geminid meteor stream | 0:25:32 | 0:25:34 | |
later in the year when the Earth passes through it? | 0:25:34 | 0:25:37 | |
That's what I think. Sounds like fascinating stuff. | 0:25:37 | 0:25:39 | |
What sort of things do you hope to get in the future? | 0:25:39 | 0:25:42 | |
You hope to discover more of these objects, presumably? | 0:25:42 | 0:25:44 | |
We've found this zoo of very strange objects lurking in the asteroid belt | 0:25:44 | 0:25:49 | |
and we'd just like to understand what they are. | 0:25:49 | 0:25:51 | |
We live in interesting times, Dave. Thank you very much. OK, you're welcome. | 0:25:51 | 0:25:54 | |
There is always time for a spot of R'n'R at these conferences. | 0:25:57 | 0:26:01 | |
I bet Pete would be good at this. Oh! | 0:26:01 | 0:26:04 | |
No luck with my lunar rover. | 0:26:04 | 0:26:07 | |
Houston, we have a problem. Oh, dear. | 0:26:07 | 0:26:10 | |
That's why I don't drive, incidentally. | 0:26:10 | 0:26:13 | |
NASA had better not rely on me | 0:26:13 | 0:26:16 | |
Time now to go back to Blackheath Common for our last section | 0:26:18 | 0:26:21 | |
in our Moore Moon Marathon, which Pete's called The Lunar Specials. | 0:26:21 | 0:26:25 | |
It's one in the morning here at Blackheath | 0:26:27 | 0:26:29 | |
and we're still going strong. | 0:26:29 | 0:26:31 | |
Somewhere there's somebody having a good view of the eclipse, | 0:26:31 | 0:26:34 | |
which is at maximum about now, but it's not us. | 0:26:34 | 0:26:37 | |
Yes, we can't see it but we know it's there. | 0:26:37 | 0:26:40 | |
Completely overcast but there's nothing one can do | 0:26:40 | 0:26:42 | |
No, absolutely not. We should move on to the Lunar Specials. | 0:26:42 | 0:26:46 | |
Christina Chester from Hertfordshire, | 0:26:46 | 0:26:48 | |
who is here somewhere, found a migrating duck | 0:26:48 | 0:26:51 | |
and a puppy with its bone up in the lunar highlands. | 0:26:51 | 0:26:54 | |
That's quite strange! | 0:26:54 | 0:26:56 | |
Well, Richard Bailey from Daventry says, "Thanks to Mr Culshaw, | 0:26:57 | 0:27:01 | |
"I now see a Cyberman on the moon." I know how he feels. | 0:27:01 | 0:27:04 | |
Sorry to ruin the old lady of the moon. | 0:27:04 | 0:27:07 | |
I think she's more like the lady from Downton Abbey, | 0:27:07 | 0:27:09 | |
I've rethought that one! | 0:27:09 | 0:27:12 | |
And Stephen Brown from Middlesbrough says, "The ghost crater Stadius | 0:27:12 | 0:27:15 | |
"was the hardest feature of the marathon for me, | 0:27:15 | 0:27:17 | |
"but I managed just about to make it out," so well done. | 0:27:17 | 0:27:20 | |
We also had some complaints about Rupes Recta, | 0:27:20 | 0:27:23 | |
various people got lost trying to find this. | 0:27:23 | 0:27:27 | |
Sammy Glastonbury said, "It was very, very, very hard to find. | 0:27:27 | 0:27:30 | |
"Very frustrating". Alan Fenner from the Wirral said that. | 0:27:30 | 0:27:34 | |
He said, "Other people seem to be able to get great views | 0:27:34 | 0:27:37 | |
"of Rupes Recta but I always find it very difficult. Harumph " | 0:27:37 | 0:27:42 | |
Well done to everyone who took part in our Moore Moon Marathon | 0:27:42 | 0:27:46 | |
And especially if you managed to complete it. | 0:27:46 | 0:27:49 | |
There's a cosmic congratulations to Wayne Young and his son, Thomas | 0:27:49 | 0:27:53 | |
who completed all three of Patrick's observing marathons. | 0:27:53 | 0:27:56 | |
Quite an achievement. | 0:27:56 | 0:27:59 | |
Our guides on what to see on the moon are still on our web page at: | 0:27:59 | 0:28:04 | |
You can also find Pete's charts | 0:28:07 | 0:28:09 | |
to find comet ISON over the next few weeks. | 0:28:09 | 0:28:12 | |
We've had a fantastic time here | 0:28:13 | 0:28:15 | |
so thank you to everyone who stayed with us. | 0:28:15 | 0:28:18 | |
That's thanks to the Flamsteed Astronomical Society | 0:28:18 | 0:28:20 | |
and the Baker Street Irregular Astronomers. | 0:28:20 | 0:28:23 | |
When we come back next month, we'll be heading for the clear skies | 0:28:23 | 0:28:25 | |
of La Palma in the Canary Islands, hoping to find a bright comet. | 0:28:25 | 0:28:29 | |
So until next month, good night | 0:28:29 | 0:28:32 | |
Subtitles by Red Bee Media Ltd | 0:28:40 | 0:28:42 |