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Hello! | 0:00:35 | 0:00:37 | |
And welcome to the UK Space Cluster here in Harwell, Oxfordshire. | 0:00:37 | 0:00:40 | |
Our robotic friend here is called Rimmer, and he's an intelligent robot | 0:00:40 | 0:00:44 | |
that's testing software that might one day run on the surface of Mars. | 0:00:44 | 0:00:48 | |
But of course, we've already got robots on the Red Planet. | 0:00:48 | 0:00:51 | |
The most recent and most powerful of them, | 0:00:51 | 0:00:53 | |
curiosity, is celebrating its first year on the Martian surface. | 0:00:53 | 0:00:58 | |
We'll be taking a look at the highlights from that first year, | 0:00:58 | 0:01:01 | |
but also finding out what it will take to get humans to | 0:01:01 | 0:01:04 | |
survive on the Red Planet. | 0:01:04 | 0:01:06 | |
Chris North will be meeting some of Rimmer's family, and Pete Lawrence | 0:01:06 | 0:01:09 | |
will be giving us tips about how to take part in the Moore Moon Marathon. | 0:01:09 | 0:01:13 | |
But first, we're off to Mars. | 0:01:13 | 0:01:16 | |
Mars. The Red Planet, and object of our fascination. | 0:01:19 | 0:01:24 | |
Since the 1960s, we've sent numerous spacecraft, landers, | 0:01:26 | 0:01:30 | |
and robots, all trying to tell us | 0:01:30 | 0:01:33 | |
more about a world which might once have been like Earth. | 0:01:33 | 0:01:38 | |
Long ago, billions of years, | 0:01:38 | 0:01:40 | |
we think there were seas on Mars, and even a thick atmosphere. | 0:01:40 | 0:01:45 | |
But Mars lost its magnetic field, | 0:01:45 | 0:01:47 | |
leaving it exposed to the corrosive power of the solar wind. | 0:01:47 | 0:01:52 | |
It seems that most of its atmosphere was stripped away | 0:01:52 | 0:01:55 | |
in the first billion years. | 0:01:55 | 0:01:58 | |
The oceans have long since disappeared, | 0:01:58 | 0:02:01 | |
leaving a seemingly dry and dusty world. | 0:02:01 | 0:02:04 | |
But is it dead? | 0:02:04 | 0:02:06 | |
Like detectives to a crime scene, we are sending missions to | 0:02:06 | 0:02:10 | |
Mars to find evidence that the conditions for life once existed. | 0:02:10 | 0:02:14 | |
Chris and I have come to the Catapult Centre at Harwell. | 0:02:16 | 0:02:20 | |
We're going to start our exploration of Mars by talking | 0:02:20 | 0:02:23 | |
about the European spacecraft Mars Express. | 0:02:23 | 0:02:27 | |
It celebrates 10 years of amazing stereo images which should | 0:02:27 | 0:02:31 | |
look great on the video wall. | 0:02:31 | 0:02:33 | |
Anu Olja, from the National Space Centre, joins us, | 0:02:35 | 0:02:38 | |
as well as Louisa Preston, a planetary geologist. | 0:02:38 | 0:02:42 | |
They use spacecraft images to tell us what Mars is like now | 0:02:42 | 0:02:45 | |
and investigate how these features may have formed. | 0:02:45 | 0:02:49 | |
The real joy of Mars Express is that over its 10 years, | 0:02:50 | 0:02:54 | |
we've seen pretty much all of the planet. | 0:02:54 | 0:02:56 | |
We get a global view of what's going on. | 0:02:56 | 0:02:58 | |
Now, this isn't a Mars Express image, this is from Viking, | 0:02:58 | 0:03:01 | |
but you can see Mars in all its glory. | 0:03:01 | 0:03:03 | |
The volcanoes here, and there's so much more here, isn't there, Anu? | 0:03:03 | 0:03:06 | |
Yeah, it's a gorgeous image. | 0:03:06 | 0:03:08 | |
We've got this enormous crack in Mars' crust. | 0:03:08 | 0:03:11 | |
This is Valles Marineris. | 0:03:11 | 0:03:13 | |
It's 4,000 kilometres long, and this really brings | 0:03:13 | 0:03:17 | |
home how on Mars, it's as if plate tectonics were struggling to | 0:03:17 | 0:03:21 | |
get started, but the internal heat engine that was driving | 0:03:21 | 0:03:24 | |
the system on Earth, the parallel on Mars never got enough energy | 0:03:24 | 0:03:28 | |
to really kick off the process. | 0:03:28 | 0:03:30 | |
And what's really nice is that Valles Marineris, of course, | 0:03:30 | 0:03:32 | |
anyone can see through a small telescope, | 0:03:32 | 0:03:34 | |
so it's really something to get out and have a look at. | 0:03:34 | 0:03:36 | |
But we've selected some images from Mars Express. | 0:03:36 | 0:03:39 | |
So, let's have a zoom-in now, | 0:03:39 | 0:03:40 | |
and look at some of the particular features on the surface. | 0:03:40 | 0:03:43 | |
This is impressive. Where are we, and what are we looking at? | 0:03:43 | 0:03:46 | |
A region called Candor Chasma. | 0:03:46 | 0:03:48 | |
And what I love about this image is that | 0:03:48 | 0:03:50 | |
although we've got this giant rift valley, | 0:03:50 | 0:03:52 | |
when we start to look closely here, we get images that we | 0:03:52 | 0:03:55 | |
think are associated with flowing water, billions of years ago. | 0:03:55 | 0:03:59 | |
The stuff that makes us really interested is what you | 0:03:59 | 0:04:01 | |
see on the edges of these valleys, all these gullies. | 0:04:01 | 0:04:04 | |
So, on Earth, we get gullies because of flowing water. | 0:04:04 | 0:04:07 | |
So, these might have been carved by past water activity, which is | 0:04:07 | 0:04:10 | |
obviously very interesting for us. | 0:04:10 | 0:04:12 | |
So, how old is this landscape? | 0:04:12 | 0:04:14 | |
When did Valles Marineris form, | 0:04:14 | 0:04:16 | |
and when would there have been water flowing down its sides? | 0:04:16 | 0:04:19 | |
This would have been very early in Mars' history. | 0:04:19 | 0:04:21 | |
This would have been 3.5 to 3.8 billion years ago. | 0:04:21 | 0:04:24 | |
So, this is an ancient Martian landscape. | 0:04:24 | 0:04:27 | |
However, some of the gullies have been identified as being much | 0:04:27 | 0:04:30 | |
-more recent in origin, am I right, Louisa? -Yes! | 0:04:30 | 0:04:32 | |
We've done time-lapse images over a period of a year and you | 0:04:32 | 0:04:36 | |
can see deposits, light-tone deposits, | 0:04:36 | 0:04:38 | |
that are potentially related to water, that come and go | 0:04:38 | 0:04:40 | |
with the season, so there might still be activity in the | 0:04:40 | 0:04:44 | |
water sense, underneath the surface that's coming out in these gullies. | 0:04:44 | 0:04:47 | |
So, where are we now? | 0:04:47 | 0:04:49 | |
This is a crater called Holden Crater and geologically, | 0:04:49 | 0:04:52 | |
-this is an absolute treasure trove of geological discovery. -Yes. | 0:04:52 | 0:04:56 | |
No, absolutely. I mean, you can see impact craters. | 0:04:56 | 0:04:59 | |
Now, this whole area as one giant impact crater, | 0:04:59 | 0:05:01 | |
but you've got smaller impact craters inside the larger one, | 0:05:01 | 0:05:03 | |
so it can help you to date it. | 0:05:03 | 0:05:05 | |
You know that the craters inside the large one are obviously younger. | 0:05:05 | 0:05:08 | |
So, you know that area is younger, which is really interesting. | 0:05:08 | 0:05:11 | |
And we have evidence of potential river systems. | 0:05:11 | 0:05:13 | |
We assume that they could be carved by water simply because | 0:05:13 | 0:05:16 | |
they look like things we see on Earth, | 0:05:16 | 0:05:18 | |
and that's our point of reference. | 0:05:18 | 0:05:19 | |
How well does that intuition hold up when you go to Mars? | 0:05:19 | 0:05:22 | |
It holds up really well. | 0:05:22 | 0:05:23 | |
Actually, Mars can tell us a lot about the Earth as well. | 0:05:23 | 0:05:25 | |
The problem is, when we see river channels on Earth, | 0:05:25 | 0:05:28 | |
we've trees in the way, plants, buildings, | 0:05:28 | 0:05:30 | |
we've got so many things actually in the way. | 0:05:30 | 0:05:32 | |
So, we only get a general idea of what river channels are doing. | 0:05:32 | 0:05:35 | |
You study Mars, you recognise them, and you learn an awful lot more. | 0:05:35 | 0:05:38 | |
So, this is the geologists' favourite planet, | 0:05:38 | 0:05:40 | |
there is no biology, there's no... | 0:05:40 | 0:05:42 | |
No, absolutely, this is a geologist's playground, it's brilliant. | 0:05:42 | 0:05:45 | |
If we go to the next image, then you'll see a close-up of, well, | 0:05:45 | 0:05:48 | |
look at that! | 0:05:48 | 0:05:49 | |
That must be an ancient... It looks like the riverbed to me. | 0:05:49 | 0:05:52 | |
It looks like I'm about to get my feet wet. | 0:05:52 | 0:05:55 | |
Is that's what I'm looking at? | 0:05:55 | 0:05:56 | |
Yes, you're basically looking at an extremely large river channel | 0:05:56 | 0:05:59 | |
and you can see all the different evidence of different flood | 0:05:59 | 0:06:02 | |
episodes, different river episodes, | 0:06:02 | 0:06:03 | |
you can see circular patterns that might be evidence of ghost craters | 0:06:03 | 0:06:07 | |
that were once there and there have been covered with sediments since. | 0:06:07 | 0:06:10 | |
Next image, where are we going next? Oh, yes! Now, this one. | 0:06:10 | 0:06:12 | |
Now, this is about the same scale, isn't it? | 0:06:12 | 0:06:15 | |
This is what I like to think of as effectively one of the largest | 0:06:15 | 0:06:18 | |
skating rinks in the solar system. | 0:06:18 | 0:06:20 | |
It's a crater about 35 kilometres across in the Martian High Arctic. | 0:06:20 | 0:06:25 | |
We've got water-ice as, effectively, a lake here, | 0:06:25 | 0:06:28 | |
and then on the edges here, it's probably water-frost, | 0:06:28 | 0:06:31 | |
or it's water-ice, that's been left there. | 0:06:31 | 0:06:33 | |
And of course, this is why Mars fascinates us so much. | 0:06:33 | 0:06:35 | |
We've all of these features that we've seen geologically that suggest | 0:06:35 | 0:06:39 | |
that billions of years ago, we had running water on Mars's surface, | 0:06:39 | 0:06:42 | |
which couldn't happen now, the air pressure's too low. | 0:06:42 | 0:06:45 | |
So, we need to try to understand, | 0:06:45 | 0:06:47 | |
A - what happened to Mars' atmosphere to change it | 0:06:47 | 0:06:49 | |
from this much more Earth-like world in the past? | 0:06:49 | 0:06:52 | |
And, B - if it lost its atmosphere, | 0:06:52 | 0:06:54 | |
what happened to the water content, | 0:06:54 | 0:06:57 | |
which is one of the other key foci of Mars Express? | 0:06:57 | 0:07:01 | |
And of course, Mars Express has found a lot of | 0:07:01 | 0:07:04 | |
frozen water on the planet and I was reading that | 0:07:04 | 0:07:06 | |
if the water was now to melt in all the craters, it would form | 0:07:06 | 0:07:10 | |
an ocean that was about 11 metres deep, which I think is a lovely way | 0:07:10 | 0:07:13 | |
of visualising the potential of Mars if it only had the atmosphere again. | 0:07:13 | 0:07:17 | |
As incredible as spacecraft images are, | 0:07:19 | 0:07:22 | |
nothing beats getting on the surface. | 0:07:22 | 0:07:26 | |
Robots have been scratching and sniffing Mars since 1976, looking | 0:07:26 | 0:07:31 | |
for evidence of water and organics, the building blocks of life. | 0:07:31 | 0:07:36 | |
Curiosity is NASA's latest mission, which landed a year ago. | 0:07:36 | 0:07:41 | |
It's the size of a small car with a plutonium power pack | 0:07:41 | 0:07:45 | |
and a whole suite of amazing instruments. | 0:07:45 | 0:07:49 | |
Its arrival at Mars was incredible and described as | 0:07:49 | 0:07:53 | |
"seven minutes of terror" with a landing platform, | 0:07:53 | 0:07:57 | |
jet thrusters, and a sky crane. | 0:07:57 | 0:07:59 | |
The relief and jubilation | 0:07:59 | 0:08:00 | |
when it touched down and opened its stereoscopic eyes was immense. | 0:08:00 | 0:08:05 | |
-MISSION CONTROL: -'Touchdown confirmed.' | 0:08:05 | 0:08:08 | |
This is the panorama of the landing site. | 0:08:08 | 0:08:11 | |
You can see Mount Sharp far off in the distance, | 0:08:11 | 0:08:14 | |
and also the scars left on the surface | 0:08:14 | 0:08:17 | |
from where Curiosity came down. | 0:08:17 | 0:08:19 | |
Now, since landing, the rover hasn't travelled very far, | 0:08:19 | 0:08:21 | |
one kilometre across the surface, in fact. | 0:08:21 | 0:08:24 | |
But even so, the rover has been incredibly busy. | 0:08:24 | 0:08:27 | |
It has. The reason it's taken so long to get going is | 0:08:27 | 0:08:30 | |
because it had to test out all of the instruments that it has on board. | 0:08:30 | 0:08:33 | |
One of the first to get a workout was its famous laser, | 0:08:33 | 0:08:37 | |
situated atop the mast and used for vaporising rocks. | 0:08:37 | 0:08:41 | |
It worked brilliantly, | 0:08:41 | 0:08:42 | |
and the team have been happily zapping things on Mars ever since. | 0:08:42 | 0:08:46 | |
There's also been a workout for the two metre-long robotic arm. | 0:08:46 | 0:08:50 | |
It's been stretched and flexed | 0:08:50 | 0:08:51 | |
and the movements have been checked and tested. | 0:08:51 | 0:08:54 | |
But in February, Curiosity tested what is probably its most | 0:08:54 | 0:08:57 | |
exciting tool, the drill that sits on the end of the robotic arm. | 0:08:57 | 0:09:01 | |
The drill allows us to get beneath the surface, taking samples from | 0:09:01 | 0:09:05 | |
the insides of rocks for the first time on a planet other than Earth. | 0:09:05 | 0:09:09 | |
Ultimately, Curiosity has its sights set on the foothills | 0:09:09 | 0:09:12 | |
of Mount Sharp, eight kilometres away. | 0:09:12 | 0:09:15 | |
But en route, it's been going through some incredibly | 0:09:15 | 0:09:18 | |
interesting science. | 0:09:18 | 0:09:19 | |
John Bridges, from Leicester University, works on CheMin, | 0:09:21 | 0:09:24 | |
the instrument which analyses rocks and soil, telling us what | 0:09:24 | 0:09:28 | |
they're made of and in particular, | 0:09:28 | 0:09:30 | |
if the conditions for life are there. | 0:09:30 | 0:09:33 | |
Curiosity is sending back stunning panoramas. | 0:09:33 | 0:09:37 | |
John and Louisa join us | 0:09:37 | 0:09:39 | |
to analyse the latest stage of this incredible journey. | 0:09:39 | 0:09:43 | |
Well, this is the marvellous view from inside Gale Crater, | 0:09:44 | 0:09:47 | |
from Curiosity's recent image. | 0:09:47 | 0:09:49 | |
You can see all sorts of things in this landscape. | 0:09:49 | 0:09:52 | |
So, John, give us a brief tour. | 0:09:52 | 0:09:54 | |
Well, we're looking down there into Yellowknife Bay. | 0:09:54 | 0:09:56 | |
We've been driving down from our landing site over there. | 0:09:56 | 0:09:59 | |
Down here, and then we went down the slope, | 0:09:59 | 0:10:01 | |
down the river bed, if you like, into Yellowknife Bay. | 0:10:01 | 0:10:03 | |
Why are we actually here, Louisa? | 0:10:03 | 0:10:05 | |
Why is this the region for Curiosity to study? | 0:10:05 | 0:10:09 | |
So, impact craters in general are fantastic sites. | 0:10:09 | 0:10:11 | |
They allow us to look back into the history of a planet, | 0:10:11 | 0:10:13 | |
due to the sheer act of an impact crater being formed. | 0:10:13 | 0:10:16 | |
-Cos they pulled stuff up from underneath? -Yep, and they eject it everywhere. | 0:10:16 | 0:10:20 | |
It's also good because from orbit, | 0:10:20 | 0:10:22 | |
we had a look and could see evidence of clay minerals, | 0:10:22 | 0:10:24 | |
and different types of minerals that would need water to form. | 0:10:24 | 0:10:27 | |
And also these minerals are very good at preserving | 0:10:27 | 0:10:29 | |
evidence of organic markers. | 0:10:29 | 0:10:31 | |
And so, we get to study this area to try | 0:10:31 | 0:10:33 | |
and find evidence of habitability. | 0:10:33 | 0:10:35 | |
And you can even see evidence in that image of some of the first scoops that got tested. | 0:10:35 | 0:10:39 | |
Let's move on to look at some of the more detailed pictures | 0:10:39 | 0:10:42 | |
that we're getting coming back. | 0:10:42 | 0:10:43 | |
We landed in a place that we call Peace Vallis, which is | 0:10:43 | 0:10:46 | |
an ancient riverbed. | 0:10:46 | 0:10:47 | |
Got right up close with our robotic arm and the mast-cam, | 0:10:47 | 0:10:50 | |
and of course, the characteristics of an ancient riverbed on Earth. | 0:10:50 | 0:10:53 | |
We found lots of little rounded clasps. | 0:10:53 | 0:10:56 | |
Is that what I'm looking at in the outcrop, but also underneath? | 0:10:56 | 0:10:59 | |
-The rounded pebbles. -Yes. Some of them have fallen down. | 0:10:59 | 0:11:01 | |
-And we think they were carried along by water? -Yes. | 0:11:01 | 0:11:04 | |
And they get rounded by being in this water. | 0:11:04 | 0:11:06 | |
They move around with each other, hit each other, | 0:11:06 | 0:11:08 | |
and they get abraded, that's how they become round. | 0:11:08 | 0:11:11 | |
-Which is why you find round pebbles on the beach. -Absolutely. | 0:11:11 | 0:11:13 | |
Exactly the same. | 0:11:13 | 0:11:15 | |
So, that's an indicator that water was definitely involved in this. | 0:11:15 | 0:11:18 | |
And so, I think I'm right in saying, | 0:11:18 | 0:11:19 | |
that Curiosity then wandered off down this riverbed | 0:11:19 | 0:11:22 | |
and I think the next image will take us a little further along. Oh, wow! | 0:11:22 | 0:11:26 | |
-Best image! -Look at that! -This is spectacular. | 0:11:26 | 0:11:29 | |
So, this is Yellowknife Bay, if I've got my bearings right. | 0:11:29 | 0:11:33 | |
This is the site for some of | 0:11:33 | 0:11:35 | |
Curiosity's most involved investigations. | 0:11:35 | 0:11:38 | |
Lo and behold, we have found clay. | 0:11:38 | 0:11:39 | |
In the two drill sites that we have, we found clay in both places. | 0:11:39 | 0:11:43 | |
Clay is the thing that gets people really excited. So, why is that? | 0:11:43 | 0:11:46 | |
Well, clay must form in the presence of water, so, if we want | 0:11:46 | 0:11:49 | |
to determine if this was a habitable environment, that's a key indicator. | 0:11:49 | 0:11:54 | |
We really need to study the composition of the clays. | 0:11:54 | 0:11:58 | |
They can preserve evidence of organic molecules, | 0:11:58 | 0:12:01 | |
biosignatures, even life, potentially. | 0:12:01 | 0:12:03 | |
So, by studying the clays, you might be able to find these elusive | 0:12:03 | 0:12:06 | |
organic compounds that we've been looking for. | 0:12:06 | 0:12:09 | |
-OK, let's move on to the next image. -Ahh! | 0:12:09 | 0:12:11 | |
So, this is what you are referring to, the clays that you see | 0:12:11 | 0:12:15 | |
just under the surface. It's amazing. | 0:12:15 | 0:12:17 | |
For so long, we've been thinking of Mars as the Red Planet, | 0:12:17 | 0:12:20 | |
but just under the surface, it's not as oxidised. | 0:12:20 | 0:12:24 | |
Yeah. Basically, you just go down centimetres, | 0:12:24 | 0:12:26 | |
and Mars is very different. | 0:12:26 | 0:12:28 | |
What I think is absolutely wonderful is that it's our first drill hole. | 0:12:28 | 0:12:31 | |
The first drill hole that we do on another planetary body, | 0:12:31 | 0:12:34 | |
we actually find our science goal, | 0:12:34 | 0:12:36 | |
finding a habitable environment, so, it's relatively easy. | 0:12:36 | 0:12:39 | |
It's about the instruments. That's the key thing. | 0:12:39 | 0:12:41 | |
It's almost like a preliminary mission. | 0:12:41 | 0:12:43 | |
This mission's going to tell us where to go and what exists, then | 0:12:43 | 0:12:46 | |
we can send a mission on afterwards to properly look for life. | 0:12:46 | 0:12:49 | |
Curiosity will spend the coming months getting to Mount Sharp, | 0:12:50 | 0:12:55 | |
where there are layers of rock, | 0:12:55 | 0:12:57 | |
each containing a chapter of Mars' ancient past. | 0:12:57 | 0:13:01 | |
Who knows what it will tell us? | 0:13:01 | 0:13:04 | |
Manned exploration of Mars is still the Holy Grail though. | 0:13:04 | 0:13:08 | |
When will WE be the ones to scratch and sniff the surface? | 0:13:08 | 0:13:11 | |
Since we landed on the moon, Mars has been our next destination. | 0:13:12 | 0:13:17 | |
Ideas for how to get to Mars | 0:13:17 | 0:13:19 | |
and live there seem to never get off the drawing board. | 0:13:19 | 0:13:23 | |
Mars seems always just around the corner. | 0:13:23 | 0:13:25 | |
Just how close are we to sending humans? | 0:13:26 | 0:13:29 | |
It's doable, but it's pushing our technology to the limits. | 0:13:29 | 0:13:32 | |
There are three main challenges for a human mission. | 0:13:32 | 0:13:34 | |
Number one, the duration. | 0:13:34 | 0:13:36 | |
Two years, approximately, away from home, there and back. | 0:13:36 | 0:13:39 | |
Secondly, surviving the radiation levels that you'll get. | 0:13:39 | 0:13:42 | |
It's survivable, but it's going to pose major challenges. | 0:13:42 | 0:13:46 | |
And finally, there's the business of landing on Mars in one piece. | 0:13:46 | 0:13:49 | |
Because, of course, it's got enough of an atmosphere that you can't | 0:13:49 | 0:13:52 | |
use an approach like we did with Apollo, | 0:13:52 | 0:13:54 | |
but the atmosphere is so tenuous, you can't just rely on parachutes. | 0:13:54 | 0:13:57 | |
So, technologically, it's feasible, | 0:13:57 | 0:14:00 | |
but it is pushing the envelope right out to its limits. | 0:14:00 | 0:14:03 | |
My fear is that I won't see it, but I'm going to be an optimist. | 0:14:03 | 0:14:06 | |
-2030s, international mission. -Louisa? | 0:14:06 | 0:14:08 | |
I can't necessarily say in my opinion | 0:14:08 | 0:14:10 | |
when humans will get to Mars. We've already sent robots. | 0:14:10 | 0:14:13 | |
I think the preparations for humans on Mars could happen | 0:14:13 | 0:14:16 | |
any time now. We can start sending the robots to start gardens on Mars. | 0:14:16 | 0:14:20 | |
We can start sending the cargo ships to set up habitats. | 0:14:20 | 0:14:23 | |
So, hopefully, | 0:14:23 | 0:14:24 | |
we'll be seeing that in the next couple of decades, for sure. | 0:14:24 | 0:14:27 | |
Mars fires the imagination. | 0:14:27 | 0:14:30 | |
It's human nature to endeavour towards the next era of exploration. | 0:14:30 | 0:14:35 | |
To get there requires investment, risk, | 0:14:35 | 0:14:38 | |
and cooperation, which we are not yet ready for. | 0:14:38 | 0:14:42 | |
For the moment, we shall have to use rovers | 0:14:42 | 0:14:45 | |
as our avatars on alien worlds. | 0:14:45 | 0:14:47 | |
Chris North is hunting down the next generation of Martian invaders. | 0:14:48 | 0:14:52 | |
I've come to find a little piece of Mars, and to meet Bridget. | 0:14:55 | 0:14:59 | |
Bridget is Europe's prototype for the mission called ExoMars. | 0:15:01 | 0:15:05 | |
She's come to test her wheels in the Mars Yard. | 0:15:05 | 0:15:08 | |
Bridget is getting a little elderly. | 0:15:13 | 0:15:15 | |
Superseded by younger models Bruno and Bradley, | 0:15:15 | 0:15:19 | |
but she's still got a bit of get up and go. | 0:15:19 | 0:15:21 | |
Today, she's being kitted out with a new instrument, and later in | 0:15:21 | 0:15:25 | |
the year, she's off for some field expeditions in the Chilean desert. | 0:15:25 | 0:15:29 | |
ExoMars will have a two metre drill to probe deep underground | 0:15:30 | 0:15:34 | |
where life might still exist. | 0:15:34 | 0:15:37 | |
Abigail Hutty is part of the team putting Bridget through her paces. | 0:15:37 | 0:15:41 | |
Yes, we're looking for any kind of organic molecules. | 0:15:42 | 0:15:46 | |
We'd love to find microbes or bacteria or something there, but any | 0:15:46 | 0:15:50 | |
kind of indicator of past or present life would be fantastic to find. | 0:15:50 | 0:15:54 | |
As well as the drill, what other stuff is it going to have on board? | 0:15:54 | 0:15:57 | |
So, obviously, we've got lots of different visual systems | 0:15:57 | 0:15:59 | |
so we can actually, pictorially, classify the Martian environment. | 0:15:59 | 0:16:04 | |
We've also got loads of spectrometers on board | 0:16:04 | 0:16:06 | |
so that we can analyse our sample to see what kind of chemical composition | 0:16:06 | 0:16:10 | |
there is of the rocks and any sands or anything else that we pick up. | 0:16:10 | 0:16:15 | |
We've got the ground-penetrating radar, | 0:16:15 | 0:16:17 | |
so that can look for icy deposits beneath the surface, | 0:16:17 | 0:16:20 | |
or different types of rocks, and their densities beneath the surface. | 0:16:20 | 0:16:24 | |
How fast do you think ExoMars is going to be able to travel? | 0:16:24 | 0:16:27 | |
Well, really the thing that prevents us | 0:16:27 | 0:16:29 | |
from going top speed is our autonomous navigation. | 0:16:29 | 0:16:34 | |
So, we've actually got to be able to process the visual | 0:16:34 | 0:16:38 | |
scene in front of us, make that into a map, classify things | 0:16:38 | 0:16:41 | |
as a dangerous area or a safe area and then plan the course through. | 0:16:41 | 0:16:45 | |
That's why we can't travel any faster than the speed that we're going to. | 0:16:45 | 0:16:49 | |
Aron Kisdi is designing intelligent robots who can | 0:16:52 | 0:16:55 | |
decide where to go and what to look at for themselves. | 0:16:55 | 0:16:59 | |
He envisages mother robots | 0:16:59 | 0:17:01 | |
with little scouts who scurry around and report back. | 0:17:01 | 0:17:04 | |
So, looking at the far future, we really need to send missions | 0:17:06 | 0:17:10 | |
up there which utilise multiple rovers. | 0:17:10 | 0:17:13 | |
Now, in my opinion, I think we want these rovers to collaborate | 0:17:13 | 0:17:17 | |
and work together to achieve the mission. | 0:17:17 | 0:17:20 | |
So, you could have one large rover like this one | 0:17:20 | 0:17:22 | |
and then smaller explorers, spreading out from it, looking | 0:17:22 | 0:17:27 | |
at the terrain ahead, making sure that the big rover has safe passage. | 0:17:27 | 0:17:32 | |
And this way, we can move much faster and move safer | 0:17:32 | 0:17:35 | |
and in case some of them fail or get damaged on the way, | 0:17:35 | 0:17:39 | |
or get stuck, then they should be able to help each other out, | 0:17:39 | 0:17:43 | |
to still achieve the goal. And that way, | 0:17:43 | 0:17:45 | |
you get a much more robust mission than just with a single rover. | 0:17:45 | 0:17:50 | |
What kind of things do you think you'll be able to ask them | 0:17:50 | 0:17:53 | |
to do on their own? I mean, apart from just drive around. | 0:17:53 | 0:17:55 | |
Mars is huge. You have the same landmass as on Earth. | 0:17:55 | 0:18:00 | |
So, we really need rovers to grow faster | 0:18:00 | 0:18:02 | |
and explore more of the surface. | 0:18:02 | 0:18:05 | |
Something I'm very interested in is cave entrances. | 0:18:05 | 0:18:09 | |
We know that there are some cave entrances on Mars. | 0:18:09 | 0:18:12 | |
We have seen them from orbit, but we have never seen a close-up image. | 0:18:12 | 0:18:16 | |
If we can design rovers which can move quicker by themselves, | 0:18:16 | 0:18:18 | |
they can get to these entrances easier or potentially | 0:18:18 | 0:18:21 | |
discover more, smaller ones, | 0:18:21 | 0:18:23 | |
and once we have a close-up of them, we can design a mission | 0:18:23 | 0:18:27 | |
to send a rover inside one of these caves and see what's | 0:18:27 | 0:18:31 | |
hiding beneath the surface of Mars. | 0:18:31 | 0:18:33 | |
-Wow. So, not just driving on Mars, caving on Mars. -Ha-ha! Absolutely. | 0:18:33 | 0:18:37 | |
Until recently, no-one could have believed that robots would | 0:18:38 | 0:18:41 | |
make such great strides on Mars. | 0:18:41 | 0:18:44 | |
But it will be some time before Man is able to scrutinise | 0:18:44 | 0:18:47 | |
the Martian soil for himself. | 0:18:47 | 0:18:49 | |
In the meantime, we shall have to watch our robot envoys with | 0:18:49 | 0:18:53 | |
envious eyes from across the gulf of space. | 0:18:53 | 0:18:56 | |
But there is one world mankind has been to - the moon. | 0:18:57 | 0:19:02 | |
Last month, we launched our Moore Moon Marathon, | 0:19:02 | 0:19:04 | |
and I've certainly enjoyed | 0:19:04 | 0:19:06 | |
keeping an eye on what the moon has been up to over the last few weeks. | 0:19:06 | 0:19:09 | |
But don't worry, you've got the rest of the summer to enter. | 0:19:09 | 0:19:12 | |
Pete Lawrence and Jon Culshaw have been down to Chipping Norton | 0:19:12 | 0:19:16 | |
to see how the people there have been getting along. | 0:19:16 | 0:19:18 | |
On this balmy summer's evening, Pete and I have joined some | 0:19:21 | 0:19:25 | |
astronomers from the Chipping Norton Amateur Astronomical Group. | 0:19:25 | 0:19:28 | |
They meet in the place called the Rollrights, which is | 0:19:28 | 0:19:32 | |
a collection of impressive Neolithic and Bronze Age stones. | 0:19:32 | 0:19:36 | |
Atmospheric and oozing with history. | 0:19:36 | 0:19:39 | |
One of the things I hope we're going to have a go at tonight is the | 0:19:39 | 0:19:42 | |
Moore Moon Marathon. I've spotted the moon. | 0:19:42 | 0:19:45 | |
It's just above the trees over there. | 0:19:45 | 0:19:47 | |
So, you can see the moon in daylight. | 0:19:47 | 0:19:49 | |
It's not particularly prominent, because the sky is very bright. | 0:19:49 | 0:19:52 | |
With great perspicacity, | 0:19:52 | 0:19:54 | |
you spotted the moon just a few moments ago between those clouds. | 0:19:54 | 0:19:57 | |
As the evening goes on, the sky will get darker, | 0:19:57 | 0:19:59 | |
the moon will be a lot more obvious, and it'll sort of roll across | 0:19:59 | 0:20:02 | |
the horizon and set over there, so, we should get a really good view. | 0:20:02 | 0:20:05 | |
CHATTING AND LAUGHTER | 0:20:08 | 0:20:10 | |
Well, the sky darkening and the moon becoming more vivid every moment, | 0:20:14 | 0:20:18 | |
and the cloud clearing as well, so here is your documentation. | 0:20:18 | 0:20:22 | |
Let me give you this, | 0:20:22 | 0:20:24 | |
so you can log down your findings in the Moore Moon Marathon. | 0:20:24 | 0:20:28 | |
It's like giving out the hymn sheets, it's rather nice, isn't it? | 0:20:28 | 0:20:31 | |
With these, you can map the moon on your own terms. | 0:20:31 | 0:20:35 | |
The naked eye, lunar seas first, and you can tick them off there, you can | 0:20:35 | 0:20:38 | |
upgrade to the binocular objects, the bright and dark craters, | 0:20:38 | 0:20:41 | |
quite a few of those will be visible. | 0:20:41 | 0:20:44 | |
Ah, we have a fellow Time Lord in our midst! | 0:20:44 | 0:20:46 | |
This shouldn't happen, only in the gravest of emergencies. | 0:20:46 | 0:20:49 | |
-It is the Moore Moon Marathon. Here is the documentation. -Thank you. | 0:20:49 | 0:20:53 | |
Some of these here, lunar specials, I don't know whether you can see | 0:20:53 | 0:20:56 | |
the face of the Old Lady in the moon, or the basketball player. | 0:20:56 | 0:21:00 | |
Mark them down on your very own chart, that Pete Lawrence made | 0:21:00 | 0:21:03 | |
-so brilliantly. -Lovely. Thank you very much. | 0:21:03 | 0:21:06 | |
Excellent. Well done, my dears. Well done. | 0:21:06 | 0:21:10 | |
Oh, sorry. | 0:21:10 | 0:21:12 | |
THEY LAUGH | 0:21:12 | 0:21:13 | |
We've just had the most beautiful sunset and the moon now very | 0:21:17 | 0:21:21 | |
vivid, very sharp-looking, perfect time to get started | 0:21:21 | 0:21:24 | |
on making the observations, so, where would be a good place to begin? | 0:21:24 | 0:21:27 | |
We've got five different sections with the Moore Moon Marathon. | 0:21:27 | 0:21:30 | |
They're sort of designed to get a bit harder as you go through them. | 0:21:30 | 0:21:33 | |
But there's another factor you have to take on board | 0:21:33 | 0:21:35 | |
and that's the phase of the moon. | 0:21:35 | 0:21:37 | |
Some of the bits and pieces can only be seen when the moon is either | 0:21:37 | 0:21:40 | |
full or beyond the full phase, which is a bit sneaky, isn't it? | 0:21:40 | 0:21:43 | |
It's always good to have those you've got to work for. | 0:21:43 | 0:21:45 | |
You've got to work for a few of them. | 0:21:45 | 0:21:47 | |
But the lunar seas, there's plenty of lunar seas | 0:21:47 | 0:21:49 | |
which are visible at the moment up there, and I think it would | 0:21:49 | 0:21:52 | |
be nice to go along and see how many people can pick those out | 0:21:52 | 0:21:54 | |
with their eyes, because that's a bit of a challenge on its own. | 0:21:54 | 0:21:57 | |
And what else can we look for? | 0:21:57 | 0:21:58 | |
We've got the bright and dark craters. | 0:21:58 | 0:22:01 | |
There are quite a number of those visible at the moment. | 0:22:01 | 0:22:04 | |
Tycho, that beautiful ray crater in the southern part of the moon, | 0:22:04 | 0:22:08 | |
doesn't look like much of a ray crater at the moment, | 0:22:08 | 0:22:10 | |
because you can't see those rays, can you? | 0:22:10 | 0:22:12 | |
That was so surprising. When it's full, you see all of the streams, | 0:22:12 | 0:22:15 | |
-it's not in shadow so much. -That's right. | 0:22:15 | 0:22:17 | |
But it is still quite prominent, isn't it? | 0:22:17 | 0:22:20 | |
You can pick it out quite well. | 0:22:20 | 0:22:21 | |
But also, because you can see half of the moon at the moment, | 0:22:21 | 0:22:24 | |
there's the Lady In the moon. | 0:22:24 | 0:22:26 | |
I can actually see the Lady if I look with the naked eye. | 0:22:26 | 0:22:28 | |
You can see her there, you can see her hair up there, her profile. | 0:22:28 | 0:22:31 | |
She's very grandmotherly, rather Victorian, isn't she? | 0:22:31 | 0:22:34 | |
Yeah, I think so. | 0:22:34 | 0:22:35 | |
Or, more chillingly, I don't know whether you've spotted this... | 0:22:35 | 0:22:38 | |
You've just ruined the Lady In the moon! | 0:22:40 | 0:22:42 | |
You've turned her into the Cyber-Lady In the moon! | 0:22:42 | 0:22:45 | |
From the William Hartnell era of Doctor Who, she's a Cyberman. | 0:22:46 | 0:22:50 | |
That's actually very, very scary, | 0:22:50 | 0:22:52 | |
because that's quite close to what it looks like. | 0:22:52 | 0:22:55 | |
That's ruined it for me, completely. | 0:22:55 | 0:22:57 | |
I'm sorry, Pete. Sorry. | 0:22:57 | 0:22:59 | |
Let's see how everyone is progressing with the Moore Moon Marathon. | 0:23:02 | 0:23:06 | |
So, Rose, you've just had your first successful spot. | 0:23:08 | 0:23:12 | |
-What was it that you saw? -We've just seen Copernicus. | 0:23:12 | 0:23:16 | |
Oh, yes, it's looking very, very bright today. | 0:23:16 | 0:23:19 | |
It's a perfect night for it. So, you've ticked that off. | 0:23:19 | 0:23:22 | |
So, what are you going to look for next? | 0:23:22 | 0:23:24 | |
Well, Mummy said that we should maybe look for Plato next. | 0:23:24 | 0:23:27 | |
So, you've done all the seas, and now you're onto this bit. | 0:23:27 | 0:23:30 | |
So, well done, you. You'll have it done before the night's out! | 0:23:30 | 0:23:33 | |
And there's another challenge afoot tonight. | 0:23:35 | 0:23:38 | |
The best shot of the moon through a mobile phone. | 0:23:38 | 0:23:42 | |
I might have a go at this one myself. | 0:23:42 | 0:23:44 | |
Wow. That is a wonderful shot there. | 0:23:45 | 0:23:48 | |
We're turning the phone on. | 0:23:48 | 0:23:50 | |
And we're really just balancing it over the top of the eyepiece | 0:23:50 | 0:23:54 | |
and already getting a lovely view. | 0:23:54 | 0:23:56 | |
Let's fill in the screen of the phone. | 0:23:56 | 0:23:59 | |
And just tap it to focus and very steadily, you just nab it, like that. | 0:23:59 | 0:24:06 | |
And that's what you end up with. | 0:24:06 | 0:24:07 | |
And that's with a camera phone. | 0:24:07 | 0:24:09 | |
It's just a case of getting the right kind of wide-angle eyepiece | 0:24:09 | 0:24:13 | |
that just syncs with the camera. Some will, some don't. | 0:24:13 | 0:24:17 | |
So, just try the one that works the best. | 0:24:17 | 0:24:19 | |
That one there is my favourite, and it gets you things like that. | 0:24:19 | 0:24:22 | |
There it is. | 0:24:22 | 0:24:23 | |
Time for the judging. Everyone's had a go. | 0:24:25 | 0:24:28 | |
Lulu and Jess. | 0:24:28 | 0:24:30 | |
I did take this one a couple of months ago. | 0:24:30 | 0:24:34 | |
SCOFFING LAUGHTER | 0:24:34 | 0:24:36 | |
-I can see the Lunar Lander! -I can see something. | 0:24:36 | 0:24:39 | |
-And the next one is Andy. -Right, here we go. There's mine. | 0:24:41 | 0:24:45 | |
-That's the Earth, Andy. Nice try. -Standing in the wrong place again. | 0:24:45 | 0:24:49 | |
That's, that's lovely! OK, last but not least, Jon Culshaw. | 0:24:50 | 0:24:55 | |
Now, we want an unbiased opinion. | 0:24:55 | 0:24:58 | |
That's terrible! | 0:24:58 | 0:25:00 | |
I'm joking. | 0:25:00 | 0:25:02 | |
-That is pretty excellent. -Exposure-wise, lovely. | 0:25:02 | 0:25:05 | |
All the wave highlights, all the way across to the terminator. | 0:25:05 | 0:25:08 | |
I'm... Not going to give you any more tips. | 0:25:08 | 0:25:11 | |
Because that's pretty good. | 0:25:11 | 0:25:13 | |
But, there can only be one winner. | 0:25:13 | 0:25:17 | |
After arduous adjudication, over to Jon. | 0:25:17 | 0:25:20 | |
Well, thank you. I'm very honoured to be presenting the prizes, | 0:25:20 | 0:25:23 | |
because it means that I haven't won. | 0:25:23 | 0:25:25 | |
LAUGHTER | 0:25:25 | 0:25:28 | |
JON IMPERSONATES SIR PATRICK MOORE: | 0:25:28 | 0:25:30 | |
And so the finest of the crop of some very, | 0:25:30 | 0:25:32 | |
very superb astral photographs indeed... | 0:25:32 | 0:25:34 | |
Alex! | 0:25:34 | 0:25:36 | |
CLAPPING AND CHEERING | 0:25:36 | 0:25:39 | |
'Well done, Alex. That's a great capture. | 0:25:41 | 0:25:44 | |
'If you've used your phone to capture the moon, | 0:25:44 | 0:25:46 | |
'why not put it on our Flickr site? At...' | 0:25:46 | 0:25:49 | |
August means one thing for Pete. The Perseid Meteor Shower. | 0:25:54 | 0:25:57 | |
This year, | 0:25:57 | 0:25:59 | |
the peak of the Perseids is actually on the evening of 12 August. | 0:25:59 | 0:26:03 | |
Ideally observed from midnight | 0:26:03 | 0:26:06 | |
through to dawn. That's when it gets | 0:26:06 | 0:26:08 | |
really high up in the sky. | 0:26:08 | 0:26:10 | |
That's when you get the maximum number of meteors that you're likely to see. | 0:26:10 | 0:26:13 | |
Well, it's been a quite superb night here. | 0:26:15 | 0:26:17 | |
Lovely skies and a great bunch of people. | 0:26:17 | 0:26:20 | |
And we have until the end of September to take | 0:26:20 | 0:26:22 | |
part in the Moore Moon Marathon. | 0:26:22 | 0:26:25 | |
Let's hope those balmy, clear nights continue. | 0:26:25 | 0:26:27 | |
Now, it's time for this month's Space Surgery, | 0:26:30 | 0:26:33 | |
so we've been joined by Chris North. | 0:26:33 | 0:26:36 | |
Well, yes, inspired by the Moore Moon Marathon, no doubt, | 0:26:36 | 0:26:38 | |
we've had people writing in with questions about the moon. | 0:26:38 | 0:26:41 | |
Our first one comes from Ben, aged 10, who asked, | 0:26:41 | 0:26:43 | |
Why doesn't the moon come out sometimes? | 0:26:43 | 0:26:45 | |
Ben, it's a good question. | 0:26:45 | 0:26:47 | |
the moon goes round an orbit once a month, so it moves through the sky. | 0:26:47 | 0:26:51 | |
Sometimes it's closer to the Sun and rises during the day, | 0:26:51 | 0:26:53 | |
and then it's quite hard to see. | 0:26:53 | 0:26:55 | |
Other times of the month, it's much further | 0:26:55 | 0:26:57 | |
away from the Sun in the sky and we see it in the middle of the night. | 0:26:57 | 0:27:00 | |
So, depending on what phase of its orbit it's in, | 0:27:00 | 0:27:02 | |
depends on what time you can see it. | 0:27:02 | 0:27:04 | |
Lucie, of course, last month we were at Stonehenge and we | 0:27:04 | 0:27:07 | |
mentioned those station stones which mark out possibly the most | 0:27:07 | 0:27:10 | |
northerly and southerly positions of moonrise and moonset. | 0:27:10 | 0:27:14 | |
Steve Charlton asks, since the moon is steadily moving away | 0:27:14 | 0:27:17 | |
from the Earth and increasing the time it takes to orbit, | 0:27:17 | 0:27:19 | |
how much closer would it have been | 0:27:19 | 0:27:21 | |
when the station stones were erected 5,000 years ago? | 0:27:21 | 0:27:25 | |
Well, the moon is moving away from us, but it's doing that very, | 0:27:25 | 0:27:28 | |
very slowly, at about the same rate as your nail grows. | 0:27:28 | 0:27:33 | |
So, that means that back when Stonehenge was built, | 0:27:33 | 0:27:35 | |
the moon would have been closer to us by about 200 metres. | 0:27:35 | 0:27:39 | |
And with that change in distance, | 0:27:39 | 0:27:41 | |
you wouldn't notice anything in the orbit of the moon around the Earth | 0:27:41 | 0:27:44 | |
and where it's rising and setting on the horizon. | 0:27:44 | 0:27:47 | |
And, Chris, possibly and a nice, simple one for you. | 0:27:47 | 0:27:49 | |
So, Steve Brown from Stokesley in North Yorkshire says, | 0:27:49 | 0:27:53 | |
Typically, how many people are in space at any given time? | 0:27:53 | 0:27:56 | |
Well, right now there are about six people, in fact, there | 0:27:56 | 0:27:59 | |
are exactly six people in the space station, and that's fairly typical. | 0:27:59 | 0:28:02 | |
We had nine a few weeks ago when the Chinese had three | 0:28:02 | 0:28:05 | |
up there as well. But typically, we've got a space station crew | 0:28:05 | 0:28:08 | |
and if you want to cheat, I tend to use a website called | 0:28:08 | 0:28:11 | |
howmanypeopleareinspacerightnow.com, | 0:28:11 | 0:28:14 | |
which gives you a nice big number and a list of people orbiting the Earth. | 0:28:14 | 0:28:17 | |
A good question, thanks very much. | 0:28:17 | 0:28:20 | |
If you have any questions for our Space Surgery from this programme | 0:28:20 | 0:28:23 | |
or in fact any area of astronomy, then contact us via the website... | 0:28:23 | 0:28:27 | |
And don't forget, | 0:28:30 | 0:28:31 | |
there's plenty of time to take part in our Moore Moon Marathon as well. | 0:28:31 | 0:28:35 | |
And with a gas cloud the size of the Earth on a doomed course | 0:28:35 | 0:28:38 | |
towards the centre of the galaxy, | 0:28:38 | 0:28:40 | |
next month we're talking about black holes with the Astronomer Royal. | 0:28:40 | 0:28:43 | |
So until then... ALL: Good night. | 0:28:43 | 0:28:46 | |
Subtitles by Red Bee Media Ltd | 0:28:51 | 0:28:54 |