Jan. 15, 2026
Mars Oceans Unveiled, Spinning Asteroids & Crew Evacuations
Exploring Mars Oceans, Fastest Asteroids, and ISS Evacuations In this captivating episode of Space Nuts, hosts Andrew Dunkley and Professor Fred Watson delve into the latest astronomical discoveries and intriguing space news. Join them as they explore...
Exploring Mars Oceans, Fastest Asteroids, and ISS Evacuations
In this captivating episode of Space Nuts, hosts Andrew Dunkley and Professor Fred Watson delve into the latest astronomical discoveries and intriguing space news. Join them as they explore new evidence suggesting that Mars once boasted vast oceans, the astonishing characteristics of the fastest spinning asteroid ever recorded, and the unprecedented evacuation of the International Space Station due to a medical issue.
Episode Highlights:
- Mars’ Ancient Oceans: Andrew and Fred discuss groundbreaking research revealing that Mars may have once had oceans comparable in size to Earth's Arctic Ocean. They explore the implications of this discovery and what it means for the search for life on the Red Planet.
- The Fastest Spinning Asteroid: The hosts introduce the asteroid 2025 MN45, which spins at an incredible rate of one rotation every 1 minute and 53 seconds. They discuss the significance of this finding and what it reveals about the asteroid's composition and history.
- ISS Medical Evacuation: Andrew and Fred provide insights into the first-ever crew evacuation from the International Space Station, prompted by a medical issue. They discuss the implications of this event and the protocols in place for astronaut safety.
For more Space Nuts, including our continuously updating newsfeed and to listen to all our episodes, visit our website. Follow us on social media at SpaceNutsPod on Facebook, X, YouTube Music Music, Tumblr, Instagram, and TikTok. We love engaging with our community, so be sure to drop us a message or comment on your favorite platform.
If you’d like to help support Space Nuts and join our growing family of insiders for commercial-free episodes and more, visit spacenutspodcast.com/about.
Stay curious, keep looking up, and join us next time for more stellar insights and cosmic wonders. Until then, clear skies and happy stargazing.
Become a supporter of this podcast: https://www.spreaker.com/podcast/space-nuts-astronomy-insights-cosmic-discoveries--2631155/support.
In this captivating episode of Space Nuts, hosts Andrew Dunkley and Professor Fred Watson delve into the latest astronomical discoveries and intriguing space news. Join them as they explore new evidence suggesting that Mars once boasted vast oceans, the astonishing characteristics of the fastest spinning asteroid ever recorded, and the unprecedented evacuation of the International Space Station due to a medical issue.
Episode Highlights:
- Mars’ Ancient Oceans: Andrew and Fred discuss groundbreaking research revealing that Mars may have once had oceans comparable in size to Earth's Arctic Ocean. They explore the implications of this discovery and what it means for the search for life on the Red Planet.
- The Fastest Spinning Asteroid: The hosts introduce the asteroid 2025 MN45, which spins at an incredible rate of one rotation every 1 minute and 53 seconds. They discuss the significance of this finding and what it reveals about the asteroid's composition and history.
- ISS Medical Evacuation: Andrew and Fred provide insights into the first-ever crew evacuation from the International Space Station, prompted by a medical issue. They discuss the implications of this event and the protocols in place for astronaut safety.
For more Space Nuts, including our continuously updating newsfeed and to listen to all our episodes, visit our website. Follow us on social media at SpaceNutsPod on Facebook, X, YouTube Music Music, Tumblr, Instagram, and TikTok. We love engaging with our community, so be sure to drop us a message or comment on your favorite platform.
If you’d like to help support Space Nuts and join our growing family of insiders for commercial-free episodes and more, visit spacenutspodcast.com/about.
Stay curious, keep looking up, and join us next time for more stellar insights and cosmic wonders. Until then, clear skies and happy stargazing.
Become a supporter of this podcast: https://www.spreaker.com/podcast/space-nuts-astronomy-insights-cosmic-discoveries--2631155/support.
WEBVTT
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Andrew Dunkley: Hi there. Thanks for joining us on another
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episode of Space Nuts. Great to have your
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company. My name is Andrew Dunkley, your host
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and I uh, hope you can stick around because
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we've got a jam packed show. We're
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once again going to Mars because
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they've looked uh, at some new evidence that
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uh, does suggest Mars oceans may have
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been vast. That is really
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exciting news. We're also going to look at
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the fastest spinning asteroid yet discovered.
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This one's uh, really in a spin.
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It's uh, making everybody dizzy. And the
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evacuation of the International Space Station
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uh, due to ill health. We'll see if we can
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get uh, some news on that because that's
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actually happening as Fred and I are uh,
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recording today. That's all coming up
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on this edition of Space Nuts. 15
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seconds. Guidance is internal.
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Voice Over Guy: 10, 9. Ignition
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sequence start. Space Nuts. 5, 4,
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3. 2. 1, 2, 3, 4, 5, 5, 4,
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3, 2, 1. Space Nuts astronauts
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report it feels good.
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Andrew Dunkley: And he's back again to furnish us with his
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knowledge. He is Professor Fred Watson,
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Astronomer at large. Hello Fred.
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Professor Fred Watson: Hello Andrew. I was just doing a quick
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calculation there for a number that I want to
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use um, later in the chat.
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Andrew Dunkley: Now I need to apologise in advance because
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ah, they're working across the road and I
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think they're using uh, dynamite because
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it's pretty noisy um, but
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hopefully it won't mess me up too much. I can
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hear it but I don't know if it's coming
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through the system. It's got all sorts of
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filters but um, some things you can't stop.
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Professor Fred Watson: Um.
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Andrew Dunkley: Now Fred, I did want to actually mention a
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couple of things before we start on our
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topics because uh, I meant to do this last
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week for our first show back of the year just
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to highlight some of the things that are
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coming up in 2026 that we can look forward to
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and that you and I will probably talk about.
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The Artemis 2 launch is
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slated. Uh, whether or not it'll be delayed
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again remains to be seen. But um, that will
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see a crew doing a lap around the moon,
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uh, and that'll be the first time humans have
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been back uh, in orbit around the moon
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since the 70s which uh, is
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exciting and probably too long but um,
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that'll be good. Um, this one I know will
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excite you. The Grace Roman Space Telescope
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is going to be launched. That one um,
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is going to um, opened so many doors for
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us I suspect, um, the
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PLATO mission, uh, which will be searching
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for rocky planets. It'll uh, be doing a lot
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more than that. But that's one of the things
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that it's being set out to do. Uh,
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China is to launch its own space
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telescope as well, um, in the hunt
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for dark matter and dark energy.
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And there's another mission that's going to
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be studying uh, the moon and Mars. Well,
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several missions, not just one. Um, more
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Chinese and Japanese missions involved there.
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And I think this is one you and I have talked
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about before. The Smile mission, uh, which
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will be studying Earth's magnetic field and
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how the sun interacts with our uh,
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atmosphere, uh, is um, due to be launched
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this year as well. I'm sure there's a lot
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more going on than that, but there's some of
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the highlights of 2026 so
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uh, we'll have a lot to talk about.
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Professor Fred Watson: Fred, could I add a couple more as well?
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Andrew Dunkley: Oh, go for it.
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Professor Fred Watson: Um, we've just uh, heard that the Pandora
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spacecraft has entered orbit, uh, which I
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think is a spacecraft, uh, again looking
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um, looking at exoplanets to try
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and sort of tell us a bit more about how
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their atmospheres might reveal stuff. Um,
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China has just filed for 200,000
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satellites constellation with the
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International Telecommunications Union which
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is. Yeah, yeah, well it's not the biggest
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yet. The biggest was back in 2020 when the
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Rwandan government filed for over
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300,000. Um, uh, since then
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they've launched one cubesat, I think. So,
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um, that looked like a filing that
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getting your foot in the door. Uh, and just
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turning to nature. We've got some interesting
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events coming up. Uh, March 3rd, total
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eclipse of the Moon visible certainly from
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our hemisphere in Australia, not sure about
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North America and Europe. Um,
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there's uh, towards the end of the year and
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this will happen twice, uh, which is great
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cause you can see it on different sides of
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the Earth. I think it's October, sometime in
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October and sometime in November there will
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be an occultation of the planet Jupiter by
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the Moon. That means the moon will pass in
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front of Jupiter and certainly for us in
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November here in Australia it will be during
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the daytime. So get your binoculars out
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during the daytime, check out the moon and
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watch for Jupiter disappearing.
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Andrew Dunkley: Oh, that'll be good. Yeah,
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that'd be a good one for a backyard
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telescope, wouldn't it?
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Professor Fred Watson: Absolutely perfect, yes.
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Andrew Dunkley: Awesome. Um, I had my
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6 year old granddaughter here uh, the other
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day and uh, the moon was, was out in the
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east and um, it was still daytime but it was
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pretty prominent. So I grabbed the telescope
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and gave her a look and uh, I tried to
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explain to her what craters were and
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she struggled with the concept. But she
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eventually I think figured it out. But uh,
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yeah, took a couple of photos of her looking
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through the telescope. She was very excited
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which she sent to me.
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Professor Fred Watson: It was uh, lovely to see them, Andrew. Yeah,
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yeah, lovely, lovely shots. A youngster
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looking through a telescop with granddad in
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the background is great. Yeah, yeah.
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Andrew Dunkley: Uh, she's got blonde hair and blue eyes and
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her brothers and sisters are all brown haired
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and brown eyed. So. Okay,
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she, she seems to have picked up Judy's side
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of the family genes because Judy's blondie,
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blonde with blue eyes. But um, she's the only
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one in the, in the family that's, that's gone
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that, that way. It happens though, doesn't
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it? It's just the way it is.
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Professor Fred Watson: Yeah.
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Andrew Dunkley: That's DNA.
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Um, okay Fred, uh,
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let's get stuck into it because uh, we're
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heading off to Mars and we're
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doing this because of a study that's just
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been published. Uh, in fact in the
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last week, uh, or two about uh,
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observations of Mars that suggest
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that its oceans were once vast. Now
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we always knew there was probably surface
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water but we didn't really know whether they
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were, you know, pockets or separate
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oceans or what. But now they're thinking
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the oceans might have been
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enormous.
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Professor Fred Watson: Uh, yes, that's right. And I mean, you know,
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we revisit this story probably on average
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once every month or two. Uh, the
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last time we covered this, and I
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wrote it up actually in um, an Australian
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Geographic article, um, not that I did the
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research, but this is other people's research
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and that was pointing in the same direction.
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Andrew. It was um, a group that looked at the
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way um, rivers, ancient rivers on Mars, uh,
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meandered, uh, because you can learn
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something from the meandering about the
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size of the body of water that they're
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emptying into. And they came to the same
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conclusion. The river meanders tell you that
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there was a large body of water at the end of
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it at the mouth of these rivers, uh, rather
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than just a few puddles or a few lakes and
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things of that sort. Uh, and this new piece
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uh, of work, um, whilst it's a different,
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uh, you know, it's got a different emphasis,
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comes up with exactly the same answer. Uh,
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and it's scientists uh, who have looked uh,
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at the, I remember rightly there in
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uh, in Switzerland. Yeah, University of Bern,
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uh, it's scientists who've looked at the
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region around Valles, uh,
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Marineris, you know, that great huge
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chasm in the, uh, in the surface of
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Mars. Near Mars's equator. Uh, something that
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makes the Grand Canyon look like a bit of a
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scratch on the, on the surface of the Earth.
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Andrew Dunkley: Yeah. Is it right that the Grand Canyon would
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fit into one of its tributaries or something?
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Professor Fred Watson: That's right. I think that's correct, yeah.
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Andrew Dunkley: Amazing.
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Professor Fred Watson: Um, so they've been looking in that region
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and certainly on the northern side and the
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northern flanks there are valleys that
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um, sort of open out onto the plains of Mars.
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Because that uh, Valles Marineris is kind
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of right at the start of the highland areas
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of the southern hemisphere of Mars. Mars has
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got this dichotomy. The northern hemisphere
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is flat and low, southern hemisphere 3km
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higher on average, full of craters, mountains
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and all around rest of it. Uh, so um, uh,
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um, what they've done is they've looked at
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regions, uh, where, you know, where there's
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this transition from the mountainous
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highlands of the south to the
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lowlands of the north. And they've looked
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very carefully at uh, data from
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uh, several orbiting spacecraft, um, I
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guess Mars Reconnaissance Orbiter is one and
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some of the other ones, um, actually even um,
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uh, um, ESO's
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ExoMars Trace Gas Orbiter. So, uh,
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Mars Express, another ESA, sorry, not ESO,
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ESA, uh, European Space Agency, Another
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um, uh, uh, orbiting spacecraft. They've
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taken the data from these, looked
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at the height, the
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topography and looked at the
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geomorphology. Let me get it right.
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Geomorphological, um,
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um, features that they can find.
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What have they spotted? They've spotted,
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ah, a whole succession of
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ancient river deltas, um, this
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is to say regions where a river mouth
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opened into what they're calling now
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an ocean, uh, and deposited
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um, its sediments. The sediments out of the
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river fall down to the floor, uh, of the
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ocean and build up basically
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a rock form, uh, which is preserved today.
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It's a kind of fossilized river delta.
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There's something similar going on, uh, as
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you and I have spoken about many times at
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Jezero Crater, which is why, um,
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perseverance is there, because there's a
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river delta there. But I think these are on a
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much larger scale. And um, the
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great thing is that when you look at them,
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they sort of define a shoreline,
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um, because these are all occurring
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at the same topographical height in
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Mars's geography. And so they
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basically uh, define a shoreline. And that
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shoreline tells you that um, there would have
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been a lot of water in Mars's northern
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hemisphere for the water level to reach the
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height that we find those deltas at.
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Uh, so really? Yeah, really nice piece
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of Work, uh, done with characteristic
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Swiss precision, I think. Uh, that's been
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widely reported. Um, there's several
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articles, uh, on the science news feeds,
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um, which basically support this idea.
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Very nice piece of research indeed.
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Andrew Dunkley: And they think it was as big as
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the Arctic Ocean on Earth, just by
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comparison. And how big as the Arctic Ocean?
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It's 14 million square kilometers or
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five and a half million square miles
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big, uh, in size. So that's a lot of
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water on Mars and uh, a lot of it's still
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there, Fred.
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Professor Fred Watson: Yeah, that's right. We um, know from
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particularly, uh, the Phoenix mission that
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just scraped the surface in the Martian
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Arctic and sure enough there was permafrost
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underneath. So a lot of it's still there.
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There's still water locked up in the two ice
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caps of Mars. Um, but probably
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not. Well, I don't know. It's actually really
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interesting. I do remember reading quite some
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time ago that if you thawed out even just the
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Antarctic ice cap of Mars, you'd cover the
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whole planet to a depth of several meters.
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Um, now whether that still holds good with
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what we've discovered since then, that was
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quite an old, I think that was probably 20
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years, 15 years ago, so that that comment
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was made. It would be interesting to know how
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we evaluate that now. But I think it's still
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true, uh, that a lot of that water is still
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there.
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Andrew Dunkley: Ah, yeah, it is, uh, a
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fascinating story.
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Professor Fred Watson: Water means life.
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Andrew Dunkley: Well, yes, yes, we've said that many times.
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And you just don't know, do you?
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Professor Fred Watson: You don't. Yeah.
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Andrew Dunkley: Although the, uh, the mission to retrieve
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those um, cylinders that contain
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potential evidence of that.
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Professor Fred Watson: Yeah.
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Andrew Dunkley: Has been scotched. So it's just going to sit
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in abeyance for um, an
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indefinite period.
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Professor Fred Watson: So, yeah, I think, um,
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so this is news that, um, the Senate have
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um, basically agreed with the White House in
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saying that um, the Mars Sample Return
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Mission, uh, should be canceled. Uh,
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and so that will probably go through. It's
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not been voted on yet, I don't think. Um,
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and so that means, yes, we've got these
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canisters on Mars, uh, carefully dropped by
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perseverance, uh, but
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with a joint European Space Agency NASA
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mission to retrieve them, uh, which, whose
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cost has blown out. Uh, we've talked about
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this before, uh, and not perhaps
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surprising that it's now had a line drawn
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under it. Now that's bad
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news because we really would like to get hold
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of these samples. There's one in particular
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that may contain actually fossilized
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microbes. Uh, you know, um,
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so it's um, there's uh, every keenness to do
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that. Um, um, and I think it
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will. There'll certainly be a revisiting
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of this idea. Esa, I think, is still going
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ahead with their half of the bargain. Which
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was, I think, to build the orbiter which
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would actually bring the samples back to
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Mars. NASA's part was gathering them up on
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the surface and sending them up to orbit
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around Mars. Uh, so, you know,
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uh, it's bad news. There's a bright side to
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it though, in that the money that's being
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saved will probably go to some of the other
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missions that are being planned.
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Name your favorite planet. You might get some
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good news out of this. I know your favorite
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and probably mine too, is Mars. Uh, but,
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um, anyway, we'll see what happens. I
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wouldn't write, uh, the Mars sample return
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off altogether in my flights of
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fantasy. Last night, while my,
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uh, respiratory tract infection was
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making me cough all night, I was thinking
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maybe the Chinese could bring them back
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because I think they're planning a sample
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return mission as well. So maybe we do a deal
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there. Which would be fabulous international
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cooperation.
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Andrew Dunkley: It would. It would indeed. Of course, we
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could always start the conspiracy and say,
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what does NASA and the US Government know
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that they're not telling us?
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Hence no return. Yeah, yeah.
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Professor Fred Watson: Be careful what you, what you say, Andrew.
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Andrew Dunkley: No, look, I'm just kidding around, but, uh,
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it's just money, isn't it? That's, that's the
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thing.
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Professor Fred Watson: It's all about money. That's right. It's not
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about finding something with legs that you
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don't want anybody to know about.
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Andrew Dunkley: Yes, that's been done in a lot of science
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fiction films.
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Professor Fred Watson: Yeah, it has. And um.
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Andrew Dunkley: Yes, all right. Great story about
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the oceans of Mars though. If you'd like to
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check it out, it's on the Phys p h y
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s.org website. Or you can read the
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paper that's been published in the journal
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NPJ Space Exploration.
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This is Space Nuts with Andrew Dunkley and
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Professor Fred Watson.
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Roger, in your labs right here.
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Also Space Nuts to our
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next story, Fred. And this
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is, uh, a really good one for a couple of
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reasons. It's something we haven't seen
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before, but it also involves the, uh,
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Rubin Observatory, which, um,
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has already, uh, done things that,
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uh, other observatories have not been able
382
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to do and promises to do so much more.
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This is the fastest spinning asteroid yet
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discovered. And a couple of headlines I've
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read suggested why hasn't it thrown itself
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to pieces because of the speed at which it's
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rotating and
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the rate is rather high when you look at what
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the average asteroid does.
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Professor Fred Watson: Yeah, so it is a record breaker.
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It's the fastest spinning asteroid
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for its size. Uh, because I think
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smaller things can spin faster than this.
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It's uh, 710 meters long, nearly
395
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three quarters of a kilometer. Uh, so
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it's not a small asteroid at all. This
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is quite a large one. Uh, and
398
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it spins at the rate of one rotation
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every one minute 53
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seconds. So that
401
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is one heck of a spin. So that's its day
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length, Andrew. If you were standing on it,
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your day will be 1 minute 53 seconds. Seconds
404
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night and day, not 24 hours. Um,
405
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but uh, you're absolutely right. I think it's
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interesting for two reasons. One is exactly
407
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as you've said. It underlines, uh, just
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how powerful the Rubin Observatory is going
409
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to be. The observations of
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this object were made during the
411
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sort of commissioning period for the
412
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telescope's instruments, which was earlier
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last year, April and May 2025. Uh,
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and um, that you know, that um,
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as you probably remember, I think they
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released uh, uh, information saying they got.
417
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They discovered more than a thousand
418
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asteroids in 10 hours of observing, which is
419
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pretty fantastic. Uh, the telescope's
420
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capabilities will allow it to survey the
421
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entire southern sky every three
422
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nights, uh, with an eight meter class
423
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telescope. That is an astonishing achievement
424
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and we.
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Andrew Dunkley: Must find something incredible.
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Professor Fred Watson: Yeah, we will. Yeah, there's going to be all
427
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kinds of things that come out of the
428
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woodwork. Uh, it's what we call, um,
429
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uh, sort of time sensitive astronomy or
430
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transient astronomy. You're looking for
431
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things that either move or change in the sky
432
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and it's going to be so good at finding them.
433
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And um. Yeah. So the real
434
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observing, uh, campaign, the Large
435
00:18:01.800 --> 00:18:04.400
Synoptic Survey, uh, will start
436
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uh, sometime this year, uh, sort of when
437
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they're ready to hit the go button. Uh, but I
438
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think everybody at the Rubin is pretty happy
439
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with the way things are going. Um, and just
440
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to sort of highlight that, you know,
441
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it's a telescope with this kind of capability
442
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to make many observations over a short period
443
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of time of the same area of sky. That has
444
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allowed uh, the scientists to
445
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discover the very rapid rotation
446
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of this asteroid. Because what you have to
447
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produce, uh, to look at the way an asteroid
448
00:18:37.620 --> 00:18:39.300
rotates is what's called a light curve. You
449
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look at the way its brightness changes. Uh,
450
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because most asteroids, asteroids are quite
451
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asymmetric. They're either shaped like a
452
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potato or a dumbbell. Very, uh, few are
453
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anything remotely spherical. Um, uh,
454
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this particular one is I think Quite
455
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elongated. And so as it rotates,
456
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uh, different sides of it catch the
457
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sunlight and you get a variation in the light
458
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that we see from it. Uh, and so that uh,
459
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has allowed, because it's, you know, it's
460
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only 1 minute 53 seconds for one
461
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complete revolution that has allowed the
462
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scientists to determine that fact,
463
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um, to the asteroid itself. You're right,
464
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it's interesting. It rejoices in the name of
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2025 MN45, a
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classic asteroid name. Um, and
467
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it's in the main asteroid belt. That's
468
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a good place for it to be between uh, Jupiter
469
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and Mars, where most of the asteroids are.
470
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Uh, but um, its rotation
471
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is what highlights um,
472
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the unusual nature of it. Because as you and
473
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I have spoken about before, many asteroids
474
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are uh, basically what we call rubble piles.
475
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They're just piles of debris which stick
476
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together loosely under their own,
477
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uh, gravity. Um, little
478
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uh, Dimorphos and Didymos, the
479
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two, uh, objects that NASA did the
480
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DART test on a few years ago, they are
481
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probably rubber piles. They've got the
482
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characteristic rubber pile shape, which is
483
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like two cones, um, uh, back to
484
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back. Uh, if it was a rubber
485
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pile, it would have flown apart
486
00:20:14.490 --> 00:20:17.450
gazillions of years ago, uh, with
487
00:20:17.450 --> 00:20:19.930
that short period of rotation, 1 minute
488
00:20:20.090 --> 00:20:23.090
53 seconds. So, um, uh, and when
489
00:20:23.090 --> 00:20:25.370
you look at the size of it and
490
00:20:25.880 --> 00:20:28.210
uh, interpret what the rotation means, it
491
00:20:28.210 --> 00:20:30.130
tells you it's probably made of absolutely
492
00:20:30.130 --> 00:20:32.570
solid rock. This is something that is
493
00:20:33.040 --> 00:20:35.570
um, going to be hard to pull apart, to
494
00:20:35.570 --> 00:20:38.450
rotate. For it to be that big rotate at that
495
00:20:38.450 --> 00:20:41.400
speed, it's got to be solid rock, um,
496
00:20:41.460 --> 00:20:43.800
um, making it uh, you know, in some ways even
497
00:20:43.800 --> 00:20:45.360
more interesting because we think the rubber
498
00:20:45.360 --> 00:20:47.340
piles are perhaps the more common uh,
499
00:20:47.480 --> 00:20:48.680
asteroids that we see.
500
00:20:49.240 --> 00:20:51.840
Andrew Dunkley: Do we, do we have any idea what would make it
501
00:20:51.840 --> 00:20:53.680
different, why it would be different? Is it a
502
00:20:53.680 --> 00:20:56.200
piece of a destroyed planet Theia?
503
00:20:57.400 --> 00:20:59.920
Professor Fred Watson: Well, yeah, could be, uh, might be part of
504
00:20:59.920 --> 00:21:02.790
Theia, the one that created the moon, uh,
505
00:21:03.400 --> 00:21:05.400
after, after it collided with the ah, Earth.
506
00:21:05.560 --> 00:21:08.240
It's more likely you're right. It's
507
00:21:08.240 --> 00:21:11.150
probably, um, you know, maybe part of the
508
00:21:11.470 --> 00:21:14.350
outer mantle of what would have been
509
00:21:14.350 --> 00:21:17.270
a protoplanet. In the early solar
510
00:21:17.270 --> 00:21:19.390
system, these things were the building blocks
511
00:21:19.390 --> 00:21:21.310
of planets. They collided and sometimes they
512
00:21:21.310 --> 00:21:23.230
blasted each other apart, sometimes
513
00:21:24.190 --> 00:21:26.990
they stuck together to form what we see
514
00:21:26.990 --> 00:21:29.510
in the solar system today. Um,
515
00:21:29.630 --> 00:21:31.990
and I, uh, think some of the collisions that
516
00:21:31.990 --> 00:21:33.510
would have happened in the early solar
517
00:21:33.510 --> 00:21:36.470
system, uh, may well have set an
518
00:21:36.470 --> 00:21:38.510
object like this spinning very rapidly. In
519
00:21:38.510 --> 00:21:41.140
fact, it might have initially been
520
00:21:41.290 --> 00:21:43.130
spinning even more rapidly. Than it is now.
521
00:21:43.290 --> 00:21:45.250
Because we're looking at probably several
522
00:21:45.250 --> 00:21:47.930
billion years ago. When whatever
523
00:21:47.930 --> 00:21:50.690
happened to it happened. So, uh, an
524
00:21:50.690 --> 00:21:53.690
object of some interest. And, um, one
525
00:21:53.690 --> 00:21:56.530
that I'm sure will be studied, uh, in
526
00:21:56.530 --> 00:21:58.770
greater detail. We might want to know things
527
00:21:58.770 --> 00:22:01.410
like, um, the infrared signature of its
528
00:22:01.410 --> 00:22:03.890
surface. Which gives you an idea of what the
529
00:22:03.890 --> 00:22:05.610
surface is like, how rough it is, whether
530
00:22:05.610 --> 00:22:08.140
it's a. Whether it's a smooth
531
00:22:08.140 --> 00:22:10.740
surface. What materials are likely to be,
532
00:22:11.090 --> 00:22:12.860
uh, found on its surface. That can all come
533
00:22:12.860 --> 00:22:15.260
from spectroscopy and also the science of
534
00:22:15.260 --> 00:22:17.500
polarimetry, which is what you look at to
535
00:22:17.500 --> 00:22:19.260
know whether something's highly reflective.
536
00:22:19.260 --> 00:22:22.020
Or rather rough and diffuse. So,
537
00:22:22.020 --> 00:22:24.340
yeah, m. I think there's lots to learn about,
538
00:22:24.530 --> 00:22:26.820
uh, 2025 MN45.
539
00:22:27.380 --> 00:22:30.380
Andrew Dunkley: Indeed. So it's in the asteroid
540
00:22:30.380 --> 00:22:32.500
belt between Mars and Jupiter.
541
00:22:32.670 --> 00:22:35.500
Um, people probably imagine
542
00:22:35.500 --> 00:22:38.020
that to be just a wall of roc.
543
00:22:38.800 --> 00:22:40.640
How do we get through it? But it's quite
544
00:22:40.640 --> 00:22:41.680
sparse, isn't it?
545
00:22:41.920 --> 00:22:44.840
Professor Fred Watson: It is, yeah. Yeah. Uh, it's
546
00:22:44.840 --> 00:22:46.880
sparse enough that, um, uh, several
547
00:22:46.880 --> 00:22:48.440
spacecraft have actually gone through it
548
00:22:48.440 --> 00:22:51.320
unscathed. Um, so,
549
00:22:51.320 --> 00:22:52.000
yes, it's.
550
00:22:52.000 --> 00:22:53.920
Andrew Dunkley: Well, I've never heard of a spacecraft
551
00:22:53.920 --> 00:22:55.600
actually running into anything out there.
552
00:22:56.720 --> 00:22:58.360
Not that there have been that many that have
553
00:22:58.360 --> 00:22:59.040
gone through, but.
554
00:22:59.200 --> 00:23:01.850
Professor Fred Watson: That's right. But, you know, as, um.
555
00:23:02.230 --> 00:23:05.040
Uh. Was it Douglas Adams. Space
556
00:23:05.040 --> 00:23:05.920
is big. Yes.
557
00:23:06.160 --> 00:23:06.560
Andrew Dunkley: Yes.
558
00:23:06.560 --> 00:23:08.440
Professor Fred Watson: You might think it's a long way down to the
559
00:23:08.440 --> 00:23:10.500
chemist at the corner of the street. But
560
00:23:10.980 --> 00:23:13.180
that's nothing compared with space. I think
561
00:23:13.180 --> 00:23:14.180
that was what he said.
562
00:23:16.100 --> 00:23:18.700
Andrew Dunkley: Yes, indeed. Uh, so if you would like to
563
00:23:18.700 --> 00:23:21.660
learn more about what the Vera C. Rubin
564
00:23:21.660 --> 00:23:23.820
Observatory has discovered, you can do
565
00:23:23.820 --> 00:23:26.620
that@the universitytoday.com website.
566
00:23:26.620 --> 00:23:28.300
Or you can read the paper in the
567
00:23:28.300 --> 00:23:31.220
Astrophysical Journal Letters. Which was,
568
00:23:31.340 --> 00:23:34.100
uh, only published on January 7th. So they're
569
00:23:34.100 --> 00:23:35.620
getting down to business early this year,
570
00:23:35.620 --> 00:23:36.100
aren't they?
571
00:23:36.260 --> 00:23:39.180
Professor Fred Watson: This is space nuts. Sorry. I was
572
00:23:39.180 --> 00:23:41.620
going to say, um, we always get a really
573
00:23:42.020 --> 00:23:44.300
good, um, crop of news stories at this time
574
00:23:44.300 --> 00:23:46.100
of year. Because it's right at the beginning
575
00:23:46.100 --> 00:23:48.700
of January that the American Astronomical
576
00:23:48.700 --> 00:23:51.060
Society has its annual meeting.
577
00:23:52.260 --> 00:23:55.060
And, um, so there's always some great
578
00:23:55.060 --> 00:23:58.020
stories. So, you know, that's why it was,
579
00:23:58.020 --> 00:23:59.540
uh. You know, it was published last week. I'm
580
00:23:59.540 --> 00:24:00.460
sure that's actually.
581
00:24:00.460 --> 00:24:02.980
Andrew Dunkley: It's actually very clever because as someone
582
00:24:02.980 --> 00:24:05.940
who worked in the media for 40 years. And
583
00:24:07.140 --> 00:24:09.380
had, um, to work a lot of Christmases and New
584
00:24:09.600 --> 00:24:12.280
Years, you quite often find you're
585
00:24:12.280 --> 00:24:14.640
struggling for stories because
586
00:24:14.880 --> 00:24:16.880
everything's shut down. So you're not getting
587
00:24:16.880 --> 00:24:19.200
the information that you normally get. So
588
00:24:19.600 --> 00:24:22.080
to actually be in a position to do stories
589
00:24:22.320 --> 00:24:25.030
like this at this time of year is
590
00:24:25.030 --> 00:24:28.000
um. Yeah, it's well
591
00:24:28.000 --> 00:24:30.830
positioned, as we would say. M. Uh,
592
00:24:30.830 --> 00:24:33.730
you can read all about it, of course. And uh,
593
00:24:33.730 --> 00:24:36.360
we uh, will certainly be keeping a very close
594
00:24:36.360 --> 00:24:38.920
eye on what the Vera C. Rubin Observatory is
595
00:24:38.920 --> 00:24:39.920
going to be doing
596
00:24:40.770 --> 00:24:43.710
um, from now on because it's uh,
597
00:24:43.710 --> 00:24:46.200
it's, it's, it's all up and running and uh,
598
00:24:46.430 --> 00:24:49.430
already doing some remarkable things. This
599
00:24:49.430 --> 00:24:51.230
is Space Nuts with Andrew Dunkley and Fred
600
00:24:51.230 --> 00:24:51.790
Watson.
601
00:24:55.869 --> 00:24:58.510
Space Nuts. Now Fred, uh, by the time
602
00:24:58.750 --> 00:25:00.670
people hear us talking about this story,
603
00:25:00.670 --> 00:25:03.630
things will have uh, changed a bit. But
604
00:25:03.630 --> 00:25:06.510
as we speak, uh, we understand that
605
00:25:06.510 --> 00:25:08.910
the Crew Dragon spacecraft
606
00:25:09.760 --> 00:25:12.520
is docking at the International Space Station
607
00:25:12.520 --> 00:25:15.160
to do the first ever crew
608
00:25:15.160 --> 00:25:17.680
evacuation. Now, after 25 years,
609
00:25:18.400 --> 00:25:20.480
I'm surprised this is the first time this has
610
00:25:20.480 --> 00:25:22.280
happened. But uh, there's been a medical
611
00:25:22.280 --> 00:25:24.560
issue. They won't elaborate on who or what,
612
00:25:25.300 --> 00:25:27.440
uh, but it's gotta be serious if somebody's
613
00:25:27.440 --> 00:25:29.440
um, if they're bringing the whole crew back.
614
00:25:29.600 --> 00:25:32.040
It's uh, a crew of four. There's seven on
615
00:25:32.040 --> 00:25:33.600
board at the moment. But they're bringing
616
00:25:33.600 --> 00:25:35.040
four back, correct?
617
00:25:35.040 --> 00:25:37.680
Professor Fred Watson: That's right. So, uh, there is a crew of
618
00:25:37.680 --> 00:25:40.680
three uh, now. So as we speak, um, I
619
00:25:40.680 --> 00:25:43.340
think they've probably undocked the crew
620
00:25:43.340 --> 00:25:45.180
Dragon spacecraft from the International
621
00:25:45.260 --> 00:25:46.980
Space Station. I think that happened an hour
622
00:25:46.980 --> 00:25:49.700
ago. And um, they
623
00:25:49.700 --> 00:25:52.700
will then re. Enter and bring the crew
624
00:25:52.700 --> 00:25:55.260
back in a pretty routine fashion,
625
00:25:55.600 --> 00:25:58.540
uh, landing in a few hours from now. Um, so
626
00:25:58.540 --> 00:26:01.460
you're right, it's Crew 11, uh,
627
00:26:01.460 --> 00:26:03.750
the SpaceX, um,
628
00:26:04.300 --> 00:26:06.140
what's called the SpaceX Crew 11 because
629
00:26:06.140 --> 00:26:07.700
they're the ones that go up and down in the
630
00:26:07.700 --> 00:26:10.460
crew Dragon, uh, rather than the Soyuts,
631
00:26:10.460 --> 00:26:12.180
which is the space vehicle that will bring
632
00:26:12.180 --> 00:26:14.720
the other uh, the remaining three astronauts
633
00:26:14.720 --> 00:26:17.720
down when their time comes to an end. Uh,
634
00:26:17.720 --> 00:26:19.840
you're right. It's a medical evacuation that
635
00:26:19.840 --> 00:26:22.640
Crew, Crew 11 consists of, um, if I
636
00:26:22.640 --> 00:26:25.490
remember rightly, two NASA, uh, uh,
637
00:26:25.490 --> 00:26:27.920
astronauts, one Russian
638
00:26:27.920 --> 00:26:30.520
cosmonaut and uh, a Japanese
639
00:26:31.070 --> 00:26:33.680
uh, astronaut as well. Uh, so they're coming
640
00:26:33.680 --> 00:26:36.440
home, uh, they're coming home something like
641
00:26:36.440 --> 00:26:39.120
a month early. And we are told as
642
00:26:39.120 --> 00:26:41.000
exactly as you've said that this is because
643
00:26:41.000 --> 00:26:43.710
of a medical issue which apparently is not
644
00:26:43.810 --> 00:26:46.710
uh, an emergency. It's not urgent, but it's
645
00:26:46.710 --> 00:26:48.630
thought to be something that is going to be
646
00:26:48.630 --> 00:26:51.630
much better dealt with on Earth. Uh, we don't
647
00:26:51.630 --> 00:26:54.030
know which of the astronauts has the issue.
648
00:26:54.650 --> 00:26:57.030
Um, I saw a picture of them posed just before
649
00:26:57.030 --> 00:26:58.990
they evacuated the spacecraft,
650
00:26:59.430 --> 00:27:02.350
uh, um, last night and they all looked
651
00:27:02.350 --> 00:27:05.230
fairly cheerful, uh, but um, so
652
00:27:05.230 --> 00:27:07.070
you know, uh, you can't really read
653
00:27:09.630 --> 00:27:11.510
from people's faces how they're feeling. Um,
654
00:27:12.410 --> 00:27:13.970
which is just as well because I feel pretty
655
00:27:13.970 --> 00:27:16.730
crook at the moment. So
656
00:27:16.970 --> 00:27:19.210
that's uh, because of my uh, uh, upper
657
00:27:19.690 --> 00:27:21.730
respiratory tract infection. Sorry to keep
658
00:27:21.730 --> 00:27:23.570
harping on about it. Anyway, going back to
659
00:27:23.570 --> 00:27:26.530
the more important story, Andrew. Well it's
660
00:27:26.530 --> 00:27:27.170
a good thing you're not.
661
00:27:27.170 --> 00:27:29.010
Andrew Dunkley: In the International Space Station feeling
662
00:27:29.010 --> 00:27:29.450
like that.
663
00:27:29.450 --> 00:27:31.290
Professor Fred Watson: Well, that's right, I, you'd have the same
664
00:27:31.290 --> 00:27:33.760
thing too. Uh, so, yeah, so,
665
00:27:33.760 --> 00:27:36.290
um, interesting. Uh, but your comment's well
666
00:27:36.290 --> 00:27:38.330
made. You know the fact that it's the first
667
00:27:38.330 --> 00:27:40.730
time in the 25 year history
668
00:27:41.290 --> 00:27:44.000
of the ISS, of the
669
00:27:44.000 --> 00:27:46.880
ISS being permanently occupied,
670
00:27:47.360 --> 00:27:49.960
um, the first time this has happened. And I
671
00:27:49.960 --> 00:27:52.360
think it was Jared Isaacman, the newly
672
00:27:52.360 --> 00:27:55.360
appointed NASA administrator, the boss of
673
00:27:55.600 --> 00:27:58.520
NASA, who made the comment. It might
674
00:27:58.520 --> 00:28:01.120
be somebody else but it is one of the
675
00:28:01.520 --> 00:28:04.240
high ups in NASA made the comment that
676
00:28:04.480 --> 00:28:06.760
when they planned the ISS and they were
677
00:28:06.760 --> 00:28:09.240
working towards it, they expected that there
678
00:28:09.240 --> 00:28:10.960
would be something like this happening every
679
00:28:10.960 --> 00:28:13.840
three years. So they've done pretty well
680
00:28:13.840 --> 00:28:16.110
to get through 2015, five years without um,
681
00:28:16.110 --> 00:28:17.820
needing to bring people home because of a
682
00:28:17.820 --> 00:28:19.580
medical issue. Yeah.
683
00:28:20.620 --> 00:28:22.460
Andrew Dunkley: While you've been talking Fred, I've just
684
00:28:22.460 --> 00:28:24.740
been looking online to see where things are
685
00:28:24.740 --> 00:28:27.660
up to and I've found a um, they did a live
686
00:28:27.740 --> 00:28:30.580
stream of the crew uh, Dragon docking at the
687
00:28:30.580 --> 00:28:32.620
International Space Station through
688
00:28:32.880 --> 00:28:35.540
uh, I think it's NASA's YouTube Music
689
00:28:35.540 --> 00:28:38.420
channel and you can, you can
690
00:28:38.420 --> 00:28:40.620
actually log on and, and watch what happens
691
00:28:40.850 --> 00:28:43.850
and see the whole process. It's quite
692
00:28:43.850 --> 00:28:45.890
incredible what we can do now isn't it with
693
00:28:45.900 --> 00:28:48.570
um, live coverage from space as ah, things
694
00:28:48.570 --> 00:28:51.410
unfold. It's uh, a far cry
695
00:28:51.410 --> 00:28:54.010
from those times back in the 60s and 70s when
696
00:28:54.010 --> 00:28:55.850
we were looking at those really fuzzy black
697
00:28:55.850 --> 00:28:57.250
and white pictures off the moon.
698
00:28:59.090 --> 00:29:00.850
Professor Fred Watson: Which was miraculous in its day.
699
00:29:00.850 --> 00:29:02.850
Andrew Dunkley: Oh it was in itself, yes. Yes.
700
00:29:03.170 --> 00:29:03.650
Professor Fred Watson: Yeah.
701
00:29:04.530 --> 00:29:07.130
Andrew Dunkley: Actually I am watching Crew Dragon detach as
702
00:29:07.130 --> 00:29:07.570
we speak.
703
00:29:07.570 --> 00:29:08.010
Professor Fred Watson: Yes, that's right.
704
00:29:08.010 --> 00:29:10.720
Andrew Dunkley: So that happened probably 30 minutes ago,
705
00:29:10.720 --> 00:29:13.640
give or take our time. Yeah,
706
00:29:13.760 --> 00:29:16.200
um, it's, it's like a slow motion ballet
707
00:29:16.200 --> 00:29:18.360
isn't it? When they uh, things in
708
00:29:18.360 --> 00:29:19.720
spacecraft.
709
00:29:19.720 --> 00:29:22.040
Professor Fred Watson: Ah, yeah, well you don't want to bang into
710
00:29:22.040 --> 00:29:22.520
anything.
711
00:29:23.080 --> 00:29:25.640
Andrew Dunkley: Yeah. Anyway, I hope all is well with
712
00:29:25.800 --> 00:29:27.910
the uh, individual involved. I'm uh,
713
00:29:28.520 --> 00:29:30.840
I'm not sure we'll ever find out what exactly
714
00:29:31.400 --> 00:29:33.480
the issue is. That's, that's subject to
715
00:29:33.480 --> 00:29:35.800
privacy from what I understand. But the fact
716
00:29:35.800 --> 00:29:38.800
that they've been able to go
717
00:29:38.800 --> 00:29:40.920
up there, get them, bring them back and deal
718
00:29:40.920 --> 00:29:43.760
with the problem is extraordinary
719
00:29:43.760 --> 00:29:46.480
because go back to the 70s when
720
00:29:46.480 --> 00:29:49.400
Skylab was in orbit. If someone got sick
721
00:29:49.400 --> 00:29:52.080
or injured in that situation,
722
00:29:52.800 --> 00:29:55.160
I don't know if we would have been able to do
723
00:29:55.160 --> 00:29:56.000
much in a hurry.
724
00:29:58.450 --> 00:30:00.640
Professor Fred Watson: Um, yeah, maybe not. I mean, there would have
725
00:30:00.640 --> 00:30:03.440
been contingency plans in place.
726
00:30:04.560 --> 00:30:07.470
It's, um. I think
727
00:30:07.710 --> 00:30:09.150
some of the things that might have brought
728
00:30:09.150 --> 00:30:11.470
somebody home from Skylab might be things
729
00:30:11.470 --> 00:30:12.710
that could have been fixed on the
730
00:30:12.710 --> 00:30:14.590
International Space Station because there is
731
00:30:14.590 --> 00:30:17.310
quite a, you know, a fair, Fair amount of
732
00:30:17.310 --> 00:30:19.670
medical expertise up there and some of the
733
00:30:19.670 --> 00:30:21.069
kit. But you don't want people taking
734
00:30:21.069 --> 00:30:23.190
appendices out and things like that in space.
735
00:30:23.190 --> 00:30:25.590
Andrew Dunkley: No, not really. You just have to wipe down
736
00:30:25.590 --> 00:30:27.710
the walls afterwards, and that's not fun.
737
00:30:28.510 --> 00:30:31.390
Although I should, um, counter it by saying
738
00:30:31.470 --> 00:30:33.910
we did recently have a situation where. Where
739
00:30:34.070 --> 00:30:36.190
a crew got stuck on the International Space
740
00:30:36.190 --> 00:30:39.030
Station for very unusual reasons due to,
741
00:30:39.190 --> 00:30:41.390
uh, incompatible spacesuits because of a
742
00:30:41.390 --> 00:30:43.830
failure in the Boeing Starliner.
743
00:30:44.230 --> 00:30:47.230
So, you know, that wasn't a quick
744
00:30:47.230 --> 00:30:49.150
rescue, that one, but it didn't involve
745
00:30:49.150 --> 00:30:51.630
illness or injury, so it wasn't as urgent.
746
00:30:51.630 --> 00:30:54.510
But, uh, sometimes it. It can be a
747
00:30:54.510 --> 00:30:57.310
slow process, but, um. Uh, yeah, but
748
00:30:57.310 --> 00:30:59.470
NASA's been very quick to point out that this
749
00:30:59.470 --> 00:31:01.590
has got nothing to do with an operational
750
00:31:01.670 --> 00:31:03.990
issue. It's, um. It's a personal issue.
751
00:31:03.990 --> 00:31:06.530
Nothing to do with an injury or accident on
752
00:31:06.530 --> 00:31:08.690
board. They want to make that pretty clear.
753
00:31:09.690 --> 00:31:11.810
Um, so, uh, yeah, we wish them well. They're
754
00:31:11.810 --> 00:31:13.530
on their way back as we speak. And by the
755
00:31:13.530 --> 00:31:16.450
time you hear this podcast, they will have
756
00:31:16.450 --> 00:31:17.650
returned, no doubt.
757
00:31:18.630 --> 00:31:21.330
Um, that's it, Fred. Gosh, we got through
758
00:31:21.330 --> 00:31:22.850
that in a mighty hurry, didn't we?
759
00:31:23.610 --> 00:31:26.530
Professor Fred Watson: Um, yes, I think
760
00:31:26.530 --> 00:31:29.170
we. We gave it due, due
761
00:31:29.170 --> 00:31:32.170
recognition. We've been talking for well over
762
00:31:32.170 --> 00:31:33.170
an hour, Andrew.
763
00:31:35.090 --> 00:31:35.730
Andrew Dunkley: Oh, have we?
764
00:31:37.810 --> 00:31:40.570
Doesn't feel like it, but no. Um.
765
00:31:42.290 --> 00:31:45.010
Professor Fred Watson: 38 minutes. I'm sorry. I'm misreading my
766
00:31:45.170 --> 00:31:46.130
clock. You're right.
767
00:31:46.130 --> 00:31:46.930
Andrew Dunkley: That's okay.
768
00:31:47.010 --> 00:31:48.530
Professor Fred Watson: Well, we got through that in a hurry.
769
00:31:49.010 --> 00:31:51.130
Andrew Dunkley: You're probably reading a Mars clock because
770
00:31:51.130 --> 00:31:53.890
we talked about it. It's going a bit
771
00:31:53.890 --> 00:31:56.810
faster. Um, now
772
00:31:56.810 --> 00:31:59.090
if you were to follow, uh, up those stories,
773
00:31:59.250 --> 00:32:00.850
I've told you where to go and look for them.
774
00:32:00.850 --> 00:32:03.770
But you, uh, can also read the show notes on
775
00:32:03.770 --> 00:32:06.430
our website, spacenutspodcast.more space
776
00:32:06.430 --> 00:32:09.230
nuts IO and while you're
777
00:32:09.230 --> 00:32:12.070
there, uh, you might like to, um, check out
778
00:32:12.070 --> 00:32:14.750
all the. All the tabs and,
779
00:32:15.050 --> 00:32:17.250
uh, links on our. On our website, the, uh,
780
00:32:17.350 --> 00:32:19.630
Astronomy Daily feed. You can subscribe for
781
00:32:19.630 --> 00:32:21.510
your daily dose of astronomy and space
782
00:32:21.510 --> 00:32:24.270
Science news. Uh, don't forget reviews.
783
00:32:24.270 --> 00:32:26.630
We really do appreciate your reviews. The
784
00:32:26.630 --> 00:32:29.630
more reviews, the more we get noticed. And
785
00:32:29.630 --> 00:32:31.150
the more we get noticed, the more people
786
00:32:31.150 --> 00:32:33.830
listen. And then, you know, we can buy
787
00:32:33.830 --> 00:32:35.550
ourselves an ice cream at the end of the day.
788
00:32:35.970 --> 00:32:38.730
Um, you can also send questions
789
00:32:38.730 --> 00:32:41.690
or comments in through the AMA link and
790
00:32:41.770 --> 00:32:43.610
so on and so forth. And don't forget to visit
791
00:32:43.610 --> 00:32:45.890
the Space Nuts shop. Uh, that's one thing
792
00:32:45.890 --> 00:32:48.810
that Huw, um, did some years ago
793
00:32:48.810 --> 00:32:51.110
and it's been very popular. All the, uh,
794
00:32:51.110 --> 00:32:53.370
Space Nuts memorabilia, if you, if you want
795
00:32:53.370 --> 00:32:54.930
to get hold of it. I've got, I've got my
796
00:32:54.930 --> 00:32:56.450
Space Nuts cup here somewhere.
797
00:32:56.450 --> 00:32:58.250
Professor Fred Watson: Here it is. Look. Look at this.
798
00:32:59.210 --> 00:32:59.850
Andrew Dunkley: There it is.
799
00:32:59.850 --> 00:33:01.530
Professor Fred Watson: I never got, I never got one of those.
800
00:33:02.650 --> 00:33:03.650
Andrew Dunkley: I, I'd buy.
801
00:33:03.650 --> 00:33:06.810
It's
802
00:33:06.810 --> 00:33:07.610
good. That's good.
803
00:33:07.850 --> 00:33:08.970
Professor Fred Watson: I'm too stingy.
804
00:33:09.830 --> 00:33:12.710
Andrew Dunkley: Got shirts. We've got hoodies, we've got, uh,
805
00:33:12.710 --> 00:33:15.230
all sorts of bits and bobs at the Space Nuts
806
00:33:15.230 --> 00:33:17.890
Shop, uh, at our website. Thank, uh,
807
00:33:18.150 --> 00:33:19.430
you, Fred. We'll leave it there. We'll catch
808
00:33:19.430 --> 00:33:20.550
you on the next episode.
809
00:33:21.030 --> 00:33:22.950
Professor Fred Watson: Look forward to it, Andrew. See you soon.
810
00:33:23.430 --> 00:33:25.669
Andrew Dunkley: Professor Fred Watson, astronomer at large.
811
00:33:25.669 --> 00:33:28.030
And thanks to Huw in the studio, who couldn't
812
00:33:28.030 --> 00:33:30.830
be with us today, had to be evacuated
813
00:33:30.830 --> 00:33:33.030
after attempting, uh, a Michael Jackson
814
00:33:33.030 --> 00:33:35.310
moonwalk. Not good at his age.
815
00:33:35.310 --> 00:33:35.670
Professor Fred Watson: No.
816
00:33:35.910 --> 00:33:37.630
Andrew Dunkley: And from me, Andrew Dunkley, thanks for your
817
00:33:37.630 --> 00:33:39.670
company. We'll catch you on the next episode
818
00:33:39.960 --> 00:33:41.160
of Space Nuts.
819
00:33:41.240 --> 00:33:41.600
Professor Fred Watson: Bye.
820
00:33:41.600 --> 00:33:44.520
Voice Over Guy: Bye. You've been listening to the
821
00:33:44.520 --> 00:33:45.880
Space Nuts podcast,
822
00:33:47.400 --> 00:33:50.280
available at Apple Podcasts, Spotify,
823
00:33:50.440 --> 00:33:53.200
iHeartRadio or your favorite podcast
824
00:33:53.200 --> 00:33:54.920
player. You can also stream on
825
00:33:54.920 --> 00:33:57.880
demand at bitesz.com. This has been another
826
00:33:57.880 --> 00:33:59.960
quality podcast production from
827
00:33:59.960 --> 00:34:01.040
bitesz.com
0
00:00:00.320 --> 00:00:01.800
Andrew Dunkley: Hi there. Thanks for joining us on another
1
00:00:01.800 --> 00:00:04.160
episode of Space Nuts. Great to have your
2
00:00:04.160 --> 00:00:06.440
company. My name is Andrew Dunkley, your host
3
00:00:06.440 --> 00:00:08.280
and I uh, hope you can stick around because
4
00:00:08.280 --> 00:00:11.120
we've got a jam packed show. We're
5
00:00:11.120 --> 00:00:13.440
once again going to Mars because
6
00:00:13.680 --> 00:00:16.560
they've looked uh, at some new evidence that
7
00:00:17.040 --> 00:00:19.720
uh, does suggest Mars oceans may have
8
00:00:19.720 --> 00:00:22.320
been vast. That is really
9
00:00:22.320 --> 00:00:24.400
exciting news. We're also going to look at
10
00:00:24.400 --> 00:00:27.000
the fastest spinning asteroid yet discovered.
11
00:00:27.000 --> 00:00:29.680
This one's uh, really in a spin.
12
00:00:29.680 --> 00:00:32.580
It's uh, making everybody dizzy. And the
13
00:00:32.580 --> 00:00:35.020
evacuation of the International Space Station
14
00:00:35.560 --> 00:00:38.060
uh, due to ill health. We'll see if we can
15
00:00:38.220 --> 00:00:39.940
get uh, some news on that because that's
16
00:00:39.940 --> 00:00:42.150
actually happening as Fred and I are uh,
17
00:00:42.150 --> 00:00:44.700
recording today. That's all coming up
18
00:00:44.940 --> 00:00:47.900
on this edition of Space Nuts. 15
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00:00:48.060 --> 00:00:49.980
seconds. Guidance is internal.
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00:00:50.220 --> 00:00:52.940
Voice Over Guy: 10, 9. Ignition
21
00:00:52.940 --> 00:00:55.706
sequence start. Space Nuts. 5, 4,
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00:00:55.774 --> 00:00:58.766
3. 2. 1, 2, 3, 4, 5, 5, 4,
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00:00:58.834 --> 00:01:01.780
3, 2, 1. Space Nuts astronauts
24
00:01:01.780 --> 00:01:02.940
report it feels good.
25
00:01:03.880 --> 00:01:06.120
Andrew Dunkley: And he's back again to furnish us with his
26
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knowledge. He is Professor Fred Watson,
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Astronomer at large. Hello Fred.
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Professor Fred Watson: Hello Andrew. I was just doing a quick
29
00:01:12.520 --> 00:01:14.800
calculation there for a number that I want to
30
00:01:14.800 --> 00:01:17.080
use um, later in the chat.
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Andrew Dunkley: Now I need to apologise in advance because
32
00:01:21.750 --> 00:01:24.200
ah, they're working across the road and I
33
00:01:24.200 --> 00:01:26.840
think they're using uh, dynamite because
34
00:01:27.720 --> 00:01:30.680
it's pretty noisy um, but
35
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hopefully it won't mess me up too much. I can
36
00:01:33.040 --> 00:01:34.400
hear it but I don't know if it's coming
37
00:01:34.400 --> 00:01:36.620
through the system. It's got all sorts of
38
00:01:36.620 --> 00:01:39.540
filters but um, some things you can't stop.
39
00:01:40.350 --> 00:01:40.490
Professor Fred Watson: Um.
40
00:01:40.740 --> 00:01:42.740
Andrew Dunkley: Now Fred, I did want to actually mention a
41
00:01:42.740 --> 00:01:44.540
couple of things before we start on our
42
00:01:44.540 --> 00:01:47.500
topics because uh, I meant to do this last
43
00:01:47.500 --> 00:01:50.460
week for our first show back of the year just
44
00:01:50.460 --> 00:01:52.060
to highlight some of the things that are
45
00:01:52.060 --> 00:01:54.660
coming up in 2026 that we can look forward to
46
00:01:54.660 --> 00:01:56.420
and that you and I will probably talk about.
47
00:01:56.900 --> 00:01:59.900
The Artemis 2 launch is
48
00:01:59.900 --> 00:02:02.590
slated. Uh, whether or not it'll be delayed
49
00:02:02.590 --> 00:02:04.950
again remains to be seen. But um, that will
50
00:02:04.950 --> 00:02:07.390
see a crew doing a lap around the moon,
51
00:02:08.080 --> 00:02:10.310
uh, and that'll be the first time humans have
52
00:02:10.310 --> 00:02:13.310
been back uh, in orbit around the moon
53
00:02:13.310 --> 00:02:15.470
since the 70s which uh, is
54
00:02:15.870 --> 00:02:18.160
exciting and probably too long but um,
55
00:02:18.160 --> 00:02:20.790
that'll be good. Um, this one I know will
56
00:02:20.790 --> 00:02:23.550
excite you. The Grace Roman Space Telescope
57
00:02:23.550 --> 00:02:26.100
is going to be launched. That one um,
58
00:02:26.430 --> 00:02:29.430
is going to um, opened so many doors for
59
00:02:29.430 --> 00:02:31.990
us I suspect, um, the
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00:02:31.990 --> 00:02:34.550
PLATO mission, uh, which will be searching
61
00:02:34.550 --> 00:02:36.630
for rocky planets. It'll uh, be doing a lot
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00:02:36.630 --> 00:02:38.750
more than that. But that's one of the things
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that it's being set out to do. Uh,
64
00:02:41.480 --> 00:02:43.710
China is to launch its own space
65
00:02:43.950 --> 00:02:46.910
telescope as well, um, in the hunt
66
00:02:46.910 --> 00:02:48.670
for dark matter and dark energy.
67
00:02:49.870 --> 00:02:52.270
And there's another mission that's going to
68
00:02:52.270 --> 00:02:54.750
be studying uh, the moon and Mars. Well,
69
00:02:54.750 --> 00:02:56.750
several missions, not just one. Um, more
70
00:02:56.750 --> 00:02:58.910
Chinese and Japanese missions involved there.
71
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And I think this is one you and I have talked
72
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about before. The Smile mission, uh, which
73
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will be studying Earth's magnetic field and
74
00:03:06.530 --> 00:03:08.180
how the sun interacts with our uh,
75
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atmosphere, uh, is um, due to be launched
76
00:03:11.170 --> 00:03:12.770
this year as well. I'm sure there's a lot
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more going on than that, but there's some of
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the highlights of 2026 so
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uh, we'll have a lot to talk about.
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00:03:19.250 --> 00:03:21.770
Professor Fred Watson: Fred, could I add a couple more as well?
81
00:03:21.770 --> 00:03:22.570
Andrew Dunkley: Oh, go for it.
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Professor Fred Watson: Um, we've just uh, heard that the Pandora
83
00:03:25.890 --> 00:03:28.450
spacecraft has entered orbit, uh, which I
84
00:03:28.450 --> 00:03:31.130
think is a spacecraft, uh, again looking
85
00:03:31.460 --> 00:03:34.270
um, looking at exoplanets to try
86
00:03:34.270 --> 00:03:36.630
and sort of tell us a bit more about how
87
00:03:36.630 --> 00:03:39.300
their atmospheres might reveal stuff. Um,
88
00:03:39.750 --> 00:03:42.070
China has just filed for 200,000
89
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satellites constellation with the
90
00:03:44.750 --> 00:03:47.470
International Telecommunications Union which
91
00:03:47.470 --> 00:03:50.070
is. Yeah, yeah, well it's not the biggest
92
00:03:50.070 --> 00:03:52.190
yet. The biggest was back in 2020 when the
93
00:03:52.190 --> 00:03:54.830
Rwandan government filed for over
94
00:03:54.830 --> 00:03:57.630
300,000. Um, uh, since then
95
00:03:57.630 --> 00:03:59.790
they've launched one cubesat, I think. So,
96
00:03:59.790 --> 00:04:02.550
um, that looked like a filing that
97
00:04:03.970 --> 00:04:05.930
getting your foot in the door. Uh, and just
98
00:04:05.930 --> 00:04:08.610
turning to nature. We've got some interesting
99
00:04:08.610 --> 00:04:11.090
events coming up. Uh, March 3rd, total
100
00:04:11.090 --> 00:04:13.730
eclipse of the Moon visible certainly from
101
00:04:13.730 --> 00:04:16.290
our hemisphere in Australia, not sure about
102
00:04:16.290 --> 00:04:18.220
North America and Europe. Um,
103
00:04:18.930 --> 00:04:21.450
there's uh, towards the end of the year and
104
00:04:21.450 --> 00:04:24.010
this will happen twice, uh, which is great
105
00:04:24.010 --> 00:04:26.050
cause you can see it on different sides of
106
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the Earth. I think it's October, sometime in
107
00:04:28.890 --> 00:04:31.200
October and sometime in November there will
108
00:04:31.200 --> 00:04:34.080
be an occultation of the planet Jupiter by
109
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the Moon. That means the moon will pass in
110
00:04:35.800 --> 00:04:38.000
front of Jupiter and certainly for us in
111
00:04:38.000 --> 00:04:40.320
November here in Australia it will be during
112
00:04:40.320 --> 00:04:42.400
the daytime. So get your binoculars out
113
00:04:42.400 --> 00:04:44.080
during the daytime, check out the moon and
114
00:04:44.080 --> 00:04:46.280
watch for Jupiter disappearing.
115
00:04:46.759 --> 00:04:49.720
Andrew Dunkley: Oh, that'll be good. Yeah,
116
00:04:49.720 --> 00:04:50.960
that'd be a good one for a backyard
117
00:04:50.960 --> 00:04:51.960
telescope, wouldn't it?
118
00:04:51.960 --> 00:04:53.640
Professor Fred Watson: Absolutely perfect, yes.
119
00:04:54.520 --> 00:04:57.500
Andrew Dunkley: Awesome. Um, I had my
120
00:04:57.500 --> 00:05:00.020
6 year old granddaughter here uh, the other
121
00:05:00.020 --> 00:05:02.900
day and uh, the moon was, was out in the
122
00:05:02.900 --> 00:05:05.740
east and um, it was still daytime but it was
123
00:05:05.740 --> 00:05:07.860
pretty prominent. So I grabbed the telescope
124
00:05:07.860 --> 00:05:10.500
and gave her a look and uh, I tried to
125
00:05:10.500 --> 00:05:12.540
explain to her what craters were and
126
00:05:13.340 --> 00:05:14.980
she struggled with the concept. But she
127
00:05:14.980 --> 00:05:17.240
eventually I think figured it out. But uh,
128
00:05:17.240 --> 00:05:19.300
yeah, took a couple of photos of her looking
129
00:05:19.300 --> 00:05:20.860
through the telescope. She was very excited
130
00:05:22.060 --> 00:05:23.060
which she sent to me.
131
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Professor Fred Watson: It was uh, lovely to see them, Andrew. Yeah,
132
00:05:25.220 --> 00:05:27.540
yeah, lovely, lovely shots. A youngster
133
00:05:27.540 --> 00:05:29.480
looking through a telescop with granddad in
134
00:05:29.480 --> 00:05:31.400
the background is great. Yeah, yeah.
135
00:05:31.860 --> 00:05:34.560
Andrew Dunkley: Uh, she's got blonde hair and blue eyes and
136
00:05:34.560 --> 00:05:36.760
her brothers and sisters are all brown haired
137
00:05:36.760 --> 00:05:38.840
and brown eyed. So. Okay,
138
00:05:39.480 --> 00:05:41.720
she, she seems to have picked up Judy's side
139
00:05:41.720 --> 00:05:44.360
of the family genes because Judy's blondie,
140
00:05:44.360 --> 00:05:47.240
blonde with blue eyes. But um, she's the only
141
00:05:47.240 --> 00:05:49.520
one in the, in the family that's, that's gone
142
00:05:49.520 --> 00:05:52.360
that, that way. It happens though, doesn't
143
00:05:52.360 --> 00:05:53.320
it? It's just the way it is.
144
00:05:53.320 --> 00:05:53.640
Professor Fred Watson: Yeah.
145
00:05:53.640 --> 00:05:54.520
Andrew Dunkley: That's DNA.
146
00:05:55.220 --> 00:05:58.180
Um, okay Fred, uh,
147
00:05:58.180 --> 00:06:00.320
let's get stuck into it because uh, we're
148
00:06:00.320 --> 00:06:03.240
heading off to Mars and we're
149
00:06:03.240 --> 00:06:06.000
doing this because of a study that's just
150
00:06:06.000 --> 00:06:08.840
been published. Uh, in fact in the
151
00:06:08.840 --> 00:06:11.740
last week, uh, or two about uh,
152
00:06:11.759 --> 00:06:14.160
observations of Mars that suggest
153
00:06:14.880 --> 00:06:17.840
that its oceans were once vast. Now
154
00:06:17.840 --> 00:06:19.680
we always knew there was probably surface
155
00:06:19.680 --> 00:06:22.280
water but we didn't really know whether they
156
00:06:22.280 --> 00:06:25.120
were, you know, pockets or separate
157
00:06:25.120 --> 00:06:28.060
oceans or what. But now they're thinking
158
00:06:28.540 --> 00:06:29.980
the oceans might have been
159
00:06:31.020 --> 00:06:31.820
enormous.
160
00:06:32.740 --> 00:06:35.580
Professor Fred Watson: Uh, yes, that's right. And I mean, you know,
161
00:06:36.540 --> 00:06:39.420
we revisit this story probably on average
162
00:06:39.420 --> 00:06:42.260
once every month or two. Uh, the
163
00:06:42.260 --> 00:06:44.940
last time we covered this, and I
164
00:06:45.100 --> 00:06:47.140
wrote it up actually in um, an Australian
165
00:06:47.140 --> 00:06:49.740
Geographic article, um, not that I did the
166
00:06:49.740 --> 00:06:51.500
research, but this is other people's research
167
00:06:51.660 --> 00:06:54.180
and that was pointing in the same direction.
168
00:06:54.180 --> 00:06:56.820
Andrew. It was um, a group that looked at the
169
00:06:56.820 --> 00:06:59.800
way um, rivers, ancient rivers on Mars, uh,
170
00:07:00.120 --> 00:07:02.600
meandered, uh, because you can learn
171
00:07:02.600 --> 00:07:05.560
something from the meandering about the
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size of the body of water that they're
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emptying into. And they came to the same
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conclusion. The river meanders tell you that
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there was a large body of water at the end of
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it at the mouth of these rivers, uh, rather
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than just a few puddles or a few lakes and
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things of that sort. Uh, and this new piece
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uh, of work, um, whilst it's a different,
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uh, you know, it's got a different emphasis,
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comes up with exactly the same answer. Uh,
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and it's scientists uh, who have looked uh,
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at the, I remember rightly there in
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uh, in Switzerland. Yeah, University of Bern,
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uh, it's scientists who've looked at the
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region around Valles, uh,
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Marineris, you know, that great huge
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chasm in the, uh, in the surface of
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Mars. Near Mars's equator. Uh, something that
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makes the Grand Canyon look like a bit of a
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scratch on the, on the surface of the Earth.
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Andrew Dunkley: Yeah. Is it right that the Grand Canyon would
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fit into one of its tributaries or something?
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Professor Fred Watson: That's right. I think that's correct, yeah.
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Andrew Dunkley: Amazing.
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Professor Fred Watson: Um, so they've been looking in that region
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and certainly on the northern side and the
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northern flanks there are valleys that
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um, sort of open out onto the plains of Mars.
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Because that uh, Valles Marineris is kind
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of right at the start of the highland areas
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of the southern hemisphere of Mars. Mars has
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got this dichotomy. The northern hemisphere
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is flat and low, southern hemisphere 3km
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higher on average, full of craters, mountains
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and all around rest of it. Uh, so um, uh,
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um, what they've done is they've looked at
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regions, uh, where, you know, where there's
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this transition from the mountainous
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highlands of the south to the
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lowlands of the north. And they've looked
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very carefully at uh, data from
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uh, several orbiting spacecraft, um, I
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guess Mars Reconnaissance Orbiter is one and
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some of the other ones, um, actually even um,
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uh, um, ESO's
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ExoMars Trace Gas Orbiter. So, uh,
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Mars Express, another ESA, sorry, not ESO,
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ESA, uh, European Space Agency, Another
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um, uh, uh, orbiting spacecraft. They've
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taken the data from these, looked
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at the height, the
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topography and looked at the
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geomorphology. Let me get it right.
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Geomorphological, um,
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um, features that they can find.
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What have they spotted? They've spotted,
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ah, a whole succession of
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ancient river deltas, um, this
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is to say regions where a river mouth
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opened into what they're calling now
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an ocean, uh, and deposited
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um, its sediments. The sediments out of the
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river fall down to the floor, uh, of the
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ocean and build up basically
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a rock form, uh, which is preserved today.
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It's a kind of fossilized river delta.
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There's something similar going on, uh, as
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you and I have spoken about many times at
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Jezero Crater, which is why, um,
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perseverance is there, because there's a
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river delta there. But I think these are on a
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much larger scale. And um, the
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great thing is that when you look at them,
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they sort of define a shoreline,
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um, because these are all occurring
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at the same topographical height in
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Mars's geography. And so they
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basically uh, define a shoreline. And that
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shoreline tells you that um, there would have
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been a lot of water in Mars's northern
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hemisphere for the water level to reach the
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height that we find those deltas at.
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Uh, so really? Yeah, really nice piece
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of Work, uh, done with characteristic
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Swiss precision, I think. Uh, that's been
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widely reported. Um, there's several
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articles, uh, on the science news feeds,
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um, which basically support this idea.
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Very nice piece of research indeed.
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Andrew Dunkley: And they think it was as big as
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the Arctic Ocean on Earth, just by
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comparison. And how big as the Arctic Ocean?
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It's 14 million square kilometers or
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five and a half million square miles
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big, uh, in size. So that's a lot of
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water on Mars and uh, a lot of it's still
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there, Fred.
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Professor Fred Watson: Yeah, that's right. We um, know from
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particularly, uh, the Phoenix mission that
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just scraped the surface in the Martian
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Arctic and sure enough there was permafrost
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underneath. So a lot of it's still there.
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There's still water locked up in the two ice
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caps of Mars. Um, but probably
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not. Well, I don't know. It's actually really
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interesting. I do remember reading quite some
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time ago that if you thawed out even just the
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Antarctic ice cap of Mars, you'd cover the
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whole planet to a depth of several meters.
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Um, now whether that still holds good with
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what we've discovered since then, that was
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quite an old, I think that was probably 20
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years, 15 years ago, so that that comment
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was made. It would be interesting to know how
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we evaluate that now. But I think it's still
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true, uh, that a lot of that water is still
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there.
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Andrew Dunkley: Ah, yeah, it is, uh, a
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fascinating story.
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Professor Fred Watson: Water means life.
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Andrew Dunkley: Well, yes, yes, we've said that many times.
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And you just don't know, do you?
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Professor Fred Watson: You don't. Yeah.
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Andrew Dunkley: Although the, uh, the mission to retrieve
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those um, cylinders that contain
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potential evidence of that.
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Professor Fred Watson: Yeah.
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Andrew Dunkley: Has been scotched. So it's just going to sit
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in abeyance for um, an
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indefinite period.
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Professor Fred Watson: So, yeah, I think, um,
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so this is news that, um, the Senate have
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um, basically agreed with the White House in
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saying that um, the Mars Sample Return
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Mission, uh, should be canceled. Uh,
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and so that will probably go through. It's
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not been voted on yet, I don't think. Um,
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and so that means, yes, we've got these
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canisters on Mars, uh, carefully dropped by
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perseverance, uh, but
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with a joint European Space Agency NASA
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mission to retrieve them, uh, which, whose
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cost has blown out. Uh, we've talked about
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this before, uh, and not perhaps
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surprising that it's now had a line drawn
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under it. Now that's bad
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news because we really would like to get hold
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of these samples. There's one in particular
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that may contain actually fossilized
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microbes. Uh, you know, um,
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so it's um, there's uh, every keenness to do
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that. Um, um, and I think it
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will. There'll certainly be a revisiting
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of this idea. Esa, I think, is still going
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ahead with their half of the bargain. Which
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was, I think, to build the orbiter which
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would actually bring the samples back to
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Mars. NASA's part was gathering them up on
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the surface and sending them up to orbit
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around Mars. Uh, so, you know,
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uh, it's bad news. There's a bright side to
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it though, in that the money that's being
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saved will probably go to some of the other
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missions that are being planned.
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Name your favorite planet. You might get some
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good news out of this. I know your favorite
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and probably mine too, is Mars. Uh, but,
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um, anyway, we'll see what happens. I
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wouldn't write, uh, the Mars sample return
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off altogether in my flights of
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fantasy. Last night, while my,
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uh, respiratory tract infection was
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making me cough all night, I was thinking
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maybe the Chinese could bring them back
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because I think they're planning a sample
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return mission as well. So maybe we do a deal
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there. Which would be fabulous international
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cooperation.
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Andrew Dunkley: It would. It would indeed. Of course, we
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could always start the conspiracy and say,
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what does NASA and the US Government know
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that they're not telling us?
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Hence no return. Yeah, yeah.
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Professor Fred Watson: Be careful what you, what you say, Andrew.
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Andrew Dunkley: No, look, I'm just kidding around, but, uh,
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it's just money, isn't it? That's, that's the
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thing.
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Professor Fred Watson: It's all about money. That's right. It's not
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about finding something with legs that you
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don't want anybody to know about.
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Andrew Dunkley: Yes, that's been done in a lot of science
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fiction films.
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Professor Fred Watson: Yeah, it has. And um.
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Andrew Dunkley: Yes, all right. Great story about
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the oceans of Mars though. If you'd like to
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check it out, it's on the Phys p h y
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s.org website. Or you can read the
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paper that's been published in the journal
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NPJ Space Exploration.
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This is Space Nuts with Andrew Dunkley and
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Professor Fred Watson.
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Roger, in your labs right here.
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Also Space Nuts to our
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next story, Fred. And this
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is, uh, a really good one for a couple of
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reasons. It's something we haven't seen
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before, but it also involves the, uh,
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Rubin Observatory, which, um,
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has already, uh, done things that,
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uh, other observatories have not been able
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to do and promises to do so much more.
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This is the fastest spinning asteroid yet
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discovered. And a couple of headlines I've
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read suggested why hasn't it thrown itself
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to pieces because of the speed at which it's
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rotating and
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the rate is rather high when you look at what
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the average asteroid does.
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Professor Fred Watson: Yeah, so it is a record breaker.
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It's the fastest spinning asteroid
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for its size. Uh, because I think
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smaller things can spin faster than this.
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It's uh, 710 meters long, nearly
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three quarters of a kilometer. Uh, so
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it's not a small asteroid at all. This
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is quite a large one. Uh, and
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it spins at the rate of one rotation
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every one minute 53
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seconds. So that
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is one heck of a spin. So that's its day
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length, Andrew. If you were standing on it,
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your day will be 1 minute 53 seconds. Seconds
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night and day, not 24 hours. Um,
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but uh, you're absolutely right. I think it's
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interesting for two reasons. One is exactly
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as you've said. It underlines, uh, just
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how powerful the Rubin Observatory is going
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to be. The observations of
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this object were made during the
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sort of commissioning period for the
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telescope's instruments, which was earlier
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last year, April and May 2025. Uh,
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and um, that you know, that um,
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as you probably remember, I think they
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released uh, uh, information saying they got.
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They discovered more than a thousand
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asteroids in 10 hours of observing, which is
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pretty fantastic. Uh, the telescope's
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capabilities will allow it to survey the
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entire southern sky every three
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nights, uh, with an eight meter class
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telescope. That is an astonishing achievement
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and we.
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Andrew Dunkley: Must find something incredible.
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Professor Fred Watson: Yeah, we will. Yeah, there's going to be all
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kinds of things that come out of the
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woodwork. Uh, it's what we call, um,
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uh, sort of time sensitive astronomy or
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transient astronomy. You're looking for
431
00:17:51.360 --> 00:17:54.120
things that either move or change in the sky
432
00:17:54.120 --> 00:17:56.400
and it's going to be so good at finding them.
433
00:17:56.720 --> 00:17:59.480
And um. Yeah. So the real
434
00:17:59.480 --> 00:18:01.800
observing, uh, campaign, the Large
435
00:18:01.800 --> 00:18:04.400
Synoptic Survey, uh, will start
436
00:18:04.790 --> 00:18:07.560
uh, sometime this year, uh, sort of when
437
00:18:07.560 --> 00:18:10.240
they're ready to hit the go button. Uh, but I
438
00:18:10.240 --> 00:18:12.060
think everybody at the Rubin is pretty happy
439
00:18:12.060 --> 00:18:14.460
with the way things are going. Um, and just
440
00:18:14.460 --> 00:18:17.340
to sort of highlight that, you know,
441
00:18:18.300 --> 00:18:21.020
it's a telescope with this kind of capability
442
00:18:21.100 --> 00:18:24.020
to make many observations over a short period
443
00:18:24.020 --> 00:18:26.860
of time of the same area of sky. That has
444
00:18:26.860 --> 00:18:29.780
allowed uh, the scientists to
445
00:18:29.780 --> 00:18:32.540
discover the very rapid rotation
446
00:18:32.700 --> 00:18:34.980
of this asteroid. Because what you have to
447
00:18:34.980 --> 00:18:37.620
produce, uh, to look at the way an asteroid
448
00:18:37.620 --> 00:18:39.300
rotates is what's called a light curve. You
449
00:18:39.300 --> 00:18:41.700
look at the way its brightness changes. Uh,
450
00:18:41.700 --> 00:18:44.280
because most asteroids, asteroids are quite
451
00:18:44.280 --> 00:18:46.000
asymmetric. They're either shaped like a
452
00:18:46.000 --> 00:18:48.840
potato or a dumbbell. Very, uh, few are
453
00:18:48.840 --> 00:18:51.560
anything remotely spherical. Um, uh,
454
00:18:51.560 --> 00:18:53.760
this particular one is I think Quite
455
00:18:53.760 --> 00:18:56.520
elongated. And so as it rotates,
456
00:18:56.980 --> 00:18:59.800
uh, different sides of it catch the
457
00:18:59.800 --> 00:19:01.680
sunlight and you get a variation in the light
458
00:19:01.680 --> 00:19:04.540
that we see from it. Uh, and so that uh,
459
00:19:04.540 --> 00:19:06.600
has allowed, because it's, you know, it's
460
00:19:06.600 --> 00:19:08.920
only 1 minute 53 seconds for one
461
00:19:09.080 --> 00:19:11.600
complete revolution that has allowed the
462
00:19:11.600 --> 00:19:14.360
scientists to determine that fact,
463
00:19:14.800 --> 00:19:17.180
um, to the asteroid itself. You're right,
464
00:19:17.180 --> 00:19:19.700
it's interesting. It rejoices in the name of
465
00:19:19.700 --> 00:19:22.220
2025 MN45, a
466
00:19:22.220 --> 00:19:25.060
classic asteroid name. Um, and
467
00:19:25.220 --> 00:19:27.780
it's in the main asteroid belt. That's
468
00:19:28.100 --> 00:19:31.020
a good place for it to be between uh, Jupiter
469
00:19:31.020 --> 00:19:33.220
and Mars, where most of the asteroids are.
470
00:19:33.700 --> 00:19:36.540
Uh, but um, its rotation
471
00:19:36.540 --> 00:19:39.060
is what highlights um,
472
00:19:39.300 --> 00:19:42.140
the unusual nature of it. Because as you and
473
00:19:42.140 --> 00:19:44.340
I have spoken about before, many asteroids
474
00:19:44.340 --> 00:19:46.980
are uh, basically what we call rubble piles.
475
00:19:46.980 --> 00:19:49.380
They're just piles of debris which stick
476
00:19:49.380 --> 00:19:52.300
together loosely under their own,
477
00:19:52.520 --> 00:19:55.020
uh, gravity. Um, little
478
00:19:55.160 --> 00:19:57.940
uh, Dimorphos and Didymos, the
479
00:19:57.940 --> 00:20:00.700
two, uh, objects that NASA did the
480
00:20:00.700 --> 00:20:02.780
DART test on a few years ago, they are
481
00:20:02.780 --> 00:20:04.580
probably rubber piles. They've got the
482
00:20:04.580 --> 00:20:06.460
characteristic rubber pile shape, which is
483
00:20:06.460 --> 00:20:09.260
like two cones, um, uh, back to
484
00:20:09.260 --> 00:20:11.940
back. Uh, if it was a rubber
485
00:20:11.940 --> 00:20:13.620
pile, it would have flown apart
486
00:20:14.490 --> 00:20:17.450
gazillions of years ago, uh, with
487
00:20:17.450 --> 00:20:19.930
that short period of rotation, 1 minute
488
00:20:20.090 --> 00:20:23.090
53 seconds. So, um, uh, and when
489
00:20:23.090 --> 00:20:25.370
you look at the size of it and
490
00:20:25.880 --> 00:20:28.210
uh, interpret what the rotation means, it
491
00:20:28.210 --> 00:20:30.130
tells you it's probably made of absolutely
492
00:20:30.130 --> 00:20:32.570
solid rock. This is something that is
493
00:20:33.040 --> 00:20:35.570
um, going to be hard to pull apart, to
494
00:20:35.570 --> 00:20:38.450
rotate. For it to be that big rotate at that
495
00:20:38.450 --> 00:20:41.400
speed, it's got to be solid rock, um,
496
00:20:41.460 --> 00:20:43.800
um, making it uh, you know, in some ways even
497
00:20:43.800 --> 00:20:45.360
more interesting because we think the rubber
498
00:20:45.360 --> 00:20:47.340
piles are perhaps the more common uh,
499
00:20:47.480 --> 00:20:48.680
asteroids that we see.
500
00:20:49.240 --> 00:20:51.840
Andrew Dunkley: Do we, do we have any idea what would make it
501
00:20:51.840 --> 00:20:53.680
different, why it would be different? Is it a
502
00:20:53.680 --> 00:20:56.200
piece of a destroyed planet Theia?
503
00:20:57.400 --> 00:20:59.920
Professor Fred Watson: Well, yeah, could be, uh, might be part of
504
00:20:59.920 --> 00:21:02.790
Theia, the one that created the moon, uh,
505
00:21:03.400 --> 00:21:05.400
after, after it collided with the ah, Earth.
506
00:21:05.560 --> 00:21:08.240
It's more likely you're right. It's
507
00:21:08.240 --> 00:21:11.150
probably, um, you know, maybe part of the
508
00:21:11.470 --> 00:21:14.350
outer mantle of what would have been
509
00:21:14.350 --> 00:21:17.270
a protoplanet. In the early solar
510
00:21:17.270 --> 00:21:19.390
system, these things were the building blocks
511
00:21:19.390 --> 00:21:21.310
of planets. They collided and sometimes they
512
00:21:21.310 --> 00:21:23.230
blasted each other apart, sometimes
513
00:21:24.190 --> 00:21:26.990
they stuck together to form what we see
514
00:21:26.990 --> 00:21:29.510
in the solar system today. Um,
515
00:21:29.630 --> 00:21:31.990
and I, uh, think some of the collisions that
516
00:21:31.990 --> 00:21:33.510
would have happened in the early solar
517
00:21:33.510 --> 00:21:36.470
system, uh, may well have set an
518
00:21:36.470 --> 00:21:38.510
object like this spinning very rapidly. In
519
00:21:38.510 --> 00:21:41.140
fact, it might have initially been
520
00:21:41.290 --> 00:21:43.130
spinning even more rapidly. Than it is now.
521
00:21:43.290 --> 00:21:45.250
Because we're looking at probably several
522
00:21:45.250 --> 00:21:47.930
billion years ago. When whatever
523
00:21:47.930 --> 00:21:50.690
happened to it happened. So, uh, an
524
00:21:50.690 --> 00:21:53.690
object of some interest. And, um, one
525
00:21:53.690 --> 00:21:56.530
that I'm sure will be studied, uh, in
526
00:21:56.530 --> 00:21:58.770
greater detail. We might want to know things
527
00:21:58.770 --> 00:22:01.410
like, um, the infrared signature of its
528
00:22:01.410 --> 00:22:03.890
surface. Which gives you an idea of what the
529
00:22:03.890 --> 00:22:05.610
surface is like, how rough it is, whether
530
00:22:05.610 --> 00:22:08.140
it's a. Whether it's a smooth
531
00:22:08.140 --> 00:22:10.740
surface. What materials are likely to be,
532
00:22:11.090 --> 00:22:12.860
uh, found on its surface. That can all come
533
00:22:12.860 --> 00:22:15.260
from spectroscopy and also the science of
534
00:22:15.260 --> 00:22:17.500
polarimetry, which is what you look at to
535
00:22:17.500 --> 00:22:19.260
know whether something's highly reflective.
536
00:22:19.260 --> 00:22:22.020
Or rather rough and diffuse. So,
537
00:22:22.020 --> 00:22:24.340
yeah, m. I think there's lots to learn about,
538
00:22:24.530 --> 00:22:26.820
uh, 2025 MN45.
539
00:22:27.380 --> 00:22:30.380
Andrew Dunkley: Indeed. So it's in the asteroid
540
00:22:30.380 --> 00:22:32.500
belt between Mars and Jupiter.
541
00:22:32.670 --> 00:22:35.500
Um, people probably imagine
542
00:22:35.500 --> 00:22:38.020
that to be just a wall of roc.
543
00:22:38.800 --> 00:22:40.640
How do we get through it? But it's quite
544
00:22:40.640 --> 00:22:41.680
sparse, isn't it?
545
00:22:41.920 --> 00:22:44.840
Professor Fred Watson: It is, yeah. Yeah. Uh, it's
546
00:22:44.840 --> 00:22:46.880
sparse enough that, um, uh, several
547
00:22:46.880 --> 00:22:48.440
spacecraft have actually gone through it
548
00:22:48.440 --> 00:22:51.320
unscathed. Um, so,
549
00:22:51.320 --> 00:22:52.000
yes, it's.
550
00:22:52.000 --> 00:22:53.920
Andrew Dunkley: Well, I've never heard of a spacecraft
551
00:22:53.920 --> 00:22:55.600
actually running into anything out there.
552
00:22:56.720 --> 00:22:58.360
Not that there have been that many that have
553
00:22:58.360 --> 00:22:59.040
gone through, but.
554
00:22:59.200 --> 00:23:01.850
Professor Fred Watson: That's right. But, you know, as, um.
555
00:23:02.230 --> 00:23:05.040
Uh. Was it Douglas Adams. Space
556
00:23:05.040 --> 00:23:05.920
is big. Yes.
557
00:23:06.160 --> 00:23:06.560
Andrew Dunkley: Yes.
558
00:23:06.560 --> 00:23:08.440
Professor Fred Watson: You might think it's a long way down to the
559
00:23:08.440 --> 00:23:10.500
chemist at the corner of the street. But
560
00:23:10.980 --> 00:23:13.180
that's nothing compared with space. I think
561
00:23:13.180 --> 00:23:14.180
that was what he said.
562
00:23:16.100 --> 00:23:18.700
Andrew Dunkley: Yes, indeed. Uh, so if you would like to
563
00:23:18.700 --> 00:23:21.660
learn more about what the Vera C. Rubin
564
00:23:21.660 --> 00:23:23.820
Observatory has discovered, you can do
565
00:23:23.820 --> 00:23:26.620
that@the universitytoday.com website.
566
00:23:26.620 --> 00:23:28.300
Or you can read the paper in the
567
00:23:28.300 --> 00:23:31.220
Astrophysical Journal Letters. Which was,
568
00:23:31.340 --> 00:23:34.100
uh, only published on January 7th. So they're
569
00:23:34.100 --> 00:23:35.620
getting down to business early this year,
570
00:23:35.620 --> 00:23:36.100
aren't they?
571
00:23:36.260 --> 00:23:39.180
Professor Fred Watson: This is space nuts. Sorry. I was
572
00:23:39.180 --> 00:23:41.620
going to say, um, we always get a really
573
00:23:42.020 --> 00:23:44.300
good, um, crop of news stories at this time
574
00:23:44.300 --> 00:23:46.100
of year. Because it's right at the beginning
575
00:23:46.100 --> 00:23:48.700
of January that the American Astronomical
576
00:23:48.700 --> 00:23:51.060
Society has its annual meeting.
577
00:23:52.260 --> 00:23:55.060
And, um, so there's always some great
578
00:23:55.060 --> 00:23:58.020
stories. So, you know, that's why it was,
579
00:23:58.020 --> 00:23:59.540
uh. You know, it was published last week. I'm
580
00:23:59.540 --> 00:24:00.460
sure that's actually.
581
00:24:00.460 --> 00:24:02.980
Andrew Dunkley: It's actually very clever because as someone
582
00:24:02.980 --> 00:24:05.940
who worked in the media for 40 years. And
583
00:24:07.140 --> 00:24:09.380
had, um, to work a lot of Christmases and New
584
00:24:09.600 --> 00:24:12.280
Years, you quite often find you're
585
00:24:12.280 --> 00:24:14.640
struggling for stories because
586
00:24:14.880 --> 00:24:16.880
everything's shut down. So you're not getting
587
00:24:16.880 --> 00:24:19.200
the information that you normally get. So
588
00:24:19.600 --> 00:24:22.080
to actually be in a position to do stories
589
00:24:22.320 --> 00:24:25.030
like this at this time of year is
590
00:24:25.030 --> 00:24:28.000
um. Yeah, it's well
591
00:24:28.000 --> 00:24:30.830
positioned, as we would say. M. Uh,
592
00:24:30.830 --> 00:24:33.730
you can read all about it, of course. And uh,
593
00:24:33.730 --> 00:24:36.360
we uh, will certainly be keeping a very close
594
00:24:36.360 --> 00:24:38.920
eye on what the Vera C. Rubin Observatory is
595
00:24:38.920 --> 00:24:39.920
going to be doing
596
00:24:40.770 --> 00:24:43.710
um, from now on because it's uh,
597
00:24:43.710 --> 00:24:46.200
it's, it's, it's all up and running and uh,
598
00:24:46.430 --> 00:24:49.430
already doing some remarkable things. This
599
00:24:49.430 --> 00:24:51.230
is Space Nuts with Andrew Dunkley and Fred
600
00:24:51.230 --> 00:24:51.790
Watson.
601
00:24:55.869 --> 00:24:58.510
Space Nuts. Now Fred, uh, by the time
602
00:24:58.750 --> 00:25:00.670
people hear us talking about this story,
603
00:25:00.670 --> 00:25:03.630
things will have uh, changed a bit. But
604
00:25:03.630 --> 00:25:06.510
as we speak, uh, we understand that
605
00:25:06.510 --> 00:25:08.910
the Crew Dragon spacecraft
606
00:25:09.760 --> 00:25:12.520
is docking at the International Space Station
607
00:25:12.520 --> 00:25:15.160
to do the first ever crew
608
00:25:15.160 --> 00:25:17.680
evacuation. Now, after 25 years,
609
00:25:18.400 --> 00:25:20.480
I'm surprised this is the first time this has
610
00:25:20.480 --> 00:25:22.280
happened. But uh, there's been a medical
611
00:25:22.280 --> 00:25:24.560
issue. They won't elaborate on who or what,
612
00:25:25.300 --> 00:25:27.440
uh, but it's gotta be serious if somebody's
613
00:25:27.440 --> 00:25:29.440
um, if they're bringing the whole crew back.
614
00:25:29.600 --> 00:25:32.040
It's uh, a crew of four. There's seven on
615
00:25:32.040 --> 00:25:33.600
board at the moment. But they're bringing
616
00:25:33.600 --> 00:25:35.040
four back, correct?
617
00:25:35.040 --> 00:25:37.680
Professor Fred Watson: That's right. So, uh, there is a crew of
618
00:25:37.680 --> 00:25:40.680
three uh, now. So as we speak, um, I
619
00:25:40.680 --> 00:25:43.340
think they've probably undocked the crew
620
00:25:43.340 --> 00:25:45.180
Dragon spacecraft from the International
621
00:25:45.260 --> 00:25:46.980
Space Station. I think that happened an hour
622
00:25:46.980 --> 00:25:49.700
ago. And um, they
623
00:25:49.700 --> 00:25:52.700
will then re. Enter and bring the crew
624
00:25:52.700 --> 00:25:55.260
back in a pretty routine fashion,
625
00:25:55.600 --> 00:25:58.540
uh, landing in a few hours from now. Um, so
626
00:25:58.540 --> 00:26:01.460
you're right, it's Crew 11, uh,
627
00:26:01.460 --> 00:26:03.750
the SpaceX, um,
628
00:26:04.300 --> 00:26:06.140
what's called the SpaceX Crew 11 because
629
00:26:06.140 --> 00:26:07.700
they're the ones that go up and down in the
630
00:26:07.700 --> 00:26:10.460
crew Dragon, uh, rather than the Soyuts,
631
00:26:10.460 --> 00:26:12.180
which is the space vehicle that will bring
632
00:26:12.180 --> 00:26:14.720
the other uh, the remaining three astronauts
633
00:26:14.720 --> 00:26:17.720
down when their time comes to an end. Uh,
634
00:26:17.720 --> 00:26:19.840
you're right. It's a medical evacuation that
635
00:26:19.840 --> 00:26:22.640
Crew, Crew 11 consists of, um, if I
636
00:26:22.640 --> 00:26:25.490
remember rightly, two NASA, uh, uh,
637
00:26:25.490 --> 00:26:27.920
astronauts, one Russian
638
00:26:27.920 --> 00:26:30.520
cosmonaut and uh, a Japanese
639
00:26:31.070 --> 00:26:33.680
uh, astronaut as well. Uh, so they're coming
640
00:26:33.680 --> 00:26:36.440
home, uh, they're coming home something like
641
00:26:36.440 --> 00:26:39.120
a month early. And we are told as
642
00:26:39.120 --> 00:26:41.000
exactly as you've said that this is because
643
00:26:41.000 --> 00:26:43.710
of a medical issue which apparently is not
644
00:26:43.810 --> 00:26:46.710
uh, an emergency. It's not urgent, but it's
645
00:26:46.710 --> 00:26:48.630
thought to be something that is going to be
646
00:26:48.630 --> 00:26:51.630
much better dealt with on Earth. Uh, we don't
647
00:26:51.630 --> 00:26:54.030
know which of the astronauts has the issue.
648
00:26:54.650 --> 00:26:57.030
Um, I saw a picture of them posed just before
649
00:26:57.030 --> 00:26:58.990
they evacuated the spacecraft,
650
00:26:59.430 --> 00:27:02.350
uh, um, last night and they all looked
651
00:27:02.350 --> 00:27:05.230
fairly cheerful, uh, but um, so
652
00:27:05.230 --> 00:27:07.070
you know, uh, you can't really read
653
00:27:09.630 --> 00:27:11.510
from people's faces how they're feeling. Um,
654
00:27:12.410 --> 00:27:13.970
which is just as well because I feel pretty
655
00:27:13.970 --> 00:27:16.730
crook at the moment. So
656
00:27:16.970 --> 00:27:19.210
that's uh, because of my uh, uh, upper
657
00:27:19.690 --> 00:27:21.730
respiratory tract infection. Sorry to keep
658
00:27:21.730 --> 00:27:23.570
harping on about it. Anyway, going back to
659
00:27:23.570 --> 00:27:26.530
the more important story, Andrew. Well it's
660
00:27:26.530 --> 00:27:27.170
a good thing you're not.
661
00:27:27.170 --> 00:27:29.010
Andrew Dunkley: In the International Space Station feeling
662
00:27:29.010 --> 00:27:29.450
like that.
663
00:27:29.450 --> 00:27:31.290
Professor Fred Watson: Well, that's right, I, you'd have the same
664
00:27:31.290 --> 00:27:33.760
thing too. Uh, so, yeah, so,
665
00:27:33.760 --> 00:27:36.290
um, interesting. Uh, but your comment's well
666
00:27:36.290 --> 00:27:38.330
made. You know the fact that it's the first
667
00:27:38.330 --> 00:27:40.730
time in the 25 year history
668
00:27:41.290 --> 00:27:44.000
of the ISS, of the
669
00:27:44.000 --> 00:27:46.880
ISS being permanently occupied,
670
00:27:47.360 --> 00:27:49.960
um, the first time this has happened. And I
671
00:27:49.960 --> 00:27:52.360
think it was Jared Isaacman, the newly
672
00:27:52.360 --> 00:27:55.360
appointed NASA administrator, the boss of
673
00:27:55.600 --> 00:27:58.520
NASA, who made the comment. It might
674
00:27:58.520 --> 00:28:01.120
be somebody else but it is one of the
675
00:28:01.520 --> 00:28:04.240
high ups in NASA made the comment that
676
00:28:04.480 --> 00:28:06.760
when they planned the ISS and they were
677
00:28:06.760 --> 00:28:09.240
working towards it, they expected that there
678
00:28:09.240 --> 00:28:10.960
would be something like this happening every
679
00:28:10.960 --> 00:28:13.840
three years. So they've done pretty well
680
00:28:13.840 --> 00:28:16.110
to get through 2015, five years without um,
681
00:28:16.110 --> 00:28:17.820
needing to bring people home because of a
682
00:28:17.820 --> 00:28:19.580
medical issue. Yeah.
683
00:28:20.620 --> 00:28:22.460
Andrew Dunkley: While you've been talking Fred, I've just
684
00:28:22.460 --> 00:28:24.740
been looking online to see where things are
685
00:28:24.740 --> 00:28:27.660
up to and I've found a um, they did a live
686
00:28:27.740 --> 00:28:30.580
stream of the crew uh, Dragon docking at the
687
00:28:30.580 --> 00:28:32.620
International Space Station through
688
00:28:32.880 --> 00:28:35.540
uh, I think it's NASA's YouTube Music
689
00:28:35.540 --> 00:28:38.420
channel and you can, you can
690
00:28:38.420 --> 00:28:40.620
actually log on and, and watch what happens
691
00:28:40.850 --> 00:28:43.850
and see the whole process. It's quite
692
00:28:43.850 --> 00:28:45.890
incredible what we can do now isn't it with
693
00:28:45.900 --> 00:28:48.570
um, live coverage from space as ah, things
694
00:28:48.570 --> 00:28:51.410
unfold. It's uh, a far cry
695
00:28:51.410 --> 00:28:54.010
from those times back in the 60s and 70s when
696
00:28:54.010 --> 00:28:55.850
we were looking at those really fuzzy black
697
00:28:55.850 --> 00:28:57.250
and white pictures off the moon.
698
00:28:59.090 --> 00:29:00.850
Professor Fred Watson: Which was miraculous in its day.
699
00:29:00.850 --> 00:29:02.850
Andrew Dunkley: Oh it was in itself, yes. Yes.
700
00:29:03.170 --> 00:29:03.650
Professor Fred Watson: Yeah.
701
00:29:04.530 --> 00:29:07.130
Andrew Dunkley: Actually I am watching Crew Dragon detach as
702
00:29:07.130 --> 00:29:07.570
we speak.
703
00:29:07.570 --> 00:29:08.010
Professor Fred Watson: Yes, that's right.
704
00:29:08.010 --> 00:29:10.720
Andrew Dunkley: So that happened probably 30 minutes ago,
705
00:29:10.720 --> 00:29:13.640
give or take our time. Yeah,
706
00:29:13.760 --> 00:29:16.200
um, it's, it's like a slow motion ballet
707
00:29:16.200 --> 00:29:18.360
isn't it? When they uh, things in
708
00:29:18.360 --> 00:29:19.720
spacecraft.
709
00:29:19.720 --> 00:29:22.040
Professor Fred Watson: Ah, yeah, well you don't want to bang into
710
00:29:22.040 --> 00:29:22.520
anything.
711
00:29:23.080 --> 00:29:25.640
Andrew Dunkley: Yeah. Anyway, I hope all is well with
712
00:29:25.800 --> 00:29:27.910
the uh, individual involved. I'm uh,
713
00:29:28.520 --> 00:29:30.840
I'm not sure we'll ever find out what exactly
714
00:29:31.400 --> 00:29:33.480
the issue is. That's, that's subject to
715
00:29:33.480 --> 00:29:35.800
privacy from what I understand. But the fact
716
00:29:35.800 --> 00:29:38.800
that they've been able to go
717
00:29:38.800 --> 00:29:40.920
up there, get them, bring them back and deal
718
00:29:40.920 --> 00:29:43.760
with the problem is extraordinary
719
00:29:43.760 --> 00:29:46.480
because go back to the 70s when
720
00:29:46.480 --> 00:29:49.400
Skylab was in orbit. If someone got sick
721
00:29:49.400 --> 00:29:52.080
or injured in that situation,
722
00:29:52.800 --> 00:29:55.160
I don't know if we would have been able to do
723
00:29:55.160 --> 00:29:56.000
much in a hurry.
724
00:29:58.450 --> 00:30:00.640
Professor Fred Watson: Um, yeah, maybe not. I mean, there would have
725
00:30:00.640 --> 00:30:03.440
been contingency plans in place.
726
00:30:04.560 --> 00:30:07.470
It's, um. I think
727
00:30:07.710 --> 00:30:09.150
some of the things that might have brought
728
00:30:09.150 --> 00:30:11.470
somebody home from Skylab might be things
729
00:30:11.470 --> 00:30:12.710
that could have been fixed on the
730
00:30:12.710 --> 00:30:14.590
International Space Station because there is
731
00:30:14.590 --> 00:30:17.310
quite a, you know, a fair, Fair amount of
732
00:30:17.310 --> 00:30:19.670
medical expertise up there and some of the
733
00:30:19.670 --> 00:30:21.069
kit. But you don't want people taking
734
00:30:21.069 --> 00:30:23.190
appendices out and things like that in space.
735
00:30:23.190 --> 00:30:25.590
Andrew Dunkley: No, not really. You just have to wipe down
736
00:30:25.590 --> 00:30:27.710
the walls afterwards, and that's not fun.
737
00:30:28.510 --> 00:30:31.390
Although I should, um, counter it by saying
738
00:30:31.470 --> 00:30:33.910
we did recently have a situation where. Where
739
00:30:34.070 --> 00:30:36.190
a crew got stuck on the International Space
740
00:30:36.190 --> 00:30:39.030
Station for very unusual reasons due to,
741
00:30:39.190 --> 00:30:41.390
uh, incompatible spacesuits because of a
742
00:30:41.390 --> 00:30:43.830
failure in the Boeing Starliner.
743
00:30:44.230 --> 00:30:47.230
So, you know, that wasn't a quick
744
00:30:47.230 --> 00:30:49.150
rescue, that one, but it didn't involve
745
00:30:49.150 --> 00:30:51.630
illness or injury, so it wasn't as urgent.
746
00:30:51.630 --> 00:30:54.510
But, uh, sometimes it. It can be a
747
00:30:54.510 --> 00:30:57.310
slow process, but, um. Uh, yeah, but
748
00:30:57.310 --> 00:30:59.470
NASA's been very quick to point out that this
749
00:30:59.470 --> 00:31:01.590
has got nothing to do with an operational
750
00:31:01.670 --> 00:31:03.990
issue. It's, um. It's a personal issue.
751
00:31:03.990 --> 00:31:06.530
Nothing to do with an injury or accident on
752
00:31:06.530 --> 00:31:08.690
board. They want to make that pretty clear.
753
00:31:09.690 --> 00:31:11.810
Um, so, uh, yeah, we wish them well. They're
754
00:31:11.810 --> 00:31:13.530
on their way back as we speak. And by the
755
00:31:13.530 --> 00:31:16.450
time you hear this podcast, they will have
756
00:31:16.450 --> 00:31:17.650
returned, no doubt.
757
00:31:18.630 --> 00:31:21.330
Um, that's it, Fred. Gosh, we got through
758
00:31:21.330 --> 00:31:22.850
that in a mighty hurry, didn't we?
759
00:31:23.610 --> 00:31:26.530
Professor Fred Watson: Um, yes, I think
760
00:31:26.530 --> 00:31:29.170
we. We gave it due, due
761
00:31:29.170 --> 00:31:32.170
recognition. We've been talking for well over
762
00:31:32.170 --> 00:31:33.170
an hour, Andrew.
763
00:31:35.090 --> 00:31:35.730
Andrew Dunkley: Oh, have we?
764
00:31:37.810 --> 00:31:40.570
Doesn't feel like it, but no. Um.
765
00:31:42.290 --> 00:31:45.010
Professor Fred Watson: 38 minutes. I'm sorry. I'm misreading my
766
00:31:45.170 --> 00:31:46.130
clock. You're right.
767
00:31:46.130 --> 00:31:46.930
Andrew Dunkley: That's okay.
768
00:31:47.010 --> 00:31:48.530
Professor Fred Watson: Well, we got through that in a hurry.
769
00:31:49.010 --> 00:31:51.130
Andrew Dunkley: You're probably reading a Mars clock because
770
00:31:51.130 --> 00:31:53.890
we talked about it. It's going a bit
771
00:31:53.890 --> 00:31:56.810
faster. Um, now
772
00:31:56.810 --> 00:31:59.090
if you were to follow, uh, up those stories,
773
00:31:59.250 --> 00:32:00.850
I've told you where to go and look for them.
774
00:32:00.850 --> 00:32:03.770
But you, uh, can also read the show notes on
775
00:32:03.770 --> 00:32:06.430
our website, spacenutspodcast.more space
776
00:32:06.430 --> 00:32:09.230
nuts IO and while you're
777
00:32:09.230 --> 00:32:12.070
there, uh, you might like to, um, check out
778
00:32:12.070 --> 00:32:14.750
all the. All the tabs and,
779
00:32:15.050 --> 00:32:17.250
uh, links on our. On our website, the, uh,
780
00:32:17.350 --> 00:32:19.630
Astronomy Daily feed. You can subscribe for
781
00:32:19.630 --> 00:32:21.510
your daily dose of astronomy and space
782
00:32:21.510 --> 00:32:24.270
Science news. Uh, don't forget reviews.
783
00:32:24.270 --> 00:32:26.630
We really do appreciate your reviews. The
784
00:32:26.630 --> 00:32:29.630
more reviews, the more we get noticed. And
785
00:32:29.630 --> 00:32:31.150
the more we get noticed, the more people
786
00:32:31.150 --> 00:32:33.830
listen. And then, you know, we can buy
787
00:32:33.830 --> 00:32:35.550
ourselves an ice cream at the end of the day.
788
00:32:35.970 --> 00:32:38.730
Um, you can also send questions
789
00:32:38.730 --> 00:32:41.690
or comments in through the AMA link and
790
00:32:41.770 --> 00:32:43.610
so on and so forth. And don't forget to visit
791
00:32:43.610 --> 00:32:45.890
the Space Nuts shop. Uh, that's one thing
792
00:32:45.890 --> 00:32:48.810
that Huw, um, did some years ago
793
00:32:48.810 --> 00:32:51.110
and it's been very popular. All the, uh,
794
00:32:51.110 --> 00:32:53.370
Space Nuts memorabilia, if you, if you want
795
00:32:53.370 --> 00:32:54.930
to get hold of it. I've got, I've got my
796
00:32:54.930 --> 00:32:56.450
Space Nuts cup here somewhere.
797
00:32:56.450 --> 00:32:58.250
Professor Fred Watson: Here it is. Look. Look at this.
798
00:32:59.210 --> 00:32:59.850
Andrew Dunkley: There it is.
799
00:32:59.850 --> 00:33:01.530
Professor Fred Watson: I never got, I never got one of those.
800
00:33:02.650 --> 00:33:03.650
Andrew Dunkley: I, I'd buy.
801
00:33:03.650 --> 00:33:06.810
It's
802
00:33:06.810 --> 00:33:07.610
good. That's good.
803
00:33:07.850 --> 00:33:08.970
Professor Fred Watson: I'm too stingy.
804
00:33:09.830 --> 00:33:12.710
Andrew Dunkley: Got shirts. We've got hoodies, we've got, uh,
805
00:33:12.710 --> 00:33:15.230
all sorts of bits and bobs at the Space Nuts
806
00:33:15.230 --> 00:33:17.890
Shop, uh, at our website. Thank, uh,
807
00:33:18.150 --> 00:33:19.430
you, Fred. We'll leave it there. We'll catch
808
00:33:19.430 --> 00:33:20.550
you on the next episode.
809
00:33:21.030 --> 00:33:22.950
Professor Fred Watson: Look forward to it, Andrew. See you soon.
810
00:33:23.430 --> 00:33:25.669
Andrew Dunkley: Professor Fred Watson, astronomer at large.
811
00:33:25.669 --> 00:33:28.030
And thanks to Huw in the studio, who couldn't
812
00:33:28.030 --> 00:33:30.830
be with us today, had to be evacuated
813
00:33:30.830 --> 00:33:33.030
after attempting, uh, a Michael Jackson
814
00:33:33.030 --> 00:33:35.310
moonwalk. Not good at his age.
815
00:33:35.310 --> 00:33:35.670
Professor Fred Watson: No.
816
00:33:35.910 --> 00:33:37.630
Andrew Dunkley: And from me, Andrew Dunkley, thanks for your
817
00:33:37.630 --> 00:33:39.670
company. We'll catch you on the next episode
818
00:33:39.960 --> 00:33:41.160
of Space Nuts.
819
00:33:41.240 --> 00:33:41.600
Professor Fred Watson: Bye.
820
00:33:41.600 --> 00:33:44.520
Voice Over Guy: Bye. You've been listening to the
821
00:33:44.520 --> 00:33:45.880
Space Nuts podcast,
822
00:33:47.400 --> 00:33:50.280
available at Apple Podcasts, Spotify,
823
00:33:50.440 --> 00:33:53.200
iHeartRadio or your favorite podcast
824
00:33:53.200 --> 00:33:54.920
player. You can also stream on
825
00:33:54.920 --> 00:33:57.880
demand at bitesz.com. This has been another
826
00:33:57.880 --> 00:33:59.960
quality podcast production from
827
00:33:59.960 --> 00:34:01.040
bitesz.com