Sept. 4, 2025
Exocomets, Martian Revelations & Habitable Zones Beyond
Sponsor Details: This episode of Space Nuts is brought to you with the support of Insta360. Capture your adventures with their latest game-changer, the GOUltra. For a special Space Nuts offer, visit...
Sponsor Details:
This episode of Space Nuts is brought to you with the support of Insta360. Capture your adventures with their latest game-changer, the GOUltra. For a special Space Nuts offer, visit store.insta360.com and use the promo code SPACENUTS at checkout. Help support Space Nuts and get a great deal. Win/win!
Cosmic Discoveries: Exo-Asteroids, Martian Secrets, and Galactic Habitable Zones
In this thrilling episode of Space Nuts, hosts Andrew Dunkley and Professor Fred Watson delve into the intriguing world of exo-asteroids, the secrets of Mars unveiled by the InSight mission, and the concept of a galactic habitable zone. With a blend of personal anecdotes and scientific exploration, this episode promises to captivate and inform.
Episode Highlights:
- Exo-Asteroid 3I Atlas: Andrew and Fred Watson discuss the recently discovered interstellar object 3I Atlas, its unusual characteristics, and the insights provided by the James Webb Space Telescope. The pair explores the peculiar ratios of gases found within the comet, raising questions about its origins and the environment of its host star system.
- Insights from Mars: The InSight mission continues to reveal fascinating details about Mars's history. Fred Watson explains how seismic data is shedding light on the planet's deep, complex interior, hinting at a tumultuous past marked by impacts and geological activity.
- The Galactic Habitable Zone: The discussion shifts to the concept of a galactic habitable zone, where conditions may be more favourable for life. Andrew and Fred Watson examine the implications of stellar migration and the significance of searching for habitable planets in specific regions of our galaxy.
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, Tumblr, Instagram, and TikTok. We love engaging with our community, so be sure to drop us a message or comment on your favourite 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.
Got a question for our Q&A episode? https://spacenutspodcast.com/ama
Become a supporter of this podcast: https://www.spreaker.com/podcast/space-nuts-astronomy-insights-cosmic-discoveries--2631155/support.
This episode of Space Nuts is brought to you with the support of Insta360. Capture your adventures with their latest game-changer, the GOUltra. For a special Space Nuts offer, visit store.insta360.com and use the promo code SPACENUTS at checkout. Help support Space Nuts and get a great deal. Win/win!
Cosmic Discoveries: Exo-Asteroids, Martian Secrets, and Galactic Habitable Zones
In this thrilling episode of Space Nuts, hosts Andrew Dunkley and Professor Fred Watson delve into the intriguing world of exo-asteroids, the secrets of Mars unveiled by the InSight mission, and the concept of a galactic habitable zone. With a blend of personal anecdotes and scientific exploration, this episode promises to captivate and inform.
Episode Highlights:
- Exo-Asteroid 3I Atlas: Andrew and Fred Watson discuss the recently discovered interstellar object 3I Atlas, its unusual characteristics, and the insights provided by the James Webb Space Telescope. The pair explores the peculiar ratios of gases found within the comet, raising questions about its origins and the environment of its host star system.
- Insights from Mars: The InSight mission continues to reveal fascinating details about Mars's history. Fred Watson explains how seismic data is shedding light on the planet's deep, complex interior, hinting at a tumultuous past marked by impacts and geological activity.
- The Galactic Habitable Zone: The discussion shifts to the concept of a galactic habitable zone, where conditions may be more favourable for life. Andrew and Fred Watson examine the implications of stellar migration and the significance of searching for habitable planets in specific regions of our galaxy.
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, Tumblr, Instagram, and TikTok. We love engaging with our community, so be sure to drop us a message or comment on your favourite 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.
Got a question for our Q&A episode? https://spacenutspodcast.com/ama
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. Look who's back.
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Yes, it's me. Back from,
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uh, everywhere we went. Everywhere. Anyway, I won't bore you with all
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of that. Andrew Dunkley here. Great to have your company
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on another episode of Space
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Nuts. And coming up on today's show,
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we will be diving into the
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weird world of exo. Asteroids
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or exocomets or whatever they are.
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30, uh, one atlas to be exact. And
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it turns out it's a bit of a strange one. Uh, also
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in Insight, uh, the Insight mission is
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unravelling Mars's secrets, uh,
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particularly its deep, dark past. And believe me,
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it's a little bit ugly. And
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a galactic habitable zone.
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Is there such a thing? What does it mean? And what are we going to
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find there? We'll find out on this episode of space
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nuts. 15 seconds. Guidance is
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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.
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Space nuts. Astronauts report it feels good.
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Andrew Dunkley: And joining us to do all the unravelling
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is Professor Fred Watson Watson, astronomer at large. Hello,
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Fred Watson.
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Professor Fred Watson: Welcome back, Andrew. It's, um, a, uh, treat
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to see your smiling face.
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Andrew Dunkley: It's a treat. It's a treat to be back and doing
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this after it's been three months. I can't believe
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that, uh, it's been. Judy and I were only saying today
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we cannot get our heads around the fact that we're away for three
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months because it doesn't feel like it. It's just,
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you know, it went so fast. But, gee, we
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had a good time, Fred Watson. We had an amazing time.
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Um, unfortunately, did not get to see the
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northern lights. And that was
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one of my. But I might get another opportunity.
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You know, it's not the last time we'll go away somewhere, so
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fingers crossed. But, um, even as far north as,
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uh, North Cape, the northern tip of Europe, right up
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inside the Arctic Circle, did not see a thing.
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Uh, probably because it was nearly daylight every
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minute of the day and night. So that doesn't
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help. Um, but,
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yeah, a terrific holiday. I don't. I wouldn't know where
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to start to tell you about it. I know I posted a lot of pictures
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that people saw, uh, every time we went away
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or went somewhere, um, but just
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saw some amazing things, met some amazing people,
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had some amazing moments. Just, um, little
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things that we didn't expect. Like, uh, the captain
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of the ship suddenly deciding at the last minute to take
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us up, um, Prince Christian
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Sound in Norway, which is
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somewhere where not many people get to go. And the
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only way to get there is by ship. And it is
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Full of icebergs and wildlife
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and just, um,
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glacier after glacier after glacier right
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there in front of you. Um, it's
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indescribable. Uh, it's just the most amazing
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scenery. Uh, we sat up on the deck
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for seven and a half hours straight just taking it
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all in. We did not move. It was that
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captivating. Um, that
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was one of the highlights. Um, Namibia was
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amazing. Loved Namibia. Uh,
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we, um, loved Scotland. Loved
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Edinburgh, Fred Watson. What a terrific place. Um,
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we had porridge for breakfast and.
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Professor Fred Watson: You have haggis for lunch, didn't you?
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Andrew Dunkley: And had haggis for lunch, which, surprise was
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surprisingly nice. I, you know, you hear horror
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stories, but it was actually quite tasty.
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Really enjoyed it. And, um, look,
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the countries we visited were, were many.
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Uh, the highlights were numerous. I wouldn't,
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I could talk for hours, which probably wouldn't work
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well on a space podcast. So I
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won't, um, I won't say too much more about that.
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Although at Tenerife we did see the
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observatory up, um, above the snow
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line there. Above the, um, uh,
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tree line, actually, not the snow line. Um,
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you drive up the hill, you've probably done this bread,
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and all of a sudden there's no vegetation, it's just gone.
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And, um, there's an observatory up there which is
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primarily a solar observatory, so.
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Professor Fred Watson: That's right, yeah. Got to have. So Tad is the
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name of the mountain, Katie.
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Andrew Dunkley: That's right.
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Professor Fred Watson: Yep, yep, yep.
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Andrew Dunkley: Yes.
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But, uh, here we are back again.
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Professor Fred Watson: Um, yeah, I do have a question for you about.
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Andrew Dunkley: Oh, ah, yeah.
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Professor Fred Watson: Andrew, did you. Did you run into any space
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nuts? I did,
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I actually did.
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Andrew Dunkley: Um, one in particular who I ran into
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in a toilet on a ship. On our
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cruise ship. I was walking out
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and this, he said, um, are you Andrew Dunkley? And I went,
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yes, he said, he said, I'm a Space Nuts
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listener, he said. And I remember he did message.
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Message me to say he'd be on the cruise and getting on in Dover and
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I'd forgotten about that. And, uh, yeah, we ran into each
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other in passing. So, um.
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And as always, I've forgotten his name and
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I apologise for that. But it was nice to catch up. So, yes,
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we did. No, it ran into a few. A few people I did
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pass, uh, or speak to on the ship knew me,
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but I don't know if they knew me from radio
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or from the podcast. We never really clarified that.
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But yeah, it was, uh, it was quite
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extraordinary. Um, but if you jump
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on Facebook, all my photos are on my Facebook page and Instagram
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So you should be able to see most of what we did.
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So I don't take up the rest of the show talking
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about it, although I'll probably, probably have
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times where I'll make references to things
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we saw and didn't. Yeah.
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Now, um, we've got a lot to talk about, but one
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of the things you do want to discuss and I think you did that with
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Heidi. Oh, and I'd like to say just
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my, um, sincere
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thanks to Heidi for stepping up and covering the last
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few months. It was a, it was a big job and she did,
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did fantastically. The feedback I've been getting,
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uh, even while I was away was, uh, was glowing.
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So well done, Heid Heidi and thank you, Much
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appreciated. Uh, and you
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talked to her last week and you want to mention again, the Australian Dark
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sky alliance is looking for some support.
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Professor Fred Watson: That's right. So if you're not
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either resident in or a citizen of Australia,
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you can zone out for a minute while I talk about
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a petition which the Australasian Dark sky
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alliance, uh, is trying to get
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put up to the, the federal government, the government
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of Australia, in order to put
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legislation in place to limit light pollution,
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to actually restrict it as an environmental
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issue, not just for astronomers, but for wildlife, for human
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health, all of the above. So if you do fall into one
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of those categories, uh, the place to go is their
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website, which is all one word,
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australasiandarkskyalliance.org
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uh, and so
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australasiandarkskyalliantiance.org will take you to
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their website, which on the front page has instructions on
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how to sign the petition. And you've got till September
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19th. And thank you for that plug and.
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Andrew Dunkley: Uh, my great pleasure. Uh, and hopefully the
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politicians will listen. Hopefully you get the numbers.
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That's the most important thing.
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And it's a really important thing. I mean, uh,
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we've talked about light pollution many,
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many times over the years. And it's just one of
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those growing problems, uh, which
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doesn't seem to get a lot of attention because no one really thinks about
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it as a problem. I suppose that's the problem.
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Professor Fred Watson: It is, uh, uh, on the other hand, it is one of the easiest to
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fix because flick of switch actually does it.
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Um, but you're right, I mean there's
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certainly regulations in regard to noise pollution,
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uh, and of course every other kind of pollution. We're
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seeing regulation coming in on plastics pollution.
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But light pollution is the orphan pollution at the
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moment. And it's an important one. It's one that's more important
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than Most people realise, and one statistic, uh, you might not
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be aware of this Andrew, but light pollution is increasing
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globally at 10% per
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year. So that comes from cities and science.
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Yeah, we know uh, that the stars are disappearing at that
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rate, 10% a year, it's very
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ugly indeed.
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Andrew Dunkley: That is, that's not good at all. And having
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witnessed now 24 hour day sunlight, I
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do understand how it could mess you with your brain.
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So it's not good for human healthy.
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Uh, so that's
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australasiandarkskyaalliance.org
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uh, 10,000 signatures by the 19th
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of September if you will.
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Uh, right, our first topic, Fred Watson, takes us
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uh, into the realm of uh, interstellar
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objects. 31 Atlas. Um, now I
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did see this one pop up in the news while I was away.
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I did try to keep in touch but um, when you're moving into
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different time zones of different parts of the world, your
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news suddenly changes, which is a little
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bit weird. Uh, but 31 Atlas,
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um, this one was only a recent discovery and it's
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hammering way through our ah, system as we speak.
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Uh, but they've been uh, able to analyse it thanks to the
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James Horace Webb Space Telescope. And this one's
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a little bit unusual.
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Professor Fred Watson: Uh, that's right. And um, because all the
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text you've read is in uh,
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Arial, uh, font, you wouldn't
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have no way of knowing that it's actually 3I
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Atlas. Holy
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circumstances. 3I
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being the third interstellar, the third interstellar,
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uh, object to pass through the solar system and uh, Atlas, of course, and
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then the facility that discovered it.
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Andrew Dunkley: I'm using jet lag as an excuse.
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Professor Fred Watson: It doesn't matter. Even if you weren't jet lag, you wouldn't have
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known because now.
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Andrew Dunkley: 31.
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Professor Fred Watson: Yeah, but it's 3i. Never mind.
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You see that's the advantage of uh, times,
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Times New Roman. That would, that would solve the problem.
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Um, anyway, this is being
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observed uh, as it flies by the solar system.
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It's closest to the sun if I remember rightly, on
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the 29th of October. So unlike
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uh, uh, unlike Oumuamua, which was one
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eye, the first um, interstellar object,
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uh, we didn't catch up with that until
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it was on its way out of the solar system Atlas,
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uh, uh, we found on the way in.
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Uh, and one reason for that is
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that it's a much bigger object. Um, I think um,
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the best estimate we got for the size of
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Oumuamua was something like 40,
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maybe 100 metres long, something of that sort. I can't remember the
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exact number but this thing is thought to be about 20
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kilometres across um and
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it's despite um the
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prognostications of Avilob who wanted uh
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it to be an interstellar spacecraft.
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It's behaving exactly like a comet in that
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it's uh, as it approaches the sun the
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material that it's made of which is a mixture of
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ice and dust uh that heats
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up the ice turns into a vapour, the dust gets
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released and it generates what we call a coma um
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coma is just a word meaning hair and it's uh,
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a sort of fuzzy bit of the uh, of the comet
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and um, develops a tail and indeed three eye
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Atlas has done that. Um it's uh,
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what's of interest uh of course is
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that there are mixed in with the dust
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there are atoms and in fact molecules of the, of
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the material that binds it together, the ices
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that bind it together. And it's not just water ice. We know that
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comets are made mostly of water ice. Water as we've
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said many times on space knots is the most
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common two element uh molecule in the
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universe. Uh so it's natural that we should find
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water in comets. But there's also
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basically uh carbon dioxide, CO2, carbon
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monoxide CO uh and those
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uh gases are revealing their presence by
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their spectra. Uh the rainbow spectra that
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you can analyse the light that's coming from them
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and indeed uh, exactly as you've said the
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James Webb Space Telescope is being
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uh used by a number of authors mostly
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in the United States. Uh Goddard Space Flight Centre
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and the Catholic University of America are two of the organisations
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represented. So you've got
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carbon monoxide, carbon dioxide, you've got something called
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carbonyl sulphide. Uh all
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of these are ah, not unexpected
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because that's what we find in comets that belong to the
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solar system. But here's the
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rub, um and it's the ratio
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of these molecules to each other
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that is uh the peculiarity of
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three I atlas uh and in particular
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the ratio of carbon uh
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dioxide to water is actually
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eight to one. So eight parts of
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carbon dioxide to one part of water
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and that's higher than any other comet that's ever been
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seen and way, way above the normal value
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um, which is I think two or three to one,
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something like that. I can't remember the exact number. Um
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however carbon monoxide
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has uh a ratio with water that's more
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or less the same as ah, um solar
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system comets. It's 1.4.
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So there's a puzzle uh why is the carbon dioxide,
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so much more abundant. Uh, and of course,
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as always, when faced with a puzzle,
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um, astronomers start trying to work out
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what's going on, uh, and
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they basically think
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that they have sort of solved
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it. Um,
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um, it's. One possibility
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is if you imagine the host
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star system in which this object was created
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and it would have formed like the, uh, solar
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system's comets, probably in an Oort cloud like
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the one we have around our solar system, which is made
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of, uh, cometary bodies, uh, which eventually
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fall in towards the inner solar system. And that's when we see
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them. Uh, there's a suggestion that if you've
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got very high levels of ultraviolet
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radiation, uh, from that
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host star, and that would be the case if it was a
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young and very massive star, um, that
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apparently could change this ratio of water
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to carbon dioxide. Um, and another
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comment that's been suggested is that
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maybe, um, it's uh, a part
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of that, um, of the solar system in which
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it was born. That's a long way from
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the host star, uh, and above the host
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star's carbon dioxide ice line.
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So beyond a certain distance you get more
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carbon dioxide in
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relation to water. Uh, and,
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you know, that's another possibility. There's
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several more that are being thought of. But, uh, the
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bottom line is, nearly as always with stories like this,
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Andrew, what we need is more observations.
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Uh, and uh, you know, we don't have very
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long before it will get too faint to
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observe. It'll be probably next year when it starts, um,
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really disappearing out of the solar system. But,
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uh, so we've got this golden opportunity to
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analyse it and, and investigate it. And that's exactly what's
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happening.
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Andrew Dunkley: How, how visible is this one going to be as
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it reaches the inner sanctum of
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our solar system?
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Professor Fred Watson: Yeah, not, not that visible
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because, um, in fact, I don't have a figure for its magnitude,
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the gobbledygook number that astronomers use for brightness.
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Uh, but it's. It's certainly, um, very much the
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province of big telescopes. The thing is, uh, its
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nearest approach to Earth, uh, um,
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I can't remember. It's more than one astronomical
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unit, I think, which is the distance between the Earth to the sun. I
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can't remember the exact distance. Uh,
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it's not that close to the sun either. Uh, and I
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think I'm right in saying that
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when it's closest to the sun, we can't see it because
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it's in the same direction. It's sort of passing behind the Sun.
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Um, that was one of the comments that ah avilaeur
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made uh suggesting that maybe uh when it was
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at its brightest um its orbit had been chosen so that we
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couldn't see it it when it was at its brightest um and the
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other thing he pointed out was that it passes very close
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to or closeish to Venus, Mars and
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Jupiter. Um and um, you know the suggestion was
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that there might be intelligent design behind that.
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But uh, I think he's the only person in the
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astronomical community he thinks.
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Andrew Dunkley: That he might be
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right. Uh, you got to give him credit
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though.
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Professor Fred Watson: He's always um. Yeah we need ideas like
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that. Absolutely.
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Andrew Dunkley: Yeah. Yeah. Okay so uh,
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and is this one honking along like the others
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at a.
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Professor Fred Watson: Greater rate of knots, 60 something kilometres
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per second which is kind of one of the things that tells you that
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it doesn't belong to our solar system. It's going too fast.
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Andrew Dunkley: Right, There you are. Okay, uh you can read up
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on that one uh@universetoday.com
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uh3iatlas
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Got it. This is Space Nuts with Andrew
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Dunkley and Professor Fred Watson Watson.
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Space Nuts, our uh next story. Fred Watson
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takes us to a place I rarely
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mention. Uh it is the red planet Mars.
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Uh INSIGHT has uh been um
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sort of examining some of the secrets of Mars
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and come up with uh new information
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that kind of might surprise people about uh
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Mars's deep dark and ugly past.
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Um, there's been a few revelations.
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Professor Fred Watson: There have, yes. Um, I mean INSIGHT is the gift that
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keeps on giving really. Um because it switched off
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in 2022. Uh
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um it's ah a spacecraft that
385
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landed near Mars's equatorial region.
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Uh I think in about 2019 was when
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it uh touched down um and you might
388
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remember we discussed a lot the instruments that are on board
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it because one of them was a seismometer uh which has
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been incredibly successful and the other one was
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the interior thermometer which was incredibly
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unsuccessful because they were trying to drill
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a hole to put this thermometer down under the
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surface of uh Mars and I think can't remember what happened.
395
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The drill correct. Kept breaking or something um
396
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unsatisfying happened uh until that part of
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the experiment was not as successful but the seismograph
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has done its job and um
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the results from that keep um on being
400
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reanalysed uh because as time goes
401
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on we've got many more analytical facilities
402
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at our disposal which we didn't have before. Uh and
403
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um, you can now look at these seismic records with a
404
00:19:10.320 --> 00:19:13.000
lot more meaning and what's
405
00:19:13.000 --> 00:19:15.780
been discovered. It's actually um, from an
406
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analysis of eight seismic Events,
407
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uh, uh, two of which were
408
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probably caused by meteorite
409
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impact on Mars. Remember um, that the
410
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two mechanisms, because Mars doesn't have plate tectonics,
411
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it's called a single uh, crust.
412
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Um, it's uh, stretching and
413
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shrinking of the crust and sort of
414
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rift valleys forming and things like that that give you the seismic
415
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events or meteorite impacts. And two of
416
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those seismic events as I said, were
417
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meteorite impacts. But um,
418
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it's the way that the uh,
419
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relative frequencies of the vibrations, the
420
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uh, seismic vibrations, the relative frequencies of these,
421
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uh, that allows people to
422
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basically examine the interior of Mars,
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uh, in a very intelligent
424
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way. Um, so you look for higher
425
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frequency waves compared with uh, low
426
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frequency waves. And basically uh,
427
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that tells you uh, about the length
428
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of transmission time uh for these different
429
00:20:22.640 --> 00:20:25.359
waves, how long it takes you to get from the site of impact,
430
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wherever that is, uh to the seismograph.
431
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And uh, one of the authors uh, of this
432
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work. I um, think there's ah, certainly authors at
433
00:20:33.760 --> 00:20:36.530
Imperial College London and uh,
434
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other institutions, uh, but one of the authors m
435
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made a comment, um, which I liked.
436
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These signals show clear signs of interference
437
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as they travel through Mars's deep interior.
438
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That's consistent with a mantle full
439
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of structures of different compositional origins,
440
00:20:53.800 --> 00:20:56.360
leftovers from Mars's early days.
441
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And what that means is so the mantle is the region
442
00:20:59.720 --> 00:21:02.720
between the crust of uh, Mars and its
443
00:21:02.720 --> 00:21:05.680
core, its hot core. Uh, we've got a
444
00:21:05.680 --> 00:21:08.580
mantle on Earth. I think Mars's mantle is rather
445
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uh, deeper than ours relative to the diameter of the
446
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planet. Um but what they found is that
447
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the mantle isn't a sort of uniform, um,
448
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uh, paste of semi
449
00:21:21.180 --> 00:21:23.700
solid rock, uh but it has
450
00:21:23.780 --> 00:21:26.660
structure in it. Uh, and that structure
451
00:21:26.980 --> 00:21:29.370
is thought to come from uh,
452
00:21:29.780 --> 00:21:32.420
events that took place during Mars
453
00:21:32.580 --> 00:21:34.960
origins. Uh and in fact what they're
454
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suggesting is that um,
455
00:21:39.160 --> 00:21:42.040
when Mars was being formed about
456
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4.5 billion years ago, um,
457
00:21:44.840 --> 00:21:47.680
it was at a time as we've talked about it
458
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before. Not long after that there was the um,
459
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what's it called, The Late Heavy Bombardment, uh
460
00:21:53.510 --> 00:21:56.480
when there was a lot of stuff careering around the solar
461
00:21:56.480 --> 00:21:59.440
system. Big objects the size of uh, many
462
00:21:59.440 --> 00:22:01.910
planets really banging into everything else.
463
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And the suggestion is
464
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that at that period some of
465
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these planetoids or planetesimals, uh
466
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actually collided with Mars and
467
00:22:13.830 --> 00:22:16.390
basically melted parts of Mars,
468
00:22:16.910 --> 00:22:19.350
uh into oceans of
469
00:22:19.590 --> 00:22:22.230
molten magma. Uh, and
470
00:22:22.710 --> 00:22:25.390
then you find that these
471
00:22:25.390 --> 00:22:27.580
regions cool, but
472
00:22:28.140 --> 00:22:31.060
when they're cooled they have
473
00:22:31.060 --> 00:22:33.500
a different structure from the stuff that didn't get
474
00:22:33.500 --> 00:22:36.460
clouted and melted, uh, by an impact
475
00:22:36.860 --> 00:22:39.860
so what you're doing is you're differentiating between
476
00:22:39.860 --> 00:22:42.540
different zones of Mars's mantle and
477
00:22:42.620 --> 00:22:45.540
what they're saying is that what they're detecting
478
00:22:45.540 --> 00:22:48.140
with this uh, inhomogeneity in
479
00:22:48.140 --> 00:22:50.980
Mars's mantle is evidence of these, what
480
00:22:50.980 --> 00:22:53.950
they describe as compositionally distinct chunks of
481
00:22:53.950 --> 00:22:56.510
material. Uh so um, you know
482
00:22:56.510 --> 00:22:59.510
Mars as mantle has got some
483
00:22:59.510 --> 00:23:02.350
bits that were never reheated and others
484
00:23:02.350 --> 00:23:05.350
that were reheated after the planet's formation by these
485
00:23:05.350 --> 00:23:08.110
collisions probably molten, uh then
486
00:23:08.110 --> 00:23:11.070
they hardened and they crystallised and that gives
487
00:23:11.070 --> 00:23:13.630
you a different structure which is what's now been seen.
488
00:23:13.870 --> 00:23:16.800
So um, it's ah, you know one of the comments, uh,
489
00:23:17.150 --> 00:23:20.110
the same author, uh, uh, who I
490
00:23:20.110 --> 00:23:22.800
just um, I just uh, mentioned most of this
491
00:23:22.800 --> 00:23:25.360
chaos likely unfolded in Mars first
492
00:23:25.360 --> 00:23:28.160
100 million years. The fact that we can still
493
00:23:28.160 --> 00:23:31.040
detect its traces after 4.5 billion years
494
00:23:31.360 --> 00:23:34.160
shows just how sluggishly Mars's interior
495
00:23:34.400 --> 00:23:37.360
has been churning ever since. Uh unlike the
496
00:23:37.360 --> 00:23:40.120
Earth's which is much more active. So yeah,
497
00:23:40.120 --> 00:23:43.040
um, the Mars story from Insight
498
00:23:43.200 --> 00:23:46.200
keeps on amazing us. We keep uh, discovering
499
00:23:46.200 --> 00:23:49.000
new facts about it and um. Long may it continue
500
00:23:49.080 --> 00:23:49.640
Andrew.
501
00:23:50.120 --> 00:23:52.300
Andrew Dunkley: Yes, yes, hopefully. Um,
502
00:23:52.760 --> 00:23:55.640
and there's so much more to learn. This is what I
503
00:23:55.720 --> 00:23:58.600
love about uh, these inner planets
504
00:23:59.100 --> 00:24:02.000
uh, and the outer planets as well. The more we look at them
505
00:24:02.000 --> 00:24:04.760
and the more we analyse the data that we're receiving
506
00:24:04.760 --> 00:24:07.760
from various missions, the more interesting they
507
00:24:07.760 --> 00:24:10.720
get and the stranger they get sometimes as is
508
00:24:10.720 --> 00:24:13.560
the case with Mars in this particular situation.
509
00:24:13.640 --> 00:24:16.520
So uh, yeah it's a fascinating place. Uh,
510
00:24:16.520 --> 00:24:19.400
cosmosmagazine.com is where you need to go
511
00:24:19.400 --> 00:24:22.260
to uh, find out more about that if you'd like to follow up on
512
00:24:22.260 --> 00:24:25.220
that story. Andrew Dunkley here, Fred Watson Watson there.
513
00:24:25.220 --> 00:24:27.140
You're listening to Space Nuts.
514
00:24:31.540 --> 00:24:32.580
Professor Fred Watson: Space Nuts.
515
00:24:32.740 --> 00:24:35.580
Andrew Dunkley: And uh, our final story today is about
516
00:24:35.580 --> 00:24:38.500
a galactic habitable zone. Now we
517
00:24:38.500 --> 00:24:41.260
know about the habitable zone in our own solar
518
00:24:41.260 --> 00:24:43.780
system, uh, which is affectionately called the
519
00:24:43.860 --> 00:24:46.860
Goldilocks Zone. And we know about that because
520
00:24:46.860 --> 00:24:49.670
we're in it. That's the only thing that keeps us alive
521
00:24:49.670 --> 00:24:52.590
really. Uh, but Fred Watson,
522
00:24:53.310 --> 00:24:56.310
my question first up is uh, are they talking about
523
00:24:56.310 --> 00:24:59.150
a Goldilocks Zone on a galactic
524
00:24:59.150 --> 00:25:00.590
scale? Is that what this is?
525
00:25:01.470 --> 00:25:04.390
Professor Fred Watson: Yeah, effectively. Um, but um, it's
526
00:25:04.390 --> 00:25:07.350
not the temperature that's not too
527
00:25:07.350 --> 00:25:10.230
hot and m not too cold but just right as it
528
00:25:10.230 --> 00:25:13.190
is in our Goldilocks Zone the temperature's just right
529
00:25:13.190 --> 00:25:16.190
at this distance from the sun for liquid water to
530
00:25:16.190 --> 00:25:18.990
exist. And we know it does because we see
531
00:25:18.990 --> 00:25:21.790
it pretty well every day uh, in our
532
00:25:21.860 --> 00:25:24.750
um, in Our reservoirs of water, whether
533
00:25:24.750 --> 00:25:27.720
they're a bathtub or a ah sea. Um,
534
00:25:27.720 --> 00:25:30.510
but that's not what the galactic habitable
535
00:25:30.510 --> 00:25:32.750
zone is about. And it is being called that the
536
00:25:32.750 --> 00:25:35.550
GHz or GHz if you're on
537
00:25:35.550 --> 00:25:38.230
the other side of the Pacific. Um,
538
00:25:38.590 --> 00:25:40.830
it's uh, it's a region where
539
00:25:41.750 --> 00:25:43.990
you might um, expect
540
00:25:44.870 --> 00:25:47.190
to find more habitable planets
541
00:25:47.830 --> 00:25:50.630
than nearer to the centre of our
542
00:25:50.630 --> 00:25:51.910
galaxy or
543
00:25:53.670 --> 00:25:56.310
further out towards the edge of the galaxy.
544
00:25:57.000 --> 00:25:58.790
Uh and it basically
545
00:26:00.390 --> 00:26:03.390
comes uh about uh. Because you can
546
00:26:03.390 --> 00:26:06.030
analyse, you know we know a lot about the way
547
00:26:06.030 --> 00:26:09.020
stars evolve. Uh and we know a
548
00:26:09.020 --> 00:26:11.820
lot about the um, chemicals
549
00:26:13.100 --> 00:26:15.660
um that have basically been found in
550
00:26:15.900 --> 00:26:18.780
stellar interiors and their atmospheres. And we
551
00:26:18.780 --> 00:26:21.500
can trace this history of stars very
552
00:26:21.500 --> 00:26:24.300
accurately. Um and we can
553
00:26:24.300 --> 00:26:27.100
also uh, look at the
554
00:26:27.100 --> 00:26:29.740
orbits of stars around the centre of our galaxy.
555
00:26:30.080 --> 00:26:33.020
Uh and we can work out to some extent where they've come from
556
00:26:33.020 --> 00:26:35.620
because uh, we think that the orbits of
557
00:26:35.620 --> 00:26:38.620
stars actually um, ah, they actually change
558
00:26:38.700 --> 00:26:40.700
in a process called stellar migration
559
00:26:41.660 --> 00:26:44.660
where stars, orbits change around the centre of the
560
00:26:44.660 --> 00:26:47.020
galaxy. Uh and you,
561
00:26:47.980 --> 00:26:50.940
you know, you can find that they uh, move.
562
00:26:51.500 --> 00:26:54.500
And so one of the studies, uh, one
563
00:26:54.500 --> 00:26:57.180
of the um, comments that's come from
564
00:26:57.180 --> 00:26:59.260
this particular study. It's actually an international
565
00:27:00.120 --> 00:27:03.020
uh team of scientists who have looked at this. Uh, this
566
00:27:03.020 --> 00:27:05.540
is published in strongly in Astrophysics, one of the main
567
00:27:05.930 --> 00:27:08.820
uh learned journals of astronomy. What they've
568
00:27:08.820 --> 00:27:11.380
discovered is that
569
00:27:11.850 --> 00:27:14.020
um, there's a five times
570
00:27:15.060 --> 00:27:18.020
greater likelihood of
571
00:27:18.340 --> 00:27:21.060
stars migrating from
572
00:27:22.100 --> 00:27:24.900
one part of a
573
00:27:24.900 --> 00:27:27.140
galaxy to another for
574
00:27:27.300 --> 00:27:30.300
habitable planets, for stars that have habitable
575
00:27:30.300 --> 00:27:33.230
planets compared to, with a lack
576
00:27:33.230 --> 00:27:35.910
of any stellar migration. So it's a
577
00:27:35.910 --> 00:27:38.670
slightly, this is a slightly obtuse thing to look
578
00:27:38.670 --> 00:27:41.590
for. Um, but um, what it
579
00:27:41.910 --> 00:27:44.790
says is, you know, it's all about
580
00:27:45.030 --> 00:27:48.029
for example whether you uh, are
581
00:27:48.029 --> 00:27:50.630
in a part of the galaxy where
582
00:27:50.630 --> 00:27:53.510
your solar system could uh, host
583
00:27:53.830 --> 00:27:56.470
gas giant planets because they would
584
00:27:57.110 --> 00:27:59.910
basically have an effect on the formation of
585
00:27:59.910 --> 00:28:02.590
the kind of rocky planets that we think are the
586
00:28:02.590 --> 00:28:05.410
habitable one. Um, so I
587
00:28:05.410 --> 00:28:08.090
might just read um, a ah, quote from
588
00:28:08.090 --> 00:28:10.970
this paper. Uh, it's a little bit
589
00:28:11.030 --> 00:28:14.010
uh, technical but um, I
590
00:28:14.010 --> 00:28:16.850
think it's an interesting quote. It sort of illuminates what we're talking
591
00:28:16.850 --> 00:28:19.330
about. Uh, in this study we have
592
00:28:19.330 --> 00:28:21.850
significantly expanded the exploration
593
00:28:22.170 --> 00:28:25.170
of the parameter space defining the galactic
594
00:28:25.170 --> 00:28:27.850
habitable zone compared to previous
595
00:28:27.850 --> 00:28:30.520
analyses present in literature. Uh, our
596
00:28:30.520 --> 00:28:33.200
findings are particularly relevant in the context of
597
00:28:33.200 --> 00:28:36.120
upcoming space missions such as the
598
00:28:36.120 --> 00:28:38.960
ESA PLATO mission, that's
599
00:28:38.960 --> 00:28:41.920
planetary transits and oscillations of stars, the uh,
600
00:28:42.040 --> 00:28:44.520
ESA Aerial Space Mission and large
601
00:28:44.520 --> 00:28:47.360
Interferometer for exoplanets. That's
602
00:28:47.360 --> 00:28:50.360
life. And these missions
603
00:28:50.360 --> 00:28:52.880
will deliver unprecedented, um, data on planetary
604
00:28:52.880 --> 00:28:55.440
properties, orbital architectures and
605
00:28:55.440 --> 00:28:58.130
atmospheric concepts, compositions. So what
606
00:28:58.130 --> 00:29:01.120
they're basically saying is, uh,
607
00:29:01.120 --> 00:29:04.090
if you're going to look for habitable planets, you want
608
00:29:04.090 --> 00:29:06.930
to be careful where you look. Because if there is
609
00:29:06.930 --> 00:29:09.890
such a thing as a stellar or a galactic habitable zone,
610
00:29:10.390 --> 00:29:13.370
um, then, uh, we want to be looking there
611
00:29:13.370 --> 00:29:16.090
if we're going to look for, uh, you know,
612
00:29:16.090 --> 00:29:19.050
for uh, habitable planets. It's an old
613
00:29:19.050 --> 00:29:21.610
idea, actually. The GHz, uh, or
614
00:29:21.610 --> 00:29:24.590
GHz, uh, comes, goes back to the 1980s.
615
00:29:25.030 --> 00:29:27.830
Um, and it's all about, you know, the um, the
616
00:29:27.830 --> 00:29:29.550
formation of the heavier elements.
617
00:29:30.670 --> 00:29:33.470
The ones that are basically work
618
00:29:33.550 --> 00:29:36.550
like iron, silicon, uh,
619
00:29:36.830 --> 00:29:39.830
oxygen, all of these elements. You've got to form
620
00:29:39.830 --> 00:29:42.430
them. You've got to form them in the right place in a galaxy.
621
00:29:42.910 --> 00:29:45.750
And uh, you've got to then, uh, let that
622
00:29:45.750 --> 00:29:48.430
environment breed these, uh, elements
623
00:29:48.430 --> 00:29:51.410
into molecules which basically
624
00:29:51.410 --> 00:29:54.210
become the, um, uh, precursors of life.
625
00:29:55.730 --> 00:29:57.970
I'm sorry, that's the Gobbler book. Uh,
626
00:29:57.970 --> 00:29:58.850
explanation.
627
00:29:59.570 --> 00:30:02.490
Andrew Dunkley: No, fair enough. Um, so
628
00:30:02.490 --> 00:30:04.770
does that mean that in our ongoing search for
629
00:30:04.770 --> 00:30:07.170
exoplanets, we should be focusing on
630
00:30:07.410 --> 00:30:10.290
the GHz areas?
631
00:30:11.330 --> 00:30:13.610
Uh, or do we not really care where the
632
00:30:13.610 --> 00:30:16.370
exoplanets are? Finding them is imperative regardless.
633
00:30:17.120 --> 00:30:20.080
Professor Fred Watson: Yeah, no, no, that's. That's exactly right.
634
00:30:20.080 --> 00:30:23.000
That's exactly what these authors are saying. We should be looking in the
635
00:30:23.000 --> 00:30:25.720
right place if we want to find, uh, habitable
636
00:30:25.720 --> 00:30:28.240
planets. Uh, and, um, uh,
637
00:30:28.720 --> 00:30:31.560
and indeed, um, you know, the, the PLATO mission, for
638
00:30:31.560 --> 00:30:34.080
example, is going to look at a million stars. It's a bit like
639
00:30:34.080 --> 00:30:36.880
Kepler. The Kepler mission, it was. It's finding
640
00:30:37.280 --> 00:30:40.200
planets by transits. Uh, so that's going
641
00:30:40.200 --> 00:30:42.940
to scan a million stars and, and
642
00:30:43.180 --> 00:30:45.660
you want to make sure you're looking at them in the right place.
643
00:30:45.660 --> 00:30:47.260
That's the, uh, bottom line.
644
00:30:47.900 --> 00:30:50.820
Andrew Dunkley: Yeah. Although some would say, well, if we
645
00:30:50.820 --> 00:30:53.580
focus only on those areas, we might miss something important
646
00:30:53.820 --> 00:30:56.140
in the not so habitable zones.
647
00:30:56.700 --> 00:30:57.740
You just never know.
648
00:30:58.390 --> 00:31:01.140
Professor Fred Watson: Uh, and part of the problem with that is that we've only got one
649
00:31:01.140 --> 00:31:04.100
example of life, and that's here on Earth. And so we're
650
00:31:04.100 --> 00:31:06.460
sort of looking for the same kind of chemical reactions
651
00:31:06.860 --> 00:31:09.780
that formed life here on Earth. Earth, uh, to, to
652
00:31:09.780 --> 00:31:12.740
form similar life elsewhere, but there might be other kinds of
653
00:31:12.740 --> 00:31:14.700
life that don't need those reactions.
654
00:31:15.180 --> 00:31:18.140
Andrew Dunkley: Yeah, Ah, it's, um, it's funny
655
00:31:18.140 --> 00:31:20.900
you mentioned that because it just reminded me while we were on our cruise
656
00:31:20.900 --> 00:31:23.860
ship, we, we played a lot of trivia because, you know,
657
00:31:23.860 --> 00:31:26.740
that's what you do. And one of the questions
658
00:31:26.740 --> 00:31:28.550
that came up was, um, um,
659
00:31:29.980 --> 00:31:32.900
what was. I can't remember the wording, but they basically wanted you
660
00:31:32.900 --> 00:31:35.860
to explain what the Drake equation was. And
661
00:31:36.340 --> 00:31:38.580
I think only two of us got it out of
662
00:31:38.980 --> 00:31:41.860
200 people. Uh, I was very
663
00:31:41.860 --> 00:31:42.900
proud of myself, actually.
664
00:31:43.060 --> 00:31:44.900
Professor Fred Watson: I'm sure you will be. Yeah. Good on you.
665
00:31:46.160 --> 00:31:48.660
Andrew Dunkley: Uh, okay, so if you want to find out more about the
666
00:31:48.660 --> 00:31:51.580
Galactic Habitable Zone, you can do
667
00:31:51.580 --> 00:31:54.460
that through the universetoday.com website. It's a
668
00:31:54.460 --> 00:31:57.060
really interesting article too. I did manage to read the first
669
00:31:57.060 --> 00:31:57.620
paragraph.
670
00:31:58.100 --> 00:32:01.060
Uh, now, um, one thing I wanted
671
00:32:01.060 --> 00:32:03.900
to mention when you were talking about Insight and Mars and Mars not
672
00:32:03.900 --> 00:32:06.700
having tectonics, I, uh, I
673
00:32:06.700 --> 00:32:09.580
meant to add this onto the end of that segment, but I'll do it
674
00:32:09.580 --> 00:32:12.060
now. While we were overseas, uh, we went to
675
00:32:12.060 --> 00:32:14.860
Iceland and what an amazing place
676
00:32:14.860 --> 00:32:17.740
Iceland is. Uh, we got to walk along
677
00:32:17.740 --> 00:32:19.900
a rift valley where the
678
00:32:20.140 --> 00:32:22.220
Eurasian tectonic plate
679
00:32:22.860 --> 00:32:25.820
and the American tectonic plate meet. You can
680
00:32:25.820 --> 00:32:28.380
actually walk along it and the American
681
00:32:28.380 --> 00:32:31.220
plate is going up and over, the Eurasian plate is
682
00:32:31.220 --> 00:32:33.790
going down and under, and you can walk
683
00:32:34.110 --> 00:32:36.950
right on top of that. And
684
00:32:36.950 --> 00:32:39.310
you're walking along thinking, isn't this amazing?
685
00:32:40.110 --> 00:32:42.710
And, um, then you start seeing the
686
00:32:42.710 --> 00:32:45.310
plaques that explain, well, this was an earthquake in
687
00:32:45.310 --> 00:32:48.270
2011, this was an earthquake in 2015.
688
00:32:48.270 --> 00:32:50.910
And you're thinking, why am I standing here?
689
00:32:52.750 --> 00:32:53.550
Quite incredible.
690
00:32:53.950 --> 00:32:56.510
Professor Fred Watson: So the place you were at is a place called Thingback.
691
00:32:57.480 --> 00:33:00.110
Uh, it's, uh, uh, not that far from
692
00:33:00.110 --> 00:33:03.010
Reykjavik. Uh, Bungs. Uh, it's not
693
00:33:03.010 --> 00:33:05.770
plates colliding, it's plates dragging apart because
694
00:33:05.770 --> 00:33:08.730
you're in the middle of. Yeah, so they're
695
00:33:08.730 --> 00:33:11.610
separating. So you need to be even more careful because if
696
00:33:11.610 --> 00:33:14.570
they separate a bit faster on the day you're walking through it, you're going to drop
697
00:33:14.570 --> 00:33:15.650
right into the hole.
698
00:33:16.130 --> 00:33:19.010
Andrew Dunkley: Well, there are a lot of cracks in the ground in that part of
699
00:33:19.010 --> 00:33:21.250
the. So it does make sense.
700
00:33:21.960 --> 00:33:24.690
Um, I must not have read the literature
701
00:33:24.690 --> 00:33:27.610
when they explained what was happening exactly, but I
702
00:33:27.610 --> 00:33:28.970
thought they said colliding.
703
00:33:28.970 --> 00:33:31.730
Professor Fred Watson: So it's coming
704
00:33:31.730 --> 00:33:34.450
apart. It's the Mid Atlantic Ridge. That is the only place
705
00:33:34.770 --> 00:33:37.170
where the Mid Atlantic Ridge is on the surface.
706
00:33:37.490 --> 00:33:40.330
And Tingviklijk is where it's
707
00:33:40.330 --> 00:33:43.330
where it's most obvious. There is another place, uh, not very
708
00:33:43.330 --> 00:33:45.330
far from there. So actually on the
709
00:33:45.490 --> 00:33:48.490
Reykjanesput Peninsula to the
710
00:33:48.490 --> 00:33:51.410
west of, uh, Reykjavik. And there, there's a
711
00:33:51.410 --> 00:33:54.400
bridge across this border. Uh,
712
00:33:54.400 --> 00:33:57.370
and you can stand on one side of the bridge and you're on the Eurasian
713
00:33:57.370 --> 00:34:00.160
plate Stand on the other. You're on the American complaint. And all the
714
00:34:00.160 --> 00:34:03.040
locals think it's a great joke because you know there are things
715
00:34:03.040 --> 00:34:05.800
like this all over the island. Basically the island splitting
716
00:34:05.800 --> 00:34:08.400
in. In pieces because of the. Of that
717
00:34:08.400 --> 00:34:09.080
separation.
718
00:34:09.080 --> 00:34:12.040
Andrew Dunkley: But yeah, saw photos of
719
00:34:12.040 --> 00:34:14.920
people doing that. But we didn't go. We didn't go there but we went to.
720
00:34:15.000 --> 00:34:17.160
Oh, we went to a lot of places in Iceland. But
721
00:34:17.610 --> 00:34:20.200
um. One of the things we
722
00:34:20.360 --> 00:34:23.280
learned about a lot in places
723
00:34:23.280 --> 00:34:25.780
like Iceland and Greenland and up in um,
724
00:34:26.120 --> 00:34:29.040
Northern Europe was how fast the glaciers
725
00:34:29.040 --> 00:34:32.040
are melting. M. And shocking.
726
00:34:32.920 --> 00:34:35.520
It is very shocking. Some of them are um,
727
00:34:35.950 --> 00:34:38.760
uh. Ah, losing 20 metres or
728
00:34:38.760 --> 00:34:41.360
200 metres a year I should say, which is
729
00:34:41.360 --> 00:34:43.080
staggering. And
730
00:34:44.840 --> 00:34:47.440
that's lost forever. Um, we can't
731
00:34:47.440 --> 00:34:50.400
reverse that. So ah, it is rather
732
00:34:50.400 --> 00:34:53.390
shocking in fact. Uh, we were, I think it was
733
00:34:53.390 --> 00:34:56.279
when we were in the um, uh,
734
00:34:56.550 --> 00:34:59.510
Saint Christian Sound, uh, Prince Christian
735
00:34:59.510 --> 00:35:02.240
Sound, uh, they were saying um,
736
00:35:02.390 --> 00:35:05.390
see that rock in front of that uh, glacier? And we
737
00:35:05.390 --> 00:35:08.150
all went yeah. Well it was actually covered in
738
00:35:08.150 --> 00:35:10.950
ice two years ago. Yeah, that's how bad it's
739
00:35:10.950 --> 00:35:13.790
getting. And this is just this rock in the middle of nowhere and the
740
00:35:13.790 --> 00:35:16.470
ice is way, way, way back. So
741
00:35:16.630 --> 00:35:19.250
yeah, pretty shocking stuff. Um,
742
00:35:19.740 --> 00:35:22.140
that's just about it. Fred Watson, thank you so much.
743
00:35:23.660 --> 00:35:26.220
Professor Fred Watson: It's a pleasure. Andrew, it's great to welcome you back
744
00:35:26.380 --> 00:35:29.100
and um, I um, look forward to
745
00:35:29.100 --> 00:35:31.900
continuing the uh, recordings at a
746
00:35:31.970 --> 00:35:34.860
um, time that you don't have to
747
00:35:34.860 --> 00:35:37.620
choose between awkward times on different sides of the
748
00:35:37.620 --> 00:35:40.580
planet. Which is what we could do. Heidi and uh, I juggling
749
00:35:40.580 --> 00:35:42.540
our uh, respective uh, days.
750
00:35:43.180 --> 00:35:46.100
Andrew Dunkley: It's a bit difficult with those time differences. Well, while we were on the
751
00:35:46.100 --> 00:35:49.090
ship we sold a few and bought a house which in the
752
00:35:49.090 --> 00:35:51.810
early phases was simple because it was only a few hours time
753
00:35:51.810 --> 00:35:54.610
difference. But when it got to the real crunch of you know,
754
00:35:54.610 --> 00:35:57.570
settling it all, uh, the time difference was 12
755
00:35:57.570 --> 00:36:00.010
hours. So it really got difficult.
756
00:36:00.330 --> 00:36:03.130
But uh, it's done now and yes, we're in our new place.
757
00:36:03.370 --> 00:36:06.330
I should show it to you. I've got the, I've got the
758
00:36:06.330 --> 00:36:09.010
um, the Yankees Red uh, Sox
759
00:36:09.010 --> 00:36:11.930
baseball game background on. Because I took that photo when we went
760
00:36:11.930 --> 00:36:14.890
and watched a game in New York the other day uh, which
761
00:36:14.890 --> 00:36:16.670
was a lot of fun and the Red Sox one.
762
00:36:16.670 --> 00:36:17.150
Professor Fred Watson: Whoops.
763
00:36:17.490 --> 00:36:20.430
Andrew Dunkley: Um, but um, yeah, I'll put a normal
764
00:36:20.430 --> 00:36:23.390
background on so you can see the new place which pretty much
765
00:36:23.390 --> 00:36:26.110
looks the same as the old place. But anyway, whatever.
766
00:36:26.430 --> 00:36:28.190
Thanks Fred Watson. We'll catch you real soon.
767
00:36:28.750 --> 00:36:30.670
Professor Fred Watson: Sounds good. Thanks Andrew. Take care.
768
00:36:31.690 --> 00:36:34.430
Andrew Dunkley: Uh, you too. And don't forget, uh, if you would like to support
769
00:36:34.430 --> 00:36:37.310
the Australasian Dark sky alliance
770
00:36:37.310 --> 00:36:40.190
and get, uh, those signatures on their petition,
771
00:36:40.430 --> 00:36:43.150
it's australiandarkskyalliance.org
772
00:36:43.880 --> 00:36:46.760
and, uh, just follow the prompts, uh, for Australian
773
00:36:47.080 --> 00:36:49.320
signatories only. Australian, uh,
774
00:36:49.320 --> 00:36:50.240
Australasian
775
00:36:50.240 --> 00:36:53.110
darkskyalliance.org uh,
776
00:36:53.110 --> 00:36:55.960
that's it from me. And, oh, I forgot to thank
777
00:36:55.960 --> 00:36:58.880
Huw in the studio, which
778
00:36:58.880 --> 00:37:01.600
I quite often do. Uh, from me, Andrew
779
00:37:01.600 --> 00:37:04.280
Dunkley. Thanks for your company. See you on the next episode of Space
780
00:37:04.280 --> 00:37:05.400
Nuts. Bye. Bye.
781
00:37:06.360 --> 00:37:09.310
Voice Over Guy: You've been listening to the Space Nuts podcast cast,
782
00:37:10.750 --> 00:37:13.550
available at Apple Podcasts, Spotify,
783
00:37:13.630 --> 00:37:16.430
iHeartRadio or your favourite podcast
784
00:37:16.430 --> 00:37:18.790
player. You can also stream On Demand at
785
00:37:18.790 --> 00:37:21.710
bitesz. com. This has been another quality
786
00:37:21.710 --> 00:37:24.090
podcast production from bitesz. com
0
00:00:00.480 --> 00:00:01.760
Andrew Dunkley: Hi there. Look who's back.
1
00:00:03.040 --> 00:00:05.600
Yes, it's me. Back from,
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00:00:06.260 --> 00:00:09.200
uh, everywhere we went. Everywhere. Anyway, I won't bore you with all
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of that. Andrew Dunkley here. Great to have your company
4
00:00:11.840 --> 00:00:14.000
on another episode of Space
5
00:00:14.240 --> 00:00:16.800
Nuts. And coming up on today's show,
6
00:00:17.200 --> 00:00:19.920
we will be diving into the
7
00:00:19.920 --> 00:00:22.800
weird world of exo. Asteroids
8
00:00:22.880 --> 00:00:25.360
or exocomets or whatever they are.
9
00:00:25.920 --> 00:00:28.720
30, uh, one atlas to be exact. And
10
00:00:28.720 --> 00:00:31.440
it turns out it's a bit of a strange one. Uh, also
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in Insight, uh, the Insight mission is
12
00:00:34.260 --> 00:00:37.120
unravelling Mars's secrets, uh,
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particularly its deep, dark past. And believe me,
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it's a little bit ugly. And
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a galactic habitable zone.
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Is there such a thing? What does it mean? And what are we going to
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find there? We'll find out on this episode of space
18
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nuts. 15 seconds. Guidance is
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internal.
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Voice Over Guy: 10, 9. Ignition
21
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sequence start. Space nuts. 5, 4,
22
00:01:00.734 --> 00:01:03.660
3. 2. 1, 2, 3, 4, 5.
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Space nuts. Astronauts report it feels good.
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Andrew Dunkley: And joining us to do all the unravelling
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is Professor Fred Watson Watson, astronomer at large. Hello,
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Fred Watson.
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Professor Fred Watson: Welcome back, Andrew. It's, um, a, uh, treat
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to see your smiling face.
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Andrew Dunkley: It's a treat. It's a treat to be back and doing
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00:01:23.840 --> 00:01:26.520
this after it's been three months. I can't believe
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that, uh, it's been. Judy and I were only saying today
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we cannot get our heads around the fact that we're away for three
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months because it doesn't feel like it. It's just,
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you know, it went so fast. But, gee, we
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had a good time, Fred Watson. We had an amazing time.
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Um, unfortunately, did not get to see the
37
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northern lights. And that was
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one of my. But I might get another opportunity.
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You know, it's not the last time we'll go away somewhere, so
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fingers crossed. But, um, even as far north as,
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uh, North Cape, the northern tip of Europe, right up
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inside the Arctic Circle, did not see a thing.
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Uh, probably because it was nearly daylight every
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minute of the day and night. So that doesn't
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help. Um, but,
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yeah, a terrific holiday. I don't. I wouldn't know where
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to start to tell you about it. I know I posted a lot of pictures
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that people saw, uh, every time we went away
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or went somewhere, um, but just
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saw some amazing things, met some amazing people,
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had some amazing moments. Just, um, little
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things that we didn't expect. Like, uh, the captain
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of the ship suddenly deciding at the last minute to take
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us up, um, Prince Christian
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Sound in Norway, which is
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somewhere where not many people get to go. And the
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only way to get there is by ship. And it is
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Full of icebergs and wildlife
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and just, um,
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glacier after glacier after glacier right
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there in front of you. Um, it's
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indescribable. Uh, it's just the most amazing
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scenery. Uh, we sat up on the deck
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for seven and a half hours straight just taking it
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all in. We did not move. It was that
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captivating. Um, that
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was one of the highlights. Um, Namibia was
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amazing. Loved Namibia. Uh,
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we, um, loved Scotland. Loved
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Edinburgh, Fred Watson. What a terrific place. Um,
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we had porridge for breakfast and.
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Professor Fred Watson: You have haggis for lunch, didn't you?
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Andrew Dunkley: And had haggis for lunch, which, surprise was
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surprisingly nice. I, you know, you hear horror
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stories, but it was actually quite tasty.
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Really enjoyed it. And, um, look,
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the countries we visited were, were many.
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Uh, the highlights were numerous. I wouldn't,
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I could talk for hours, which probably wouldn't work
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well on a space podcast. So I
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won't, um, I won't say too much more about that.
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Although at Tenerife we did see the
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observatory up, um, above the snow
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line there. Above the, um, uh,
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tree line, actually, not the snow line. Um,
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you drive up the hill, you've probably done this bread,
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and all of a sudden there's no vegetation, it's just gone.
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And, um, there's an observatory up there which is
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primarily a solar observatory, so.
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Professor Fred Watson: That's right, yeah. Got to have. So Tad is the
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name of the mountain, Katie.
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Andrew Dunkley: That's right.
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Professor Fred Watson: Yep, yep, yep.
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Andrew Dunkley: Yes.
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But, uh, here we are back again.
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Professor Fred Watson: Um, yeah, I do have a question for you about.
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Andrew Dunkley: Oh, ah, yeah.
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Professor Fred Watson: Andrew, did you. Did you run into any space
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nuts? I did,
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I actually did.
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Andrew Dunkley: Um, one in particular who I ran into
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in a toilet on a ship. On our
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cruise ship. I was walking out
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and this, he said, um, are you Andrew Dunkley? And I went,
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yes, he said, he said, I'm a Space Nuts
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listener, he said. And I remember he did message.
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Message me to say he'd be on the cruise and getting on in Dover and
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I'd forgotten about that. And, uh, yeah, we ran into each
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other in passing. So, um.
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And as always, I've forgotten his name and
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I apologise for that. But it was nice to catch up. So, yes,
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we did. No, it ran into a few. A few people I did
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pass, uh, or speak to on the ship knew me,
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but I don't know if they knew me from radio
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or from the podcast. We never really clarified that.
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But yeah, it was, uh, it was quite
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extraordinary. Um, but if you jump
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on Facebook, all my photos are on my Facebook page and Instagram
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So you should be able to see most of what we did.
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So I don't take up the rest of the show talking
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about it, although I'll probably, probably have
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times where I'll make references to things
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we saw and didn't. Yeah.
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Now, um, we've got a lot to talk about, but one
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of the things you do want to discuss and I think you did that with
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Heidi. Oh, and I'd like to say just
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my, um, sincere
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thanks to Heidi for stepping up and covering the last
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few months. It was a, it was a big job and she did,
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did fantastically. The feedback I've been getting,
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uh, even while I was away was, uh, was glowing.
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So well done, Heid Heidi and thank you, Much
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appreciated. Uh, and you
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talked to her last week and you want to mention again, the Australian Dark
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sky alliance is looking for some support.
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Professor Fred Watson: That's right. So if you're not
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either resident in or a citizen of Australia,
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you can zone out for a minute while I talk about
139
00:06:27.090 --> 00:06:29.930
a petition which the Australasian Dark sky
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alliance, uh, is trying to get
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put up to the, the federal government, the government
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of Australia, in order to put
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legislation in place to limit light pollution,
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to actually restrict it as an environmental
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issue, not just for astronomers, but for wildlife, for human
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00:06:46.560 --> 00:06:49.560
health, all of the above. So if you do fall into one
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00:06:49.560 --> 00:06:52.480
of those categories, uh, the place to go is their
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website, which is all one word,
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australasiandarkskyalliance.org
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uh, and so
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australasiandarkskyalliantiance.org will take you to
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their website, which on the front page has instructions on
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00:07:05.960 --> 00:07:08.680
how to sign the petition. And you've got till September
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00:07:08.840 --> 00:07:11.480
19th. And thank you for that plug and.
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Andrew Dunkley: Uh, my great pleasure. Uh, and hopefully the
156
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politicians will listen. Hopefully you get the numbers.
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That's the most important thing.
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And it's a really important thing. I mean, uh,
159
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we've talked about light pollution many,
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many times over the years. And it's just one of
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those growing problems, uh, which
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doesn't seem to get a lot of attention because no one really thinks about
163
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it as a problem. I suppose that's the problem.
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Professor Fred Watson: It is, uh, uh, on the other hand, it is one of the easiest to
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fix because flick of switch actually does it.
166
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Um, but you're right, I mean there's
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certainly regulations in regard to noise pollution,
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uh, and of course every other kind of pollution. We're
169
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seeing regulation coming in on plastics pollution.
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But light pollution is the orphan pollution at the
171
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moment. And it's an important one. It's one that's more important
172
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than Most people realise, and one statistic, uh, you might not
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be aware of this Andrew, but light pollution is increasing
174
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globally at 10% per
175
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year. So that comes from cities and science.
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Yeah, we know uh, that the stars are disappearing at that
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rate, 10% a year, it's very
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ugly indeed.
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Andrew Dunkley: That is, that's not good at all. And having
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witnessed now 24 hour day sunlight, I
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do understand how it could mess you with your brain.
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So it's not good for human healthy.
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Uh, so that's
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australasiandarkskyaalliance.org
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uh, 10,000 signatures by the 19th
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of September if you will.
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Uh, right, our first topic, Fred Watson, takes us
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uh, into the realm of uh, interstellar
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objects. 31 Atlas. Um, now I
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did see this one pop up in the news while I was away.
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I did try to keep in touch but um, when you're moving into
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different time zones of different parts of the world, your
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news suddenly changes, which is a little
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bit weird. Uh, but 31 Atlas,
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um, this one was only a recent discovery and it's
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hammering way through our ah, system as we speak.
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Uh, but they've been uh, able to analyse it thanks to the
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James Horace Webb Space Telescope. And this one's
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a little bit unusual.
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Professor Fred Watson: Uh, that's right. And um, because all the
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text you've read is in uh,
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Arial, uh, font, you wouldn't
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have no way of knowing that it's actually 3I
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Atlas. Holy
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circumstances. 3I
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being the third interstellar, the third interstellar,
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uh, object to pass through the solar system and uh, Atlas, of course, and
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then the facility that discovered it.
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Andrew Dunkley: I'm using jet lag as an excuse.
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Professor Fred Watson: It doesn't matter. Even if you weren't jet lag, you wouldn't have
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known because now.
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Andrew Dunkley: 31.
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Professor Fred Watson: Yeah, but it's 3i. Never mind.
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You see that's the advantage of uh, times,
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Times New Roman. That would, that would solve the problem.
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Um, anyway, this is being
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observed uh, as it flies by the solar system.
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It's closest to the sun if I remember rightly, on
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the 29th of October. So unlike
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uh, uh, unlike Oumuamua, which was one
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eye, the first um, interstellar object,
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uh, we didn't catch up with that until
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it was on its way out of the solar system Atlas,
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uh, uh, we found on the way in.
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Uh, and one reason for that is
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that it's a much bigger object. Um, I think um,
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the best estimate we got for the size of
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Oumuamua was something like 40,
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maybe 100 metres long, something of that sort. I can't remember the
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exact number but this thing is thought to be about 20
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kilometres across um and
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it's despite um the
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prognostications of Avilob who wanted uh
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it to be an interstellar spacecraft.
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It's behaving exactly like a comet in that
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it's uh, as it approaches the sun the
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material that it's made of which is a mixture of
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ice and dust uh that heats
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up the ice turns into a vapour, the dust gets
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released and it generates what we call a coma um
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coma is just a word meaning hair and it's uh,
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a sort of fuzzy bit of the uh, of the comet
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and um, develops a tail and indeed three eye
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Atlas has done that. Um it's uh,
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what's of interest uh of course is
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that there are mixed in with the dust
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there are atoms and in fact molecules of the, of
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the material that binds it together, the ices
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that bind it together. And it's not just water ice. We know that
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comets are made mostly of water ice. Water as we've
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said many times on space knots is the most
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common two element uh molecule in the
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universe. Uh so it's natural that we should find
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water in comets. But there's also
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basically uh carbon dioxide, CO2, carbon
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monoxide CO uh and those
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uh gases are revealing their presence by
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their spectra. Uh the rainbow spectra that
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you can analyse the light that's coming from them
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and indeed uh, exactly as you've said the
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James Webb Space Telescope is being
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uh used by a number of authors mostly
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in the United States. Uh Goddard Space Flight Centre
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and the Catholic University of America are two of the organisations
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represented. So you've got
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carbon monoxide, carbon dioxide, you've got something called
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carbonyl sulphide. Uh all
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of these are ah, not unexpected
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because that's what we find in comets that belong to the
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solar system. But here's the
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rub, um and it's the ratio
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of these molecules to each other
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that is uh the peculiarity of
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three I atlas uh and in particular
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the ratio of carbon uh
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dioxide to water is actually
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eight to one. So eight parts of
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carbon dioxide to one part of water
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and that's higher than any other comet that's ever been
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seen and way, way above the normal value
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um, which is I think two or three to one,
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something like that. I can't remember the exact number. Um
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however carbon monoxide
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has uh a ratio with water that's more
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or less the same as ah, um solar
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system comets. It's 1.4.
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So there's a puzzle uh why is the carbon dioxide,
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so much more abundant. Uh, and of course,
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as always, when faced with a puzzle,
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um, astronomers start trying to work out
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what's going on, uh, and
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they basically think
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that they have sort of solved
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it. Um,
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um, it's. One possibility
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is if you imagine the host
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star system in which this object was created
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and it would have formed like the, uh, solar
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system's comets, probably in an Oort cloud like
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the one we have around our solar system, which is made
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of, uh, cometary bodies, uh, which eventually
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fall in towards the inner solar system. And that's when we see
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them. Uh, there's a suggestion that if you've
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got very high levels of ultraviolet
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radiation, uh, from that
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host star, and that would be the case if it was a
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young and very massive star, um, that
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apparently could change this ratio of water
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to carbon dioxide. Um, and another
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comment that's been suggested is that
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maybe, um, it's uh, a part
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of that, um, of the solar system in which
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it was born. That's a long way from
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the host star, uh, and above the host
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star's carbon dioxide ice line.
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So beyond a certain distance you get more
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carbon dioxide in
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relation to water. Uh, and,
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you know, that's another possibility. There's
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several more that are being thought of. But, uh, the
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bottom line is, nearly as always with stories like this,
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Andrew, what we need is more observations.
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Uh, and uh, you know, we don't have very
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long before it will get too faint to
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observe. It'll be probably next year when it starts, um,
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really disappearing out of the solar system. But,
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uh, so we've got this golden opportunity to
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analyse it and, and investigate it. And that's exactly what's
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happening.
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Andrew Dunkley: How, how visible is this one going to be as
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it reaches the inner sanctum of
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our solar system?
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Professor Fred Watson: Yeah, not, not that visible
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because, um, in fact, I don't have a figure for its magnitude,
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the gobbledygook number that astronomers use for brightness.
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Uh, but it's. It's certainly, um, very much the
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province of big telescopes. The thing is, uh, its
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nearest approach to Earth, uh, um,
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I can't remember. It's more than one astronomical
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unit, I think, which is the distance between the Earth to the sun. I
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can't remember the exact distance. Uh,
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it's not that close to the sun either. Uh, and I
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think I'm right in saying that
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when it's closest to the sun, we can't see it because
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it's in the same direction. It's sort of passing behind the Sun.
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Um, that was one of the comments that ah avilaeur
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made uh suggesting that maybe uh when it was
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at its brightest um its orbit had been chosen so that we
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couldn't see it it when it was at its brightest um and the
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other thing he pointed out was that it passes very close
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to or closeish to Venus, Mars and
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Jupiter. Um and um, you know the suggestion was
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that there might be intelligent design behind that.
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But uh, I think he's the only person in the
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astronomical community he thinks.
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Andrew Dunkley: That he might be
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right. Uh, you got to give him credit
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though.
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Professor Fred Watson: He's always um. Yeah we need ideas like
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that. Absolutely.
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Andrew Dunkley: Yeah. Yeah. Okay so uh,
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and is this one honking along like the others
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at a.
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Professor Fred Watson: Greater rate of knots, 60 something kilometres
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per second which is kind of one of the things that tells you that
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it doesn't belong to our solar system. It's going too fast.
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Andrew Dunkley: Right, There you are. Okay, uh you can read up
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on that one uh@universetoday.com
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uh3iatlas
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Got it. This is Space Nuts with Andrew
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Dunkley and Professor Fred Watson Watson.
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Space Nuts, our uh next story. Fred Watson
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takes us to a place I rarely
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mention. Uh it is the red planet Mars.
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Uh INSIGHT has uh been um
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sort of examining some of the secrets of Mars
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and come up with uh new information
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that kind of might surprise people about uh
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Mars's deep dark and ugly past.
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Um, there's been a few revelations.
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Professor Fred Watson: There have, yes. Um, I mean INSIGHT is the gift that
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keeps on giving really. Um because it switched off
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in 2022. Uh
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um it's ah a spacecraft that
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landed near Mars's equatorial region.
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Uh I think in about 2019 was when
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it uh touched down um and you might
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remember we discussed a lot the instruments that are on board
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it because one of them was a seismometer uh which has
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been incredibly successful and the other one was
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the interior thermometer which was incredibly
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unsuccessful because they were trying to drill
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a hole to put this thermometer down under the
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surface of uh Mars and I think can't remember what happened.
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The drill correct. Kept breaking or something um
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unsatisfying happened uh until that part of
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the experiment was not as successful but the seismograph
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has done its job and um
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the results from that keep um on being
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reanalysed uh because as time goes
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on we've got many more analytical facilities
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at our disposal which we didn't have before. Uh and
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um, you can now look at these seismic records with a
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lot more meaning and what's
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been discovered. It's actually um, from an
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analysis of eight seismic Events,
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uh, uh, two of which were
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probably caused by meteorite
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impact on Mars. Remember um, that the
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two mechanisms, because Mars doesn't have plate tectonics,
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it's called a single uh, crust.
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Um, it's uh, stretching and
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shrinking of the crust and sort of
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rift valleys forming and things like that that give you the seismic
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events or meteorite impacts. And two of
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those seismic events as I said, were
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meteorite impacts. But um,
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it's the way that the uh,
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relative frequencies of the vibrations, the
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uh, seismic vibrations, the relative frequencies of these,
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uh, that allows people to
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basically examine the interior of Mars,
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uh, in a very intelligent
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way. Um, so you look for higher
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frequency waves compared with uh, low
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frequency waves. And basically uh,
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that tells you uh, about the length
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of transmission time uh for these different
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waves, how long it takes you to get from the site of impact,
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wherever that is, uh to the seismograph.
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And uh, one of the authors uh, of this
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work. I um, think there's ah, certainly authors at
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Imperial College London and uh,
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other institutions, uh, but one of the authors m
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made a comment, um, which I liked.
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These signals show clear signs of interference
437
00:20:45.240 --> 00:20:47.800
as they travel through Mars's deep interior.
438
00:20:48.040 --> 00:20:50.880
That's consistent with a mantle full
439
00:20:50.880 --> 00:20:53.720
of structures of different compositional origins,
440
00:20:53.800 --> 00:20:56.360
leftovers from Mars's early days.
441
00:20:56.600 --> 00:20:59.320
And what that means is so the mantle is the region
442
00:20:59.720 --> 00:21:02.720
between the crust of uh, Mars and its
443
00:21:02.720 --> 00:21:05.680
core, its hot core. Uh, we've got a
444
00:21:05.680 --> 00:21:08.580
mantle on Earth. I think Mars's mantle is rather
445
00:21:09.080 --> 00:21:11.980
uh, deeper than ours relative to the diameter of the
446
00:21:11.980 --> 00:21:14.660
planet. Um but what they found is that
447
00:21:14.820 --> 00:21:17.740
the mantle isn't a sort of uniform, um,
448
00:21:18.340 --> 00:21:21.180
uh, paste of semi
449
00:21:21.180 --> 00:21:23.700
solid rock, uh but it has
450
00:21:23.780 --> 00:21:26.660
structure in it. Uh, and that structure
451
00:21:26.980 --> 00:21:29.370
is thought to come from uh,
452
00:21:29.780 --> 00:21:32.420
events that took place during Mars
453
00:21:32.580 --> 00:21:34.960
origins. Uh and in fact what they're
454
00:21:34.960 --> 00:21:37.820
suggesting is that um,
455
00:21:39.160 --> 00:21:42.040
when Mars was being formed about
456
00:21:42.040 --> 00:21:44.600
4.5 billion years ago, um,
457
00:21:44.840 --> 00:21:47.680
it was at a time as we've talked about it
458
00:21:47.680 --> 00:21:50.620
before. Not long after that there was the um,
459
00:21:50.620 --> 00:21:53.510
what's it called, The Late Heavy Bombardment, uh
460
00:21:53.510 --> 00:21:56.480
when there was a lot of stuff careering around the solar
461
00:21:56.480 --> 00:21:59.440
system. Big objects the size of uh, many
462
00:21:59.440 --> 00:22:01.910
planets really banging into everything else.
463
00:22:02.070 --> 00:22:04.790
And the suggestion is
464
00:22:05.030 --> 00:22:07.950
that at that period some of
465
00:22:07.950 --> 00:22:10.710
these planetoids or planetesimals, uh
466
00:22:10.710 --> 00:22:13.270
actually collided with Mars and
467
00:22:13.830 --> 00:22:16.390
basically melted parts of Mars,
468
00:22:16.910 --> 00:22:19.350
uh into oceans of
469
00:22:19.590 --> 00:22:22.230
molten magma. Uh, and
470
00:22:22.710 --> 00:22:25.390
then you find that these
471
00:22:25.390 --> 00:22:27.580
regions cool, but
472
00:22:28.140 --> 00:22:31.060
when they're cooled they have
473
00:22:31.060 --> 00:22:33.500
a different structure from the stuff that didn't get
474
00:22:33.500 --> 00:22:36.460
clouted and melted, uh, by an impact
475
00:22:36.860 --> 00:22:39.860
so what you're doing is you're differentiating between
476
00:22:39.860 --> 00:22:42.540
different zones of Mars's mantle and
477
00:22:42.620 --> 00:22:45.540
what they're saying is that what they're detecting
478
00:22:45.540 --> 00:22:48.140
with this uh, inhomogeneity in
479
00:22:48.140 --> 00:22:50.980
Mars's mantle is evidence of these, what
480
00:22:50.980 --> 00:22:53.950
they describe as compositionally distinct chunks of
481
00:22:53.950 --> 00:22:56.510
material. Uh so um, you know
482
00:22:56.510 --> 00:22:59.510
Mars as mantle has got some
483
00:22:59.510 --> 00:23:02.350
bits that were never reheated and others
484
00:23:02.350 --> 00:23:05.350
that were reheated after the planet's formation by these
485
00:23:05.350 --> 00:23:08.110
collisions probably molten, uh then
486
00:23:08.110 --> 00:23:11.070
they hardened and they crystallised and that gives
487
00:23:11.070 --> 00:23:13.630
you a different structure which is what's now been seen.
488
00:23:13.870 --> 00:23:16.800
So um, it's ah, you know one of the comments, uh,
489
00:23:17.150 --> 00:23:20.110
the same author, uh, uh, who I
490
00:23:20.110 --> 00:23:22.800
just um, I just uh, mentioned most of this
491
00:23:22.800 --> 00:23:25.360
chaos likely unfolded in Mars first
492
00:23:25.360 --> 00:23:28.160
100 million years. The fact that we can still
493
00:23:28.160 --> 00:23:31.040
detect its traces after 4.5 billion years
494
00:23:31.360 --> 00:23:34.160
shows just how sluggishly Mars's interior
495
00:23:34.400 --> 00:23:37.360
has been churning ever since. Uh unlike the
496
00:23:37.360 --> 00:23:40.120
Earth's which is much more active. So yeah,
497
00:23:40.120 --> 00:23:43.040
um, the Mars story from Insight
498
00:23:43.200 --> 00:23:46.200
keeps on amazing us. We keep uh, discovering
499
00:23:46.200 --> 00:23:49.000
new facts about it and um. Long may it continue
500
00:23:49.080 --> 00:23:49.640
Andrew.
501
00:23:50.120 --> 00:23:52.300
Andrew Dunkley: Yes, yes, hopefully. Um,
502
00:23:52.760 --> 00:23:55.640
and there's so much more to learn. This is what I
503
00:23:55.720 --> 00:23:58.600
love about uh, these inner planets
504
00:23:59.100 --> 00:24:02.000
uh, and the outer planets as well. The more we look at them
505
00:24:02.000 --> 00:24:04.760
and the more we analyse the data that we're receiving
506
00:24:04.760 --> 00:24:07.760
from various missions, the more interesting they
507
00:24:07.760 --> 00:24:10.720
get and the stranger they get sometimes as is
508
00:24:10.720 --> 00:24:13.560
the case with Mars in this particular situation.
509
00:24:13.640 --> 00:24:16.520
So uh, yeah it's a fascinating place. Uh,
510
00:24:16.520 --> 00:24:19.400
cosmosmagazine.com is where you need to go
511
00:24:19.400 --> 00:24:22.260
to uh, find out more about that if you'd like to follow up on
512
00:24:22.260 --> 00:24:25.220
that story. Andrew Dunkley here, Fred Watson Watson there.
513
00:24:25.220 --> 00:24:27.140
You're listening to Space Nuts.
514
00:24:31.540 --> 00:24:32.580
Professor Fred Watson: Space Nuts.
515
00:24:32.740 --> 00:24:35.580
Andrew Dunkley: And uh, our final story today is about
516
00:24:35.580 --> 00:24:38.500
a galactic habitable zone. Now we
517
00:24:38.500 --> 00:24:41.260
know about the habitable zone in our own solar
518
00:24:41.260 --> 00:24:43.780
system, uh, which is affectionately called the
519
00:24:43.860 --> 00:24:46.860
Goldilocks Zone. And we know about that because
520
00:24:46.860 --> 00:24:49.670
we're in it. That's the only thing that keeps us alive
521
00:24:49.670 --> 00:24:52.590
really. Uh, but Fred Watson,
522
00:24:53.310 --> 00:24:56.310
my question first up is uh, are they talking about
523
00:24:56.310 --> 00:24:59.150
a Goldilocks Zone on a galactic
524
00:24:59.150 --> 00:25:00.590
scale? Is that what this is?
525
00:25:01.470 --> 00:25:04.390
Professor Fred Watson: Yeah, effectively. Um, but um, it's
526
00:25:04.390 --> 00:25:07.350
not the temperature that's not too
527
00:25:07.350 --> 00:25:10.230
hot and m not too cold but just right as it
528
00:25:10.230 --> 00:25:13.190
is in our Goldilocks Zone the temperature's just right
529
00:25:13.190 --> 00:25:16.190
at this distance from the sun for liquid water to
530
00:25:16.190 --> 00:25:18.990
exist. And we know it does because we see
531
00:25:18.990 --> 00:25:21.790
it pretty well every day uh, in our
532
00:25:21.860 --> 00:25:24.750
um, in Our reservoirs of water, whether
533
00:25:24.750 --> 00:25:27.720
they're a bathtub or a ah sea. Um,
534
00:25:27.720 --> 00:25:30.510
but that's not what the galactic habitable
535
00:25:30.510 --> 00:25:32.750
zone is about. And it is being called that the
536
00:25:32.750 --> 00:25:35.550
GHz or GHz if you're on
537
00:25:35.550 --> 00:25:38.230
the other side of the Pacific. Um,
538
00:25:38.590 --> 00:25:40.830
it's uh, it's a region where
539
00:25:41.750 --> 00:25:43.990
you might um, expect
540
00:25:44.870 --> 00:25:47.190
to find more habitable planets
541
00:25:47.830 --> 00:25:50.630
than nearer to the centre of our
542
00:25:50.630 --> 00:25:51.910
galaxy or
543
00:25:53.670 --> 00:25:56.310
further out towards the edge of the galaxy.
544
00:25:57.000 --> 00:25:58.790
Uh and it basically
545
00:26:00.390 --> 00:26:03.390
comes uh about uh. Because you can
546
00:26:03.390 --> 00:26:06.030
analyse, you know we know a lot about the way
547
00:26:06.030 --> 00:26:09.020
stars evolve. Uh and we know a
548
00:26:09.020 --> 00:26:11.820
lot about the um, chemicals
549
00:26:13.100 --> 00:26:15.660
um that have basically been found in
550
00:26:15.900 --> 00:26:18.780
stellar interiors and their atmospheres. And we
551
00:26:18.780 --> 00:26:21.500
can trace this history of stars very
552
00:26:21.500 --> 00:26:24.300
accurately. Um and we can
553
00:26:24.300 --> 00:26:27.100
also uh, look at the
554
00:26:27.100 --> 00:26:29.740
orbits of stars around the centre of our galaxy.
555
00:26:30.080 --> 00:26:33.020
Uh and we can work out to some extent where they've come from
556
00:26:33.020 --> 00:26:35.620
because uh, we think that the orbits of
557
00:26:35.620 --> 00:26:38.620
stars actually um, ah, they actually change
558
00:26:38.700 --> 00:26:40.700
in a process called stellar migration
559
00:26:41.660 --> 00:26:44.660
where stars, orbits change around the centre of the
560
00:26:44.660 --> 00:26:47.020
galaxy. Uh and you,
561
00:26:47.980 --> 00:26:50.940
you know, you can find that they uh, move.
562
00:26:51.500 --> 00:26:54.500
And so one of the studies, uh, one
563
00:26:54.500 --> 00:26:57.180
of the um, comments that's come from
564
00:26:57.180 --> 00:26:59.260
this particular study. It's actually an international
565
00:27:00.120 --> 00:27:03.020
uh team of scientists who have looked at this. Uh, this
566
00:27:03.020 --> 00:27:05.540
is published in strongly in Astrophysics, one of the main
567
00:27:05.930 --> 00:27:08.820
uh learned journals of astronomy. What they've
568
00:27:08.820 --> 00:27:11.380
discovered is that
569
00:27:11.850 --> 00:27:14.020
um, there's a five times
570
00:27:15.060 --> 00:27:18.020
greater likelihood of
571
00:27:18.340 --> 00:27:21.060
stars migrating from
572
00:27:22.100 --> 00:27:24.900
one part of a
573
00:27:24.900 --> 00:27:27.140
galaxy to another for
574
00:27:27.300 --> 00:27:30.300
habitable planets, for stars that have habitable
575
00:27:30.300 --> 00:27:33.230
planets compared to, with a lack
576
00:27:33.230 --> 00:27:35.910
of any stellar migration. So it's a
577
00:27:35.910 --> 00:27:38.670
slightly, this is a slightly obtuse thing to look
578
00:27:38.670 --> 00:27:41.590
for. Um, but um, what it
579
00:27:41.910 --> 00:27:44.790
says is, you know, it's all about
580
00:27:45.030 --> 00:27:48.029
for example whether you uh, are
581
00:27:48.029 --> 00:27:50.630
in a part of the galaxy where
582
00:27:50.630 --> 00:27:53.510
your solar system could uh, host
583
00:27:53.830 --> 00:27:56.470
gas giant planets because they would
584
00:27:57.110 --> 00:27:59.910
basically have an effect on the formation of
585
00:27:59.910 --> 00:28:02.590
the kind of rocky planets that we think are the
586
00:28:02.590 --> 00:28:05.410
habitable one. Um, so I
587
00:28:05.410 --> 00:28:08.090
might just read um, a ah, quote from
588
00:28:08.090 --> 00:28:10.970
this paper. Uh, it's a little bit
589
00:28:11.030 --> 00:28:14.010
uh, technical but um, I
590
00:28:14.010 --> 00:28:16.850
think it's an interesting quote. It sort of illuminates what we're talking
591
00:28:16.850 --> 00:28:19.330
about. Uh, in this study we have
592
00:28:19.330 --> 00:28:21.850
significantly expanded the exploration
593
00:28:22.170 --> 00:28:25.170
of the parameter space defining the galactic
594
00:28:25.170 --> 00:28:27.850
habitable zone compared to previous
595
00:28:27.850 --> 00:28:30.520
analyses present in literature. Uh, our
596
00:28:30.520 --> 00:28:33.200
findings are particularly relevant in the context of
597
00:28:33.200 --> 00:28:36.120
upcoming space missions such as the
598
00:28:36.120 --> 00:28:38.960
ESA PLATO mission, that's
599
00:28:38.960 --> 00:28:41.920
planetary transits and oscillations of stars, the uh,
600
00:28:42.040 --> 00:28:44.520
ESA Aerial Space Mission and large
601
00:28:44.520 --> 00:28:47.360
Interferometer for exoplanets. That's
602
00:28:47.360 --> 00:28:50.360
life. And these missions
603
00:28:50.360 --> 00:28:52.880
will deliver unprecedented, um, data on planetary
604
00:28:52.880 --> 00:28:55.440
properties, orbital architectures and
605
00:28:55.440 --> 00:28:58.130
atmospheric concepts, compositions. So what
606
00:28:58.130 --> 00:29:01.120
they're basically saying is, uh,
607
00:29:01.120 --> 00:29:04.090
if you're going to look for habitable planets, you want
608
00:29:04.090 --> 00:29:06.930
to be careful where you look. Because if there is
609
00:29:06.930 --> 00:29:09.890
such a thing as a stellar or a galactic habitable zone,
610
00:29:10.390 --> 00:29:13.370
um, then, uh, we want to be looking there
611
00:29:13.370 --> 00:29:16.090
if we're going to look for, uh, you know,
612
00:29:16.090 --> 00:29:19.050
for uh, habitable planets. It's an old
613
00:29:19.050 --> 00:29:21.610
idea, actually. The GHz, uh, or
614
00:29:21.610 --> 00:29:24.590
GHz, uh, comes, goes back to the 1980s.
615
00:29:25.030 --> 00:29:27.830
Um, and it's all about, you know, the um, the
616
00:29:27.830 --> 00:29:29.550
formation of the heavier elements.
617
00:29:30.670 --> 00:29:33.470
The ones that are basically work
618
00:29:33.550 --> 00:29:36.550
like iron, silicon, uh,
619
00:29:36.830 --> 00:29:39.830
oxygen, all of these elements. You've got to form
620
00:29:39.830 --> 00:29:42.430
them. You've got to form them in the right place in a galaxy.
621
00:29:42.910 --> 00:29:45.750
And uh, you've got to then, uh, let that
622
00:29:45.750 --> 00:29:48.430
environment breed these, uh, elements
623
00:29:48.430 --> 00:29:51.410
into molecules which basically
624
00:29:51.410 --> 00:29:54.210
become the, um, uh, precursors of life.
625
00:29:55.730 --> 00:29:57.970
I'm sorry, that's the Gobbler book. Uh,
626
00:29:57.970 --> 00:29:58.850
explanation.
627
00:29:59.570 --> 00:30:02.490
Andrew Dunkley: No, fair enough. Um, so
628
00:30:02.490 --> 00:30:04.770
does that mean that in our ongoing search for
629
00:30:04.770 --> 00:30:07.170
exoplanets, we should be focusing on
630
00:30:07.410 --> 00:30:10.290
the GHz areas?
631
00:30:11.330 --> 00:30:13.610
Uh, or do we not really care where the
632
00:30:13.610 --> 00:30:16.370
exoplanets are? Finding them is imperative regardless.
633
00:30:17.120 --> 00:30:20.080
Professor Fred Watson: Yeah, no, no, that's. That's exactly right.
634
00:30:20.080 --> 00:30:23.000
That's exactly what these authors are saying. We should be looking in the
635
00:30:23.000 --> 00:30:25.720
right place if we want to find, uh, habitable
636
00:30:25.720 --> 00:30:28.240
planets. Uh, and, um, uh,
637
00:30:28.720 --> 00:30:31.560
and indeed, um, you know, the, the PLATO mission, for
638
00:30:31.560 --> 00:30:34.080
example, is going to look at a million stars. It's a bit like
639
00:30:34.080 --> 00:30:36.880
Kepler. The Kepler mission, it was. It's finding
640
00:30:37.280 --> 00:30:40.200
planets by transits. Uh, so that's going
641
00:30:40.200 --> 00:30:42.940
to scan a million stars and, and
642
00:30:43.180 --> 00:30:45.660
you want to make sure you're looking at them in the right place.
643
00:30:45.660 --> 00:30:47.260
That's the, uh, bottom line.
644
00:30:47.900 --> 00:30:50.820
Andrew Dunkley: Yeah. Although some would say, well, if we
645
00:30:50.820 --> 00:30:53.580
focus only on those areas, we might miss something important
646
00:30:53.820 --> 00:30:56.140
in the not so habitable zones.
647
00:30:56.700 --> 00:30:57.740
You just never know.
648
00:30:58.390 --> 00:31:01.140
Professor Fred Watson: Uh, and part of the problem with that is that we've only got one
649
00:31:01.140 --> 00:31:04.100
example of life, and that's here on Earth. And so we're
650
00:31:04.100 --> 00:31:06.460
sort of looking for the same kind of chemical reactions
651
00:31:06.860 --> 00:31:09.780
that formed life here on Earth. Earth, uh, to, to
652
00:31:09.780 --> 00:31:12.740
form similar life elsewhere, but there might be other kinds of
653
00:31:12.740 --> 00:31:14.700
life that don't need those reactions.
654
00:31:15.180 --> 00:31:18.140
Andrew Dunkley: Yeah, Ah, it's, um, it's funny
655
00:31:18.140 --> 00:31:20.900
you mentioned that because it just reminded me while we were on our cruise
656
00:31:20.900 --> 00:31:23.860
ship, we, we played a lot of trivia because, you know,
657
00:31:23.860 --> 00:31:26.740
that's what you do. And one of the questions
658
00:31:26.740 --> 00:31:28.550
that came up was, um, um,
659
00:31:29.980 --> 00:31:32.900
what was. I can't remember the wording, but they basically wanted you
660
00:31:32.900 --> 00:31:35.860
to explain what the Drake equation was. And
661
00:31:36.340 --> 00:31:38.580
I think only two of us got it out of
662
00:31:38.980 --> 00:31:41.860
200 people. Uh, I was very
663
00:31:41.860 --> 00:31:42.900
proud of myself, actually.
664
00:31:43.060 --> 00:31:44.900
Professor Fred Watson: I'm sure you will be. Yeah. Good on you.
665
00:31:46.160 --> 00:31:48.660
Andrew Dunkley: Uh, okay, so if you want to find out more about the
666
00:31:48.660 --> 00:31:51.580
Galactic Habitable Zone, you can do
667
00:31:51.580 --> 00:31:54.460
that through the universetoday.com website. It's a
668
00:31:54.460 --> 00:31:57.060
really interesting article too. I did manage to read the first
669
00:31:57.060 --> 00:31:57.620
paragraph.
670
00:31:58.100 --> 00:32:01.060
Uh, now, um, one thing I wanted
671
00:32:01.060 --> 00:32:03.900
to mention when you were talking about Insight and Mars and Mars not
672
00:32:03.900 --> 00:32:06.700
having tectonics, I, uh, I
673
00:32:06.700 --> 00:32:09.580
meant to add this onto the end of that segment, but I'll do it
674
00:32:09.580 --> 00:32:12.060
now. While we were overseas, uh, we went to
675
00:32:12.060 --> 00:32:14.860
Iceland and what an amazing place
676
00:32:14.860 --> 00:32:17.740
Iceland is. Uh, we got to walk along
677
00:32:17.740 --> 00:32:19.900
a rift valley where the
678
00:32:20.140 --> 00:32:22.220
Eurasian tectonic plate
679
00:32:22.860 --> 00:32:25.820
and the American tectonic plate meet. You can
680
00:32:25.820 --> 00:32:28.380
actually walk along it and the American
681
00:32:28.380 --> 00:32:31.220
plate is going up and over, the Eurasian plate is
682
00:32:31.220 --> 00:32:33.790
going down and under, and you can walk
683
00:32:34.110 --> 00:32:36.950
right on top of that. And
684
00:32:36.950 --> 00:32:39.310
you're walking along thinking, isn't this amazing?
685
00:32:40.110 --> 00:32:42.710
And, um, then you start seeing the
686
00:32:42.710 --> 00:32:45.310
plaques that explain, well, this was an earthquake in
687
00:32:45.310 --> 00:32:48.270
2011, this was an earthquake in 2015.
688
00:32:48.270 --> 00:32:50.910
And you're thinking, why am I standing here?
689
00:32:52.750 --> 00:32:53.550
Quite incredible.
690
00:32:53.950 --> 00:32:56.510
Professor Fred Watson: So the place you were at is a place called Thingback.
691
00:32:57.480 --> 00:33:00.110
Uh, it's, uh, uh, not that far from
692
00:33:00.110 --> 00:33:03.010
Reykjavik. Uh, Bungs. Uh, it's not
693
00:33:03.010 --> 00:33:05.770
plates colliding, it's plates dragging apart because
694
00:33:05.770 --> 00:33:08.730
you're in the middle of. Yeah, so they're
695
00:33:08.730 --> 00:33:11.610
separating. So you need to be even more careful because if
696
00:33:11.610 --> 00:33:14.570
they separate a bit faster on the day you're walking through it, you're going to drop
697
00:33:14.570 --> 00:33:15.650
right into the hole.
698
00:33:16.130 --> 00:33:19.010
Andrew Dunkley: Well, there are a lot of cracks in the ground in that part of
699
00:33:19.010 --> 00:33:21.250
the. So it does make sense.
700
00:33:21.960 --> 00:33:24.690
Um, I must not have read the literature
701
00:33:24.690 --> 00:33:27.610
when they explained what was happening exactly, but I
702
00:33:27.610 --> 00:33:28.970
thought they said colliding.
703
00:33:28.970 --> 00:33:31.730
Professor Fred Watson: So it's coming
704
00:33:31.730 --> 00:33:34.450
apart. It's the Mid Atlantic Ridge. That is the only place
705
00:33:34.770 --> 00:33:37.170
where the Mid Atlantic Ridge is on the surface.
706
00:33:37.490 --> 00:33:40.330
And Tingviklijk is where it's
707
00:33:40.330 --> 00:33:43.330
where it's most obvious. There is another place, uh, not very
708
00:33:43.330 --> 00:33:45.330
far from there. So actually on the
709
00:33:45.490 --> 00:33:48.490
Reykjanesput Peninsula to the
710
00:33:48.490 --> 00:33:51.410
west of, uh, Reykjavik. And there, there's a
711
00:33:51.410 --> 00:33:54.400
bridge across this border. Uh,
712
00:33:54.400 --> 00:33:57.370
and you can stand on one side of the bridge and you're on the Eurasian
713
00:33:57.370 --> 00:34:00.160
plate Stand on the other. You're on the American complaint. And all the
714
00:34:00.160 --> 00:34:03.040
locals think it's a great joke because you know there are things
715
00:34:03.040 --> 00:34:05.800
like this all over the island. Basically the island splitting
716
00:34:05.800 --> 00:34:08.400
in. In pieces because of the. Of that
717
00:34:08.400 --> 00:34:09.080
separation.
718
00:34:09.080 --> 00:34:12.040
Andrew Dunkley: But yeah, saw photos of
719
00:34:12.040 --> 00:34:14.920
people doing that. But we didn't go. We didn't go there but we went to.
720
00:34:15.000 --> 00:34:17.160
Oh, we went to a lot of places in Iceland. But
721
00:34:17.610 --> 00:34:20.200
um. One of the things we
722
00:34:20.360 --> 00:34:23.280
learned about a lot in places
723
00:34:23.280 --> 00:34:25.780
like Iceland and Greenland and up in um,
724
00:34:26.120 --> 00:34:29.040
Northern Europe was how fast the glaciers
725
00:34:29.040 --> 00:34:32.040
are melting. M. And shocking.
726
00:34:32.920 --> 00:34:35.520
It is very shocking. Some of them are um,
727
00:34:35.950 --> 00:34:38.760
uh. Ah, losing 20 metres or
728
00:34:38.760 --> 00:34:41.360
200 metres a year I should say, which is
729
00:34:41.360 --> 00:34:43.080
staggering. And
730
00:34:44.840 --> 00:34:47.440
that's lost forever. Um, we can't
731
00:34:47.440 --> 00:34:50.400
reverse that. So ah, it is rather
732
00:34:50.400 --> 00:34:53.390
shocking in fact. Uh, we were, I think it was
733
00:34:53.390 --> 00:34:56.279
when we were in the um, uh,
734
00:34:56.550 --> 00:34:59.510
Saint Christian Sound, uh, Prince Christian
735
00:34:59.510 --> 00:35:02.240
Sound, uh, they were saying um,
736
00:35:02.390 --> 00:35:05.390
see that rock in front of that uh, glacier? And we
737
00:35:05.390 --> 00:35:08.150
all went yeah. Well it was actually covered in
738
00:35:08.150 --> 00:35:10.950
ice two years ago. Yeah, that's how bad it's
739
00:35:10.950 --> 00:35:13.790
getting. And this is just this rock in the middle of nowhere and the
740
00:35:13.790 --> 00:35:16.470
ice is way, way, way back. So
741
00:35:16.630 --> 00:35:19.250
yeah, pretty shocking stuff. Um,
742
00:35:19.740 --> 00:35:22.140
that's just about it. Fred Watson, thank you so much.
743
00:35:23.660 --> 00:35:26.220
Professor Fred Watson: It's a pleasure. Andrew, it's great to welcome you back
744
00:35:26.380 --> 00:35:29.100
and um, I um, look forward to
745
00:35:29.100 --> 00:35:31.900
continuing the uh, recordings at a
746
00:35:31.970 --> 00:35:34.860
um, time that you don't have to
747
00:35:34.860 --> 00:35:37.620
choose between awkward times on different sides of the
748
00:35:37.620 --> 00:35:40.580
planet. Which is what we could do. Heidi and uh, I juggling
749
00:35:40.580 --> 00:35:42.540
our uh, respective uh, days.
750
00:35:43.180 --> 00:35:46.100
Andrew Dunkley: It's a bit difficult with those time differences. Well, while we were on the
751
00:35:46.100 --> 00:35:49.090
ship we sold a few and bought a house which in the
752
00:35:49.090 --> 00:35:51.810
early phases was simple because it was only a few hours time
753
00:35:51.810 --> 00:35:54.610
difference. But when it got to the real crunch of you know,
754
00:35:54.610 --> 00:35:57.570
settling it all, uh, the time difference was 12
755
00:35:57.570 --> 00:36:00.010
hours. So it really got difficult.
756
00:36:00.330 --> 00:36:03.130
But uh, it's done now and yes, we're in our new place.
757
00:36:03.370 --> 00:36:06.330
I should show it to you. I've got the, I've got the
758
00:36:06.330 --> 00:36:09.010
um, the Yankees Red uh, Sox
759
00:36:09.010 --> 00:36:11.930
baseball game background on. Because I took that photo when we went
760
00:36:11.930 --> 00:36:14.890
and watched a game in New York the other day uh, which
761
00:36:14.890 --> 00:36:16.670
was a lot of fun and the Red Sox one.
762
00:36:16.670 --> 00:36:17.150
Professor Fred Watson: Whoops.
763
00:36:17.490 --> 00:36:20.430
Andrew Dunkley: Um, but um, yeah, I'll put a normal
764
00:36:20.430 --> 00:36:23.390
background on so you can see the new place which pretty much
765
00:36:23.390 --> 00:36:26.110
looks the same as the old place. But anyway, whatever.
766
00:36:26.430 --> 00:36:28.190
Thanks Fred Watson. We'll catch you real soon.
767
00:36:28.750 --> 00:36:30.670
Professor Fred Watson: Sounds good. Thanks Andrew. Take care.
768
00:36:31.690 --> 00:36:34.430
Andrew Dunkley: Uh, you too. And don't forget, uh, if you would like to support
769
00:36:34.430 --> 00:36:37.310
the Australasian Dark sky alliance
770
00:36:37.310 --> 00:36:40.190
and get, uh, those signatures on their petition,
771
00:36:40.430 --> 00:36:43.150
it's australiandarkskyalliance.org
772
00:36:43.880 --> 00:36:46.760
and, uh, just follow the prompts, uh, for Australian
773
00:36:47.080 --> 00:36:49.320
signatories only. Australian, uh,
774
00:36:49.320 --> 00:36:50.240
Australasian
775
00:36:50.240 --> 00:36:53.110
darkskyalliance.org uh,
776
00:36:53.110 --> 00:36:55.960
that's it from me. And, oh, I forgot to thank
777
00:36:55.960 --> 00:36:58.880
Huw in the studio, which
778
00:36:58.880 --> 00:37:01.600
I quite often do. Uh, from me, Andrew
779
00:37:01.600 --> 00:37:04.280
Dunkley. Thanks for your company. See you on the next episode of Space
780
00:37:04.280 --> 00:37:05.400
Nuts. Bye. Bye.
781
00:37:06.360 --> 00:37:09.310
Voice Over Guy: You've been listening to the Space Nuts podcast cast,
782
00:37:10.750 --> 00:37:13.550
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783
00:37:13.630 --> 00:37:16.430
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784
00:37:16.430 --> 00:37:18.790
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785
00:37:18.790 --> 00:37:21.710
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786
00:37:21.710 --> 00:37:24.090
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