WEBVTT

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<v Speaker 1>Oh hey, it's the stranger's dog who just licked your mouth.

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<v Speaker 1>Ali Ward, and let's turn our gaze and ears to

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<v Speaker 1>the sky currently at the moment, one hundred and fifty

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<v Speaker 1>nine million miles away to the planet of Venus. Taking

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<v Speaker 1>us on that journey. Is one of the most charming

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<v Speaker 1>and informatively enthusiastic ologists in planetary history. A global geologist

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<v Speaker 1>who studies both Earth and the other orbs in our

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<v Speaker 1>solar system, with a focus on what Venus can tell

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<v Speaker 1>us about our own home. And They graduated from Carlton College,

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<v Speaker 1>got a master's from the University of Montana and a

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<v Speaker 1>PhD from UCLA, before becoming a professor at Southern Methodist

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<v Speaker 1>University and then heading to the University of Minnesota Duluth

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<v Speaker 1>as a mcnight Presidential Endowed Professor of Earth and Planetary Scientists.

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<v Speaker 1>They have worked for the US Geological Survey and done

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<v Speaker 1>field work from Antarctica to the Arctic Yukon Territory. And

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<v Speaker 1>just a little quick warning, you will fall in love

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<v Speaker 1>with them and rock and Venus. But before we cast

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<v Speaker 1>that spell, let's thank the folks who sent in great

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<v Speaker 1>questions for them via Patreon dot com. Slash Ologies where

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<v Speaker 1>you two can support the show for as little as

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<v Speaker 1>a dollar a month and send your burning nine hundred

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<v Speaker 1>degree questions. Thank you also to everyone out there in

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<v Speaker 1>ologies merch from ologiesmerch dot com and of course, for

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<v Speaker 1>zero dollars a month, you can support the show just

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<v Speaker 1>by reviewing it and I read all the reviews. I

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<v Speaker 1>prove it with a recent one like this one from

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<v Speaker 1>listener and nurse Sara nine to sixteen, who wrote that

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<v Speaker 1>the show takes listeners on a magic school bus like

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<v Speaker 1>auditory journey, spanning from the smallest molecules to the largest

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<v Speaker 1>existential topics. And Sara nine to sixteen, thank you for that,

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<v Speaker 1>and thank you Lee E who tells their group therapy

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<v Speaker 1>clients to listen. Hey, everyone who leaves reviews, it truly

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<v Speaker 1>means the world keeps me going. I appreciate them and

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<v Speaker 1>it helps boost the show so much, which means we're

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<v Speaker 1>able to donate to a cause of theologists choosing each week.

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<v Speaker 1>Thank you to sponsors of the show.

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<v Speaker 2>Drivers know what trouble sounds like?

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<v Speaker 1>No? No, okay forward?

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<v Speaker 4>about it. Sure, I'm driving ten years and parallel parking.

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<v Speaker 4>Still that isn't me.

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<v Speaker 2>the Central Bank of Ireland.

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<v Speaker 5>Hey Mark, how are you?

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<v Speaker 6>Oh?

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<v Speaker 1>I'm not great a sore throat.

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<v Speaker 2>I think I'm coming down with cold.

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<v Speaker 5>Oh no, you should try a Vogel sore throat spray.

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<v Speaker 5>It's a natural remedy with echinata and sage and can

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<v Speaker 5>treat symptoms of coals and flus, including sore throats.

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<v Speaker 1>Perfect I'd give that a try.

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<v Speaker 5>So we'll leave sore throats symptoms with a Vogel. A

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<v Speaker 5>keen of force sore throat spray made from echinasia and

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<v Speaker 5>sage herbs and designed to reach irritated parts of the throat,

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<v Speaker 5>available from health stores and pharmacies nationwide.

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<v Speaker 1>Always read the leaflet okay from the smallest molecules to

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<v Speaker 1>the planets themselves. Let's blast off into this instant classic

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<v Speaker 1>an episode that had me beaming every second of the interview.

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<v Speaker 1>Here we go into the world of mission recon noodle data,

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<v Speaker 1>melting machinery, swimming in air, baby siblings, goddess vibes, men,

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<v Speaker 1>women and off the mark, self help books, sci fi,

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<v Speaker 1>How to Endure a long day, atmosphere of old factory wonders,

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<v Speaker 1>and whether or not it's a good idea to visit

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<v Speaker 1>the Planet of Love with planetary geologists, comparative planetologist, Galactic

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<v Speaker 1>treasure and venosologist doctor Vicki Hansen. So I'm trying to

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<v Speaker 1>figure out there is an ology for this, right like,

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<v Speaker 1>it's is it Venuology?

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<v Speaker 6>Well, you know, that's really an interesting question because some

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<v Speaker 6>say it's like Venusian or that those are the people.

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<v Speaker 6>So venus ology, you know, I think would go just

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<v Speaker 6>as well as anything than good.

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<v Speaker 1>Are there a lot of people who are out there

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<v Speaker 1>studying Venus? Do you all get together? Do you all

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<v Speaker 1>know each other? Is it a relatively small number compared

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<v Speaker 1>to Mars.

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<v Speaker 6>Yes, it is a small number compared to Mars. It

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<v Speaker 6>is an expanding community. When we had the Magellan Mission.

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<v Speaker 6>Back in the late eighties early nineties. It was really

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<v Speaker 6>a small community and we all met in one room

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<v Speaker 6>at Caltech and Pasadena. Wow, you know. And now it's expanded,

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<v Speaker 6>but it will never be as big as Mars, I'm sure,

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<v Speaker 6>which it deserves to be much bigger, because Venus is

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<v Speaker 6>much more exciting.

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<v Speaker 1>And which is to us. I understand, Venus is larger

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<v Speaker 1>than Mars. Yes, which is closer.

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<v Speaker 6>Venus is closer to Us, and Venus is between Us

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<v Speaker 6>and the Sun.

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<v Speaker 1>And then we've got Mercury Venus Us, yes.

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<v Speaker 6>Mars exactly, and then the asteroid belt, and then we

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<v Speaker 6>go out to the bigger planets.

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<v Speaker 1>And how big is Venus in comparison to Earth.

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<v Speaker 6>It's about eighty percent of the size of Earth. So

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<v Speaker 6>it's just it's little sister by a not much amount,

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<v Speaker 6>but that could be important.

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<v Speaker 1>So Venus closer to Earth than Mars, larger than Mars,

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<v Speaker 1>and like a sibling that's like an inch and a

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<v Speaker 1>half shorter than us. But mysterious and overlooked. Why do

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<v Speaker 1>you think people are so hung up on Mars more

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<v Speaker 1>so than Venus.

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<v Speaker 6>Well, first of all, they say men are from Mars

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<v Speaker 6>and women are from yes, So there we go.

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<v Speaker 1>Mars distant red, named for the god of war, Venus

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<v Speaker 1>bright in the sky, the spectacular goddess of love, and

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<v Speaker 1>the only planet in our solar system named after our

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<v Speaker 1>female deity. But in terms of attention battles over beauty,

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<v Speaker 1>it figures.

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<v Speaker 6>No more need to be said. But I think it's

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<v Speaker 6>because there's this incredible search for life, and so people

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<v Speaker 6>think that Mars might have a better chance of life.

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<v Speaker 6>In fact, I'm not sure that's true. Another reason I

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<v Speaker 6>think is just because Venus, like a woman, she keeps

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<v Speaker 6>herself shrouded in clouds, and so she's called the morning

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<v Speaker 6>star in the evening Star, and that's because the sun's

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<v Speaker 6>light is reflected off of her surface, and so she

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<v Speaker 6>really looks like a star. And we can't see through

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<v Speaker 6>those clouds unless we have radar, and radar was not

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<v Speaker 6>developed until really quite recently, especially compared to telescope. So

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<v Speaker 6>we can with telescopes actually see the surface of Mars

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<v Speaker 6>and Venus. We need radar to see through otherwise we

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<v Speaker 6>just see these clouds and nothing else.

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<v Speaker 1>What are those clouds made of?

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<v Speaker 6>Those clouds are made up of mostly CO two and

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<v Speaker 6>then some sulfuric acid and a tiny bit of water

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<v Speaker 6>and other things thrown into the mix. The cloud bank

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<v Speaker 6>is really, really thick and sits much higher above the

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<v Speaker 6>planet than our own cloud bank. Way up there, very

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<v Speaker 6>very dense and actually is a greenhouse effect that keeps

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<v Speaker 6>a lot of heat into the planet. But what's really

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<v Speaker 6>cool about those clouds is that there are layers within them.

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<v Speaker 6>Because they're so thick, there's convection or flow because they're

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<v Speaker 6>a gas, and that's actually where there might be life

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<v Speaker 6>on Venus in the clouds, in the clouds, because the

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<v Speaker 6>surfaces we'll find out is super hot, super dry, not

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<v Speaker 6>good for life as we define it.

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<v Speaker 1>So that's on land maybe not.

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<v Speaker 6>Does it really exist, but up in the clouds, if

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<v Speaker 6>we were up in the cloud bank, it would be

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<v Speaker 6>about the same temperature and pressure as you and I

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<v Speaker 6>sitting here. Oh, so we could exist in the clouds,

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<v Speaker 6>maybe not so much oxygen at the surface. We'd be

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<v Speaker 6>squashed flat because it would be like being under a

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<v Speaker 6>couple of kilometers of water in the ocean. And it's

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<v Speaker 6>basically nine hundred degrees fahrenheit, so super hot. Big temperature

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<v Speaker 6>differential between here and Duluth, Minnesota, for sure. But in

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<v Speaker 6>the clouds because they have the circulation. You could have again,

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<v Speaker 6>not life like us, but life existing in those clouds

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<v Speaker 6>and they just ride those convection cells. But they also

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<v Speaker 6>the different chemicals that are in the clouds they could

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<v Speaker 6>be feeding on and so there could be life there.

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<v Speaker 6>We don't know, but there could. Isn't that cool?

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<v Speaker 1>Yes, I mean, let me go get a scoop of this?

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<v Speaker 1>How do we find out?

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<v Speaker 6>Well, yeah, we need various missions, and so people have

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<v Speaker 6>tried to say, maybe we can look into the clouds

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<v Speaker 6>and see if there are geochemical indicators. There's nothing absolutely unique,

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<v Speaker 6>so some things that could be but that's not the

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<v Speaker 6>only way get a scoop. That hasn't been planned yet.

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<v Speaker 1>So the vapor cloak around Venus may hold the answer,

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<v Speaker 1>and by answer I mean aliens. Vicky says that there

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<v Speaker 1>are various missions whose sites are set in the clouds

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<v Speaker 1>and even going through the clouds and down to the

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<v Speaker 1>surface like kind of diving through whipped cream to get

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<v Speaker 1>into an ice cream Sunday, but one that is four

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<v Speaker 1>hundred and sixty four degrees celsius. We're a blistering eight

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<v Speaker 1>hundred and sixty seven degrees fahrenheit, But.

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<v Speaker 6>That would just be one shot and would just give

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<v Speaker 6>us kind of one pass. So but yeah, missions are

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<v Speaker 6>what we need to do to explore it. And that's

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<v Speaker 6>why we need more interest in Venus than perhaps.

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<v Speaker 1>Mars, which is where you come in.

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<v Speaker 6>Well, it's just such a fascinating planet. But fundamentally as

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<v Speaker 6>humans and for myself, what I really want to learn

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<v Speaker 6>about is Earth, and Venus has so much more to

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<v Speaker 6>teach us about the Earth than Mars does. And you

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<v Speaker 6>say why, because it is back to what you said,

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<v Speaker 6>it's about the same size, it's about the same density.

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<v Speaker 6>That means it's made up of generally the same materials.

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<v Speaker 6>It's a similar proximity to the Sun. And they were very,

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<v Speaker 6>very similar when they were born. I don't know if

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<v Speaker 6>you have sisters. I do, and you know we're similar.

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<v Speaker 6>Our photographs are interchangeable. Now we've gone completely different ways.

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<v Speaker 6>But Mars is this tiny little weenie bean. You know,

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<v Speaker 6>it's nothing like the Earth. You know, so size matters

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<v Speaker 6>in terms of how planets work, because that's how much

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<v Speaker 6>heat they have and how do they get rid of heat.

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<v Speaker 6>If you take a big potato, put it in the microwave,

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<v Speaker 6>it'll retain its heat for a long time. If you

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<v Speaker 6>take a little potato cool off really quickly. Well, the

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<v Speaker 6>way that that heat escapes is the mode of tectanism

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<v Speaker 6>and volcanism or tectonics, not to be confused with plate tectonics.

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<v Speaker 6>That's Earth's kind of tectonism. Venus has tectonics but not

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<v Speaker 6>plate tectonics. So you immediately say, well why not why

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<v Speaker 6>doesn't it have plate tectonics, or more why does Earth

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<v Speaker 6>have plate tectonics? And so we can learn so so

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<v Speaker 6>much more about Earth by studying Venus than we can Mars.

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<v Speaker 1>Well what is a tectonic and how is it different

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<v Speaker 1>than a plate tectonic?

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<v Speaker 6>Okay, so let's talk what plate tectonics is, because we

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<v Speaker 6>know what that is and tectonics be any other way.

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<v Speaker 6>So plate tectonics, we have plates on the surface. The

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<v Speaker 6>plates are made on the lithosphere rock sphere. Litho rock

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<v Speaker 6>rock sphere, the outer sphere of a planet. And what

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<v Speaker 6>that happens we can all do this with our hands,

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<v Speaker 6>is that lithosphere slides around and it can pull apart

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<v Speaker 6>and make new lithosphere. That's what Earth does at the

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<v Speaker 6>spreading centers, and then it can also subduct and recycle

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<v Speaker 6>that lithosphere. So how a planet cools is its tectonics.

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<v Speaker 6>We cool by sweating dogs put their bellies down on

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<v Speaker 6>the ground or pant right, and the Earth does it

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<v Speaker 6>by spreading and by subduction because this is a cold lithosphere.

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<v Speaker 6>And when I put it back down into that hot

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<v Speaker 6>mantles like taking your cold hand putting it on your

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<v Speaker 6>belly and you go, oh, that's going to cool me down.

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<v Speaker 6>So that's the way Earth cools. And then there's volcanism

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<v Speaker 6>that is associated with that. Volcanism as we spread the

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<v Speaker 6>plates apart, volcanism as we subduct one plate beneath the other.

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<v Speaker 6>So those are the plates. How Venus doesn't have plates.

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<v Speaker 1>So what's it doing?

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<v Speaker 6>So what's it doing? That's exactly right? And why do

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<v Speaker 6>we care? Well, Earth, it wasn't born with plate tectonics.

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<v Speaker 6>You don't start having plate tectonics, So we want to

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<v Speaker 6>know what did Earth do early on? Oh, well, Venus

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<v Speaker 6>doesn't have and I will say never did have. Now

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<v Speaker 6>some people say, oh, maybe it did in the past. Well,

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<v Speaker 6>all of the earliest rocks that we have that there's

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<v Speaker 6>a lot of debate on Venus, but most people agree

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<v Speaker 6>the earliest rocks are a kind of rock called tesra.

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<v Speaker 1>So a tesra is a weird geological formation. They look

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<v Speaker 1>kind of like creepy wrinkles in fabric, or these ribbons

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<v Speaker 1>of deep fissures and chasms. Sometimes they look like honeycombs

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<v Speaker 1>of domes and pits. And according to the twenty twenty

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<v Speaker 1>paper in the Journal Geology titled Venus Tessaie feature layered,

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<v Speaker 1>folded and eroded rocks, Tessai cover about eight percent of

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<v Speaker 1>the surface of Venus, and there's seen more run the

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<v Speaker 1>equator and some of the northern latitudes. They're usually the

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<v Speaker 1>oldest thing in their regions, are up to seven hundred

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<v Speaker 1>and fifty million years old, and scientists think they're caused

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<v Speaker 1>by volcanic activity.

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<v Speaker 6>They're very distinctive and we can map those out, and

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<v Speaker 6>when we map those out across the surface, they make

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<v Speaker 6>huge coherent global patterns, and they're the earliest record we have.

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<v Speaker 6>So if we can set that and say, okay, but

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<v Speaker 6>plate tectonics maybe happened after that, because that's the earliest record,

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<v Speaker 6>then when I subduct things, I'm removing parts of the surface,

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<v Speaker 6>and so I'm going to lose parts of that overall

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<v Speaker 6>coherent pattern. They're going to be dissected interrupted and we

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<v Speaker 6>don't see that. So I would say that's evidence that

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<v Speaker 6>Venus never had plate tectonics. So if you want to

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<v Speaker 6>say she had it, because Earthlings we love it. We

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<v Speaker 6>just want everyone to have plate tectonics. If you want

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<v Speaker 6>to say Venus had plate tectonics, then you have to say, well, yes,

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<v Speaker 6>she had it, but we just have no record of it,

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<v Speaker 6>and that's just not good science.

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<v Speaker 1>I also just want to note that there are so

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<v Speaker 1>many different formations that aren't even tessory on Venus's lithosphere

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<v Speaker 1>or the rockscape, her rockscape. But my favorite might be

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<v Speaker 1>this huge volcanic caldera with these fans of ridges extending

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<v Speaker 1>from it, and it's called the tick. It looks so

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<v Speaker 1>much like a tick. But yeah, if Venus had a

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<v Speaker 1>bunch of shifting plates on her surface, there would be

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<v Speaker 1>remnants of all that movement, but there isn't anything credible. Well,

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<v Speaker 1>what's on the surface. Let's say that I were to

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<v Speaker 1>get through those clouds, what does it even look like?

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<v Speaker 6>Yeah, so what it looks like is, first of all,

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<v Speaker 6>it's hot, okay, but it is there is no water,

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<v Speaker 6>there's no nasty biological layer at all, it's basically rock

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<v Speaker 6>everywhere that you look. Depending on where you are, you

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<v Speaker 6>could be huge flat open areas that if you were

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<v Speaker 6>to go into Kilauea and down onto the lava lake

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<v Speaker 6>there when it's not erupting, but expand that and look

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<v Speaker 6>around and just see that forever, you might see something

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<v Speaker 6>like that. But you might also land in huge mountain

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<v Speaker 6>range areas that the highest region on the planet is

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<v Speaker 6>higher than the highest region on Earth. Or you might

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<v Speaker 6>land actually in these relatively deep chasms, in which case

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<v Speaker 6>you would be sort of like in the Marianas Trench

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<v Speaker 6>on Earth, except not quite so deep. Other places, if

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<v Speaker 6>you're walking around on Tessra, which I would love to do,

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<v Speaker 6>you're going to be in these just at a much

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<v Speaker 6>smaller scale. But consider your fingers. With ridges and troughs

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<v Speaker 6>and ridges and troughs and ridges and truughs that would

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<v Speaker 6>be steep drops. You could walk along the ridge, but

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<v Speaker 6>you would drop into a trough, and as far as

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<v Speaker 6>you can see, that's what you would see, incredibly incredibly varied.

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<v Speaker 6>Other places, you might be on extensive lava flows like

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<v Speaker 6>Pahoihuai flows that are on Hawaii, but go for much, much,

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<v Speaker 6>much further distances. So on the surface there's all these

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<v Speaker 6>amazing features to see, but no biology, no water, and

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<v Speaker 6>you would have impact craters, absolutely pristinely preserved impact craters

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<v Speaker 6>relative to earther Mars.

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<v Speaker 1>Well, so it has active volcanoes, I would say, yes, Okay,

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<v Speaker 1>we are getting more and more evidence that there are

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<v Speaker 1>huge volcanic features.

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<v Speaker 6>I think most of us at this point would be

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<v Speaker 6>really surprised if they weren't active, and there's enough tantalizing

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<v Speaker 6>data to say, yeah, we probably have active volcanism. There

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<v Speaker 6>are these regions that are called volcanic rises, and they

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<v Speaker 6>are huge provinces. If we take one volcanic rise, it

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<v Speaker 6>would cover all of Australia, No, all of Australia. It's

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<v Speaker 6>probably formed in the similar way to Hawaii, of a

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<v Speaker 6>massive plume underneath that lithosphere. But because on Earth, here

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<v Speaker 6>comes the plume and the lithosphere moves across, So Hawaii

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<v Speaker 6>makes these chains of volcanoes right m But on Venus

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<v Speaker 6>the plates don't move. There aren't plates. It's like a

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<v Speaker 6>one plate planet, and so the plume sits there and

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<v Speaker 6>it bows up the surface, actually much much higher, just

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<v Speaker 6>because when things are hotter, they expand, including the rock,

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<v Speaker 6>so it bows it way up. But there you have

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<v Speaker 6>massive flows that we see on the surface, rock flows

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<v Speaker 6>that are all volcanic flows. You can look at those

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<v Speaker 6>and go, oh my god. You know, it doesn't take

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<v Speaker 6>a geologist to say, these are amazing volcanic flows that

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<v Speaker 6>go for tens and tens and hundreds of miles. Now,

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<v Speaker 6>are they active today? It'd be pretty hard to say

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<v Speaker 6>they're not, because that heat source is still there. Now,

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<v Speaker 6>did it happen yesterday? Well no, but geologically is it active?

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<v Speaker 6>I bet my life on it.

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<v Speaker 1>Well, okay, you told me that way back when you

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<v Speaker 1>first started studying this, there were a few of you

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<v Speaker 1>in a room.

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<v Speaker 6>Right yeah, about there were sixty two one hundred people,

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<v Speaker 6>that's pretty much who studied venus, and I was new.

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<v Speaker 6>Like people went around and said, where did you come from?

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<v Speaker 6>Because no one knew me from anything except my one

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<v Speaker 6>colleague at Southern Methodist University at the time, in his students.

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<v Speaker 1>And now when they say where did you come from?

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<v Speaker 1>Did you tell them Caltech Capacadya.

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<v Speaker 6>No. They would go through that and they would say,

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<v Speaker 6>you weren't just so and so students, You weren't just

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<v Speaker 6>so and so students, you weren't just so and so

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<v Speaker 6>to it. I was a young professor, but I spent

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<v Speaker 6>my entire career on Earth and just absolute serendipitously ended

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<v Speaker 6>up on Venus. It was a holiday party. I'm talking

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<v Speaker 6>to grad students and postdocs of my colleague Roger Phillips,

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<v Speaker 6>and they're saying, this mission is going to Venus, and

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<v Speaker 6>I I was just making polite conversation. I'm not interested

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<v Speaker 6>in Venus. I can't find it in the sky. But

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<v Speaker 6>so I say, tell me about it. So they did,

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<v Speaker 6>and they said, well, Venus is a planet that we

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<v Speaker 6>think has a strong weak, strong relogy of this layer.

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<v Speaker 6>And I thought that's fascinating, because that's like continental crust,

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<v Speaker 6>and to think a whole planet of that. I don't

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<v Speaker 6>think that is the case now, but I said, that

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<v Speaker 6>would be amazing to have a whole planet like that.

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<v Speaker 6>And then they said, and we have places like mid

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<v Speaker 6>ocean ridges on the Earth, and I said, those two

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<v Speaker 6>can't be true. Those two views of Venus are in

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<v Speaker 6>contradiction because if you pull apart layers that are strong

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<v Speaker 6>week strong, which the Earth has done in the Southwest Desert,

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<v Speaker 6>we get something called metamorphic core complex. We don't get

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<v Speaker 6>a mid ocean spreading center. So they said really, and

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<v Speaker 6>I said, yeah, it's just relogy. Relogy is the study

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<v Speaker 6>of flow. You know, how do things bend, break and fold?

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<v Speaker 6>They said, you have to talk to Roger. So I

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<v Speaker 6>went and talked to Roger and that started my thing

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<v Speaker 6>on Venus. And then as a grad student and I

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<v Speaker 6>wrote a proposal to NASA and it was funded and

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<v Speaker 6>we said, oh my goodness, okay, and it was just

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<v Speaker 6>going to be a one time thing, but it's been

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<v Speaker 6>so fascinating that I can't pull away.

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<v Speaker 1>You stuck around.

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<v Speaker 6>I stuck around. I stuck around. And then after that

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<v Speaker 6>was when I learned that, oh my gosh, Venus is

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<v Speaker 6>who's going to tell me about early Earth, which is

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<v Speaker 6>what I am really interested in. And Venus has a

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<v Speaker 6>record of early Venus. Earth doesn't because it's been destroyed

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<v Speaker 6>by plate tectonics. Oh, go back to the baby books.

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<v Speaker 6>Venus never develop plate tectonics, and we have this beautiful

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<v Speaker 6>record through radar of her surface, like nothing like what

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<v Speaker 6>we have of Earth. And so if I learned to

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<v Speaker 6>read Venus's baby book, I can stand those in for Earth.

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<v Speaker 6>I'm I'm the middle of five kids, but I had

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<v Speaker 6>two older sisters. Well there are no baby pictures of

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00:22:23.400 --> 00:22:26.000
<v Speaker 6>me because there my sisters by the time it got

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<v Speaker 6>to me, and they're like, okay, just use this one,

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00:22:28.160 --> 00:22:32.559
<v Speaker 6>you know, And that works. So Earth and Venus they're

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00:22:32.599 --> 00:22:37.079
<v Speaker 6>probably interchangeable or not interchangeable. But Venus has a lot

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<v Speaker 6>to tell us, and she's preserved her baby book. Earth

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00:22:40.440 --> 00:22:41.279
<v Speaker 6>is ripped it apart.

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<v Speaker 1>I love her. I love her. Oh so what was

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<v Speaker 1>it about Earth that got you down that path? At

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00:22:49.799 --> 00:22:52.599
<v Speaker 1>what point were you like, I want to be a geologist.

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<v Speaker 1>I want to be a planetary scientist. Yes, so pretty.

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<v Speaker 6>Silly more more sarendifit. I was at Carlton College. I

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00:23:02.839 --> 00:23:06.759
<v Speaker 6>was a chemistry major and doing art on the side,

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<v Speaker 6>and a friend and I geology and chemistry shared the

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<v Speaker 6>same building, and we thought the geology students looked like

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<v Speaker 6>they were having a lot more fun than we was chemist.

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<v Speaker 6>So Sandra and I decided to take a geology class

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<v Speaker 6>and it was full. So the professor said, well, you

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<v Speaker 6>can only take it if you're thinking about majoring. So

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<v Speaker 6>of course we lied. We had no intention of majoring,

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00:23:30.839 --> 00:23:34.599
<v Speaker 6>but we just said, oh, yes, yes, we're thinking about majoring.

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<v Speaker 6>In it. Well, Lynn Tennyson, the professor, she got the

401
00:23:38.799 --> 00:23:43.200
<v Speaker 6>last laugh because both Sandra and I were just smitten

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<v Speaker 6>with it. Sandra went on to be a geochemist and

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<v Speaker 6>I went on to do geology, but more of structural geology,

404
00:23:53.519 --> 00:23:55.720
<v Speaker 6>which is how things bend, breaking fold, more of a

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<v Speaker 6>physics and mechanics of it.

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<v Speaker 1>Did you keep in touch with that professor to say,

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<v Speaker 1>like you converted us?

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00:24:02.240 --> 00:24:05.799
<v Speaker 6>You know, she went back to industry, but I did say,

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<v Speaker 6>you know, Lynn, you got the last laugh because.

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<v Speaker 1>Here we are are you. I have a friend. She's

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<v Speaker 1>a planetary geologist and she her name is Racal, which

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00:24:17.839 --> 00:24:21.960
<v Speaker 1>is fun because her nickname was Rocky. Yeah, growing man,

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<v Speaker 1>Oh that's incredible. We had her on for the Selenology

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<v Speaker 1>Moon episode.

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<v Speaker 6>Oh fun.

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<v Speaker 1>She's wonderful. But she was saying that she always tricks

417
00:24:33.000 --> 00:24:36.319
<v Speaker 1>her husband into going on vacations where there's a lot

418
00:24:36.359 --> 00:24:36.839
<v Speaker 1>of rocks.

419
00:24:37.680 --> 00:24:41.799
<v Speaker 6>That's great. Well, and our family we have two kids

420
00:24:41.799 --> 00:24:44.759
<v Speaker 6>who are now adults, but they would say, can we

421
00:24:44.799 --> 00:24:48.960
<v Speaker 6>go on a vacation where there's no geology? Because my

422
00:24:49.039 --> 00:24:52.119
<v Speaker 6>husband and I are both geologists, we said, sure, you

423
00:24:52.200 --> 00:24:55.599
<v Speaker 6>come up with it and that's where we'll go. So

424
00:24:55.839 --> 00:24:58.799
<v Speaker 6>they got their heads together and they decided on Iceland,

425
00:25:00.160 --> 00:25:03.920
<v Speaker 6>which has a lot of geology. We went to Iceland.

426
00:25:04.000 --> 00:25:06.200
<v Speaker 6>We all had a great time. But they never complained

427
00:25:06.240 --> 00:25:10.799
<v Speaker 6>about going on vacations. There wasn't any geology.

428
00:25:10.640 --> 00:25:16.720
<v Speaker 1>They had some great geology, exactly. Jokes on that, right, yep. Well,

429
00:25:16.880 --> 00:25:18.599
<v Speaker 1>what can you tell me a little bit about the

430
00:25:18.640 --> 00:25:23.200
<v Speaker 1>missions to Venus? Like I don't know much about Magellan,

431
00:25:23.279 --> 00:25:24.799
<v Speaker 1>Like I'm a blank slate here.

432
00:25:24.880 --> 00:25:28.559
<v Speaker 6>Okay, So Magell. So first there were missions where they

433
00:25:28.559 --> 00:25:32.680
<v Speaker 6>were looking at radar, but not very high quality, okay.

434
00:25:32.799 --> 00:25:36.480
<v Speaker 6>And then the Russians Soviets excuse me, actually put some

435
00:25:36.640 --> 00:25:40.359
<v Speaker 6>landers down on the surface of Venia and that that's

436
00:25:40.400 --> 00:25:43.160
<v Speaker 6>really pretty amazing because they did that in the nineteen

437
00:25:43.440 --> 00:25:44.839
<v Speaker 6>sixties and seventies.

438
00:25:44.920 --> 00:25:48.880
<v Speaker 1>Oh, just a quick aside here. Between nineteen sixty one

439
00:25:48.960 --> 00:25:52.079
<v Speaker 1>and nineteen eighty four, the Soviet Union launched a series

440
00:25:52.079 --> 00:25:56.319
<v Speaker 1>of thirteen space probes within their Veniera missions, and ten

441
00:25:56.440 --> 00:26:01.200
<v Speaker 1>probes landed on the surface of Venus. They lasted a flash.

442
00:26:01.319 --> 00:26:04.480
<v Speaker 1>The longest visit was two hours and the shortest was

443
00:26:04.599 --> 00:26:07.839
<v Speaker 1>twenty three minutes. All that work for twenty three minutes,

444
00:26:07.880 --> 00:26:11.720
<v Speaker 1>but the program yielded a bunch of firsts in space exploration,

445
00:26:11.799 --> 00:26:17.160
<v Speaker 1>including images and sounds from the surface of another planet

446
00:26:17.400 --> 00:26:22.240
<v Speaker 1>and high res radar scans. Also fun facts. Vaniera shares

447
00:26:22.279 --> 00:26:25.279
<v Speaker 1>the same root word as the verb to venerate or

448
00:26:25.279 --> 00:26:29.799
<v Speaker 1>to regard very highly, coming from Venus, the goddess of love.

449
00:26:30.480 --> 00:26:33.559
<v Speaker 1>So does venereal disease. And if your ears just perked up,

450
00:26:33.599 --> 00:26:36.119
<v Speaker 1>you can stay tuned for an entire episode on sexually

451
00:26:36.119 --> 00:26:40.720
<v Speaker 1>transmitted infections, which is coming very soon anyway, Yes, Vaniera missions.

452
00:26:40.319 --> 00:26:45.000
<v Speaker 6>Those were really incredible because even today with the technology

453
00:26:45.000 --> 00:26:47.400
<v Speaker 6>if we have, if we land something on the surface

454
00:26:47.400 --> 00:26:51.200
<v Speaker 6>of Venus, given the horrid conditions, it wouldn't last a

455
00:26:51.200 --> 00:26:54.359
<v Speaker 6>week and probably a couple of days wow at most

456
00:26:54.480 --> 00:26:57.400
<v Speaker 6>at most, and that's with new technology. But the Magellan

457
00:26:57.440 --> 00:27:01.799
<v Speaker 6>mission was an amazing mission. It was the first NASA

458
00:27:01.960 --> 00:27:05.720
<v Speaker 6>all digital mission just across NASA. But what it did

459
00:27:06.200 --> 00:27:10.519
<v Speaker 6>was had collected four data sets, three of which were

460
00:27:10.559 --> 00:27:13.599
<v Speaker 6>extremely useful and they're all global. The first is the

461
00:27:13.720 --> 00:27:18.160
<v Speaker 6>radar synthetic aperture radar, and it's the highest resolution. We

462
00:27:18.319 --> 00:27:21.839
<v Speaker 6>have ninety eight percent of the planet covered in one

463
00:27:21.960 --> 00:27:25.720
<v Speaker 6>hundred meters per pixel resolution, a lot. To put that

464
00:27:25.759 --> 00:27:28.920
<v Speaker 6>in perspective, we have no data set like that on Earth,

465
00:27:29.200 --> 00:27:31.880
<v Speaker 6>none like on our planet. And you say, well, why

466
00:27:31.920 --> 00:27:36.920
<v Speaker 6>not because the radar doesn't see well through the oceans,

467
00:27:37.359 --> 00:27:40.359
<v Speaker 6>and two thirds of our planet is ocean, and so

468
00:27:40.440 --> 00:27:45.720
<v Speaker 6>we know very very little about the ocean floors. Actually,

469
00:27:46.200 --> 00:27:48.960
<v Speaker 6>we have a better data set of Venus, and that's incredible.

470
00:27:49.480 --> 00:27:52.839
<v Speaker 6>When we first got it, the computers that we're dealing

471
00:27:52.880 --> 00:27:56.400
<v Speaker 6>with right now didn't exist. But now really anyone with

472
00:27:56.440 --> 00:27:59.160
<v Speaker 6>a web connection can pull up and look at those images,

473
00:27:59.200 --> 00:28:02.279
<v Speaker 6>and anyone can study them, and anyone can put their

474
00:28:02.319 --> 00:28:05.039
<v Speaker 6>two cents in, which is really really good for science

475
00:28:05.160 --> 00:28:08.759
<v Speaker 6>and is why there's been much more interest in it

476
00:28:08.839 --> 00:28:10.319
<v Speaker 6>because of the accessibility of that.

477
00:28:10.640 --> 00:28:12.559
<v Speaker 1>Just some quick definitions in case you feel kind of

478
00:28:12.559 --> 00:28:15.880
<v Speaker 1>lost in the darkness of space here. So altimetry think

479
00:28:16.039 --> 00:28:20.240
<v Speaker 1>altitude for height is just the measurements of height of objects.

480
00:28:20.279 --> 00:28:23.960
<v Speaker 1>And to measure the highs and lows of this Venusian terrain,

481
00:28:24.400 --> 00:28:28.000
<v Speaker 1>planetary geologists use radar, where this pulse of microwave energy

482
00:28:28.119 --> 00:28:30.039
<v Speaker 1>is sent to the surface of the planet at a

483
00:28:30.079 --> 00:28:33.480
<v Speaker 1>slight angle, and then the amount of energy that reflects

484
00:28:33.519 --> 00:28:36.039
<v Speaker 1>back can tell us about what it's hitting down there,

485
00:28:36.160 --> 00:28:38.839
<v Speaker 1>and they can also process that data for higher resolution,

486
00:28:39.000 --> 00:28:42.920
<v Speaker 1>which is called synthetic aperture radar, and there are files

487
00:28:42.960 --> 00:28:46.240
<v Speaker 1>accessible to the public via NASA's Open Data Portal, which

488
00:28:46.240 --> 00:28:50.079
<v Speaker 1>has various types of measurements and info in addition to

489
00:28:50.119 --> 00:28:51.359
<v Speaker 1>those collected by radar.

490
00:28:51.559 --> 00:28:55.400
<v Speaker 6>So the radar data. Then there is the topography data

491
00:28:55.480 --> 00:28:58.359
<v Speaker 6>or called ltimetry, but that's the shape of the surface.

492
00:28:58.759 --> 00:29:02.640
<v Speaker 6>It's lower resolution, but it too is global and we

493
00:29:02.680 --> 00:29:06.240
<v Speaker 6>can tell a lot about the topography. So on Venus

494
00:29:06.240 --> 00:29:10.480
<v Speaker 6>we have some very high regions that have volcanic features

495
00:29:10.519 --> 00:29:12.319
<v Speaker 6>all across the surface, and we can say, oh, those

496
00:29:12.359 --> 00:29:15.799
<v Speaker 6>are young because they sit high because of the heat

497
00:29:15.799 --> 00:29:18.519
<v Speaker 6>beneath them. And the topography is such that at a

498
00:29:18.559 --> 00:29:21.519
<v Speaker 6>broad scale it's very gentle. And that's what heat does

499
00:29:21.839 --> 00:29:24.680
<v Speaker 6>to make something, because it transfers. If I'm a hot

500
00:29:24.720 --> 00:29:26.799
<v Speaker 6>body and a cold body, then I'm going to see

501
00:29:26.799 --> 00:29:29.240
<v Speaker 6>a gradient from hot to cold, which means I'm going

502
00:29:29.279 --> 00:29:32.720
<v Speaker 6>to see a gradient in my topography. On Venus, we

503
00:29:32.920 --> 00:29:36.039
<v Speaker 6>refer everything to mean planetary radius.

504
00:29:36.440 --> 00:29:38.400
<v Speaker 1>What does that mean? On Earth we.

505
00:29:38.440 --> 00:29:41.759
<v Speaker 6>Refer everything to sea level. Yes, we don't have any water.

506
00:29:42.000 --> 00:29:46.200
<v Speaker 6>We don't have any water on Venus. And also Venus

507
00:29:46.319 --> 00:29:51.440
<v Speaker 6>is almost a perfect sphere So Earth is an oblate spheroid. Okay,

508
00:29:51.640 --> 00:29:54.400
<v Speaker 6>it's got a big bulge at its belly, at its equator.

509
00:29:54.680 --> 00:29:57.240
<v Speaker 6>And why does it have that Because the interior is

510
00:29:57.279 --> 00:29:59.880
<v Speaker 6>a little sloshy and it's spinning.

511
00:30:00.119 --> 00:30:04.279
<v Speaker 1>Okay, yeah, so Earth is like a gusher in the center,

512
00:30:04.519 --> 00:30:07.839
<v Speaker 1>spinning relatively fast. The Venus not so much.

513
00:30:08.240 --> 00:30:12.759
<v Speaker 6>Venus, its interior is probably still a little sloshy. But

514
00:30:13.000 --> 00:30:18.839
<v Speaker 6>she rotates so slowly. So in fact, on Venus, her

515
00:30:19.200 --> 00:30:23.400
<v Speaker 6>day is longer than her year. A day is how

516
00:30:23.440 --> 00:30:26.799
<v Speaker 6>long it takes to go on. It's at doing rotation.

517
00:30:27.519 --> 00:30:29.440
<v Speaker 6>Just knocked down the microphone. I get so excited.

518
00:30:31.440 --> 00:30:34.799
<v Speaker 1>I love it, Honestly, her excitement about Venus makes me

519
00:30:34.920 --> 00:30:38.480
<v Speaker 1>feel like Venus is a friend. Now. It's a beautiful delusion.

520
00:30:38.839 --> 00:30:42.920
<v Speaker 6>And what's a year? It's the trip around the sun.

521
00:30:43.359 --> 00:30:46.960
<v Speaker 6>So Venus rotates so slowly. Because she rotates so slowly,

522
00:30:47.400 --> 00:30:51.519
<v Speaker 6>she maintains a perfect sphere. She's just all, you know, perfectly.

523
00:30:51.640 --> 00:30:54.279
<v Speaker 6>Her doo is not must at all, right, she's not

524
00:30:54.359 --> 00:30:57.079
<v Speaker 6>going to smash at the equator.

525
00:30:58.440 --> 00:31:01.359
<v Speaker 1>So a day is long than a year, So that

526
00:31:01.440 --> 00:31:05.559
<v Speaker 1>means it's in darkness and light for so long.

527
00:31:05.400 --> 00:31:08.400
<v Speaker 6>Right, yes, for so long? Exactly.

528
00:31:08.880 --> 00:31:11.640
<v Speaker 1>So, yes, you will circle the sun and have another

529
00:31:11.799 --> 00:31:15.480
<v Speaker 1>birthday before the day ends. This is great if you

530
00:31:15.640 --> 00:31:18.559
<v Speaker 1>like cake. This is not good if you're just having

531
00:31:18.559 --> 00:31:21.480
<v Speaker 1>a random bad day, or if you have a five

532
00:31:21.599 --> 00:31:24.400
<v Speaker 1>day work week. Then so let's say that you were

533
00:31:24.440 --> 00:31:27.880
<v Speaker 1>to beam me down on the surface. It would the

534
00:31:28.000 --> 00:31:31.480
<v Speaker 1>rocks would look like, are they grayish? Are they big?

535
00:31:31.519 --> 00:31:34.759
<v Speaker 1>Would it smell farty because of the sulfur.

536
00:31:34.799 --> 00:31:37.839
<v Speaker 6>Well, yeah it would be, but you probably couldn't smell

537
00:31:37.880 --> 00:31:41.559
<v Speaker 6>because your nose won't work because it's nine hundred degrees. Yeah,

538
00:31:41.599 --> 00:31:43.799
<v Speaker 6>so take your oven, you know, and turn it out

539
00:31:43.880 --> 00:31:47.640
<v Speaker 6>so it would rain sulfuric acid. I mean, I've worked

540
00:31:47.680 --> 00:31:50.319
<v Speaker 6>with the lab. I don't think that smells like sulfur does,

541
00:31:50.960 --> 00:31:53.079
<v Speaker 6>so I don't know about the smells.

542
00:31:53.759 --> 00:31:57.440
<v Speaker 1>So this has been a hot ghastly debated a bit,

543
00:31:57.640 --> 00:32:01.680
<v Speaker 1>and I floated through data on this science of interplanetary

544
00:32:01.680 --> 00:32:05.359
<v Speaker 1>fart smells here on Earth emanating from your very bowels.

545
00:32:05.480 --> 00:32:09.039
<v Speaker 1>You can blame hydrogen sulfides for necessitating rolling down a

546
00:32:09.039 --> 00:32:12.960
<v Speaker 1>car window, but sulfuric acid itself, also known oddly as

547
00:32:13.039 --> 00:32:17.279
<v Speaker 1>oil of vitriol, in its pure state, is colorless and odorless,

548
00:32:17.680 --> 00:32:22.559
<v Speaker 1>so would meeting with the albeit scant water vapor in

549
00:32:22.599 --> 00:32:28.079
<v Speaker 1>the clouds cause stinky hydrogen sulfide. I don't know. There

550
00:32:28.119 --> 00:32:31.279
<v Speaker 1>are several pop science articles saying that, yeah, Mars and

551
00:32:31.400 --> 00:32:34.640
<v Speaker 1>Venus stink like toots. But I also went onto Blue

552
00:32:34.640 --> 00:32:36.839
<v Speaker 1>Sky to ask a bevy of smart people about this

553
00:32:37.160 --> 00:32:40.000
<v Speaker 1>posting any chemist friends here, I have a gaseous question.

554
00:32:40.319 --> 00:32:42.759
<v Speaker 1>If you had sulfuric acid in the clouds of a

555
00:32:42.799 --> 00:32:45.759
<v Speaker 1>planet as well as scant water vapor, would the process

556
00:32:45.759 --> 00:32:49.839
<v Speaker 1>of dissociation create hydrogen sulfide and thus would it smell

557
00:32:49.880 --> 00:32:52.480
<v Speaker 1>like farts? Just doing some fact checking here, to which

558
00:32:52.519 --> 00:32:56.519
<v Speaker 1>tot's Grodi responded, more like fart checking true. But then

559
00:32:56.680 --> 00:32:59.640
<v Speaker 1>doctor Michelle Frankel, a professor of chemistry and author of

560
00:32:59.640 --> 00:33:02.839
<v Speaker 1>the books Deeped about the science of tea, replied, I

561
00:33:02.839 --> 00:33:08.480
<v Speaker 1>think it's usually sulfur dioxide to sulfuric acid and oxidation process,

562
00:33:08.759 --> 00:33:11.279
<v Speaker 1>and you can have a reducing atmosphere, but I don't

563
00:33:11.279 --> 00:33:15.160
<v Speaker 1>think they're generally strong enough to reduce sulfate to sulfide.

564
00:33:15.240 --> 00:33:18.440
<v Speaker 1>And then this assistant professor of organic chemistry, doctor Patrick Lutz,

565
00:33:18.519 --> 00:33:21.519
<v Speaker 1>told me that water is neither reducing nor oxidizing in

566
00:33:21.559 --> 00:33:24.720
<v Speaker 1>this specific scenario, So I don't think it would be farty,

567
00:33:24.960 --> 00:33:29.240
<v Speaker 1>but Jack adly noted, despite whatever chemistry, the rankness wouldn't

568
00:33:29.319 --> 00:33:32.480
<v Speaker 1>hit you because your sense of smell is unlikely to

569
00:33:32.559 --> 00:33:35.720
<v Speaker 1>function in the kind of atmosphere that would support this scenario.

570
00:33:36.200 --> 00:33:39.960
<v Speaker 1>So if a sulfur sulfur's in the vapor and no

571
00:33:40.000 --> 00:33:42.839
<v Speaker 1>one is there to smell it, does it make a stink?

572
00:33:43.079 --> 00:33:46.559
<v Speaker 1>A last smell is in the nose of the beholder. Now,

573
00:33:46.599 --> 00:33:48.599
<v Speaker 1>in light of that, how about the beauty.

574
00:33:49.160 --> 00:33:52.559
<v Speaker 6>The lighting would be very different because the sun is

575
00:33:52.599 --> 00:33:56.440
<v Speaker 6>coming through these very thick clouds, but you would have

576
00:33:56.640 --> 00:34:01.200
<v Speaker 6>lots of daylight or not. And it probably wouldn't be

577
00:34:01.359 --> 00:34:06.960
<v Speaker 6>very windy because the wind is basically by pressure differentials,

578
00:34:06.960 --> 00:34:10.360
<v Speaker 6>which are temperature differentials. And so when we think about

579
00:34:10.440 --> 00:34:14.719
<v Speaker 6>the overall broad global cycles of the winds on Earth,

580
00:34:14.960 --> 00:34:18.360
<v Speaker 6>they're driven by the suns is much more intense at

581
00:34:18.400 --> 00:34:22.159
<v Speaker 6>the equatorial regions than going north and on Venus. With

582
00:34:22.239 --> 00:34:26.800
<v Speaker 6>this blanket, it's probably a pretty similar temperature. As you

583
00:34:26.840 --> 00:34:30.119
<v Speaker 6>go polar it will be somewhat different, but not greatly.

584
00:34:30.239 --> 00:34:35.239
<v Speaker 6>Because of that surface, the rocks will probably look sort

585
00:34:35.239 --> 00:34:38.920
<v Speaker 6>of dark black. We don't really know, but we think

586
00:34:39.000 --> 00:34:43.000
<v Speaker 6>that they're mostly of basaltic rocks, which on Earth, if

587
00:34:43.039 --> 00:34:45.039
<v Speaker 6>we want to just pick out two rocks, we would

588
00:34:45.079 --> 00:34:48.360
<v Speaker 6>say granite, which are a lighter colored rock that we

589
00:34:48.400 --> 00:34:52.719
<v Speaker 6>associate with the continents and continental crust, and basalts, which

590
00:34:53.000 --> 00:34:55.960
<v Speaker 6>are what we would see in Hawaii or the ocean

591
00:34:56.079 --> 00:35:02.119
<v Speaker 6>floor below the sediments. And we think that Venus mostly basaltic,

592
00:35:02.559 --> 00:35:06.360
<v Speaker 6>but there's probably granitic type rocks. They may not be

593
00:35:06.480 --> 00:35:09.239
<v Speaker 6>at the surface because granite has a hard time getting

594
00:35:09.280 --> 00:35:11.400
<v Speaker 6>to the surface. It mostly gets stuck at depth.

595
00:35:12.039 --> 00:35:15.360
<v Speaker 1>And so is there a huge temperature difference on one

596
00:35:15.400 --> 00:35:16.639
<v Speaker 1>side of Venus versus the other.

597
00:35:17.039 --> 00:35:20.559
<v Speaker 6>That's a good question, and I've heard this debated, and

598
00:35:21.079 --> 00:35:24.480
<v Speaker 6>it's not at all like Mars. Mars is a huge

599
00:35:24.599 --> 00:35:30.000
<v Speaker 6>temperature difference because there's basically no very little atmosphere to

600
00:35:30.079 --> 00:35:32.320
<v Speaker 6>keep you warm, and that's what the atmosphere is, like

601
00:35:32.360 --> 00:35:35.159
<v Speaker 6>a big down comforter Okay and on Earth we have

602
00:35:35.199 --> 00:35:38.440
<v Speaker 6>a pretty nice down comforter. Venus has a you know

603
00:35:38.599 --> 00:35:44.000
<v Speaker 6>down comforter on steroids, it's very warm. And so I

604
00:35:44.039 --> 00:35:47.559
<v Speaker 6>think that there is some temperature difference. I don't know

605
00:35:47.599 --> 00:35:50.239
<v Speaker 6>what that is. People would and what it would be

606
00:35:50.320 --> 00:35:54.280
<v Speaker 6>postulated to be. But then you have to say, you know,

607
00:35:54.400 --> 00:35:57.000
<v Speaker 6>there you are in darkness for so long as you said,

608
00:35:57.000 --> 00:35:59.079
<v Speaker 6>because your days and nights are much longer.

609
00:35:59.719 --> 00:36:02.400
<v Speaker 1>Because remember, Venus does a whole circle around the Sun

610
00:36:02.480 --> 00:36:05.679
<v Speaker 1>a year, and the equivalent of seven or so months

611
00:36:05.719 --> 00:36:08.199
<v Speaker 1>on Earth or two hundred and twenty five days, but

612
00:36:08.320 --> 00:36:11.360
<v Speaker 1>it spins so slowly that it takes two hundred and

613
00:36:11.400 --> 00:36:15.159
<v Speaker 1>forty three Earth days to go from dawn until the

614
00:36:15.199 --> 00:36:15.719
<v Speaker 1>next dawn.

615
00:36:16.280 --> 00:36:19.079
<v Speaker 6>But then the other thing is is if you were

616
00:36:19.119 --> 00:36:22.760
<v Speaker 6>to touch the surface, the surface would be much much

617
00:36:22.840 --> 00:36:26.000
<v Speaker 6>warmer than here, so it's going to be giving off

618
00:36:26.039 --> 00:36:30.519
<v Speaker 6>heat into beneath that blanket. But at a human scale,

619
00:36:30.599 --> 00:36:34.400
<v Speaker 6>it would just all be pretty hotter than be Jesus.

620
00:36:34.320 --> 00:36:37.679
<v Speaker 1>Yeah, it wouldn't be like going under a sun umbrella

621
00:36:37.920 --> 00:36:38.719
<v Speaker 1>versus standing.

622
00:36:39.000 --> 00:36:41.400
<v Speaker 6>Yes, not like that, Yeah, not like that at all.

623
00:36:41.639 --> 00:36:44.000
<v Speaker 1>So gravity data also tells us a lot about a

624
00:36:44.039 --> 00:36:46.800
<v Speaker 1>space object, and according to this twenty twenty five paper

625
00:36:46.840 --> 00:36:50.519
<v Speaker 1>in the Planetary Science Journal titled Mapping Venus's gravity field

626
00:36:50.519 --> 00:36:54.280
<v Speaker 1>with a Feritest mission, this planned twenty thirty one mission

627
00:36:54.599 --> 00:36:56.840
<v Speaker 1>seeks to improve the data that we have on this

628
00:36:57.039 --> 00:37:01.239
<v Speaker 1>using quote a key onboard element for the expeeriment called

629
00:37:01.360 --> 00:37:05.880
<v Speaker 1>the Integrated Deep Space Transponder. Sounds like sci fi, it's

630
00:37:05.960 --> 00:37:08.360
<v Speaker 1>real stuff. So it's kind of like when your friend

631
00:37:08.599 --> 00:37:11.320
<v Speaker 1>has a kid and they send out the announcement with

632
00:37:11.440 --> 00:37:14.559
<v Speaker 1>like the weight and the inches and a photo. We

633
00:37:14.599 --> 00:37:17.400
<v Speaker 1>want as many details as possible. I would like to

634
00:37:17.480 --> 00:37:18.320
<v Speaker 1>see the baby.

635
00:37:18.840 --> 00:37:21.519
<v Speaker 6>Another thing about the surface that is just so fun.

636
00:37:22.079 --> 00:37:25.960
<v Speaker 6>So thanks to a past graduate student, we can take

637
00:37:26.000 --> 00:37:29.760
<v Speaker 6>that topography data, that altimetry data and put it together

638
00:37:30.000 --> 00:37:33.920
<v Speaker 6>with the radar data, which is like like black and

639
00:37:33.920 --> 00:37:36.159
<v Speaker 6>white photos of the surface, and we can put on

640
00:37:36.239 --> 00:37:39.400
<v Speaker 6>red blue glasses and then you can see three D

641
00:37:40.440 --> 00:37:44.719
<v Speaker 6>of the surface. And with our technology today you can

642
00:37:44.800 --> 00:37:48.000
<v Speaker 6>zoom around and actually be like you have endless helicopter

643
00:37:48.079 --> 00:37:51.800
<v Speaker 6>time flying around in these things. And you can do

644
00:37:51.920 --> 00:37:55.440
<v Speaker 6>this for for public talks. It's just so fun. You know,

645
00:37:55.480 --> 00:37:57.800
<v Speaker 6>have people put on the red blue glasses and you can,

646
00:37:58.159 --> 00:38:00.480
<v Speaker 6>you know, show them. So I would have to beam

647
00:38:00.519 --> 00:38:02.719
<v Speaker 6>you down. I'd say, here, we are a whole group,

648
00:38:02.840 --> 00:38:05.239
<v Speaker 6>let's all go to Venus and now let's go over here,

649
00:38:05.280 --> 00:38:06.280
<v Speaker 6>and now let's go over here.

650
00:38:06.480 --> 00:38:08.639
<v Speaker 1>Vicky was doing this for a talk to a general

651
00:38:08.639 --> 00:38:10.880
<v Speaker 1>audience into luth and she says she loves talking about

652
00:38:10.920 --> 00:38:13.079
<v Speaker 1>venus to the public because they have great questions.

653
00:38:13.440 --> 00:38:16.400
<v Speaker 6>So at the end of this talk, this little girl

654
00:38:16.480 --> 00:38:21.320
<v Speaker 6>comes up afterwards and she says, so I want to know.

655
00:38:22.039 --> 00:38:26.760
<v Speaker 6>So there's some really really steep, steep, steep slopes and

656
00:38:26.760 --> 00:38:29.280
<v Speaker 6>it'd be like being in the Marianna's Trench in a sense,

657
00:38:29.360 --> 00:38:31.840
<v Speaker 6>not quite that, but that's a big drop. And she says,

658
00:38:32.159 --> 00:38:35.360
<v Speaker 6>if I was up here, and if I jumped off

659
00:38:35.880 --> 00:38:39.960
<v Speaker 6>and went all the way down, and we're talking miles,

660
00:38:40.480 --> 00:38:43.559
<v Speaker 6>she said, how long would it take me to fall?

661
00:38:43.599 --> 00:38:45.000
<v Speaker 6>And first I was all I was like, well, we

662
00:38:45.039 --> 00:38:46.559
<v Speaker 6>have to talk to your mom. This sounds like a

663
00:38:46.559 --> 00:38:50.519
<v Speaker 6>little bit of a you know, we're not doing any jumping, kiddo,

664
00:38:51.119 --> 00:38:55.320
<v Speaker 6>but I'd never thought of it before. But her question,

665
00:38:55.440 --> 00:39:00.719
<v Speaker 6>I said, you know what, you wouldn't fall. What you

666
00:39:00.880 --> 00:39:05.800
<v Speaker 6>would not fall because to the to the depths there,

667
00:39:05.920 --> 00:39:11.159
<v Speaker 6>because the atmosphere is so dense. It's this dense coe too,

668
00:39:11.559 --> 00:39:15.199
<v Speaker 6>so it would be like if we were all underwater

669
00:39:15.320 --> 00:39:17.960
<v Speaker 6>and you just jumped off, you would just float. No,

670
00:39:18.199 --> 00:39:20.320
<v Speaker 6>And she would be like a penguin that she could

671
00:39:20.360 --> 00:39:26.280
<v Speaker 6>just sit there and be flying. She could not sink

672
00:39:26.440 --> 00:39:29.559
<v Speaker 6>because she would be too buoyant. Isn't that fun?

673
00:39:30.320 --> 00:39:37.559
<v Speaker 1>That's bonkers bonkers. Okay, so maybe at nine hundred degrees

674
00:39:37.599 --> 00:39:40.199
<v Speaker 1>this would have its drawbacks. Well, I mean, I know

675
00:39:40.239 --> 00:39:43.440
<v Speaker 1>it's very hot there, but I want to go check

676
00:39:43.480 --> 00:39:43.840
<v Speaker 1>it out.

677
00:39:44.039 --> 00:39:50.000
<v Speaker 6>Wouldn't it be right? Like talk about a what kids

678
00:39:50.119 --> 00:39:52.039
<v Speaker 6>used to say? I'm sure not anymore, but an e

679
00:39:52.280 --> 00:39:53.840
<v Speaker 6>ride at Disneyland, you know.

680
00:39:54.960 --> 00:39:58.199
<v Speaker 1>And do we have any missions even planned coming up?

681
00:39:59.159 --> 00:40:03.360
<v Speaker 6>Well, that's a really quick question. There are actually three

682
00:40:03.400 --> 00:40:07.000
<v Speaker 6>missions to Venus in the plans, but they kind of

683
00:40:07.079 --> 00:40:11.559
<v Speaker 6>keep being put off. So there's a European mission to

684
00:40:11.599 --> 00:40:15.199
<v Speaker 6>go to Venus. There are two NASA emissions, and when

685
00:40:15.239 --> 00:40:18.719
<v Speaker 6>we say that the US would coordinate with the European

686
00:40:18.760 --> 00:40:23.119
<v Speaker 6>mission and vice versa. Within the nasamissions there is Da

687
00:40:23.199 --> 00:40:26.400
<v Speaker 6>Vinci and that is to go down through the clouds

688
00:40:26.840 --> 00:40:29.800
<v Speaker 6>and get a lot of data through the clouds and

689
00:40:29.840 --> 00:40:34.840
<v Speaker 6>through the atmosphere and then basically photograph the surface and

690
00:40:34.920 --> 00:40:38.000
<v Speaker 6>with the target being this Testra terrain that I said,

691
00:40:38.079 --> 00:40:41.719
<v Speaker 6>is this very old and unique and distinctive terrain. The

692
00:40:41.800 --> 00:40:47.559
<v Speaker 6>other is the Veritas mission, and that is one that

693
00:40:47.800 --> 00:40:51.920
<v Speaker 6>is like Magellan in that it is a global data

694
00:40:51.960 --> 00:40:57.480
<v Speaker 6>collection and it will have much higher resolution of basically

695
00:40:57.559 --> 00:41:00.920
<v Speaker 6>all of the Magellan data sets. But all of these

696
00:41:00.960 --> 00:41:05.480
<v Speaker 6>missions keep getting put off further and further into the future.

697
00:41:06.039 --> 00:41:09.039
<v Speaker 1>And do those circle and use radar as opposed to

698
00:41:09.079 --> 00:41:10.480
<v Speaker 1>getting through those clouds.

699
00:41:10.559 --> 00:41:13.440
<v Speaker 6>Yeah, so the Da Vinci will actually something will go

700
00:41:13.639 --> 00:41:17.840
<v Speaker 6>down through the clouds. I mean a spacecraft will go

701
00:41:17.960 --> 00:41:22.800
<v Speaker 6>down through and photograph and ultimately become one with the planet. Okay,

702
00:41:22.880 --> 00:41:25.280
<v Speaker 6>it'll go there because it's going to burn up. It's

703
00:41:25.360 --> 00:41:28.519
<v Speaker 6>going to burn up exactly. Remember I said that Venus

704
00:41:28.599 --> 00:41:31.960
<v Speaker 6>rotates very very slowly. Yeah, so normally we think about

705
00:41:31.960 --> 00:41:35.760
<v Speaker 6>things going around, okay, and you can go around things

706
00:41:35.760 --> 00:41:38.920
<v Speaker 6>both in a pole or orbit or an equatorial orbit.

707
00:41:39.039 --> 00:41:43.360
<v Speaker 1>So over the top and underside or around the middle.

708
00:41:43.559 --> 00:41:46.280
<v Speaker 1>But the spacecraft, pickI says, doesn't even have to move much,

709
00:41:46.679 --> 00:41:48.719
<v Speaker 1>just kind of like sitting on a bench and watching

710
00:41:48.760 --> 00:41:49.800
<v Speaker 1>a carousel go by.

711
00:41:50.400 --> 00:41:54.440
<v Speaker 6>But Venus, because she's rotating, we can just stay in

712
00:41:54.519 --> 00:41:59.320
<v Speaker 6>one plane and she just rotates underneath us, kind of

713
00:41:59.360 --> 00:42:02.679
<v Speaker 6>like rolling of yarn, you know. And that's the way

714
00:42:02.880 --> 00:42:06.239
<v Speaker 6>Magellan collected. All of these data sets are all in

715
00:42:06.280 --> 00:42:09.280
<v Speaker 6>these little noodles, and that's what they were called. But

716
00:42:09.320 --> 00:42:11.840
<v Speaker 6>it's just like one little noodle and another little noodle.

717
00:42:11.880 --> 00:42:14.280
<v Speaker 6>They're about twenty five kilometers wide, and then they were

718
00:42:14.320 --> 00:42:16.960
<v Speaker 6>just all stitched together. Oh wow, to give us this

719
00:42:17.079 --> 00:42:21.639
<v Speaker 6>incredible global picture. Isn't that elegant?

720
00:42:21.840 --> 00:42:22.840
<v Speaker 1>Yes, And they.

721
00:42:22.800 --> 00:42:25.960
<v Speaker 6>Fully knew that at some point we're going to get

722
00:42:26.000 --> 00:42:28.119
<v Speaker 6>so close that we're just gonna get sucked right in,

723
00:42:28.320 --> 00:42:31.920
<v Speaker 6>and you know, there goes Magellan. Magellan is now one

724
00:42:32.000 --> 00:42:33.039
<v Speaker 6>with Venus.

725
00:42:33.079 --> 00:42:38.800
<v Speaker 1>Very poltic. Before this planned nineteen ninety four crash into Venus,

726
00:42:39.119 --> 00:42:42.480
<v Speaker 1>Magellan had arrived in her orbit in nineteen ninety to

727
00:42:42.679 --> 00:42:47.400
<v Speaker 1>make detailed measurements and also using arrow braking into the

728
00:42:47.400 --> 00:42:50.599
<v Speaker 1>clouds to slow it down when it needed to, and

729
00:42:50.639 --> 00:42:52.960
<v Speaker 1>it saved up to nine times the fuel just by

730
00:42:53.039 --> 00:42:55.159
<v Speaker 1>using the atmosphere itself. Very clever.

731
00:42:56.079 --> 00:42:59.599
<v Speaker 6>So there you are working with that planet in a

732
00:42:59.639 --> 00:43:02.360
<v Speaker 6>way that you couldn't work with Mars or with Earth

733
00:43:03.079 --> 00:43:05.320
<v Speaker 6>because of its differences. So I don't know how we

734
00:43:05.360 --> 00:43:06.360
<v Speaker 6>got on that, but it's.

735
00:43:06.239 --> 00:43:09.639
<v Speaker 1>Just I love it. I have some great questions from listeners,

736
00:43:09.639 --> 00:43:10.599
<v Speaker 1>can I ask? Oh?

737
00:43:10.679 --> 00:43:12.559
<v Speaker 6>Absolutely, a goad. No, I don't like questions.

738
00:43:13.760 --> 00:43:16.719
<v Speaker 1>And before we get into that mail bag, let's launch

739
00:43:16.760 --> 00:43:19.280
<v Speaker 1>some cash at a cause close to the ologist's heart.

740
00:43:19.320 --> 00:43:22.079
<v Speaker 1>And this week, we're splitting it between the nonprofit Planetary

741
00:43:22.119 --> 00:43:25.679
<v Speaker 1>Science Institute, which is dedicated to solar system exploration. They

742
00:43:25.719 --> 00:43:29.199
<v Speaker 1>conduct fieldwork on all continents around the world. They're also

743
00:43:29.320 --> 00:43:33.679
<v Speaker 1>actively involved in science education and public outreach through school programs,

744
00:43:33.800 --> 00:43:37.760
<v Speaker 1>children's books, popular science books, and art. I suppose also

745
00:43:37.800 --> 00:43:42.000
<v Speaker 1>podcasts will donate to them, as well as Vicky's beloved

746
00:43:42.079 --> 00:43:45.239
<v Speaker 1>Nature Conservancy. She says to take care that our precious

747
00:43:45.280 --> 00:43:48.239
<v Speaker 1>planet might continue to allow us to be part of it,

748
00:43:48.559 --> 00:43:50.480
<v Speaker 1>and links to those causes are in the show notes.

749
00:43:50.480 --> 00:43:52.960
<v Speaker 1>And thank you to sponsors for enabling us to donate

750
00:43:53.039 --> 00:43:53.920
<v Speaker 1>to them.

751
00:43:54.360 --> 00:43:56.360
<v Speaker 3>Drivers know what trouble sounds like?

752
00:43:56.480 --> 00:44:03.920
<v Speaker 1>No, no, okay, forward, oh no, oh pretty, So.

753
00:44:06.119 --> 00:44:09.440
<v Speaker 3>That's why they get covered from Ireland's soundest car insurance provider,

754
00:44:09.679 --> 00:44:10.880
<v Speaker 3>Supervalue Insurance.

755
00:44:11.159 --> 00:44:13.480
<v Speaker 4>Thanks for calling us in and don't pat yourself up

756
00:44:13.480 --> 00:44:16.320
<v Speaker 4>about it. Sure I'm driving ten years and parallel parking.

757
00:44:16.360 --> 00:44:17.239
<v Speaker 4>Still that isn't me.

758
00:44:18.119 --> 00:44:20.719
<v Speaker 2>Get a quote from Supervalue Car Insurance to get ten

759
00:44:20.760 --> 00:44:23.440
<v Speaker 2>percent off online and we'll even throw in forty euro

760
00:44:23.519 --> 00:44:26.719
<v Speaker 2>in vouchers. Teacenc's apply vouchers include two twenty euro or

761
00:44:26.719 --> 00:44:29.480
<v Speaker 2>forty eurospend. This car insurance is underwritten by ax Insurance

762
00:44:29.519 --> 00:44:32.400
<v Speaker 2>Deck super Value Financial Servicestack, trading as supervalue insurance is

763
00:44:32.440 --> 00:44:33.880
<v Speaker 2>regulated by the Central Bank of Ireland.

764
00:44:34.719 --> 00:44:37.840
<v Speaker 1>Okay, your Venus questions patrons, If you would like to

765
00:44:37.880 --> 00:44:40.559
<v Speaker 1>know what topics we have coming up and submit your questions,

766
00:44:40.559 --> 00:44:42.440
<v Speaker 1>you can hit up patreon dot com slash ologies to

767
00:44:42.519 --> 00:44:44.360
<v Speaker 1>join for a buck a month, and we do our

768
00:44:44.360 --> 00:44:47.440
<v Speaker 1>best to ask as many as conversationally possible. This is

769
00:44:47.480 --> 00:44:50.360
<v Speaker 1>what I should have asked up front, but I Rennebe,

770
00:44:50.440 --> 00:44:55.880
<v Speaker 1>Scott Umaya, Sam Meghan the librarian, r J Deutsche Kaya

771
00:44:56.039 --> 00:45:00.400
<v Speaker 1>and Jasmine wanted to know. Irnabe ask why have we

772
00:45:00.639 --> 00:45:04.679
<v Speaker 1>gendered the planets? Why do we say she when we

773
00:45:04.719 --> 00:45:05.559
<v Speaker 1>talk about her?

774
00:45:05.920 --> 00:45:08.679
<v Speaker 6>Well, I don't know why we gendered the planets. I

775
00:45:08.760 --> 00:45:11.760
<v Speaker 6>think that goes back to the Greeks and Romans, because

776
00:45:11.960 --> 00:45:15.920
<v Speaker 6>those were you know, of gods and goddesses. And why

777
00:45:15.960 --> 00:45:20.360
<v Speaker 6>did we decide that Mars was a male god and

778
00:45:20.519 --> 00:45:23.840
<v Speaker 6>Venus was a female god. I have no idea I

779
00:45:23.840 --> 00:45:27.800
<v Speaker 6>could imagine that with Venus, because she's an evening star

780
00:45:28.000 --> 00:45:31.079
<v Speaker 6>and a morning star and so sort of some beauty

781
00:45:31.199 --> 00:45:35.159
<v Speaker 6>and elusiveness. But I'm like them, inquiring minds want to know.

782
00:45:36.679 --> 00:45:39.920
<v Speaker 1>In scientific surface is she referred to as a she

783
00:45:40.079 --> 00:45:40.480
<v Speaker 1>or earn it?

784
00:45:41.119 --> 00:45:43.599
<v Speaker 6>You know, that's really funny. It's all a personal thing.

785
00:45:44.199 --> 00:45:48.519
<v Speaker 6>So some people get really upset when you refer to

786
00:45:48.679 --> 00:45:52.320
<v Speaker 6>planets as him or her. But you know, for me,

787
00:45:52.559 --> 00:45:55.840
<v Speaker 6>for Venus, we haven't even scratched the surface. We don't

788
00:45:55.840 --> 00:45:59.199
<v Speaker 6>know the surface age. That is the age of her,

789
00:45:59.559 --> 00:46:03.000
<v Speaker 6>her skin very well, she's veiled in things, and so

790
00:46:03.559 --> 00:46:06.440
<v Speaker 6>I don't like cultural differences between males and female. But

791
00:46:06.480 --> 00:46:09.719
<v Speaker 6>that's a cultural thing that seems to fit for this planet.

792
00:46:09.760 --> 00:46:13.320
<v Speaker 6>But it's totally personal, and a lot of people don't care,

793
00:46:13.400 --> 00:46:15.960
<v Speaker 6>and some people it gets to be in their bonnet.

794
00:46:16.559 --> 00:46:18.880
<v Speaker 1>Oh I like it. I do too. I think it's

795
00:46:18.920 --> 00:46:21.280
<v Speaker 1>cute as long as one does not take things too

796
00:46:21.400 --> 00:46:26.239
<v Speaker 1>literally or literarily. Speaking of which, a blockbuster bestselling nineteen

797
00:46:26.280 --> 00:46:28.920
<v Speaker 1>ninety two book that continues to live in the minds

798
00:46:28.960 --> 00:46:31.719
<v Speaker 1>of humans is titled Men Are From Mars, Women Are

799
00:46:31.719 --> 00:46:35.119
<v Speaker 1>from Venus. A Practical Guide for improving communication and getting

800
00:46:35.119 --> 00:46:39.280
<v Speaker 1>what you want in your relationships. And this heteronormative tone

801
00:46:39.639 --> 00:46:42.480
<v Speaker 1>begins with this touching tale from the author, who is

802
00:46:42.519 --> 00:46:46.960
<v Speaker 1>a relationship counselor with an unaccredited PhD and his wife Bonnie,

803
00:46:47.079 --> 00:46:50.159
<v Speaker 1>who had just given birth to their daughter and whose

804
00:46:50.199 --> 00:46:53.599
<v Speaker 1>nether regions were torn to shreds and the baby had

805
00:46:53.679 --> 00:46:56.119
<v Speaker 1>kept them awake for days on end. But less than

806
00:46:56.119 --> 00:47:00.239
<v Speaker 1>a week after Bonnie gave birth, when she couldn't walk

807
00:47:00.400 --> 00:47:03.199
<v Speaker 1>and she was on painkillers, the author went back to

808
00:47:03.280 --> 00:47:06.760
<v Speaker 1>work five days later, leaving her home out of medicine

809
00:47:06.960 --> 00:47:09.480
<v Speaker 1>and too afraid to call him at work and disrupt

810
00:47:09.480 --> 00:47:11.599
<v Speaker 1>his day, so she called his brother, who forgot to

811
00:47:11.639 --> 00:47:14.320
<v Speaker 1>pick up her medicine. When the author got home, and

812
00:47:14.360 --> 00:47:18.039
<v Speaker 1>she said, I've been in excruciating pain and your brother flaked.

813
00:47:18.079 --> 00:47:20.159
<v Speaker 1>It's been a bad day. The author writes of his

814
00:47:20.280 --> 00:47:24.280
<v Speaker 1>reaction at this point, I exploded. My fuse was also

815
00:47:24.480 --> 00:47:26.880
<v Speaker 1>very short that day. I was angry that she hadn't

816
00:47:26.920 --> 00:47:29.440
<v Speaker 1>called me. I was furious that she was blaming me

817
00:47:29.800 --> 00:47:32.280
<v Speaker 1>when I didn't even know she was in pain. After

818
00:47:32.320 --> 00:47:35.480
<v Speaker 1>exchanging a few harsh words, I headed for the door.

819
00:47:35.840 --> 00:47:39.400
<v Speaker 1>I was fired, irritable and had hurt enough. We both

820
00:47:39.400 --> 00:47:42.960
<v Speaker 1>had reached our limits. Then his wife cries and begs

821
00:47:43.039 --> 00:47:47.039
<v Speaker 1>him to comfort her, and a book about male female

822
00:47:47.079 --> 00:47:50.679
<v Speaker 1>relations was born, tearing a new asshole into the self

823
00:47:50.719 --> 00:47:54.760
<v Speaker 1>help genre and selling fifteen million copies, and Men Are

824
00:47:54.760 --> 00:47:57.800
<v Speaker 1>from Mars, Women Are from Venus includes hot chapters such

825
00:47:57.840 --> 00:48:00.920
<v Speaker 1>as men go to their caves and women talk, and

826
00:48:01.239 --> 00:48:05.360
<v Speaker 1>how to motivate the opposite sex and scoring points with

827
00:48:05.440 --> 00:48:09.159
<v Speaker 1>the opposite sex. It also provided a foundation of thoughts

828
00:48:09.159 --> 00:48:12.320
<v Speaker 1>such as two people of different genders have no common

829
00:48:12.360 --> 00:48:15.159
<v Speaker 1>ground as humans, but have to approach each other like

830
00:48:15.239 --> 00:48:18.760
<v Speaker 1>aliens to be manipulated via their native language. It also

831
00:48:18.800 --> 00:48:21.480
<v Speaker 1>probably confused a lot of people who didn't know much

832
00:48:21.519 --> 00:48:27.519
<v Speaker 1>about astronomy or evolution on Earth. Were you already studying

833
00:48:27.880 --> 00:48:32.079
<v Speaker 1>Venus and also your husband a geologist? When mena for Mars,

834
00:48:32.119 --> 00:48:35.360
<v Speaker 1>Women are from Venus? Did that book piss you off?

835
00:48:35.559 --> 00:48:37.519
<v Speaker 6>I'd have to look that up, but I think Men

836
00:48:37.559 --> 00:48:41.119
<v Speaker 6>Are from Mars, Women Are from Venus came out before

837
00:48:41.239 --> 00:48:43.880
<v Speaker 6>the Magellan mission, and that's when I would have gotten

838
00:48:44.199 --> 00:48:46.440
<v Speaker 6>onto all of that. I think the book did piss

839
00:48:46.480 --> 00:48:48.840
<v Speaker 6>me off a bit, but totally independent of this, because

840
00:48:48.880 --> 00:48:50.559
<v Speaker 6>I was like, this is just as stupid.

841
00:48:50.960 --> 00:48:54.320
<v Speaker 1>Yes, exactly exactly.

842
00:48:54.800 --> 00:49:00.000
<v Speaker 6>But that was like, I don't associate that with Venus

843
00:49:00.239 --> 00:49:01.800
<v Speaker 6>the planet. She's just above all that.

844
00:49:02.400 --> 00:49:03.480
<v Speaker 1>Yeah, exactly.

845
00:49:03.679 --> 00:49:03.800
<v Speaker 7>So.

846
00:49:03.840 --> 00:49:07.880
<v Speaker 1>In terms of pop cultural references like Lady Gaga songs,

847
00:49:08.280 --> 00:49:11.800
<v Speaker 1>or b York Crooning about Venus as a boy and

848
00:49:11.920 --> 00:49:15.159
<v Speaker 1>Ray Bradberry's All Summer in a Day, or the short

849
00:49:15.199 --> 00:49:18.920
<v Speaker 1>story The Long Rain about the Venus Atmosphere, Wonder Woman's

850
00:49:19.000 --> 00:49:22.360
<v Speaker 1>Venusian Allies, and a bunch of space age movies and

851
00:49:22.400 --> 00:49:24.840
<v Speaker 1>comic books. Well, in spite of all that.

852
00:49:24.760 --> 00:49:27.679
<v Speaker 6>I'm not much of a science fiction person, unlike most

853
00:49:27.719 --> 00:49:32.760
<v Speaker 6>planetary people are all about science fiction, and I'm not

854
00:49:32.960 --> 00:49:35.960
<v Speaker 6>that fascinated by it. I'm just more fascinated by the planet,

855
00:49:36.000 --> 00:49:41.400
<v Speaker 6>and to me, it's much more interesting than any science fiction.

856
00:49:41.519 --> 00:49:43.760
<v Speaker 6>So I won't remember who the author was, but there

857
00:49:43.800 --> 00:49:46.239
<v Speaker 6>was a recent like within the last couple of years.

858
00:49:46.239 --> 00:49:50.159
<v Speaker 1>An author, Annilie Knuitz is the author of The Terrorformers,

859
00:49:50.159 --> 00:49:52.000
<v Speaker 1>and Vicki says it's not about Venus per se, but

860
00:49:52.039 --> 00:49:54.719
<v Speaker 1>takes place in the far future on another planet, and

861
00:49:54.880 --> 00:49:58.159
<v Speaker 1>inspiration from Venus was their motivation for reaching out to Vicky,

862
00:49:58.280 --> 00:50:00.920
<v Speaker 1>who says that she loves anything that makes one think

863
00:50:00.960 --> 00:50:02.719
<v Speaker 1>in different ways and that it's a really fun book.

864
00:50:02.800 --> 00:50:06.039
<v Speaker 1>So anyway, Annali, journalist and science author and now using

865
00:50:06.119 --> 00:50:10.480
<v Speaker 1>vey them pronouns, reached out to chat Planetary Geology, who.

866
00:50:10.280 --> 00:50:12.760
<v Speaker 6>Wrote a book about Venus and called me and said,

867
00:50:12.760 --> 00:50:14.360
<v Speaker 6>you know, I want to check some things out. And

868
00:50:14.400 --> 00:50:16.719
<v Speaker 6>so it was so much fun to talk to her

869
00:50:16.719 --> 00:50:19.000
<v Speaker 6>because I was like, no, no, no, no, no, this planet

870
00:50:19.079 --> 00:50:25.079
<v Speaker 6>is much much more interesting than the credit you're giving it.

871
00:50:25.119 --> 00:50:27.599
<v Speaker 6>And that actually made her change the way she was

872
00:50:27.679 --> 00:50:31.239
<v Speaker 6>writing about it because she had plate tectonics in it,

873
00:50:31.280 --> 00:50:35.559
<v Speaker 6>and it's like, no, but more other fascinating things. And

874
00:50:35.639 --> 00:50:38.280
<v Speaker 6>I read the book, but I read a book. I

875
00:50:38.360 --> 00:50:40.440
<v Speaker 6>enjoy it, and then I put it down and it's gone.

876
00:50:40.599 --> 00:50:43.360
<v Speaker 6>If it's in science it sticks, but books it doesn't.

877
00:50:43.400 --> 00:50:45.119
<v Speaker 6>It was a wonderful book and a lot of fun.

878
00:50:45.679 --> 00:50:49.800
<v Speaker 6>But I'm just not much of a science fiction reader.

879
00:50:49.880 --> 00:50:52.679
<v Speaker 1>Yeah, I mean, truth is more fascinating than fiction.

880
00:50:53.199 --> 00:50:54.760
<v Speaker 6>To me, it is to you it is.

881
00:50:55.360 --> 00:50:59.920
<v Speaker 1>What about private missions? Kelly Shaver and Milan Yeki wanted

882
00:50:59.920 --> 00:51:04.320
<v Speaker 1>to know Sarah Sager's Venus life Finder missions are very exciting.

883
00:51:04.679 --> 00:51:07.679
<v Speaker 1>What do you think about robotic exploration? Is that on

884
00:51:07.719 --> 00:51:08.280
<v Speaker 1>the table?

885
00:51:08.800 --> 00:51:12.800
<v Speaker 6>Well, you know, robotic exploration to me, is absolutely the

886
00:51:12.800 --> 00:51:15.400
<v Speaker 6>way to go for all of these things. If we

887
00:51:15.559 --> 00:51:18.639
<v Speaker 6>don't pollute a planet, we don't have to take so

888
00:51:18.719 --> 00:51:23.159
<v Speaker 6>many other energies. We can have robots do things are

889
00:51:23.199 --> 00:51:28.079
<v Speaker 6>they geologists. No, they're not geologists. Eyes on things. But

890
00:51:28.239 --> 00:51:31.519
<v Speaker 6>we can get so so so much more data, so

891
00:51:31.639 --> 00:51:36.039
<v Speaker 6>much more comprehensive data, so many different data sets. We're

892
00:51:36.119 --> 00:51:40.360
<v Speaker 6>just not limited by the limits of humans. And it's

893
00:51:40.480 --> 00:51:44.880
<v Speaker 6>just to me, absolutely scientifically the way to go.

894
00:51:45.440 --> 00:51:48.760
<v Speaker 1>So Vicki does not yearn for the bouncing among Venus's

895
00:51:48.880 --> 00:51:50.440
<v Speaker 1>hot clouds. She's like, I'm good.

896
00:51:50.800 --> 00:51:52.599
<v Speaker 6>I mean, if I'm going to go on adventures, I'll

897
00:51:52.599 --> 00:51:56.239
<v Speaker 6>go out and do some great biking or snowshoeing or

898
00:51:56.360 --> 00:51:59.440
<v Speaker 6>a you know, canoe trip or things. There's so much

899
00:51:59.440 --> 00:52:01.239
<v Speaker 6>on Earth that I I'm going to do for an adventure.

900
00:52:01.760 --> 00:52:04.400
<v Speaker 6>But if I want adventures in science, I want really

901
00:52:04.440 --> 00:52:07.360
<v Speaker 6>good data, and robotics are the way to go. I

902
00:52:07.400 --> 00:52:10.960
<v Speaker 6>think for basically all of our missions for Venus, you said,

903
00:52:11.119 --> 00:52:14.519
<v Speaker 6>you know what about could we sample things? There's so

904
00:52:14.599 --> 00:52:17.239
<v Speaker 6>many clever things to look at the clouds, but you

905
00:52:17.280 --> 00:52:21.440
<v Speaker 6>could have a mission that what you send is basically

906
00:52:21.920 --> 00:52:27.719
<v Speaker 6>a glider plane and you put solar panels on the wings,

907
00:52:28.159 --> 00:52:31.840
<v Speaker 6>and you put collectors all under the winds, like all

908
00:52:31.960 --> 00:52:35.800
<v Speaker 6>kinds of you just load that baby up, okay, like

909
00:52:36.199 --> 00:52:40.480
<v Speaker 6>payload up the wazoo and this glider. It goes down

910
00:52:40.599 --> 00:52:43.559
<v Speaker 6>through the clouds and collects all this data. It can

911
00:52:43.599 --> 00:52:47.079
<v Speaker 6>even go beneath the clouds, collect all kinds of data

912
00:52:47.400 --> 00:52:51.400
<v Speaker 6>on the surface. It starts to say robotically, oh, I'm

913
00:52:51.440 --> 00:52:53.840
<v Speaker 6>running out of energy, so it just sends it back up,

914
00:52:54.119 --> 00:52:58.800
<v Speaker 6>recharges those goes back down and it could go endlessly,

915
00:52:59.159 --> 00:53:02.400
<v Speaker 6>you know. And so you could have time sensitive data,

916
00:53:02.760 --> 00:53:06.719
<v Speaker 6>you could have tracking that would go for years. You

917
00:53:06.800 --> 00:53:09.599
<v Speaker 6>could have so much different things. And so there's just

918
00:53:09.800 --> 00:53:14.000
<v Speaker 6>so many elegant types of missions that you could have.

919
00:53:14.519 --> 00:53:18.239
<v Speaker 6>And you could do this with someone who's got extra

920
00:53:18.360 --> 00:53:22.599
<v Speaker 6>change to throw around, you know me. But there one

921
00:53:22.599 --> 00:53:28.079
<v Speaker 6>could actually like really look at fascinating questions about venus,

922
00:53:28.159 --> 00:53:30.880
<v Speaker 6>the plow blank but also the surface but also life.

923
00:53:30.920 --> 00:53:34.239
<v Speaker 6>And it could be amazing and at probably a fraction

924
00:53:34.480 --> 00:53:35.079
<v Speaker 6>of a cost.

925
00:53:35.880 --> 00:53:38.920
<v Speaker 1>What about when they're collecting, when that glider would be

926
00:53:38.960 --> 00:53:42.360
<v Speaker 1>collecting all of that data, does it analyze it on

927
00:53:42.440 --> 00:53:44.320
<v Speaker 1>board and then beam it back to us? How does

928
00:53:44.320 --> 00:53:44.679
<v Speaker 1>that work?

929
00:53:45.360 --> 00:53:48.840
<v Speaker 6>Also really really great question, and this when the Magellan

930
00:53:48.880 --> 00:53:52.320
<v Speaker 6>mission went, which gave us amazing data, The people who

931
00:53:52.360 --> 00:53:58.880
<v Speaker 6>designed that mission had to use nineteen seventies technology. Now

932
00:53:58.920 --> 00:54:02.360
<v Speaker 6>probably a lot of your audience. You know, they're like,

933
00:54:02.559 --> 00:54:07.119
<v Speaker 6>that's older than my grandparents. Yeah, but that's the technology

934
00:54:07.320 --> 00:54:10.679
<v Speaker 6>they were using. So now we have so much more

935
00:54:10.719 --> 00:54:12.639
<v Speaker 6>things are so much smaller, and we can do a

936
00:54:12.639 --> 00:54:16.400
<v Speaker 6>lot more processing on board. But what you do is

937
00:54:16.440 --> 00:54:19.800
<v Speaker 6>when you come back up above the clouds, you're beaming

938
00:54:20.199 --> 00:54:23.320
<v Speaker 6>that data back to Earth. You have to be at

939
00:54:23.360 --> 00:54:25.559
<v Speaker 6>the right orientation to the Earth and you have to

940
00:54:25.599 --> 00:54:27.719
<v Speaker 6>have a place on Earth that can accept it.

941
00:54:28.119 --> 00:54:30.079
<v Speaker 1>And it's nuts that the Soviets were able to do

942
00:54:30.119 --> 00:54:31.199
<v Speaker 1>this in the sixties.

943
00:54:31.679 --> 00:54:35.440
<v Speaker 6>I mean, well that is nutty and not they just

944
00:54:35.480 --> 00:54:38.440
<v Speaker 6>didn't put down one lander, I mean several of them,

945
00:54:38.719 --> 00:54:41.559
<v Speaker 6>and they're what they did is the landers went down,

946
00:54:41.639 --> 00:54:46.239
<v Speaker 6>the landers stayed there, but they beamed data back. It

947
00:54:46.360 --> 00:54:51.800
<v Speaker 6>is truly truly mind boggling what they did. And you know,

948
00:54:51.880 --> 00:54:54.679
<v Speaker 6>you can say and people do complain about the data

949
00:54:54.719 --> 00:54:57.519
<v Speaker 6>and it's like, well, oh my goodness, you know it's

950
00:54:57.559 --> 00:55:01.639
<v Speaker 6>not the quality, no, but just they that is amazing.

951
00:55:01.719 --> 00:55:06.000
<v Speaker 6>And they actually have photographs of the surface that were

952
00:55:06.199 --> 00:55:10.679
<v Speaker 6>beamed back, but true surface photographs, you know, of like

953
00:55:10.719 --> 00:55:14.119
<v Speaker 6>the rocky surface right where they landed. It is it

954
00:55:14.199 --> 00:55:19.800
<v Speaker 6>is mind boggling what they did, truly, like you know amazing.

955
00:55:20.239 --> 00:55:23.320
<v Speaker 1>And two first time question askers, Emma Krookmeyer and Ashley

956
00:55:23.360 --> 00:55:25.840
<v Speaker 1>p wanted to know, in Emma's words, why is the

957
00:55:25.880 --> 00:55:29.079
<v Speaker 1>atmosphere on Venus the way it is? And Ashley Pe asked,

958
00:55:29.159 --> 00:55:32.159
<v Speaker 1>does it rain chemicals there like it does water here?

959
00:55:32.719 --> 00:55:36.840
<v Speaker 1>Would the sulfuric acid? Would the acid rain destroy a

960
00:55:36.880 --> 00:55:37.320
<v Speaker 1>lot of that?

961
00:55:37.800 --> 00:55:42.519
<v Speaker 6>Yes? Yeah, So when we're looking at all the electronics,

962
00:55:42.880 --> 00:55:47.880
<v Speaker 6>the heat and the caustic environment are just going to that,

963
00:55:48.440 --> 00:55:51.440
<v Speaker 6>just fry them, just wipe them out. But if you

964
00:55:52.239 --> 00:55:55.960
<v Speaker 6>are up under the cloud bank, then you're not in

965
00:55:56.000 --> 00:56:00.760
<v Speaker 6>that caustic environment. So landing on the surface is one thing.

966
00:56:01.039 --> 00:56:04.760
<v Speaker 6>But back to that glide or people have proposed balloons

967
00:56:04.880 --> 00:56:07.760
<v Speaker 6>or something, but a glider we'd have a lot more

968
00:56:07.800 --> 00:56:12.119
<v Speaker 6>control of than a balloon. But there you can keep

969
00:56:12.199 --> 00:56:17.079
<v Speaker 6>your instruments much safer and out of that caustic environment

970
00:56:17.400 --> 00:56:19.440
<v Speaker 6>than if you're landing on the surface.

971
00:56:20.239 --> 00:56:24.199
<v Speaker 1>Well, what about the past of it? Milena que first

972
00:56:24.199 --> 00:56:28.239
<v Speaker 1>time question askers as longtime listener fest asker Caro Young,

973
00:56:28.400 --> 00:56:32.840
<v Speaker 1>as well as Thistlebuzunger Nick writer Michael are A. Victor

974
00:56:32.960 --> 00:56:37.079
<v Speaker 1>Lilly wanted to know, in Molena's words, is there any

975
00:56:37.119 --> 00:56:40.159
<v Speaker 1>truth to the idea that Venus was once habitable. Could

976
00:56:40.159 --> 00:56:42.119
<v Speaker 1>it ever become habitable once again?

977
00:56:42.880 --> 00:56:47.360
<v Speaker 6>Was it ever habitable? Well, the surface might have been

978
00:56:47.519 --> 00:56:51.639
<v Speaker 6>early on Earth. We keep pushing life back early and

979
00:56:51.760 --> 00:56:56.599
<v Speaker 6>earlier on Earth, and the two planets were probably the

980
00:56:56.639 --> 00:57:00.480
<v Speaker 6>most similar for the first two point five billillion years

981
00:57:00.519 --> 00:57:03.719
<v Speaker 6>of their history, that's basically half of their history. And

982
00:57:04.119 --> 00:57:08.599
<v Speaker 6>life was established on Earth well within that at three

983
00:57:08.639 --> 00:57:11.679
<v Speaker 6>point five and probably we keep pushing it back further

984
00:57:12.079 --> 00:57:14.840
<v Speaker 6>billion years. Three point five billion years.

985
00:57:14.639 --> 00:57:18.960
<v Speaker 1>So Earth and Venus sister sibling planets about four point

986
00:57:19.119 --> 00:57:21.920
<v Speaker 1>six billion years old, who looked a lot alike in

987
00:57:21.960 --> 00:57:24.960
<v Speaker 1>their youth. And some scientists are now saying that life

988
00:57:25.000 --> 00:57:29.320
<v Speaker 1>on Earth may have started at its relative infancy around

989
00:57:29.440 --> 00:57:32.719
<v Speaker 1>four point two billion years ago. And by the way,

990
00:57:32.719 --> 00:57:35.800
<v Speaker 1>did you know that, like how a century is one

991
00:57:35.880 --> 00:57:38.920
<v Speaker 1>hundred years in a millennium is one thousand. A billion

992
00:57:39.000 --> 00:57:41.480
<v Speaker 1>years has a name, it's called a gigantis.

993
00:57:42.440 --> 00:57:46.719
<v Speaker 6>So Venus certainly could have been. We think that there

994
00:57:47.079 --> 00:57:50.400
<v Speaker 6>was Venus once had an ocean of water. Now we

995
00:57:50.519 --> 00:57:53.920
<v Speaker 6>always want to say that life is required water and

996
00:57:53.960 --> 00:57:56.239
<v Speaker 6>that's life as we know it, but we really have

997
00:57:56.320 --> 00:57:58.880
<v Speaker 6>to think about how we define life, and that's something

998
00:57:59.199 --> 00:58:01.639
<v Speaker 6>that is a whole nother conversation. But if we just

999
00:58:01.679 --> 00:58:05.320
<v Speaker 6>stick with water based life, Venus could have had that

1000
00:58:05.719 --> 00:58:09.719
<v Speaker 6>early in her history, as Earth has early life. As

1001
00:58:09.719 --> 00:58:13.599
<v Speaker 6>I say that now, on the surface of Venus we've

1002
00:58:13.639 --> 00:58:17.119
<v Speaker 6>never found extremophiles. We find extremophiles on Earth that are

1003
00:58:17.119 --> 00:58:20.280
<v Speaker 6>in extreme conditions, but not as extreme as what we

1004
00:58:20.320 --> 00:58:24.400
<v Speaker 6>see on the surface of Venus. However, that life could

1005
00:58:24.519 --> 00:58:28.239
<v Speaker 6>be up in the clouds and could have stayed, you know,

1006
00:58:28.320 --> 00:58:33.079
<v Speaker 6>existed there, or could have moved there, just as life

1007
00:58:33.079 --> 00:58:36.679
<v Speaker 6>has moved around, you know on Earth. In the future.

1008
00:58:37.199 --> 00:58:41.039
<v Speaker 6>It's a hot, hot, dry, dry planet and it's probably

1009
00:58:41.079 --> 00:58:45.039
<v Speaker 6>only going to get hotter and drier, and so we're

1010
00:58:45.039 --> 00:58:48.920
<v Speaker 6>not going to ever terraform Venus the way we may

1011
00:58:49.000 --> 00:58:53.320
<v Speaker 6>or may not do the Moon or Mars. And plate

1012
00:58:53.320 --> 00:58:56.679
<v Speaker 6>tectonics is something that is a real regulator of the

1013
00:58:56.679 --> 00:59:00.480
<v Speaker 6>Earth of our climate, and Venus doesn't have plate techs.

1014
00:59:00.639 --> 00:59:03.880
<v Speaker 6>And if she was ever to develop it, it probably

1015
00:59:03.920 --> 00:59:06.559
<v Speaker 6>had to be early in her history in a tight

1016
00:59:06.639 --> 00:59:10.519
<v Speaker 6>window of conditions, and she lost her chance. And so

1017
00:59:11.239 --> 00:59:13.320
<v Speaker 6>you know, in terms of it cooling down as a

1018
00:59:13.360 --> 00:59:14.719
<v Speaker 6>planet or anything like that.

1019
00:59:15.280 --> 00:59:18.719
<v Speaker 1>No, yeah, well, a few people had great questions Bugging

1020
00:59:18.760 --> 00:59:22.239
<v Speaker 1>and Rug and Killian sentpal and rob h wanted to

1021
00:59:22.280 --> 00:59:26.480
<v Speaker 1>ask about and red headed scientists. Bug and Rugg said, Okay,

1022
00:59:26.800 --> 00:59:29.039
<v Speaker 1>so I heard it's scientifically possible that there could be

1023
00:59:29.079 --> 00:59:31.920
<v Speaker 1>life in the atmosphere of Venus. Is this real? But

1024
00:59:32.079 --> 00:59:36.000
<v Speaker 1>I thought Killian's question of could the life be anaerobic

1025
00:59:36.320 --> 00:59:38.480
<v Speaker 1>since there's so much carbon dioxide.

1026
00:59:38.760 --> 00:59:41.440
<v Speaker 6>Yeah, we could have all different kinds of life there

1027
00:59:41.480 --> 00:59:44.840
<v Speaker 6>in that. Absolutely, when we look at the life at

1028
00:59:44.880 --> 00:59:49.880
<v Speaker 6>mid ocean spreading centers on Earth, very very different. They

1029
00:59:49.880 --> 00:59:53.960
<v Speaker 6>don't live on sunlight, so yeah, absolutely, and there could

1030
00:59:54.000 --> 00:59:58.079
<v Speaker 6>be forms that exist on Earth in unique environments, but

1031
00:59:58.159 --> 01:00:01.039
<v Speaker 6>that could be what is very typical on Venus. And

1032
01:00:01.119 --> 01:00:05.599
<v Speaker 6>there could be a range of different life styles that

1033
01:00:05.880 --> 01:00:10.480
<v Speaker 6>consume different things on Venus within the clouds. So that's

1034
01:00:10.840 --> 01:00:13.880
<v Speaker 6>such an open question. And I think what we need

1035
01:00:14.039 --> 01:00:18.880
<v Speaker 6>are data and we need open minds, and sometimes open

1036
01:00:18.920 --> 01:00:21.800
<v Speaker 6>minds are harder to come by than the data. And

1037
01:00:21.840 --> 01:00:24.519
<v Speaker 6>the open minds are just like your listeners to say, well,

1038
01:00:24.559 --> 01:00:27.440
<v Speaker 6>wait a second, maybe it could be life that does

1039
01:00:27.800 --> 01:00:31.639
<v Speaker 6>you know X, Y or Z instead of ABC as

1040
01:00:31.679 --> 01:00:33.559
<v Speaker 6>we want to force it into on Earth.

1041
01:00:34.440 --> 01:00:37.440
<v Speaker 1>We have a whole episode on Aliens with a NASA scientist,

1042
01:00:37.559 --> 01:00:40.119
<v Speaker 1>doctor Kevin Hand. We also have a UFO episode, so

1043
01:00:40.239 --> 01:00:42.719
<v Speaker 1>if you need more info on those, here's your sign.

1044
01:00:43.159 --> 01:00:47.599
<v Speaker 1>Speaking of signs, let's see some people asked about a

1045
01:00:47.599 --> 01:00:51.199
<v Speaker 1>lot of people asked about Venus associated with love and astrology.

1046
01:00:51.480 --> 01:00:52.400
<v Speaker 6>What's not to love?

1047
01:00:53.880 --> 01:00:56.800
<v Speaker 1>Does that come up in conversations? A lot of people like, oh,

1048
01:00:56.800 --> 01:01:01.440
<v Speaker 1>my god, in my son house, did like a bobblehead

1049
01:01:01.559 --> 01:01:06.800
<v Speaker 1>going down a gravel road. Yeah, yes, yes, I don't

1050
01:01:06.840 --> 01:01:08.480
<v Speaker 1>know much about that myself, but.

1051
01:01:09.719 --> 01:01:10.760
<v Speaker 6>I don't either.

1052
01:01:11.440 --> 01:01:14.400
<v Speaker 1>And is uh to find her in the sky? Is it?

1053
01:01:14.440 --> 01:01:17.679
<v Speaker 1>Is it like look for just the brightest star in

1054
01:01:17.719 --> 01:01:18.679
<v Speaker 1>the morning or evening.

1055
01:01:19.079 --> 01:01:21.519
<v Speaker 6>Yeah, and it's going to be low in the horizon.

1056
01:01:21.719 --> 01:01:25.599
<v Speaker 6>She never rises up high. Why because she's between us

1057
01:01:25.639 --> 01:01:26.360
<v Speaker 6>and the sun.

1058
01:01:27.320 --> 01:01:29.920
<v Speaker 1>So think of Venus as being closer to the sun.

1059
01:01:30.159 --> 01:01:32.599
<v Speaker 1>So you're going to see her near the sun, but

1060
01:01:32.760 --> 01:01:35.320
<v Speaker 1>at the darkest time of day when the sun isn't

1061
01:01:35.400 --> 01:01:39.400
<v Speaker 1>quite outshining her. Hence she's low in the eastern sky

1062
01:01:39.719 --> 01:01:43.800
<v Speaker 1>before sunrise as the morning star, or in the western

1063
01:01:43.880 --> 01:01:47.000
<v Speaker 1>sky after sunset as the evening star.

1064
01:01:47.480 --> 01:01:52.280
<v Speaker 6>So Mars, because it's it's away from us in the sun,

1065
01:01:52.440 --> 01:01:57.039
<v Speaker 6>it can be see it. Mars, I have no problem

1066
01:01:57.119 --> 01:02:00.800
<v Speaker 6>calling it. Mars can be high in the sky, Jupiter,

1067
01:02:00.960 --> 01:02:03.920
<v Speaker 6>Saturn can be high in the sky, but Venus can

1068
01:02:03.960 --> 01:02:07.280
<v Speaker 6>only be low in the sky. And you're exactly right,

1069
01:02:07.679 --> 01:02:10.960
<v Speaker 6>brightest thing in the morning and in the evening. And

1070
01:02:11.480 --> 01:02:14.519
<v Speaker 6>you know, depending on what it is the other thing

1071
01:02:14.519 --> 01:02:19.519
<v Speaker 6>that Venus will sometimes appear brighter and other times less

1072
01:02:19.559 --> 01:02:23.199
<v Speaker 6>bright because she's between us and the sun. Think about

1073
01:02:23.239 --> 01:02:26.679
<v Speaker 6>sometimes she's very close to us and yet still reflecting

1074
01:02:26.679 --> 01:02:28.880
<v Speaker 6>the Sun's light, and other times when she's on the

1075
01:02:28.920 --> 01:02:32.119
<v Speaker 6>opposite side of the Sun, we can still see it

1076
01:02:32.239 --> 01:02:34.840
<v Speaker 6>reflecting the sun's light, but she's very far from us,

1077
01:02:35.280 --> 01:02:38.760
<v Speaker 6>and so she actually will look different in size. But

1078
01:02:39.000 --> 01:02:42.000
<v Speaker 6>like the moon, if you can resolve at which we

1079
01:02:42.079 --> 01:02:44.719
<v Speaker 6>can't with our naked eye, but you could actually see

1080
01:02:44.920 --> 01:02:47.679
<v Speaker 6>Venus can have phases in the same way the moon can,

1081
01:02:47.840 --> 01:02:51.360
<v Speaker 6>because you could see just half of Venus lit.

1082
01:02:52.000 --> 01:02:54.840
<v Speaker 1>Oh that's so cool. Well, I know that you are

1083
01:02:54.960 --> 01:02:57.840
<v Speaker 1>an Earth scientist and this is a big question on

1084
01:02:57.840 --> 01:03:02.159
<v Speaker 1>all over minds. Joel Henderson, Karen Nongasa, Arami Pharias wondering

1085
01:03:02.199 --> 01:03:06.239
<v Speaker 1>why all Embardo's Jones girl Averroz, Kate Our Victor and

1086
01:03:06.719 --> 01:03:13.079
<v Speaker 1>avios Le and Thistle wanted to know about Earth and Venus,

1087
01:03:13.159 --> 01:03:16.639
<v Speaker 1>and Kate asked, might climate change increase the likelihood of

1088
01:03:16.760 --> 01:03:20.679
<v Speaker 1>Earth's atmosphere following the path of Venus a lot about

1089
01:03:20.960 --> 01:03:23.920
<v Speaker 1>kind of the climate change. What can we learn about

1090
01:03:24.079 --> 01:03:27.920
<v Speaker 1>climate change and greenhouse gases here that we are looking

1091
01:03:28.000 --> 01:03:29.800
<v Speaker 1>at on Venus.

1092
01:03:30.199 --> 01:03:35.159
<v Speaker 6>Yeah, so Venus is a greenhouse planet, and what we

1093
01:03:35.199 --> 01:03:38.920
<v Speaker 6>can learn is we don't want to go there. Yeah, yeah,

1094
01:03:39.079 --> 01:03:43.480
<v Speaker 6>you know, we don't want greenhouse gases. Now, she's an

1095
01:03:43.480 --> 01:03:48.800
<v Speaker 6>extreme because we all know that CO two is such

1096
01:03:48.840 --> 01:03:53.679
<v Speaker 6>a powerful greenhouse gas, so is methane. But Venus has

1097
01:03:53.719 --> 01:03:58.360
<v Speaker 6>probably as much carbon dioxide as the Earth. But Earth

1098
01:03:58.920 --> 01:04:05.639
<v Speaker 6>has locked that carbon dioxide into rocks, So limestones and

1099
01:04:06.039 --> 01:04:10.719
<v Speaker 6>marbles and those sorts of things are all carbon dioxide,

1100
01:04:11.960 --> 01:04:14.880
<v Speaker 6>have lots and lots of carbon dioxide trapped within them.

1101
01:04:15.320 --> 01:04:19.199
<v Speaker 6>So if we wanted to make Earth like Venus really quickly,

1102
01:04:19.440 --> 01:04:24.239
<v Speaker 6>we would somehow release all that carbon dioxide. So that's

1103
01:04:24.320 --> 01:04:27.760
<v Speaker 6>going to the extreme. But we are making our planet

1104
01:04:28.159 --> 01:04:30.960
<v Speaker 6>too hot. Well, we make it hot so that plate

1105
01:04:31.000 --> 01:04:36.440
<v Speaker 6>tectonics will shut down and regulate. Probably not what we

1106
01:04:36.480 --> 01:04:39.599
<v Speaker 6>will do to this planet going the way we are

1107
01:04:40.280 --> 01:04:43.920
<v Speaker 6>is we are going to make it so that humans

1108
01:04:44.599 --> 01:04:48.320
<v Speaker 6>can't live on this planet anymore. I think the planet

1109
01:04:48.559 --> 01:04:52.119
<v Speaker 6>is going to go on and without us, and we

1110
01:04:52.159 --> 01:04:54.960
<v Speaker 6>will be a blip and it will probably say good

1111
01:04:55.039 --> 01:04:58.960
<v Speaker 6>riddance on that one. Yeah, And so that's what we

1112
01:04:59.039 --> 01:05:02.239
<v Speaker 6>can learn is that you know, this is serious and

1113
01:05:02.440 --> 01:05:05.559
<v Speaker 6>we don't want to go there because it's we're not

1114
01:05:05.599 --> 01:05:07.559
<v Speaker 6>going to ruin the Earth, but we're talking about the

1115
01:05:07.559 --> 01:05:10.119
<v Speaker 6>Earth for us. The Earth is a planet is going

1116
01:05:10.199 --> 01:05:13.239
<v Speaker 6>to go on. It's whether we're going to be a

1117
01:05:13.280 --> 01:05:15.320
<v Speaker 6>part of that or not. And the rate we're going

1118
01:05:16.119 --> 01:05:16.440
<v Speaker 6>it's not.

1119
01:05:17.079 --> 01:05:20.519
<v Speaker 1>Yeah. Are a lot of are more space agencies looking

1120
01:05:20.559 --> 01:05:25.320
<v Speaker 1>to Venus as sort of a prediction model.

1121
01:05:27.840 --> 01:05:32.840
<v Speaker 6>Well, people say that for missions to say, I think

1122
01:05:32.840 --> 01:05:36.519
<v Speaker 6>it's political. Frankly, Oh, we'll learn from And I want

1123
01:05:36.559 --> 01:05:39.320
<v Speaker 6>to say, no, we don't have to take a mission

1124
01:05:39.360 --> 01:05:42.800
<v Speaker 6>there to learn more. We know what we need to

1125
01:05:42.840 --> 01:05:45.920
<v Speaker 6>do and we just have to do it. And by

1126
01:05:45.920 --> 01:05:49.000
<v Speaker 6>saying Venus is going to give us magical answers with that, No,

1127
01:05:49.239 --> 01:05:52.639
<v Speaker 6>we know what we need to do. Yeah, stop procrastinating

1128
01:05:52.760 --> 01:05:56.519
<v Speaker 6>and do it. Yeah, we have the data we need. Yeah,

1129
01:05:56.719 --> 01:05:59.920
<v Speaker 6>Venus is fascinating to study. But not for those reasons.

1130
01:06:00.199 --> 01:06:02.960
<v Speaker 1>Yeah, what is the hardest part about your job? Look,

1131
01:06:03.000 --> 01:06:05.199
<v Speaker 1>get you. It could be petty, it could be huge.

1132
01:06:05.800 --> 01:06:08.760
<v Speaker 6>Yeah. So I'll first say the most fun part of

1133
01:06:08.800 --> 01:06:13.920
<v Speaker 6>my job is doing the exploration with open minds, with students,

1134
01:06:14.440 --> 01:06:18.639
<v Speaker 6>with colleagues, with people in public forums that cause us

1135
01:06:18.679 --> 01:06:21.440
<v Speaker 6>to just ask questions, which I think is so human.

1136
01:06:21.800 --> 01:06:25.159
<v Speaker 6>It's just so human to ask questions. And that's what's

1137
01:06:25.239 --> 01:06:28.480
<v Speaker 6>so much fun. What I don't like about it is

1138
01:06:29.079 --> 01:06:34.719
<v Speaker 6>the science becomes about individuals and about me, me, me,

1139
01:06:35.119 --> 01:06:39.039
<v Speaker 6>and you lose sight of the data and it should

1140
01:06:39.079 --> 01:06:42.000
<v Speaker 6>just be fun to be able to try out different

1141
01:06:42.079 --> 01:06:47.159
<v Speaker 6>hypotheses and say, oh my gosh, okay, that was wrong,

1142
01:06:47.519 --> 01:06:50.760
<v Speaker 6>but we got somewhere because we did the data for

1143
01:06:50.800 --> 01:06:55.079
<v Speaker 6>this reason and that reason. And my colleague Roger Phillips,

1144
01:06:55.239 --> 01:06:59.320
<v Speaker 6>who was that geof physicists who first got me onto venus.

1145
01:06:59.519 --> 01:07:02.360
<v Speaker 6>What was so much fun was working with Roger because

1146
01:07:02.519 --> 01:07:06.000
<v Speaker 6>we could listen to each other, learn from each other,

1147
01:07:06.199 --> 01:07:08.880
<v Speaker 6>bounce things back and forth, and then we could come

1148
01:07:08.960 --> 01:07:10.559
<v Speaker 6>up with something and say ba ba blah, and then

1149
01:07:10.599 --> 01:07:14.320
<v Speaker 6>we come up with other data and say, oh gosh,

1150
01:07:14.559 --> 01:07:17.639
<v Speaker 6>we were wrong, and we could actually even put that

1151
01:07:17.760 --> 01:07:21.239
<v Speaker 6>in the scientific literature. That was an idea at the

1152
01:07:21.280 --> 01:07:24.119
<v Speaker 6>time it fit the data, But now we have more

1153
01:07:24.199 --> 01:07:27.639
<v Speaker 6>data that was wrong, and that's okay. If you're not

1154
01:07:27.840 --> 01:07:31.760
<v Speaker 6>making mistakes, you are not doing science. Oh I love that,

1155
01:07:32.079 --> 01:07:36.320
<v Speaker 6>And that's my biggest frustration. And I see that so

1156
01:07:36.800 --> 01:07:40.320
<v Speaker 6>much of hanging on to things that I know people

1157
01:07:40.480 --> 01:07:43.519
<v Speaker 6>know are wrong, and when we're looking at something so

1158
01:07:44.119 --> 01:07:48.320
<v Speaker 6>interesting and exciting as how planets work and evolve and

1159
01:07:48.440 --> 01:07:52.199
<v Speaker 6>interact through time, is that we're going to be wrong

1160
01:07:52.679 --> 01:07:56.320
<v Speaker 6>so much of the time. And that's okay, that's how

1161
01:07:56.320 --> 01:07:58.920
<v Speaker 6>we learn. But the fun of it is to put

1162
01:07:58.960 --> 01:08:03.800
<v Speaker 6>things together, and you need consistency and that attitude that

1163
01:08:03.960 --> 01:08:09.480
<v Speaker 6>science is right, science is fluid, science is ever changing.

1164
01:08:09.920 --> 01:08:13.960
<v Speaker 6>And that's what bugs me the most is that not

1165
01:08:14.079 --> 01:08:17.479
<v Speaker 6>making mistakes, you know, and not admitting that we're wrong.

1166
01:08:17.640 --> 01:08:20.880
<v Speaker 6>I'm wrong so many times, so so so many times,

1167
01:08:21.000 --> 01:08:22.039
<v Speaker 6>and that's how I learn.

1168
01:08:22.319 --> 01:08:25.039
<v Speaker 1>That's the best message ever. And I feel like, even

1169
01:08:25.279 --> 01:08:28.840
<v Speaker 1>even for a creative field, it's like, make mistakes, try something.

1170
01:08:28.880 --> 01:08:30.960
<v Speaker 1>It does not have to be perfect the first time out.

1171
01:08:31.279 --> 01:08:33.840
<v Speaker 6>No, or the tenth or the what happened? I just

1172
01:08:33.960 --> 01:08:36.880
<v Speaker 6>keep you know. I'm a potter. I play with Clay,

1173
01:08:36.920 --> 01:08:39.279
<v Speaker 6>I love it and it's like, oh yead, I just

1174
01:08:39.399 --> 01:08:43.760
<v Speaker 6>absolutely blew that, and you know, I learn from it.

1175
01:08:43.840 --> 01:08:46.640
<v Speaker 6>Sometimes it takes me several times before I learn from it.

1176
01:08:46.760 --> 01:08:49.199
<v Speaker 6>But if I didn't make those mistakes, I wouldn't learn.

1177
01:08:49.239 --> 01:08:51.960
<v Speaker 6>And you're right, it has to go with every bit

1178
01:08:52.000 --> 01:08:54.920
<v Speaker 6>of life that we're going to make mistakes and that's

1179
01:08:54.960 --> 01:08:57.600
<v Speaker 6>how we learn. And that's okay.

1180
01:08:57.840 --> 01:09:00.920
<v Speaker 1>Do you have a favorite thing about Venus that like

1181
01:09:01.359 --> 01:09:06.560
<v Speaker 1>someone is absolutely disinterested, like what is your favorite? Like boom,

1182
01:09:06.680 --> 01:09:09.159
<v Speaker 1>and then some's like holy smokes.

1183
01:09:09.279 --> 01:09:13.279
<v Speaker 6>Oh wow, that's a really interesting question. You know. I

1184
01:09:13.279 --> 01:09:16.600
<v Speaker 6>think it's different for different people, and so my favorite

1185
01:09:16.680 --> 01:09:22.760
<v Speaker 6>thing is to talk to people about Venus because there

1186
01:09:22.760 --> 01:09:27.159
<v Speaker 6>are so many different ways you can surprise them and

1187
01:09:27.800 --> 01:09:30.640
<v Speaker 6>say and it's never going to be the same for

1188
01:09:30.720 --> 01:09:34.439
<v Speaker 6>all people. Like thinking that you could fly across the

1189
01:09:34.479 --> 01:09:38.199
<v Speaker 6>surface is just mind boggling. To think that you could

1190
01:09:38.279 --> 01:09:42.159
<v Speaker 6>have two birthdays and one day will blow some people's minds.

1191
01:09:42.399 --> 01:09:45.600
<v Speaker 6>There are so many amazing things that she tells us,

1192
01:09:45.800 --> 01:09:47.239
<v Speaker 6>and I think that's the fun.

1193
01:09:47.600 --> 01:09:50.119
<v Speaker 1>I feel like I know her so much better now.

1194
01:09:50.359 --> 01:09:51.560
<v Speaker 1>I feel like she's a friend.

1195
01:09:52.359 --> 01:09:56.000
<v Speaker 6>She is she she's a friend, She's a tease. She

1196
01:09:56.439 --> 01:10:01.000
<v Speaker 6>laughs a lot. You know, she is just you know,

1197
01:10:01.039 --> 01:10:02.439
<v Speaker 6>she's having a great time up there.

1198
01:10:02.680 --> 01:10:05.920
<v Speaker 1>Yeah. I love this. I'll look for her in the sky.

1199
01:10:06.920 --> 01:10:09.439
<v Speaker 6>Yeah, and she will smile down on you.

1200
01:10:09.760 --> 01:10:13.880
<v Speaker 1>Yeah. This has been amazing. Vickey, you are just a gem,

1201
01:10:13.960 --> 01:10:20.760
<v Speaker 1>an absolute gem, as are you. So ask planetary people

1202
01:10:21.039 --> 01:10:23.920
<v Speaker 1>ambiguous questions because that is how you learn and that

1203
01:10:24.079 --> 01:10:26.079
<v Speaker 1>is how you make friends. So thank you so much,

1204
01:10:26.119 --> 01:10:28.640
<v Speaker 1>doctor Vicki Hanson for spending your time with me to

1205
01:10:28.760 --> 01:10:32.479
<v Speaker 1>wax scientific about our new planet of obsession. I love Venus.

1206
01:10:32.520 --> 01:10:34.520
<v Speaker 1>Now you can find out more about Vicki at the

1207
01:10:34.560 --> 01:10:36.520
<v Speaker 1>links in the show notes, and of course more links

1208
01:10:36.560 --> 01:10:38.960
<v Speaker 1>to studies and mission data and photos and books are

1209
01:10:39.000 --> 01:10:41.479
<v Speaker 1>on our website at aliward dot com, slash ology slash

1210
01:10:41.640 --> 01:10:44.560
<v Speaker 1>venus Ology. We are at Ologies on Blue Sky and Instagram.

1211
01:10:44.560 --> 01:10:47.319
<v Speaker 1>I'm at Ali Ward. Ali has one l on both.

1212
01:10:47.520 --> 01:10:49.920
<v Speaker 1>Thank you again to patrons of ologies for supporting the

1213
01:10:49.960 --> 01:10:51.960
<v Speaker 1>show for as little as a dollar a month. Thanks

1214
01:10:52.000 --> 01:10:55.119
<v Speaker 1>to all those out there in ologies, merch promologiesmerch dot

1215
01:10:55.199 --> 01:10:59.239
<v Speaker 1>com also heads Upsmologies are shorter kid friendly versions of

1216
01:10:59.279 --> 01:11:02.439
<v Speaker 1>ologies episode. They're in their own podcast speed so just

1217
01:11:02.680 --> 01:11:05.840
<v Speaker 1>search for smologies SMO L O G I E. S.

1218
01:11:05.880 --> 01:11:09.279
<v Speaker 1>Wherever you get your podcasts, please do subscribe. Tell Friends.

1219
01:11:09.560 --> 01:11:13.119
<v Speaker 1>Aaron Talbert admins Theologies podcast Facebook group. Aveline Malik makes

1220
01:11:13.159 --> 01:11:16.079
<v Speaker 1>our professional transcripts. Kelly ar dwired as the website. Noel

1221
01:11:16.199 --> 01:11:20.119
<v Speaker 1>Dilworth works out our trajectories as scheduling producer. Mission Captain

1222
01:11:20.199 --> 01:11:23.000
<v Speaker 1>is managing director. Susan Hale. Jake Chafey stitches all our

1223
01:11:23.079 --> 01:11:26.680
<v Speaker 1>data together as editor and overseeing those pieces as lead editor.

1224
01:11:26.760 --> 01:11:30.039
<v Speaker 1>Mercedes Maitland of Maitland Audio. Nick Thorburn made the theme music.

1225
01:11:30.039 --> 01:11:31.439
<v Speaker 1>And if you stick around to the very very end,

1226
01:11:31.520 --> 01:11:33.079
<v Speaker 1>you know I may tell you a secret this week.

1227
01:11:33.319 --> 01:11:37.319
<v Speaker 1>Secret number one the evening of January fifteenth, twenty twenty six,

1228
01:11:37.479 --> 01:11:39.840
<v Speaker 1>in La, I'm co hosting like a Drink and Draw

1229
01:11:39.920 --> 01:11:42.760
<v Speaker 1>kind of community art and science event with your favorite

1230
01:11:42.880 --> 01:11:46.520
<v Speaker 1>squid expert, doctor Sarah McNulty. And tickets are fifteen bucks.

1231
01:11:46.560 --> 01:11:48.039
<v Speaker 1>I'll link them in the show notes, but we only

1232
01:11:48.079 --> 01:11:50.439
<v Speaker 1>have about thirty tickets left, so you can get them

1233
01:11:50.439 --> 01:11:53.960
<v Speaker 1>while they are as hot as Venus rocks, folks. It'll

1234
01:11:54.000 --> 01:11:58.600
<v Speaker 1>sell out pretty quickly. Second secret is that I fully

1235
01:11:58.680 --> 01:12:02.560
<v Speaker 1>thought Venus was a gas planet until this conversation I'm

1236
01:12:02.600 --> 01:12:05.119
<v Speaker 1>not a big planet person. I don't know as much

1237
01:12:05.159 --> 01:12:08.439
<v Speaker 1>as like a third grader, but I knew gases were involved.

1238
01:12:08.680 --> 01:12:11.319
<v Speaker 1>I thought maybe the whole thing was gas. And now

1239
01:12:11.439 --> 01:12:13.840
<v Speaker 1>I know so much more about venus. And now I

1240
01:12:13.920 --> 01:12:15.960
<v Speaker 1>care about venus because I asked more questions. So let

1241
01:12:16.000 --> 01:12:18.239
<v Speaker 1>that be a lesson to assault. So go forth into

1242
01:12:18.279 --> 01:12:21.760
<v Speaker 1>this dawn of twenty twenty six. Do things quickly, do

1243
01:12:21.840 --> 01:12:25.920
<v Speaker 1>them imperfectly. Learn as you go. Things worth doing have

1244
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<v Speaker 1>to pass through these thick, noxious clouds of fear and apprehension.

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<v Speaker 1>No one is immune to them. Don't let fear waste

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<v Speaker 1>your precious time on Earth. Just go forth do this stuff,

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<v Speaker 1>okay forbye?

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<v Speaker 7>Pachadermatologymmeology, crypto zoology, lithology, technology, meteorology, feratology, nathology, seriology, elinology.

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<v Speaker 6>You are a beautiful venus.

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<v Speaker 5>You make time to move, to breathe, to check your stamina,

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<v Speaker 5>your sleep, your steps.

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<v Speaker 6>But when did you last look at health insurance.

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<v Speaker 1>For you or those you care about?

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<v Speaker 6>With the Health Insurance Authority Comparison Tool, you can. It's quick,

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<v Speaker 6>free and completely impartial. Compare every health insurance plan and

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<v Speaker 6>find the right cover for you. The health insurance Authority

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<v Speaker 6>time online, spend well, make your next click count h

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<v Speaker 6>I A dot Ie. The Health Insurance Authority is a

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<v Speaker 6>regulatory body under the Government of Ireland.
