1 00:00:03,000 --> 00:00:06,760 Speaker 1: Welcome to Stuff to Blow Your Mind production of iHeartRadio. 2 00:00:12,720 --> 00:00:15,160 Speaker 2: Hey, welcome to Stuff to Blow Your Mind. My name 3 00:00:15,200 --> 00:00:16,520 Speaker 2: is Robert Lamb and. 4 00:00:16,440 --> 00:00:18,919 Speaker 3: I am Joe McCormick, and we're back with part two 5 00:00:19,079 --> 00:00:23,279 Speaker 3: in our series on Jupiter's innermost moon, Io, the most 6 00:00:23,360 --> 00:00:27,080 Speaker 3: volcanic body in our Solar system, and, as I argued 7 00:00:27,120 --> 00:00:29,560 Speaker 3: in the last episode, one of the most fascinating and 8 00:00:29,680 --> 00:00:33,120 Speaker 3: dramatic places we know of beyond Earth. So if you 9 00:00:33,120 --> 00:00:35,479 Speaker 3: haven't heard part one, we would recommend going back to 10 00:00:35,520 --> 00:00:38,440 Speaker 3: listen to that one first. But for a brief recap 11 00:00:38,479 --> 00:00:41,280 Speaker 3: of what we talked about last time. We started off 12 00:00:41,320 --> 00:00:44,840 Speaker 3: talking about how I got interested in revisiting Io because 13 00:00:44,840 --> 00:00:47,440 Speaker 3: we did do a series of episodes on Jupiter's moons 14 00:00:47,479 --> 00:00:50,480 Speaker 3: at large several years back, but I wanted to come 15 00:00:50,520 --> 00:00:53,120 Speaker 3: back and do a closer pass on Io, in particular 16 00:00:53,400 --> 00:00:56,920 Speaker 3: because I got visually obsessed with some images produced by 17 00:00:56,960 --> 00:00:59,800 Speaker 3: the NASA Juno mission in the past year or so. 18 00:01:00,000 --> 00:01:02,280 Speaker 3: Guess it's actually little bit over a year because some 19 00:01:02,360 --> 00:01:04,560 Speaker 3: of the data that we were looking at was collected 20 00:01:04,560 --> 00:01:07,840 Speaker 3: in late twenty twenty three. But we talked about several 21 00:01:07,880 --> 00:01:13,000 Speaker 3: of these images in detail, about the strangely polychrome surface 22 00:01:13,040 --> 00:01:17,920 Speaker 3: of the Moon and its truly fascinating surface features, including 23 00:01:18,000 --> 00:01:25,120 Speaker 3: gigantic blade like mountains, vast sulfurous plains, hundreds of erupting volcanoes, 24 00:01:25,640 --> 00:01:30,240 Speaker 3: enormous hellish lava lakes rippling with lava waves, and lava 25 00:01:30,280 --> 00:01:35,280 Speaker 3: flows stretching hundreds of kilometers, all situated within a land 26 00:01:35,360 --> 00:01:38,800 Speaker 3: that is at once burning hot and freezing cold. So 27 00:01:38,840 --> 00:01:41,400 Speaker 3: it is, as Bart Simpson might say, a land of contrasts, 28 00:01:41,440 --> 00:01:46,119 Speaker 3: but also just a place of enormous physical and sort 29 00:01:46,120 --> 00:01:49,640 Speaker 3: of geological drama. We also talked a little bit about 30 00:01:49,680 --> 00:01:52,400 Speaker 3: the history of the exploration of Io, at least going 31 00:01:52,400 --> 00:01:55,680 Speaker 3: back to Carl Sagan's account of the discoveries made by 32 00:01:55,680 --> 00:02:00,480 Speaker 3: the Voyager Probe in nineteen seventy nine. Around then talked 33 00:02:00,480 --> 00:02:04,840 Speaker 3: about the extremely thin sulfur dioxide atmosphere of Io, which 34 00:02:04,880 --> 00:02:09,080 Speaker 3: is generated initially by venting from the Moon's volcanoes and 35 00:02:09,120 --> 00:02:13,720 Speaker 3: subsequently by the cyclical freezing and sublimation of sulfur dioxide 36 00:02:13,760 --> 00:02:16,600 Speaker 3: frost on the surface, freezing when the Moon passes into 37 00:02:16,680 --> 00:02:20,440 Speaker 3: Jupiter's shadow, then transitioning into gas again once back in 38 00:02:20,440 --> 00:02:23,480 Speaker 3: the sunlight. We also talked a good bit about the 39 00:02:23,680 --> 00:02:27,840 Speaker 3: Greek myth of the Moon's namesake, sort of the themes of 40 00:02:27,880 --> 00:02:32,280 Speaker 3: the Io story, especially in Ovid's telling and other versions 41 00:02:32,280 --> 00:02:35,000 Speaker 3: of the story, and the way the tale was said 42 00:02:35,080 --> 00:02:40,080 Speaker 3: in ancient times to interlock with Egyptian religious figures such 43 00:02:40,080 --> 00:02:43,160 Speaker 3: as the goddess Isis, Shepherd of the dead, and the 44 00:02:43,200 --> 00:02:46,400 Speaker 3: Sacred Mother of Pharaoh's And we are back today to 45 00:02:46,480 --> 00:02:48,120 Speaker 3: talk once again about Io. 46 00:02:48,440 --> 00:02:48,960 Speaker 2: That's right. 47 00:02:49,560 --> 00:02:53,079 Speaker 3: So there's something we didn't really talk about at all 48 00:02:53,200 --> 00:02:56,880 Speaker 3: last time, and that was the use of IO as 49 00:02:56,919 --> 00:03:00,600 Speaker 3: a setting or plot device in science fiction, which, you know, 50 00:03:00,800 --> 00:03:03,880 Speaker 3: despite all of its, at least to me, really apparent 51 00:03:03,960 --> 00:03:07,560 Speaker 3: aesthetic virtues as a setting for a story, it doesn't 52 00:03:07,720 --> 00:03:10,200 Speaker 3: really seem to be a favorite place within our solar 53 00:03:10,200 --> 00:03:12,720 Speaker 3: system for sci fi writers. Or maybe I'm wrong about that. 54 00:03:12,760 --> 00:03:14,880 Speaker 3: Maybe it's just not in a lot of stories I've read. 55 00:03:14,919 --> 00:03:18,720 Speaker 3: But I was having trouble thinking of many examples in 56 00:03:18,760 --> 00:03:22,120 Speaker 3: which it featured in stories I knew. I think it 57 00:03:22,240 --> 00:03:26,840 Speaker 3: showed up at some point briefly in the Expanse, and 58 00:03:27,360 --> 00:03:29,679 Speaker 3: I can't really think of many other examples. 59 00:03:29,600 --> 00:03:32,880 Speaker 2: Yeah, even in the Expanse. And I'm a little foggy 60 00:03:32,960 --> 00:03:36,440 Speaker 2: on where it shows up or doesn't show up if 61 00:03:36,480 --> 00:03:39,320 Speaker 2: it's in the novels by James S. A. Corey, or 62 00:03:39,360 --> 00:03:41,960 Speaker 2: if it's in the TV adaptation. I've only read the 63 00:03:42,000 --> 00:03:44,440 Speaker 2: first book in the series, Leviathan Wiggs, but I watched 64 00:03:44,480 --> 00:03:48,000 Speaker 2: the entire run of the show. But even then, I 65 00:03:48,040 --> 00:03:50,520 Speaker 2: think maybe it only partially factored in there. And I 66 00:03:50,520 --> 00:03:54,840 Speaker 2: think one of the possibilities here is that i Owe 67 00:03:55,000 --> 00:03:58,480 Speaker 2: is a moon that we know to be rather extreme 68 00:03:58,520 --> 00:04:03,760 Speaker 2: and hostile, for even our sci fi visions and fantasies 69 00:04:04,160 --> 00:04:07,000 Speaker 2: tend to give it a little safe distance. 70 00:04:07,040 --> 00:04:10,320 Speaker 3: You know, it doesn't seem like a top candidate for colonization. 71 00:04:11,000 --> 00:04:15,960 Speaker 4: Yeah, yeah, in well, I don't want to spoil too 72 00:04:16,040 --> 00:04:18,800 Speaker 4: much of the plot if people aren't familiar with the expanse, 73 00:04:18,839 --> 00:04:21,520 Speaker 4: but I do remember it pops up as the location 74 00:04:21,680 --> 00:04:23,680 Speaker 4: of a quite cursed laboratory. 75 00:04:24,520 --> 00:04:28,040 Speaker 2: Yes, they're working on a particular molecule. Yes, yes. Now. 76 00:04:28,040 --> 00:04:31,159 Speaker 2: One place you do see Io pop up as a 77 00:04:31,200 --> 00:04:35,080 Speaker 2: setting is the nineteen eighty one gritty sci fi western Outland. 78 00:04:35,880 --> 00:04:39,279 Speaker 2: This one starred Sean Connery and Peter Boyle, has some 79 00:04:39,320 --> 00:04:42,520 Speaker 2: other fairly big names sprinkled throughout the cast as well. 80 00:04:42,560 --> 00:04:45,400 Speaker 2: Directed by Peter Hyam's and I guess they chose Io 81 00:04:45,520 --> 00:04:48,040 Speaker 2: as a setting here because it would be such a 82 00:04:48,080 --> 00:04:52,560 Speaker 2: horrible place to work. It's the horrible working conditions and 83 00:04:52,760 --> 00:04:55,479 Speaker 2: there's a lot of like labor dispute in this particular 84 00:04:55,560 --> 00:04:58,080 Speaker 2: sci fi vision, you know, eighty one, that's not too 85 00:04:58,120 --> 00:05:01,680 Speaker 2: long after Ridley Scott's a and it's a film that 86 00:05:01,720 --> 00:05:05,440 Speaker 2: you could almost assume to be in the same universe, 87 00:05:05,520 --> 00:05:10,120 Speaker 2: you know. It's that sort of very gritty, essentially near 88 00:05:10,240 --> 00:05:14,920 Speaker 2: future vision of science fiction that is very much focused 89 00:05:14,960 --> 00:05:17,120 Speaker 2: on like the working man in space. 90 00:05:17,560 --> 00:05:19,760 Speaker 3: I have meant to see this for years and never 91 00:05:19,839 --> 00:05:22,920 Speaker 3: have it. It's intrigued me ever since my days of 92 00:05:22,960 --> 00:05:26,359 Speaker 3: like in high school flipping through you know, stacks of 93 00:05:26,440 --> 00:05:30,640 Speaker 3: DVDs at the used bookstore in town because it really 94 00:05:30,680 --> 00:05:34,160 Speaker 3: pops because it's Sean Connery holding a shotgun, dressed like 95 00:05:34,200 --> 00:05:38,240 Speaker 3: a cop, except he's in space. So strange vibes from 96 00:05:38,279 --> 00:05:40,800 Speaker 3: the get go. But I've read that if you didn't 97 00:05:40,800 --> 00:05:43,359 Speaker 3: already say this, I've read that this one is supposed 98 00:05:43,400 --> 00:05:45,520 Speaker 3: to be like a Western but in space. 99 00:05:45,920 --> 00:05:48,360 Speaker 2: Correct. Yeah, And I saw it many many years ago, 100 00:05:48,520 --> 00:05:51,680 Speaker 2: but I'm a little foggy on the details. But it 101 00:05:51,760 --> 00:05:54,120 Speaker 2: is gritty, it is very much a Western in space. 102 00:05:54,800 --> 00:05:59,200 Speaker 2: A lot of it concerns explosive decompression, people's heads exploding 103 00:05:59,240 --> 00:06:04,920 Speaker 2: inside a set of suits, and yeah, terrible labor conditions. Now, 104 00:06:04,920 --> 00:06:06,920 Speaker 2: one thing about it that I wasn't familiar with until 105 00:06:06,960 --> 00:06:09,800 Speaker 2: very recently is there was a comic book adaptation of 106 00:06:09,839 --> 00:06:14,839 Speaker 2: it for heavy metal, I believe, by comics legend Jim Staranco, 107 00:06:15,480 --> 00:06:17,920 Speaker 2: and I include a few stills from it here for you, Joe. 108 00:06:17,920 --> 00:06:21,240 Speaker 2: I've seen people talk about this online almost in terms 109 00:06:21,240 --> 00:06:23,680 Speaker 2: of like a lost classic, Like it's apparently hard to 110 00:06:23,680 --> 00:06:27,520 Speaker 2: get your hands on, but it's got some very impressive 111 00:06:27,600 --> 00:06:31,920 Speaker 2: line work and just some really beautiful imagery. I mean, 112 00:06:32,520 --> 00:06:34,960 Speaker 2: like I say that the film itself has a very 113 00:06:35,320 --> 00:06:39,320 Speaker 2: gritty air to it, and that flavor is still present 114 00:06:39,360 --> 00:06:41,800 Speaker 2: in the comic book apparently, but it also has this 115 00:06:41,880 --> 00:06:44,960 Speaker 2: like extra like wilder vibe going on. 116 00:06:45,520 --> 00:06:48,039 Speaker 3: Oh yeah, it's one of those comic book art styles 117 00:06:48,080 --> 00:06:53,080 Speaker 3: where even apparently static objects seem to radiate with energy. 118 00:06:53,240 --> 00:06:56,239 Speaker 3: It's just I don't know what you call that style, 119 00:06:56,240 --> 00:07:00,479 Speaker 3: but it's where everything looks dynamic, like the style of 120 00:07:00,600 --> 00:07:04,200 Speaker 3: drawing is of a reality in which everything is about 121 00:07:04,240 --> 00:07:05,000 Speaker 3: to explode. 122 00:07:05,440 --> 00:07:07,239 Speaker 2: Yeah, I'd be very interested to hear from anyone who's 123 00:07:07,240 --> 00:07:09,280 Speaker 2: read the comic book. There was also an Alan Deine 124 00:07:09,320 --> 00:07:12,360 Speaker 2: Foster novelization, so it has that in common with Alien 125 00:07:12,920 --> 00:07:18,720 Speaker 2: and Aliens and Alien three as well. But as far 126 00:07:18,800 --> 00:07:22,920 Speaker 2: as the treatment of Io in the motion picture and 127 00:07:22,960 --> 00:07:26,520 Speaker 2: in the comic book, basically it's a hell world where 128 00:07:26,560 --> 00:07:30,440 Speaker 2: they just decided to put a mining colony of some 129 00:07:30,480 --> 00:07:35,800 Speaker 2: sort and then prioritize profits over human safety. Yeah, so 130 00:07:35,840 --> 00:07:37,520 Speaker 2: it's the perfect setting for that. Now I had to 131 00:07:37,600 --> 00:07:40,240 Speaker 2: hunt around a little bit more defined examples of Io 132 00:07:40,560 --> 00:07:42,920 Speaker 2: being used as a setting in other sci fi visions. 133 00:07:43,240 --> 00:07:46,280 Speaker 2: There's a nineteen ninety four mini series titled Escape from 134 00:07:46,360 --> 00:07:50,720 Speaker 2: Jupiter that concerns an escape from Io. Apparently it's an 135 00:07:50,760 --> 00:07:55,040 Speaker 2: Australian kids adventure and it's also has Steve Bisley in it, 136 00:07:55,080 --> 00:07:56,840 Speaker 2: who's in a number of I think it was in 137 00:07:56,880 --> 00:07:58,480 Speaker 2: at least one of the Mad Max films. 138 00:07:58,800 --> 00:08:01,840 Speaker 3: Oh, okay, I don't reckon him by name. Yeah, well 139 00:08:01,920 --> 00:08:04,480 Speaker 3: maybe what if I saw him? Is this a screenshot 140 00:08:04,520 --> 00:08:06,080 Speaker 3: you've got from it with the bright colors? 141 00:08:06,400 --> 00:08:09,760 Speaker 2: Yes, it's one of the most nineteen nineties TV images 142 00:08:09,800 --> 00:08:11,600 Speaker 2: you could possibly look up online. 143 00:08:11,760 --> 00:08:13,880 Speaker 3: Yeah, what what was the name of it? Wasn't there 144 00:08:13,920 --> 00:08:17,480 Speaker 3: like a Canadian kids sci fi show, sort of a 145 00:08:17,480 --> 00:08:21,240 Speaker 3: Star Trek for kids that was on Nickelodeon in the nineties. 146 00:08:21,360 --> 00:08:23,560 Speaker 3: It was like Space Cases or something. 147 00:08:24,440 --> 00:08:26,600 Speaker 2: Maybe that's ringing a bell only. 148 00:08:26,480 --> 00:08:28,960 Speaker 3: The foggiest memory, but this is reminding me of that, 149 00:08:29,000 --> 00:08:31,440 Speaker 3: except I recall that had a darker look and this 150 00:08:31,560 --> 00:08:32,480 Speaker 3: is very pastel. 151 00:08:33,840 --> 00:08:38,640 Speaker 2: Now. There's also a twenty nineteen film titled Io. This 152 00:08:38,760 --> 00:08:41,400 Speaker 2: was apparently one that was put out on Netflix and 153 00:08:41,480 --> 00:08:44,720 Speaker 2: I haven't seen it, but it concerns refugees of a 154 00:08:44,760 --> 00:08:48,440 Speaker 2: destroyed Earth living on a space station near Io. It 155 00:08:48,520 --> 00:08:52,520 Speaker 2: stars Margaret Qualley of the Substance fame, Anthony Mackie, and 156 00:08:52,640 --> 00:08:54,960 Speaker 2: Danny Houston. Again, I haven't seen this one, but apparently 157 00:08:54,960 --> 00:08:58,559 Speaker 2: it's one. It was released on Netflix. I have to say, 158 00:08:58,600 --> 00:09:00,680 Speaker 2: in the one still I found from or a production 159 00:09:01,160 --> 00:09:05,040 Speaker 2: image promotionary image, doesn't look very pizza in the background. 160 00:09:05,480 --> 00:09:08,880 Speaker 3: No looks this is very gray. One of those shows 161 00:09:08,880 --> 00:09:11,520 Speaker 3: where all the colors washed out. To be fair, this 162 00:09:11,600 --> 00:09:13,560 Speaker 3: is just a still. I don't know the show, but 163 00:09:14,320 --> 00:09:17,280 Speaker 3: marketing department is not selling me on it with this 164 00:09:17,800 --> 00:09:18,640 Speaker 3: color here. 165 00:09:20,200 --> 00:09:23,480 Speaker 2: All right. Now, In terms of written sci fi, there 166 00:09:23,480 --> 00:09:25,800 Speaker 2: are at least there at least two examples to call out. 167 00:09:26,000 --> 00:09:29,920 Speaker 2: There's The Mad Moon by Stanley Jen g Weinbaum. This 168 00:09:29,960 --> 00:09:34,400 Speaker 2: is from nineteen thirty five, same individual who wrote a 169 00:09:34,400 --> 00:09:38,440 Speaker 2: Martian Odyssey, and it features two different alien species that 170 00:09:38,480 --> 00:09:40,760 Speaker 2: are supposed to be native to Io and there's a 171 00:09:40,800 --> 00:09:43,640 Speaker 2: human colony. I haven't read that one, but I did 172 00:09:43,720 --> 00:09:46,320 Speaker 2: read a story he wrote titled The Planet of Doubt, 173 00:09:46,760 --> 00:09:48,959 Speaker 2: which I did a Monster Fact episode back in twenty 174 00:09:49,000 --> 00:09:51,440 Speaker 2: twenty three, So I'm going to make sure that I 175 00:09:51,520 --> 00:09:55,040 Speaker 2: re air that one either this week or the following 176 00:09:55,080 --> 00:09:57,040 Speaker 2: week so you don't have to go look it up again. 177 00:09:57,080 --> 00:09:59,959 Speaker 2: But it's a pretty fun one. This guy had a real, 178 00:10:00,000 --> 00:10:04,440 Speaker 2: real creative mind for dreaming up alien creatures that you know, 179 00:10:04,520 --> 00:10:09,280 Speaker 2: often reflected some of the stranger biological examples we have 180 00:10:09,320 --> 00:10:11,720 Speaker 2: on our own planet, but with you know, a nineteen 181 00:10:11,800 --> 00:10:14,840 Speaker 2: thirties or slightly later sci fi spin. 182 00:10:15,400 --> 00:10:18,760 Speaker 3: But now nineteen thirties, so that's long before Voyager. I'm 183 00:10:18,800 --> 00:10:21,720 Speaker 3: wondering what did we actually know about Io at that 184 00:10:21,800 --> 00:10:25,320 Speaker 3: point to inform a vision of the biology that would 185 00:10:25,320 --> 00:10:26,000 Speaker 3: arise there. 186 00:10:26,640 --> 00:10:29,200 Speaker 2: Well, that may maybe not enough to know that two 187 00:10:29,240 --> 00:10:34,000 Speaker 2: indigenous species of any human colony were not maybe that likely. 188 00:10:34,880 --> 00:10:37,880 Speaker 2: We have some caveats on the whole life on IO thing. Well, 189 00:10:37,920 --> 00:10:41,000 Speaker 2: we'll come back to it though. Another one that came 190 00:10:41,000 --> 00:10:44,079 Speaker 2: out though is The Very Pulse of the Machine by 191 00:10:44,160 --> 00:10:48,000 Speaker 2: Michael Swanwick. This is from nineteen ninety eight and it 192 00:10:48,080 --> 00:10:52,920 Speaker 2: concerns a possibly sentient IO. It was adapted into an 193 00:10:52,920 --> 00:10:56,720 Speaker 2: episode of Love, Death and Robots on Netflix again, Netflix 194 00:10:56,760 --> 00:11:00,679 Speaker 2: loves Io with the main character voice by McKinsey Davis, 195 00:11:01,400 --> 00:11:03,319 Speaker 2: who's been in things like Halden Catch Fire and I 196 00:11:03,360 --> 00:11:05,200 Speaker 2: believe the more recent Blade Runner of film. 197 00:11:05,559 --> 00:11:08,319 Speaker 3: So when you say sentient io, you're talking about the 198 00:11:08,920 --> 00:11:12,960 Speaker 3: moon itself, the planetary body being a sentient organism or 199 00:11:13,080 --> 00:11:14,240 Speaker 3: sentient in some way. 200 00:11:14,600 --> 00:11:17,440 Speaker 2: Yes, I believe so, And I haven't read the story, 201 00:11:17,520 --> 00:11:21,480 Speaker 2: but I have seen this episode of Love, Death and Robots, 202 00:11:22,080 --> 00:11:24,240 Speaker 2: and I just the only thing I remember about it 203 00:11:24,280 --> 00:11:27,320 Speaker 2: is that it looked beautiful and it concerned bad things 204 00:11:27,360 --> 00:11:29,480 Speaker 2: happening in space on the Moon. 205 00:11:31,400 --> 00:11:34,480 Speaker 3: That sounds kind of like silarious, But having not seen it, 206 00:11:34,520 --> 00:11:37,360 Speaker 3: I don't want to be overly broad about that. 207 00:11:37,600 --> 00:11:41,720 Speaker 2: But there's a fair amount of variety in Love, Death 208 00:11:41,760 --> 00:11:44,640 Speaker 2: and Robots. It's a really fun series, but there are 209 00:11:44,679 --> 00:11:47,120 Speaker 2: a number of episodes I think that you can describe 210 00:11:47,160 --> 00:11:50,600 Speaker 2: as bad things happen to people in space. So maybe 211 00:11:50,640 --> 00:11:52,520 Speaker 2: some of those bleed together in my memory. 212 00:11:52,840 --> 00:11:54,920 Speaker 3: I'm going to write some sci fi where only good 213 00:11:54,960 --> 00:11:56,400 Speaker 3: things happen to people in space. 214 00:11:56,679 --> 00:11:58,160 Speaker 2: There you go, That's what we need, you know, we 215 00:11:58,160 --> 00:12:01,560 Speaker 2: need a dash of the more of the Star Trek 216 00:12:01,600 --> 00:12:02,920 Speaker 2: optimism these days. 217 00:12:03,400 --> 00:12:06,600 Speaker 3: Like page three hundred, people just wake up, Oh splendid 218 00:12:06,679 --> 00:12:10,440 Speaker 3: day once again, smooth sailing. 219 00:12:11,160 --> 00:12:12,840 Speaker 2: So that's what I've got. Now, there may be some 220 00:12:12,920 --> 00:12:17,720 Speaker 2: other fantastic examples or just even marginally interesting examples of 221 00:12:17,760 --> 00:12:20,680 Speaker 2: IO in science fiction. So if you have any of those, 222 00:12:21,000 --> 00:12:24,040 Speaker 2: do write in. We'd love to share them with everyone 223 00:12:24,040 --> 00:12:25,880 Speaker 2: else on a future listener mail episode. 224 00:12:26,080 --> 00:12:28,720 Speaker 3: Yeah, especially if it's something that takes the real physical 225 00:12:28,800 --> 00:12:32,600 Speaker 3: characteristics of IO seriously as either a source of creating 226 00:12:32,640 --> 00:12:35,360 Speaker 3: alien biology or something people on the planet would have 227 00:12:35,600 --> 00:12:37,760 Speaker 3: on the moon would have to live with. Yeah, right 228 00:12:37,840 --> 00:12:40,320 Speaker 3: in contact at stuff to Blow your mind dot com. 229 00:12:40,679 --> 00:12:43,240 Speaker 2: Yeah again. One of the challenges though, is we've been 230 00:12:43,240 --> 00:12:45,600 Speaker 2: discussing it and will continue to discuss It's just it's 231 00:12:45,600 --> 00:12:49,160 Speaker 2: a very extreme place. There are there are I'm not 232 00:12:49,200 --> 00:12:51,880 Speaker 2: going to say there are more interesting Jovian moons, But 233 00:12:51,960 --> 00:12:54,840 Speaker 2: there are other Jovian moons that are better candidates for 234 00:12:54,960 --> 00:12:58,880 Speaker 2: things like some sort of life form being present there potentially, 235 00:12:59,120 --> 00:13:04,600 Speaker 2: or there being some possibility for human colonization or outpost efforts, 236 00:13:04,600 --> 00:13:05,040 Speaker 2: and so. 237 00:13:04,960 --> 00:13:17,000 Speaker 3: Forth, bridging to the next thing I wanted to talk about. 238 00:13:17,040 --> 00:13:20,080 Speaker 3: Even though Io, and as you said, we'll get into 239 00:13:20,080 --> 00:13:22,440 Speaker 3: this a bit more later, might not be the best 240 00:13:22,520 --> 00:13:26,520 Speaker 3: place to search for alien life, might not be the 241 00:13:26,559 --> 00:13:29,600 Speaker 3: best place for humans to colonize, that doesn't mean it 242 00:13:29,640 --> 00:13:32,880 Speaker 3: is a place without mysteries of its own. There can 243 00:13:32,920 --> 00:13:35,920 Speaker 3: be mysteries of a quite inorganic nature that I still 244 00:13:35,960 --> 00:13:39,520 Speaker 3: think are pretty compelling, and I wanted to bring up 245 00:13:39,520 --> 00:13:44,320 Speaker 3: one of those, the mystery dunes of Io. So Rob 246 00:13:44,400 --> 00:13:46,640 Speaker 3: to start off with, I'm gonna have you look at 247 00:13:46,640 --> 00:13:49,080 Speaker 3: two images side by side in our outline here, and 248 00:13:49,120 --> 00:13:51,360 Speaker 3: folks at home, we will describe them for you so 249 00:13:51,679 --> 00:13:54,480 Speaker 3: you understand what we're looking at. On the right, we 250 00:13:54,600 --> 00:13:58,839 Speaker 3: have a satellite image. This is taken from above the 251 00:13:59,200 --> 00:14:03,120 Speaker 3: Namib Desert, which is on the west facing Atlantic coast 252 00:14:03,200 --> 00:14:06,679 Speaker 3: of Southern Africa, and that desert covers parts of the 253 00:14:06,920 --> 00:14:12,400 Speaker 3: coastal region of Angola, South Africa, and primarily Namibia. Now, 254 00:14:12,440 --> 00:14:16,040 Speaker 3: looking down at this desert from an orbital perspective, we 255 00:14:16,160 --> 00:14:21,200 Speaker 3: can see a beautiful, almost hypnotic pattern repeating across the 256 00:14:21,240 --> 00:14:27,400 Speaker 3: sandy expanse. Those are dunes, and sand dunes are characteristic 257 00:14:27,480 --> 00:14:30,920 Speaker 3: of many, but certainly not all, desert environments on Earth. 258 00:14:30,960 --> 00:14:34,520 Speaker 3: Some desert environments are very rocky, others are very cold, 259 00:14:34,800 --> 00:14:38,520 Speaker 3: places you might find ice fields, and then other desert 260 00:14:38,600 --> 00:14:41,520 Speaker 3: environments are the places you would find vast expanses of 261 00:14:41,640 --> 00:14:47,480 Speaker 3: sand dunes. Sand Dunes on Earth are formed primarily by 262 00:14:47,520 --> 00:14:51,840 Speaker 3: what are called Eolian forces, meaning they're created by the 263 00:14:51,920 --> 00:14:56,080 Speaker 3: action of wind, and actually the influence of wind comes 264 00:14:56,120 --> 00:14:58,880 Speaker 3: in at multiple stages because if you go way back 265 00:14:58,920 --> 00:15:03,440 Speaker 3: to the point of of the sand, wind along with water, 266 00:15:03,880 --> 00:15:08,280 Speaker 3: plays a role in the weathering and the transportation of rocks. 267 00:15:08,440 --> 00:15:11,040 Speaker 3: So you start off with rocks. You might have rocks 268 00:15:11,080 --> 00:15:13,640 Speaker 3: in the mountains or something, and they are broken up 269 00:15:13,680 --> 00:15:16,320 Speaker 3: by weathering, they get rained on, or they get the 270 00:15:16,600 --> 00:15:20,640 Speaker 3: wind blows on them, and various forces break those rocks 271 00:15:20,720 --> 00:15:25,240 Speaker 3: up into smaller pieces which can then be transported by 272 00:15:25,520 --> 00:15:29,520 Speaker 3: water and by wind downhill into places where they collect, 273 00:15:29,800 --> 00:15:32,600 Speaker 3: and over time those pieces of rock are continually broken 274 00:15:32,680 --> 00:15:36,600 Speaker 3: down into smaller and smaller pieces by further weathering and 275 00:15:36,680 --> 00:15:41,240 Speaker 3: erosion and transport, and the smallest sizes of mineral grains. 276 00:15:41,240 --> 00:15:43,080 Speaker 3: You might remember this if you listen to our series 277 00:15:43,120 --> 00:15:47,080 Speaker 3: on dust, are known as from larger to smaller are 278 00:15:47,080 --> 00:15:51,680 Speaker 3: known as sand, silt, and then clay. Sand Dunes are 279 00:15:51,720 --> 00:15:55,680 Speaker 3: created in areas where sand collects, So after the rocks 280 00:15:56,280 --> 00:15:59,040 Speaker 3: are weathered and eroded and then the sand is broken 281 00:15:59,080 --> 00:16:02,280 Speaker 3: down in transport, it'll sort of end up in some 282 00:16:02,400 --> 00:16:07,480 Speaker 3: kind of catching place, a depression, usually a lower lying area, 283 00:16:07,840 --> 00:16:11,280 Speaker 3: And when the wind blows it can move sand particles 284 00:16:11,360 --> 00:16:14,440 Speaker 3: along with it, And this is something yet again we 285 00:16:14,480 --> 00:16:17,600 Speaker 3: talked about in our series on dust. The term for 286 00:16:17,800 --> 00:16:21,000 Speaker 3: the process by which sand is moved around by the 287 00:16:21,040 --> 00:16:25,760 Speaker 3: wind is known as saltation. So you can get different 288 00:16:25,960 --> 00:16:30,800 Speaker 3: ways that the wind interacts with sediments and rock pieces 289 00:16:30,800 --> 00:16:33,640 Speaker 3: of different sizes. So you know, a larger rock, the 290 00:16:33,680 --> 00:16:36,720 Speaker 3: wind blows against it, it's not going anywhere. Maybe a 291 00:16:36,760 --> 00:16:38,920 Speaker 3: pebble the wind blows against it, it might kind of 292 00:16:38,960 --> 00:16:40,680 Speaker 3: move it a little bit, or a pebble might get 293 00:16:40,720 --> 00:16:43,120 Speaker 3: blown off another a pile of other pebbles and kind 294 00:16:43,120 --> 00:16:44,880 Speaker 3: of tumble a little bit, but it doesn't really go 295 00:16:45,000 --> 00:16:48,400 Speaker 3: much of anywhere unless you get really high winds. And 296 00:16:48,480 --> 00:16:50,680 Speaker 3: then meanwhile, if you go all the way down to 297 00:16:50,760 --> 00:16:54,000 Speaker 3: the sort of the dust size of grains of sediment, 298 00:16:54,440 --> 00:16:56,480 Speaker 3: the wind can pick it up and carry it up 299 00:16:56,520 --> 00:16:58,840 Speaker 3: into the atmosphere and then the dust just you know, 300 00:16:59,120 --> 00:17:01,320 Speaker 3: it is borne a lot for a long long time. 301 00:17:01,320 --> 00:17:03,840 Speaker 3: It can travel anywhere. It can travel across the land, 302 00:17:03,840 --> 00:17:07,560 Speaker 3: across the ocean, end up in different places. But sand 303 00:17:07,640 --> 00:17:11,000 Speaker 3: is in this middle zone where it's subject primarily to 304 00:17:11,160 --> 00:17:14,560 Speaker 3: the forces known as saltation. When wind blows on sand, 305 00:17:15,000 --> 00:17:17,679 Speaker 3: the sand will be blown along the surface of the ground, 306 00:17:17,760 --> 00:17:21,040 Speaker 3: or will follow the surface of whatever sort of the 307 00:17:21,320 --> 00:17:24,840 Speaker 3: base layer of the earth is, and it will will 308 00:17:24,880 --> 00:17:27,680 Speaker 3: be kicked up, and it'll kind of jump and bounce 309 00:17:27,760 --> 00:17:30,640 Speaker 3: and then come back down and hit the sand, and 310 00:17:30,720 --> 00:17:33,320 Speaker 3: that will cause other pieces of sand to kind of 311 00:17:33,359 --> 00:17:36,520 Speaker 3: get knocked out of place when the initial piece of 312 00:17:36,560 --> 00:17:41,240 Speaker 3: sand lands, So it creates this kind of bouncing, jumping, 313 00:17:41,480 --> 00:17:45,080 Speaker 3: hopping motion as sand is blown along by the wind, 314 00:17:45,880 --> 00:17:48,440 Speaker 3: As sand gets blown along by the wind, as saltation 315 00:17:48,640 --> 00:17:52,119 Speaker 3: is going on. At some point the flow of wind 316 00:17:52,200 --> 00:17:57,359 Speaker 3: driven sand can become obstructed. Maybe it gets caught on 317 00:17:57,560 --> 00:18:01,240 Speaker 3: an obstacle like there's a bush, or maybe it falls 318 00:18:01,280 --> 00:18:04,520 Speaker 3: behind an obstacle like a bush or piece of vegetation, 319 00:18:04,880 --> 00:18:07,439 Speaker 3: and then the wind cannot exert as much of a 320 00:18:07,480 --> 00:18:10,000 Speaker 3: force on it anymore, so it just kind of like 321 00:18:10,080 --> 00:18:12,960 Speaker 3: sits there and grains can pile up, or maybe it 322 00:18:13,000 --> 00:18:17,080 Speaker 3: gets blown against the side of a slightly elevated pile 323 00:18:17,240 --> 00:18:20,440 Speaker 3: of other grains of sand and it gets stuck there 324 00:18:20,560 --> 00:18:24,800 Speaker 3: instead of moving on and from here, these places where 325 00:18:24,960 --> 00:18:29,680 Speaker 3: sand starts to collect can be a self reinforcing process, 326 00:18:30,080 --> 00:18:32,800 Speaker 3: where a mound of sand just gets bigger and bigger 327 00:18:33,320 --> 00:18:37,359 Speaker 3: as the wind forces blowing sand particles against it cause 328 00:18:37,480 --> 00:18:41,120 Speaker 3: the particles to collect around this mound in one way 329 00:18:41,200 --> 00:18:44,760 Speaker 3: or another. So a common format of sand dune that 330 00:18:44,800 --> 00:18:48,080 Speaker 3: you will get in places, especially where the dominant winds 331 00:18:48,119 --> 00:18:52,960 Speaker 3: are blowing primarily in one direction, is that the side 332 00:18:53,000 --> 00:18:58,120 Speaker 3: of the sand dune facing the wind will be a smoother, slower, 333 00:18:58,200 --> 00:19:00,880 Speaker 3: more gradual slope, and then the side of the sand 334 00:19:00,960 --> 00:19:03,480 Speaker 3: dune facing away from the dominant winds will be a 335 00:19:03,560 --> 00:19:07,119 Speaker 3: much steeper, sharper slope. And what's usually happening is the 336 00:19:07,119 --> 00:19:11,400 Speaker 3: wind is blowing sand along and it's eroding sand from 337 00:19:11,480 --> 00:19:15,000 Speaker 3: the middle of the rising slope on the windward side, 338 00:19:15,320 --> 00:19:18,200 Speaker 3: and then trying to deposit it right at the crest, 339 00:19:18,320 --> 00:19:22,720 Speaker 3: right at the peak of the dune. And in this way, 340 00:19:22,760 --> 00:19:25,840 Speaker 3: over years and years, more and more sand accumulates. But 341 00:19:26,160 --> 00:19:30,320 Speaker 3: sand dunes don't just grow higher and higher forever. Eventually 342 00:19:30,440 --> 00:19:35,920 Speaker 3: a sand dune will collapse, not totally disappearing, but losing height. 343 00:19:36,040 --> 00:19:39,160 Speaker 3: And this happens when one side of the dune becomes 344 00:19:39,359 --> 00:19:45,440 Speaker 3: too steep, exceeding what is called the angle of repose. Now, 345 00:19:45,480 --> 00:19:48,040 Speaker 3: this is a kind of cool physics principle. I think 346 00:19:48,080 --> 00:19:50,000 Speaker 3: we may have talked about this on the show before, 347 00:19:50,040 --> 00:19:54,639 Speaker 3: but the angle of repose is the steepest angle that 348 00:19:54,800 --> 00:20:00,199 Speaker 3: a pile of sediment or whatever other granular substance can 349 00:20:00,320 --> 00:20:04,120 Speaker 3: attain before it collapses under its own weight. In fact, 350 00:20:04,160 --> 00:20:06,359 Speaker 3: I wonder if we talked about the angle of repose 351 00:20:06,880 --> 00:20:09,960 Speaker 3: in when we were talking about the ant lion, because 352 00:20:10,000 --> 00:20:12,399 Speaker 3: I believe that is a factor in the construction of 353 00:20:12,400 --> 00:20:16,159 Speaker 3: their conical traps. That you know, they make them so 354 00:20:16,960 --> 00:20:19,920 Speaker 3: just so that they're sort of right on the edge, 355 00:20:19,960 --> 00:20:22,679 Speaker 3: and it's easy for the sides to start collapsing and 356 00:20:22,760 --> 00:20:24,640 Speaker 3: pull an ant down if they fall in. 357 00:20:25,359 --> 00:20:27,680 Speaker 2: That may be a place where it's come up before. Yeah. 358 00:20:27,800 --> 00:20:31,879 Speaker 3: Yeah, Now, the angle of repose is not a universal constant. 359 00:20:32,000 --> 00:20:35,479 Speaker 3: It instead depends on a number of variables about the 360 00:20:35,520 --> 00:20:39,760 Speaker 3: material you're piling up. So you know, different types of sand, 361 00:20:39,800 --> 00:20:43,959 Speaker 3: different grain sizes of sand, like the amount of friction 362 00:20:44,119 --> 00:20:47,439 Speaker 3: between the particles, how big the particles are on average, 363 00:20:47,440 --> 00:20:49,960 Speaker 3: stuff like that will all affect what the angle of 364 00:20:50,000 --> 00:20:53,359 Speaker 3: repose is for a pile of this stuff. But I 365 00:20:53,400 --> 00:20:56,439 Speaker 3: was reading that. I was reading on an information page 366 00:20:56,440 --> 00:20:59,480 Speaker 3: by the USGS. This was a page about Sand Dune's 367 00:20:59,560 --> 00:21:02,879 Speaker 3: National Park in Colorado. The angle of repose for sand 368 00:21:02,960 --> 00:21:06,879 Speaker 3: is usually between thirty and thirty four degrees, so once 369 00:21:07,080 --> 00:21:11,200 Speaker 3: it gets steeper than that, the dune will collapse. And this, 370 00:21:11,280 --> 00:21:14,080 Speaker 3: in part explains why when you're looking at pictures of 371 00:21:14,160 --> 00:21:16,720 Speaker 3: sand dunes in the desert, you will, as I said, 372 00:21:16,840 --> 00:21:19,840 Speaker 3: often see them with this one smooth side, kind of 373 00:21:20,080 --> 00:21:23,479 Speaker 3: a gentler slope on one side ascending at a shallower angle, 374 00:21:23,800 --> 00:21:25,919 Speaker 3: and then the other side will fall off at a 375 00:21:25,920 --> 00:21:29,120 Speaker 3: steeper angle with an almost kind of sheared off texture. 376 00:21:29,560 --> 00:21:32,400 Speaker 2: Yeah, looking like someone is sliced into it to get 377 00:21:33,160 --> 00:21:36,160 Speaker 2: a little bit of the dessert. That's sort of a look. 378 00:21:36,320 --> 00:21:39,520 Speaker 3: Yes, exactly. So generally the smoother side is facing the 379 00:21:39,520 --> 00:21:44,040 Speaker 3: dominant winds, where the sediment continues to be eroded from 380 00:21:44,160 --> 00:21:46,840 Speaker 3: the slope going up and then tries, and then the 381 00:21:46,880 --> 00:21:49,600 Speaker 3: wind deposits more and more of it at the crest, 382 00:21:50,560 --> 00:21:53,399 Speaker 3: and then it gets steeper and steeper on the downwind 383 00:21:53,480 --> 00:21:56,520 Speaker 3: side until it collapses. And of course there's also going 384 00:21:56,600 --> 00:22:00,040 Speaker 3: to be some sand grains falling over the top of 385 00:21:59,840 --> 00:22:02,720 Speaker 3: the dune and then ending up down sort of in 386 00:22:02,760 --> 00:22:06,560 Speaker 3: the shelter from the wind on the leeward side. And 387 00:22:06,720 --> 00:22:09,560 Speaker 3: sand dunes are really interesting, you know, you can if 388 00:22:09,600 --> 00:22:13,120 Speaker 3: you watch them over long periods of time, they can 389 00:22:13,600 --> 00:22:17,600 Speaker 3: start to seem less like the geological formations we're used to. 390 00:22:17,600 --> 00:22:19,840 Speaker 3: I mean, we know that mountains move over time, but 391 00:22:20,680 --> 00:22:23,720 Speaker 3: you know, it's really hard to imagine how mountains move. 392 00:22:23,760 --> 00:22:26,000 Speaker 3: You really have to just sort of think outside of 393 00:22:26,000 --> 00:22:30,080 Speaker 3: the human timescale. Dunes are kind of somewhere in between 394 00:22:30,480 --> 00:22:34,239 Speaker 3: mountains and the waves in the ocean. Over periods of 395 00:22:34,400 --> 00:22:37,640 Speaker 3: you know, months or years, dunes will will creep across 396 00:22:37,680 --> 00:22:40,760 Speaker 3: the surface of the Earth. So that's dunes on Earth. However, 397 00:22:40,880 --> 00:22:42,600 Speaker 3: Rob I want to come back and have you look 398 00:22:42,640 --> 00:22:44,920 Speaker 3: at the photos we started with, So the one we 399 00:22:44,920 --> 00:22:48,719 Speaker 3: were looking at first is sand dunes on Earth. But 400 00:22:48,760 --> 00:22:51,280 Speaker 3: then the photo I've got for you here on the 401 00:22:51,359 --> 00:22:55,399 Speaker 3: left is a photo of Io. So what we see 402 00:22:55,400 --> 00:22:57,720 Speaker 3: on the lower left hand side of the image is 403 00:22:57,760 --> 00:23:01,200 Speaker 3: a kind of dark spreading expanse that has a sort 404 00:23:01,240 --> 00:23:04,320 Speaker 3: of creepy organic outline, kind of like if you zoom 405 00:23:04,320 --> 00:23:09,280 Speaker 3: way out, like a flood pouring through topography. And researchers 406 00:23:09,400 --> 00:23:12,119 Speaker 3: think that this area in the photo of Io is 407 00:23:12,200 --> 00:23:15,879 Speaker 3: probably one of those relatively fresh lava flows that we 408 00:23:15,920 --> 00:23:18,119 Speaker 3: talked about last time. You know, a lot of the 409 00:23:18,119 --> 00:23:20,800 Speaker 3: surface of Io is affected by lava flows, and that 410 00:23:20,840 --> 00:23:24,399 Speaker 3: they can be huge, enormous, hundreds of kilometers of just 411 00:23:24,720 --> 00:23:30,679 Speaker 3: lava flows. And this helps contribute, of course to what 412 00:23:30,760 --> 00:23:33,199 Speaker 3: Carl Sagan said about the moon right. He said that 413 00:23:33,280 --> 00:23:37,320 Speaker 3: Io is a place of relatively rapid change by planetary standards. 414 00:23:37,800 --> 00:23:40,480 Speaker 3: Major changes to the surface of Io can occur on 415 00:23:40,520 --> 00:23:43,479 Speaker 3: a timescale of months. But if you look at the 416 00:23:43,520 --> 00:23:47,080 Speaker 3: other side of this image from Galileo, not the dark side, 417 00:23:47,359 --> 00:23:50,880 Speaker 3: but the lighter colored side, we see not lava flows, 418 00:23:50,920 --> 00:23:56,040 Speaker 3: but these pale reflective ripples thousands of them arrayed in 419 00:23:56,119 --> 00:23:59,520 Speaker 3: a repeating pattern, kind of like what you would see 420 00:23:59,560 --> 00:24:01,639 Speaker 3: in like when you can see a standing wave of 421 00:24:01,680 --> 00:24:04,879 Speaker 3: emerging in a fluid, or you know, if you like 422 00:24:04,960 --> 00:24:08,439 Speaker 3: a rattle, you like rattle a speaker, and then on 423 00:24:08,480 --> 00:24:10,920 Speaker 3: top of it there's some sand. You get these emerging things. 424 00:24:11,480 --> 00:24:13,359 Speaker 3: One thing I wanted to compare it to was like 425 00:24:13,400 --> 00:24:16,040 Speaker 3: a silver reptile skin. It has almost kind of a 426 00:24:16,080 --> 00:24:17,639 Speaker 3: pebbly lizard texture. 427 00:24:18,080 --> 00:24:18,560 Speaker 2: It does. 428 00:24:18,840 --> 00:24:21,960 Speaker 3: But actually when you see him side by side here 429 00:24:22,000 --> 00:24:25,359 Speaker 3: this looks quite a lot like satellite photos of desert 430 00:24:25,400 --> 00:24:28,640 Speaker 3: dunes on Earth. But could that really be what they are? 431 00:24:29,640 --> 00:24:32,320 Speaker 3: Because remember what we talked about in the previous episode. 432 00:24:32,760 --> 00:24:37,960 Speaker 3: Io only has the most tenuous, ghost like suggestion of 433 00:24:38,000 --> 00:24:42,520 Speaker 3: an atmosphere. It's composed primarily of sulfur dioxide with a 434 00:24:42,560 --> 00:24:47,000 Speaker 3: few other trace constituents. And for a comparison of how 435 00:24:47,080 --> 00:24:50,359 Speaker 3: thin Io's atmosphere is, I was looking for, you know, 436 00:24:50,400 --> 00:24:53,359 Speaker 3: what's the difference between Earth's atmosphere and iOS And I 437 00:24:53,400 --> 00:24:55,840 Speaker 3: actually found a twenty twenty press release from the National 438 00:24:55,880 --> 00:24:59,359 Speaker 3: Science Foundation that addressed this. They crunch the numbers and 439 00:24:59,400 --> 00:25:02,480 Speaker 3: they say that i Io's atmosphere is roughly a billion 440 00:25:02,720 --> 00:25:07,080 Speaker 3: times thinner than Earth's It is barely an atmosphere at all, 441 00:25:07,520 --> 00:25:11,440 Speaker 3: thicker than the even more tenuous exosphere of Earth's moon, 442 00:25:11,920 --> 00:25:14,960 Speaker 3: which I was looking that up. Also, apparently Earth's moon 443 00:25:15,800 --> 00:25:18,000 Speaker 3: has such a thin layer of gas that there are 444 00:25:18,040 --> 00:25:21,280 Speaker 3: only about one hundred molecules of gas per cubic centimeter 445 00:25:21,440 --> 00:25:25,199 Speaker 3: near its surface. So iOS is thicker than that, but 446 00:25:25,280 --> 00:25:28,199 Speaker 3: still not thick enough to cause irrosive wind patterns like 447 00:25:28,240 --> 00:25:31,439 Speaker 3: we have on Earth. So if there's not enough of 448 00:25:31,440 --> 00:25:36,120 Speaker 3: an atmosphere to sustain significant winds on Io, and if 449 00:25:36,240 --> 00:25:41,119 Speaker 3: dunes are generally created by Eolien forces by wind, what's 450 00:25:41,160 --> 00:25:45,360 Speaker 3: making the dunes or are they actually dunes at all? 451 00:25:45,440 --> 00:25:47,679 Speaker 3: So just a couple of years ago, there was a 452 00:25:47,720 --> 00:25:51,520 Speaker 3: paper that actually addressed this question. It was published in 453 00:25:51,640 --> 00:25:55,040 Speaker 3: Nature Communications by MacDonald at All and the title is 454 00:25:55,560 --> 00:25:59,080 Speaker 3: this will answer some of the questions Eolian sediment transport 455 00:25:59,119 --> 00:26:03,800 Speaker 3: on IO from lava frost interactions and for context. I 456 00:26:03,840 --> 00:26:07,159 Speaker 3: was also reading about this in a Rutgers University press 457 00:26:07,200 --> 00:26:10,720 Speaker 3: release by Kiddy Macpheerson from April twenty twenty two that 458 00:26:10,800 --> 00:26:14,240 Speaker 3: had some quotes from the authors. So, first of all, 459 00:26:14,280 --> 00:26:19,639 Speaker 3: to answer the question, are these dunes previous researchers had 460 00:26:19,680 --> 00:26:23,360 Speaker 3: noted that the features which are generally turned termed ridges 461 00:26:23,640 --> 00:26:29,000 Speaker 3: in the astronomy context or the planetary science context. These 462 00:26:29,000 --> 00:26:32,600 Speaker 3: features that they had been noticed for their similarity to 463 00:26:32,760 --> 00:26:35,920 Speaker 3: eli and sand dunes on planets like Earth and Mars. 464 00:26:36,000 --> 00:26:42,480 Speaker 3: Mars has dunes as well, But these previous investigations usually argued, no, 465 00:26:42,800 --> 00:26:46,040 Speaker 3: these are probably not dunes formed by wind. For the 466 00:26:46,080 --> 00:26:49,720 Speaker 3: reasons that we've already raised. The atmosphere of Io is 467 00:26:49,840 --> 00:26:53,320 Speaker 3: not thick enough to really have wind. It's not thick 468 00:26:53,400 --> 00:26:57,920 Speaker 3: enough to lift sediment and move it around. And again, 469 00:26:58,000 --> 00:27:01,000 Speaker 3: this moving around of sediment by s particles by wind 470 00:27:01,040 --> 00:27:04,800 Speaker 3: would be saltation. So remember that when it comes up 471 00:27:04,840 --> 00:27:08,520 Speaker 3: in these quotes. The authors of the paperwright quote choosing 472 00:27:08,640 --> 00:27:13,200 Speaker 3: zero point one nanobars as a representative atmospheric pressure. One 473 00:27:13,240 --> 00:27:17,439 Speaker 3: study estimated a twenty kilometer per second threshold friction speed 474 00:27:17,760 --> 00:27:21,359 Speaker 3: to move grains on Io, two orders of magnitude greater 475 00:27:21,520 --> 00:27:26,080 Speaker 3: than Io's roughly three hundred meters per second wins, concluding 476 00:27:26,200 --> 00:27:30,120 Speaker 3: that an Eolian origin for these features was impossible. Formation 477 00:27:30,320 --> 00:27:36,000 Speaker 3: by tidal forces was favored. Now, tidal forces means the 478 00:27:36,040 --> 00:27:41,000 Speaker 3: interaction of different gravitational forces on matter exerting a pulling 479 00:27:41,160 --> 00:27:46,480 Speaker 3: or a stretching force. So this alternate explanation previously favored 480 00:27:46,480 --> 00:27:49,879 Speaker 3: because Io can't sustain wins, is that there's something about 481 00:27:49,880 --> 00:27:55,200 Speaker 3: the gravity that is causing these ridge features to emerge. However, 482 00:27:55,480 --> 00:27:59,920 Speaker 3: despite agreeing that saltation is not possible under the ambient 483 00:28:00,080 --> 00:28:04,119 Speaker 3: atmospheric conditions of Io, the authors note that there really 484 00:28:04,240 --> 00:28:06,920 Speaker 3: are a number of similarities between the features seen in 485 00:28:06,960 --> 00:28:11,280 Speaker 3: these images and Eolian dunes. They mentioned quote the ridges, 486 00:28:11,400 --> 00:28:18,760 Speaker 3: regular spacing, slightly meandering forms, and possession of crestline defects. 487 00:28:19,400 --> 00:28:22,679 Speaker 3: So these are all features that are very similar, so 488 00:28:22,880 --> 00:28:26,800 Speaker 3: similar to wind formed dunes on Earth and Mars that 489 00:28:26,840 --> 00:28:28,679 Speaker 3: it would be kind of strange if that's not what 490 00:28:28,760 --> 00:28:32,520 Speaker 3: they were. So is there any way that these features 491 00:28:32,520 --> 00:28:36,120 Speaker 3: could have been formed by something like wind, even though 492 00:28:36,359 --> 00:28:40,200 Speaker 3: you know, even given the limitations we know of Io's atmosphere. Well, 493 00:28:40,320 --> 00:28:43,680 Speaker 3: the authors of the paper note that the thickness of 494 00:28:43,720 --> 00:28:48,960 Speaker 3: Io's atmosphere is not consistent across its surface, so the 495 00:28:49,040 --> 00:28:52,800 Speaker 3: density of surface gas could actually be much higher at 496 00:28:52,840 --> 00:28:57,520 Speaker 3: certain times and in certain areas, specifically in the vicinity 497 00:28:57,520 --> 00:29:01,360 Speaker 3: of volcanic vents, which are rapidly viewing so two gas 498 00:29:01,440 --> 00:29:05,280 Speaker 3: as they erupt. The authors ask, what if there is 499 00:29:05,320 --> 00:29:09,200 Speaker 3: a sort of you could say, quote unquote wind that 500 00:29:09,360 --> 00:29:13,160 Speaker 3: is present locally, not globally, on the surface of Io, 501 00:29:13,760 --> 00:29:19,520 Speaker 3: consisting of some kind of rush of gases from subsurface 502 00:29:19,600 --> 00:29:24,680 Speaker 3: interactions from volcanism or from downstream effects of volcanic eruptions, 503 00:29:24,960 --> 00:29:28,320 Speaker 3: And what if this is responsible for crafting the dunes? 504 00:29:28,800 --> 00:29:31,560 Speaker 3: And this is in fact what they find support for 505 00:29:31,640 --> 00:29:35,200 Speaker 3: in their paper and the author's write quote here we 506 00:29:35,280 --> 00:29:39,840 Speaker 3: demonstrate that interactions between lava from volcanic eruptions and the 507 00:29:39,880 --> 00:29:46,520 Speaker 3: sulfur dioxide frost blanketing Io's surface can produce localized sublimation 508 00:29:46,760 --> 00:29:52,800 Speaker 3: vapor flows with sufficient gas densities to enable saltation. So 509 00:29:52,960 --> 00:29:55,440 Speaker 3: I thought that was really interesting. So what would these 510 00:29:55,480 --> 00:29:59,040 Speaker 3: interactions be. To be clear, they're not talking about their 511 00:29:59,360 --> 00:30:04,080 Speaker 3: quote unquote wind being the gases that burst directly from 512 00:30:04,200 --> 00:30:07,520 Speaker 3: volcanic eruptions. You know, it's not like the gas comes 513 00:30:07,560 --> 00:30:10,720 Speaker 3: out of the volcano and that is the wind. They're 514 00:30:10,760 --> 00:30:14,640 Speaker 3: talking instead about a secondary mechanism that they find probable, 515 00:30:15,120 --> 00:30:19,280 Speaker 3: which is that you have hot lava flowing just underneath 516 00:30:19,400 --> 00:30:23,960 Speaker 3: the surface of the frost layer here, and it's creating 517 00:30:24,000 --> 00:30:27,880 Speaker 3: this interaction with the sulfur dioxide frost on the surface, 518 00:30:28,160 --> 00:30:32,520 Speaker 3: causing the sulfur dioxide to sublimate. Essentially, it heats it 519 00:30:32,640 --> 00:30:36,600 Speaker 3: up and it causes an outgasing process. So suddenly a 520 00:30:36,640 --> 00:30:39,840 Speaker 3: bunch of this SO two turns into gas and then 521 00:30:39,920 --> 00:30:43,000 Speaker 3: they find that that would be capable of driving saltation. 522 00:30:43,760 --> 00:30:47,320 Speaker 3: So lead author George MacDonald, quoted in the press release, says, 523 00:30:47,880 --> 00:30:50,280 Speaker 3: our studies point to the possibility of Io as a 524 00:30:50,320 --> 00:30:54,520 Speaker 3: new dune world. We have proposed and quantitatively tested a 525 00:30:54,600 --> 00:30:57,600 Speaker 3: mechanism by which sand grains can move and in turn 526 00:30:57,920 --> 00:31:02,120 Speaker 3: dunes could be forming there. And I really they actually 527 00:31:02,120 --> 00:31:04,840 Speaker 3: come through in the in the press release there the 528 00:31:04,880 --> 00:31:08,120 Speaker 3: authors are like referencing the book Dune and talking about 529 00:31:08,120 --> 00:31:09,760 Speaker 3: how it could be like a racket. So I like 530 00:31:09,880 --> 00:31:12,920 Speaker 3: the dedication to like we have we have determined how 531 00:31:12,960 --> 00:31:14,400 Speaker 3: it can be a dune world. 532 00:31:14,680 --> 00:31:17,480 Speaker 2: We have captured a sand worm and will soon begin 533 00:31:17,600 --> 00:31:19,880 Speaker 2: the spice spice production on another planet. 534 00:31:19,960 --> 00:31:22,760 Speaker 3: Yes, now, if this is in fact the mechanism, it 535 00:31:22,760 --> 00:31:25,000 Speaker 3: would explain a number of things. It would explain the 536 00:31:25,040 --> 00:31:29,080 Speaker 3: similarity to dunes created by wind on the other planets 537 00:31:29,080 --> 00:31:32,840 Speaker 3: of course, it would also explain, sort of going against 538 00:31:32,960 --> 00:31:38,760 Speaker 3: the tidal forces argument, why you see dunes in different orientations, 539 00:31:38,840 --> 00:31:41,560 Speaker 3: because the authors say, you know, if it was tidal forces, 540 00:31:41,600 --> 00:31:43,959 Speaker 3: it seems like you'd be more likely to see all 541 00:31:43,960 --> 00:31:48,280 Speaker 3: the dunes kind of aligned along with certain gravitational axes, 542 00:31:48,320 --> 00:31:52,440 Speaker 3: but instead you see dunes facing different directions. But another 543 00:31:52,480 --> 00:31:55,160 Speaker 3: thing is that if this really is the mechanism, you 544 00:31:55,240 --> 00:31:59,320 Speaker 3: might expect to see more dunes forming, like around the 545 00:31:59,480 --> 00:32:02,479 Speaker 3: edges offs like we see in this image we started with, 546 00:32:02,760 --> 00:32:05,720 Speaker 3: where you've got this black glassy area on one part 547 00:32:05,760 --> 00:32:08,200 Speaker 3: of the image. You know, that's where the lava is flowing, 548 00:32:08,520 --> 00:32:10,920 Speaker 3: and then at the edge of that it's probably interacting 549 00:32:11,000 --> 00:32:14,720 Speaker 3: with these these planes of so two frost, and that 550 00:32:14,760 --> 00:32:17,560 Speaker 3: could be creating the winds that blow that blow over 551 00:32:17,600 --> 00:32:21,560 Speaker 3: the surface and help form the dunes. Interesting, So I 552 00:32:21,560 --> 00:32:24,320 Speaker 3: feel like sci fi writers, we're just feeding you, We're 553 00:32:24,360 --> 00:32:26,040 Speaker 3: just you know, like you can you can do a 554 00:32:26,120 --> 00:32:28,280 Speaker 3: dune type thing on io that'll work here. 555 00:32:28,920 --> 00:32:32,120 Speaker 2: Yeah, yeah, absolutely. I mean it's a again, this is 556 00:32:32,160 --> 00:32:36,080 Speaker 2: it's an exciting world and perhaps a little too exciting, 557 00:32:36,560 --> 00:32:39,240 Speaker 2: and I think that's what maybe scares away even some 558 00:32:39,280 --> 00:32:40,200 Speaker 2: sci fi visions. 559 00:32:40,440 --> 00:32:42,920 Speaker 3: Yeah, once again. I mean, I agree, that's fair. Like 560 00:32:42,960 --> 00:32:45,960 Speaker 3: I understand, especially if you're trying to write hard or 561 00:32:46,000 --> 00:32:48,479 Speaker 3: semi hard sci fi, like dealing with the real uh 562 00:32:49,240 --> 00:32:51,400 Speaker 3: what we actually know and how that would inform the 563 00:32:51,440 --> 00:32:55,480 Speaker 3: story creates problems. But I think this is really enticing 564 00:32:55,560 --> 00:32:59,120 Speaker 3: because Okay, so we've seen Arakis, We've seen Dune as 565 00:32:59,120 --> 00:33:02,920 Speaker 3: a hot world, but imagine a freezing cold Dune world 566 00:33:03,000 --> 00:33:05,200 Speaker 3: but also super hot in certain areas. 567 00:33:05,800 --> 00:33:07,320 Speaker 2: I guess one of the things to keep in mind, 568 00:33:07,480 --> 00:33:09,440 Speaker 2: kind of going back to our full episodes on the 569 00:33:10,200 --> 00:33:14,160 Speaker 2: Jovian moons, is like they're all kind of terrible, you know, 570 00:33:14,400 --> 00:33:15,920 Speaker 2: compared to what we have here on Earth. I mean 571 00:33:15,920 --> 00:33:18,080 Speaker 2: the same can be said for pretty much everywhere else 572 00:33:18,160 --> 00:33:21,000 Speaker 2: in our Solar system and the known universe, you know, 573 00:33:21,080 --> 00:33:22,959 Speaker 2: like this this is the world we can live on, 574 00:33:23,480 --> 00:33:26,680 Speaker 2: this is the world we have to make work, and 575 00:33:26,800 --> 00:33:28,440 Speaker 2: the rest of them. It's kind of like looking at 576 00:33:28,480 --> 00:33:30,680 Speaker 2: the I don't know Batman's rogue gallery and saying, well, 577 00:33:30,680 --> 00:33:33,160 Speaker 2: which one is the like the least awful, And you 578 00:33:33,240 --> 00:33:35,719 Speaker 2: might be like, well, mister Freeze has some you know, 579 00:33:35,800 --> 00:33:39,960 Speaker 2: some virtues to him, yes, but he's still a murderous madman. Killer. 580 00:33:40,440 --> 00:33:43,120 Speaker 3: That's a very good comparison. Weirdly, and I've sort of 581 00:33:43,160 --> 00:33:45,280 Speaker 3: had this on my mind lately. I mean, this is 582 00:33:45,320 --> 00:33:47,680 Speaker 3: something I think of every now and then, ever since 583 00:33:47,720 --> 00:33:51,400 Speaker 3: I read Kim Stanley Robinson's Aurora, which is a book 584 00:33:51,720 --> 00:33:55,440 Speaker 3: very much about It's a space exploration book that I 585 00:33:55,440 --> 00:33:57,360 Speaker 3: don't want to spoil too much for people who haven't 586 00:33:57,360 --> 00:33:59,160 Speaker 3: read it, but it ends up being very much about 587 00:33:59,160 --> 00:34:00,000 Speaker 3: the virtues of Earth. 588 00:34:00,040 --> 00:34:00,280 Speaker 2: Earth. 589 00:34:01,240 --> 00:34:04,280 Speaker 3: Yeah, and you know, the preciousness of the planet we 590 00:34:04,320 --> 00:34:08,320 Speaker 3: already have. Uh, and so that's a wonderful theme. It's 591 00:34:08,360 --> 00:34:12,400 Speaker 3: you know, some people I love space, space exploration and 592 00:34:12,440 --> 00:34:15,080 Speaker 3: space colonization as a setting for a science fiction story. 593 00:34:15,080 --> 00:34:17,920 Speaker 3: I mean, I love that as much as anybody. But 594 00:34:17,920 --> 00:34:22,560 Speaker 3: but also sometimes in people who are real advocates of 595 00:34:22,719 --> 00:34:25,759 Speaker 3: space exploration, you almost get a sense of that they're 596 00:34:25,800 --> 00:34:27,920 Speaker 3: just kind of done with Earth. It's like, yeah, okay, 597 00:34:27,960 --> 00:34:29,600 Speaker 3: we've used that up, we can kick that out. We 598 00:34:29,680 --> 00:34:31,920 Speaker 3: just got to move on to the next thing. I 599 00:34:31,960 --> 00:34:33,920 Speaker 3: don't I don't think that's a good basket to put 600 00:34:33,920 --> 00:34:34,600 Speaker 3: your chickens in. 601 00:34:35,320 --> 00:34:37,759 Speaker 2: No. No, I mean, you know this has come up 602 00:34:37,800 --> 00:34:40,040 Speaker 2: in various conversations in the show before, but you know, 603 00:34:40,120 --> 00:34:45,319 Speaker 2: you pretty much any model for near to medium term 604 00:34:45,719 --> 00:34:50,080 Speaker 2: colonization efforts, you know elsewhere in the Solar System, those 605 00:34:50,120 --> 00:34:54,120 Speaker 2: are all going to be completely dependent upon Earth. You know, 606 00:34:54,160 --> 00:34:57,640 Speaker 2: There's there's no deshackling from that planet. You know, even 607 00:34:57,640 --> 00:34:59,440 Speaker 2: in your you know, sci fi visions. You know, it's 608 00:34:59,440 --> 00:35:02,600 Speaker 2: like you have to really look at far future scenarios 609 00:35:02,600 --> 00:35:06,560 Speaker 2: where it would even become possibly feasible for there to 610 00:35:06,600 --> 00:35:11,520 Speaker 2: be truly independent colonies, independent systems that are not depending 611 00:35:12,040 --> 00:35:15,959 Speaker 2: on this place where we evolve to thrive. Yeah. 612 00:35:16,160 --> 00:35:19,320 Speaker 3: I couldn't agree more. And to be clear, once again, 613 00:35:19,560 --> 00:35:23,360 Speaker 3: I'm not against space exploration or even necessarily space colonization. 614 00:35:25,440 --> 00:35:27,400 Speaker 3: See the beauty and the excitement in those kind of 615 00:35:27,440 --> 00:35:31,320 Speaker 3: grand projects. But I don't know, I find it revolting 616 00:35:31,600 --> 00:35:35,640 Speaker 3: when that kind of grand ambition brings along with it 617 00:35:36,000 --> 00:35:38,440 Speaker 3: contempt for the planet that we need right now and 618 00:35:38,480 --> 00:35:42,600 Speaker 3: will need for the foreseeable future. You gotta love Earth now. 619 00:35:42,640 --> 00:35:45,680 Speaker 2: This is a commentary that has existed in the zeitgeist 620 00:35:45,680 --> 00:35:49,000 Speaker 2: for a while. I always come back to a particular 621 00:35:49,560 --> 00:35:53,959 Speaker 2: nineteen ninety four talk given by Terrence McKenna in which 622 00:35:53,960 --> 00:35:57,040 Speaker 2: he refers to the Earth as quote, an incredible pearl, 623 00:35:57,120 --> 00:36:01,759 Speaker 2: flung out in a universe of ashes and darkness. And 624 00:36:01,760 --> 00:36:04,800 Speaker 2: and he's making a larger point in referencing this about 625 00:36:05,200 --> 00:36:07,680 Speaker 2: a decision to be made regarding human nature and how 626 00:36:07,719 --> 00:36:10,279 Speaker 2: we view ourselves and our place in the universe. But 627 00:36:10,480 --> 00:36:12,960 Speaker 2: I keep coming back to that idea. Our earth is 628 00:36:12,960 --> 00:36:16,520 Speaker 2: this incredible pearl, and because it is the place where 629 00:36:16,520 --> 00:36:19,080 Speaker 2: there is life, it is the place where we are 630 00:36:19,160 --> 00:36:22,360 Speaker 2: meant to be. And you know, we may expand out 631 00:36:22,400 --> 00:36:25,600 Speaker 2: and explore these other places, we may expand out and 632 00:36:25,640 --> 00:36:28,759 Speaker 2: make new homes on these other places, but this, this 633 00:36:28,920 --> 00:36:32,040 Speaker 2: is the place from which we arose. This is our 634 00:36:32,040 --> 00:36:34,400 Speaker 2: true home. This is the only place we can count 635 00:36:34,440 --> 00:36:38,080 Speaker 2: on to sustain us as long as we cherish it. 636 00:36:38,440 --> 00:36:40,880 Speaker 3: Everywhere else is a gamble, And you don't bet the 637 00:36:40,920 --> 00:36:44,160 Speaker 3: home world on a gamble, you know, that's right. Nothing 638 00:36:44,160 --> 00:36:45,080 Speaker 3: else is a sure thing. 639 00:36:45,400 --> 00:36:49,120 Speaker 2: And you certainly don't bet on Io. Yeah no, because 640 00:36:49,120 --> 00:36:51,799 Speaker 2: I don't think anybody's realistically betting on Io. They may, 641 00:36:52,239 --> 00:36:55,880 Speaker 2: they may be placing moderate bets on other destinations in 642 00:36:55,920 --> 00:36:59,799 Speaker 2: our solar system, but Io is the odds are great. 643 00:37:00,120 --> 00:37:02,880 Speaker 2: You're a gambler, but it's not likely going to be 644 00:37:03,360 --> 00:37:03,680 Speaker 2: a win. 645 00:37:04,200 --> 00:37:08,280 Speaker 3: However, greatly worth studying, if not the number one candidate 646 00:37:08,360 --> 00:37:12,319 Speaker 3: for a little for a base out there. One thing 647 00:37:12,360 --> 00:37:14,600 Speaker 3: I did observe about that quote before we move on, though, 648 00:37:14,840 --> 00:37:18,560 Speaker 3: I actually think the pearl is a wonderful metaphor for Earth, 649 00:37:19,000 --> 00:37:21,239 Speaker 3: not just because it's a ball, you know, like Earth 650 00:37:21,280 --> 00:37:25,359 Speaker 3: is roughly spherical and pearl is usually somewhat spherical, Not 651 00:37:25,440 --> 00:37:27,879 Speaker 3: just because it is precious. I mean, pearl, of course 652 00:37:27,960 --> 00:37:30,040 Speaker 3: is a type of jewel, so it's precious just like 653 00:37:30,080 --> 00:37:34,480 Speaker 3: the Earth is. But it is also essentially a mineral 654 00:37:34,600 --> 00:37:38,359 Speaker 3: product at its material base, which most of the Earth is, 655 00:37:38,480 --> 00:37:41,560 Speaker 3: but also a biofact. You know, a pearl is created 656 00:37:41,600 --> 00:37:44,560 Speaker 3: by life, and the way the Earth is now it 657 00:37:45,200 --> 00:37:47,719 Speaker 3: was also in a way created by life. Life is 658 00:37:47,800 --> 00:37:51,480 Speaker 3: defined what the planet is down to its very physical substance. 659 00:37:51,920 --> 00:37:52,799 Speaker 2: Yeah. Absolutely. 660 00:38:02,920 --> 00:38:05,120 Speaker 3: Oh now, Rob, I remembered something we said we were 661 00:38:05,120 --> 00:38:07,880 Speaker 3: going to come back to, was the question of the 662 00:38:07,920 --> 00:38:10,960 Speaker 3: possibility of io sustaining life. We've already said that it's 663 00:38:11,239 --> 00:38:14,840 Speaker 3: probably not, you know, just from from what we already know. 664 00:38:14,920 --> 00:38:18,480 Speaker 3: Probably not the first candidate to look for life elsewhere 665 00:38:18,480 --> 00:38:22,200 Speaker 3: in our solar system. But you know, with with most 666 00:38:22,239 --> 00:38:24,920 Speaker 3: planetary bodies out there, people have kind of done the 667 00:38:24,960 --> 00:38:27,600 Speaker 3: work to say, like what sort of thing would be 668 00:38:27,640 --> 00:38:29,960 Speaker 3: most plausible here? And I know you'd been reading a 669 00:38:29,960 --> 00:38:32,440 Speaker 3: bit about io and life, so once you turn up. 670 00:38:33,239 --> 00:38:36,600 Speaker 2: Well, yeah, again, it is an extreme environment and it's 671 00:38:36,640 --> 00:38:39,920 Speaker 2: by no means the best option for life in amid 672 00:38:39,960 --> 00:38:43,600 Speaker 2: the Jovian Moons. The best options I think are arguably 673 00:38:43,719 --> 00:38:47,120 Speaker 2: Europa and Ganymede. But you know, we know, based on 674 00:38:47,160 --> 00:38:49,440 Speaker 2: our own model of life here on Earth, that life 675 00:38:49,480 --> 00:38:52,080 Speaker 2: can thrive in extreme environments. And you know, over the 676 00:38:52,080 --> 00:38:54,839 Speaker 2: past several decades, I think that's become you know, more 677 00:38:54,840 --> 00:38:59,560 Speaker 2: and more crystallized in our understanding that you know, life 678 00:38:59,640 --> 00:39:02,920 Speaker 2: here on Earth is pretty rugged and certain models of 679 00:39:02,960 --> 00:39:06,960 Speaker 2: it can survive in very hostile conditions. So it's not 680 00:39:07,040 --> 00:39:09,879 Speaker 2: completely out of the question that something could evolve, either 681 00:39:09,920 --> 00:39:15,239 Speaker 2: evolve within those hostile conditions on another world, or survive 682 00:39:17,640 --> 00:39:20,200 Speaker 2: in such conditions, you know, after the loss of a 683 00:39:20,320 --> 00:39:25,200 Speaker 2: previous habitat. And so I was looking around in one 684 00:39:25,280 --> 00:39:29,440 Speaker 2: individual in particular that has speculated a fair amount concerning 685 00:39:29,480 --> 00:39:35,600 Speaker 2: IO is German astrobiologist Dirk Schultz Makouch speculated in twenty 686 00:39:35,680 --> 00:39:39,840 Speaker 2: twenty three on Big Think about the possibility. The title 687 00:39:39,880 --> 00:39:43,239 Speaker 2: of the Big Think article that he crafted is there 688 00:39:43,280 --> 00:39:47,640 Speaker 2: could be life on hot volcanic Io. Jupiter's quote pizza met. 689 00:39:48,880 --> 00:39:51,080 Speaker 3: We talked about the pizza surface in the last episode. 690 00:39:51,120 --> 00:39:52,839 Speaker 3: It looks like it's got I don't know, what would 691 00:39:52,840 --> 00:39:56,520 Speaker 3: you say? The topping selection is definitely pepperoni and olives. 692 00:39:56,600 --> 00:39:59,560 Speaker 2: Yeah, yeah, and cheese of course, the fair amount of cheese, 693 00:40:00,040 --> 00:40:05,000 Speaker 2: mozzarella and or parmesan on top. And of course Schultz 694 00:40:05,120 --> 00:40:09,000 Speaker 2: macouch has has also a third and co authored a 695 00:40:09,040 --> 00:40:12,160 Speaker 2: number of peer reviewed articles that the Big Think article 696 00:40:12,239 --> 00:40:15,719 Speaker 2: is more is more general audience. But but he goes through, 697 00:40:15,840 --> 00:40:18,640 Speaker 2: you know, all the major points that he hits in 698 00:40:18,680 --> 00:40:22,320 Speaker 2: some of these other articles, and he drives home that 699 00:40:22,719 --> 00:40:26,120 Speaker 2: the Juno mission revealed much more about Io than we 700 00:40:26,200 --> 00:40:30,879 Speaker 2: previously knew, and that based on these more recent discoveries, 701 00:40:31,200 --> 00:40:34,719 Speaker 2: you know, it's reasonable to hypothesize that while Io is 702 00:40:34,800 --> 00:40:39,600 Speaker 2: now this volcanic world of extreme cold and extreme hot temperatures, 703 00:40:40,040 --> 00:40:43,040 Speaker 2: it may have once had as much liquid water as 704 00:40:43,080 --> 00:40:46,440 Speaker 2: Europa and Ganny meat and during those early days, the 705 00:40:46,440 --> 00:40:50,840 Speaker 2: combination combination of liquid water and geothermal heat again you know, 706 00:40:50,920 --> 00:40:55,440 Speaker 2: highly volcanic world could have led to the development of life. However, 707 00:40:55,520 --> 00:40:58,279 Speaker 2: of course, this wouldn't be the case today. Io would 708 00:40:58,320 --> 00:41:01,040 Speaker 2: have gone on to lose most of the water due 709 00:41:01,040 --> 00:41:05,400 Speaker 2: to Jupiter's radiation and tidal forces, and this is pretty 710 00:41:05,440 --> 00:41:09,600 Speaker 2: much left the surface of Io quite uninhabitable. But what 711 00:41:09,719 --> 00:41:14,400 Speaker 2: about the underground, Well, Schulzmakouch stresses that it might still 712 00:41:14,480 --> 00:41:17,879 Speaker 2: prove too violent beneath Io's surface for life, Like it's 713 00:41:17,920 --> 00:41:21,960 Speaker 2: still it's still you know, not the best bat, but 714 00:41:22,520 --> 00:41:24,800 Speaker 2: you know. He says that there's a chance it could 715 00:41:25,360 --> 00:41:29,200 Speaker 2: survive there due to the possibibility of remaining abundant water 716 00:41:30,239 --> 00:41:36,160 Speaker 2: carbon and reduce sulfur compounds. So a dynamic, though possibly 717 00:41:36,239 --> 00:41:40,120 Speaker 2: too dynamic environment for life. Maybe not on the surface 718 00:41:40,160 --> 00:41:44,920 Speaker 2: of Io, but perhaps maybe underneath the surface of the planet, 719 00:41:45,440 --> 00:41:47,239 Speaker 2: beneath the planet of the pizza if you will. 720 00:41:47,880 --> 00:41:51,080 Speaker 3: Yeah, that's where the remnants of their civilization worship a 721 00:41:51,120 --> 00:41:51,919 Speaker 3: giant pizza oven. 722 00:41:52,200 --> 00:41:56,600 Speaker 2: Yeah yeah, So where would we look for them, if 723 00:41:56,960 --> 00:41:59,480 Speaker 2: we could at all look look for them on this world, 724 00:41:59,680 --> 00:42:03,560 Speaker 2: We suggests lava tubes, which should be common on such 725 00:42:03,600 --> 00:42:06,720 Speaker 2: a volcanically active world. These would of course be beneath 726 00:42:06,760 --> 00:42:09,759 Speaker 2: the surface of Io, where they would possibly serve as 727 00:42:09,760 --> 00:42:13,319 Speaker 2: a safe haven for life, protected to some degree from 728 00:42:13,440 --> 00:42:19,120 Speaker 2: radiation and subject to warm at least semi constant temperatures. 729 00:42:19,800 --> 00:42:22,360 Speaker 2: And he stresses that lava tubes here on Earth, you know, 730 00:42:22,400 --> 00:42:24,600 Speaker 2: they provide a great example because they are often home 731 00:42:24,640 --> 00:42:28,719 Speaker 2: to extremophile and microbial life, regardless of the region in 732 00:42:28,760 --> 00:42:31,200 Speaker 2: which you find them. You know, this is true of 733 00:42:31,280 --> 00:42:33,920 Speaker 2: lava tubes in the desert as well as in Iceland, 734 00:42:33,920 --> 00:42:37,200 Speaker 2: in places like that. And on top of that, lava 735 00:42:37,239 --> 00:42:43,839 Speaker 2: tubes on Mars, according to schulsmaccooch the most plausible place 736 00:42:43,880 --> 00:42:47,080 Speaker 2: to find life on the Red planet. So lava tubes 737 00:42:47,120 --> 00:42:49,800 Speaker 2: in general great place to look for. It seems like 738 00:42:49,960 --> 00:42:52,680 Speaker 2: lava tubes should be present beneath the surface of Io 739 00:42:52,760 --> 00:42:55,319 Speaker 2: as well. Now, he also discusses that if there's not 740 00:42:55,480 --> 00:42:58,400 Speaker 2: enough water for life on Io, it's also feasible that 741 00:42:58,520 --> 00:43:02,320 Speaker 2: hydrogen sulfide might and in for water, though he stresses 742 00:43:02,360 --> 00:43:05,920 Speaker 2: that quote suggesting an alternative alternative solvent for life is 743 00:43:06,000 --> 00:43:09,480 Speaker 2: always very very speculative. Yeah, So I do want to 744 00:43:09,480 --> 00:43:12,360 Speaker 2: make sure I'm doing justice to what he has written 745 00:43:12,960 --> 00:43:16,200 Speaker 2: and said about this, because he's not saying there's definitely 746 00:43:16,239 --> 00:43:18,239 Speaker 2: life on ioh. He's saying, you know, we have to 747 00:43:18,719 --> 00:43:22,800 Speaker 2: keep an open mind about these things and discuss how 748 00:43:22,880 --> 00:43:26,120 Speaker 2: it could exist there based on what we know of 749 00:43:26,239 --> 00:43:27,160 Speaker 2: life here on Earth. 750 00:43:27,440 --> 00:43:29,240 Speaker 3: Right. Well, as you said that this is a common 751 00:43:29,320 --> 00:43:32,600 Speaker 3: experiment a lot of you know, people who are interested 752 00:43:32,640 --> 00:43:36,560 Speaker 3: in astrobiology go through. Is not to say there is 753 00:43:36,719 --> 00:43:40,120 Speaker 3: definitely life on Titan or whatever it is, but to say, Okay, 754 00:43:40,160 --> 00:43:43,719 Speaker 3: given the conditions we know about here, what could you 755 00:43:43,800 --> 00:43:46,759 Speaker 3: imagine working there? If we were to discover life in 756 00:43:46,840 --> 00:43:49,640 Speaker 3: this kind of place, where would we expect to find it, 757 00:43:49,680 --> 00:43:51,560 Speaker 3: What form would we expect it to take? 758 00:43:52,239 --> 00:43:54,920 Speaker 2: Yeah, and it sounds like the possibility here would be 759 00:43:54,960 --> 00:43:59,279 Speaker 2: some sort of you know, microbial extremeophile life form that 760 00:43:59,320 --> 00:44:02,680 Speaker 2: again is living in certain lava tubes where they're protected 761 00:44:02,680 --> 00:44:07,399 Speaker 2: from the radiation, where there's something like consistent warmth going 762 00:44:07,440 --> 00:44:10,279 Speaker 2: on and it's not subject to like massive freezes and 763 00:44:10,320 --> 00:44:15,400 Speaker 2: then massive you know, boiling temperatures. So but again it 764 00:44:15,400 --> 00:44:17,640 Speaker 2: would be down in these lava tubes. And one of 765 00:44:17,640 --> 00:44:19,799 Speaker 2: the things that he points out is that, yeah, these 766 00:44:20,239 --> 00:44:22,160 Speaker 2: we just have to speculate like this, This would be 767 00:44:22,239 --> 00:44:26,680 Speaker 2: very hard to just to explore one hundred percent for 768 00:44:26,719 --> 00:44:29,600 Speaker 2: a number of reasons. It's very difficult to figure out 769 00:44:29,600 --> 00:44:31,520 Speaker 2: how you would like land a craft or a rover 770 00:44:31,680 --> 00:44:35,080 Speaker 2: on IO and then dig down underneath the surface. It's 771 00:44:35,120 --> 00:44:38,719 Speaker 2: a very hostile world. However, there's still plenty of room 772 00:44:38,840 --> 00:44:42,879 Speaker 2: to explore it from an orbital standpoint, and we can 773 00:44:42,920 --> 00:44:45,880 Speaker 2: continue to learn more about the surface of Io and 774 00:44:45,960 --> 00:44:49,120 Speaker 2: the composition of IO, and in doing so we might 775 00:44:49,160 --> 00:44:52,200 Speaker 2: be able to make even better guesses about what might 776 00:44:52,239 --> 00:44:55,520 Speaker 2: be beneath the surface. All right, Well, on that note, 777 00:44:55,640 --> 00:44:58,439 Speaker 2: we're going to close out this episode, but we'll come 778 00:44:58,480 --> 00:45:02,239 Speaker 2: back with one more episode on Io this Thursday. In 779 00:45:02,280 --> 00:45:04,759 Speaker 2: the meantime, definitely feel free to write into us. We'd 780 00:45:04,760 --> 00:45:07,440 Speaker 2: love to hear from you your thoughts about anything we 781 00:45:07,520 --> 00:45:11,840 Speaker 2: discussed here. Examples of IO from science fiction. All of 782 00:45:11,840 --> 00:45:14,600 Speaker 2: that is fair Game will remind you the stuff to 783 00:45:14,640 --> 00:45:16,800 Speaker 2: blow your mind. Is primarily a science and culture podcast, 784 00:45:16,800 --> 00:45:19,320 Speaker 2: with core episodes on Tuesdays and Thursdays, short form episodes 785 00:45:19,320 --> 00:45:22,120 Speaker 2: on Wednesdays and on Fridays. We set aside most serious 786 00:45:22,120 --> 00:45:24,400 Speaker 2: concerns to just talk about a weird film on Weird 787 00:45:24,400 --> 00:45:27,160 Speaker 2: House Cinema. Maybe we'll get to Outland someday. It's been 788 00:45:27,160 --> 00:45:28,799 Speaker 2: on kind of like the shortlist for a little bit, 789 00:45:29,840 --> 00:45:34,040 Speaker 2: but maybe maybe someday soon If you would like us 790 00:45:34,040 --> 00:45:38,360 Speaker 2: to cover Outland on Weird House Cinema, write in and encourage. 791 00:45:38,040 --> 00:45:41,040 Speaker 3: Us, Sir, Sean just looks so serious. 792 00:45:41,400 --> 00:45:44,960 Speaker 2: Yeah, yeah, he's very serious in this one. I think 793 00:45:45,000 --> 00:45:46,680 Speaker 2: maybe that's why I've held off on this one, like 794 00:45:46,800 --> 00:45:49,239 Speaker 2: this is a gritty film, or at least that's my 795 00:45:49,360 --> 00:45:52,840 Speaker 2: memory of it. Very gritty, not a lot of fun 796 00:45:54,440 --> 00:45:58,200 Speaker 2: to be had, you know, it's it's a dirty future. 797 00:45:58,440 --> 00:46:00,279 Speaker 3: Oh, I've got a note. Does he just use his 798 00:46:00,360 --> 00:46:03,000 Speaker 3: normal accent or does he pretend to have a different accent? 799 00:46:04,040 --> 00:46:06,399 Speaker 2: Well, I don't remember, but if added that, I would say, 800 00:46:06,480 --> 00:46:10,720 Speaker 2: just normal accent. Okay, that's normally how it shakes out. 801 00:46:10,840 --> 00:46:15,399 Speaker 3: I would want to hear Sean Connery doing cowboy voice. Well, 802 00:46:15,440 --> 00:46:21,400 Speaker 3: howdy partner, all right, huge, Thanks as always to our 803 00:46:21,480 --> 00:46:25,040 Speaker 3: excellent audio producer JJ Posway. If you would like to 804 00:46:25,040 --> 00:46:27,360 Speaker 3: get in touch with us with feedback on this episode 805 00:46:27,440 --> 00:46:29,600 Speaker 3: or any other, to suggest a topic for the future, 806 00:46:29,680 --> 00:46:31,879 Speaker 3: or just to say hi, you can email us at 807 00:46:31,960 --> 00:46:42,240 Speaker 3: contact at stuff to Blow your Mind dot com. 808 00:46:42,440 --> 00:46:45,360 Speaker 1: Stuff to Blow Your Mind is production of iHeartRadio. For 809 00:46:45,440 --> 00:46:48,240 Speaker 1: more podcasts from my Heart Radio, visit the iHeartRadio app, 810 00:46:48,400 --> 00:46:56,480 Speaker 1: Apple Podcasts, or wherever you're listening to your favorite shows 811 00:47:00,040 --> 00:47:02,640 Speaker 2: The same priest with rapt