WEBVTT - How Ice Ages Work

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<v Speaker 1>This episode of Stuff you Should Know is brought to

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<v Speaker 1>website apart. Welcome to Stuff you Should Know from House

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<v Speaker 1>Stuff Works dot com. Hey, I'm welcome to the podcast.

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<v Speaker 1>I'm Josh Clark, and there's Charles W. Chuck Bryant and

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<v Speaker 1>uh guests. Who's over there being quiet as a church mouse.

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<v Speaker 1>The producer who may or may not exist, Jerry. People

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<v Speaker 1>still think that. I think a few people do. Yeah,

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<v Speaker 1>she's real, says you. She's real because I can always

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<v Speaker 1>smell her me. So from here? Oh man? I um,

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<v Speaker 1>so I like avocado a lot, right, So I like

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<v Speaker 1>avocado a lot. Basically an avocado a day. Um, And

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<v Speaker 1>normally I make guacamole. As you know, I make probably

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<v Speaker 1>the best guacamole on the planet. Sometimes, okay, we'll have

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<v Speaker 1>a guac off one day. Well, yeah, but it's personal taste,

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<v Speaker 1>you know, you know that whole thing. Remember, no taste

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<v Speaker 1>is absolute. Um. So it's sometimes it's just too much

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<v Speaker 1>to make guac sure, right, that's where avocado toast comes in. Yeah,

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<v Speaker 1>it's so easy, but and it's totally different too. So

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<v Speaker 1>if you start to get sick of guacamole, you like,

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<v Speaker 1>I'll have some avocado toast. Anyway. The upshot is is

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<v Speaker 1>I recently took antibiotics, which are disgusting poison, but just

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<v Speaker 1>had to have them this time because my body would

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<v Speaker 1>not get rid of whatever had um. And so I've

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<v Speaker 1>been like repopulating my gut flora with fermented stuff like

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<v Speaker 1>mis Took some miso, put it in some avocado, whipped

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<v Speaker 1>it up, spread it on some toasts. It was great.

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<v Speaker 1>And avocado, being a fibrous vegetable, should be a prebiotic.

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<v Speaker 1>It will probably provide the conditions for that miso to

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<v Speaker 1>ripen into some really top notch gut flora. Well I'm

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<v Speaker 1>grossed out now, are you really? Yeah? I found that

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<v Speaker 1>stuff fascinating. All that your gut flora. It's a matter

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<v Speaker 1>of personal taste. I guess. It's like people like the

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<v Speaker 1>smell of their own poop. That's not two different things.

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<v Speaker 1>Do you like the smelling your own poop? Great? Really? Yeah?

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<v Speaker 1>I like all my smells. I got you. Do you

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<v Speaker 1>like ice? Ay? Just I do? We're in one yeah,

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<v Speaker 1>well can we be in a noisy age? It's hottest wherever, right,

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<v Speaker 1>but the climb is not changing. Why this summer has

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<v Speaker 1>been awful? Yeah, supposedly every year we just keep getting

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<v Speaker 1>hotter and hotter. Yeah, And I'm like, I have a

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<v Speaker 1>feeling here and Georgia, it's going to be hot into October.

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<v Speaker 1>I noticed the change take place to day Oh really?

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<v Speaker 1>Uh not me. I was out there this morning, but

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<v Speaker 1>momo out well yeah, and I was like, oh, it's

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<v Speaker 1>not muggy night. Nights are getting cooler. That's where it

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<v Speaker 1>starts to change. Yeah, but it's still like up in

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<v Speaker 1>the nineties during the day. During the day is still

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<v Speaker 1>kind of nasty. But it feels different to me, like

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<v Speaker 1>the air feels different. Yeah, not me yet. Yeah, that

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<v Speaker 1>that first fall blasts I haven't experienced. Maybe it's seeing

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<v Speaker 1>like cinnamon brooms and Kroger that's put me in the

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<v Speaker 1>fall mood already. I'm just noticing it where it's not

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<v Speaker 1>the Christmas decorations, right, yeah, Halloween stuff's been out since August. Man,

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<v Speaker 1>just ridiculous. So back to ice ages. Um, like you said,

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<v Speaker 1>we are actually in an ice age. To be specific,

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<v Speaker 1>we are in the Holocene epoch right, yes, which features

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<v Speaker 1>the Quaternary ice age, and specifically we're in the flandry

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<v Speaker 1>and interglacial period. But still, even though it's interglacial, it's

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<v Speaker 1>still an ice age that we're in. It's a mouthful,

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<v Speaker 1>it is. Who wrote this? Was this? Molly? Molly Edmonds,

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<v Speaker 1>our dear old friend. Yes, she she put out quality

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<v Speaker 1>she did. Um. Yeah, Molly points out quite astutely that, uh,

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<v Speaker 1>you know, if you look at Antarctica in Greenland, you

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<v Speaker 1>still see ice sheets and um ice ages. Though are

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<v Speaker 1>it's not you know, we don't have to have the

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<v Speaker 1>entire or a third of the earth covered in ice

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<v Speaker 1>to be in an ice age, because within an ice

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<v Speaker 1>age there's periods of cooler weather and warmer weather, and

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<v Speaker 1>right now that you know, glacials and interglacials respectively, and

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<v Speaker 1>right now we're in an interglacial. That's all it is.

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<v Speaker 1>But like I said, when people look around, they don't

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<v Speaker 1>think of as being in an ice age, because we're

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<v Speaker 1>just during one of those warmer periods, right. But I

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<v Speaker 1>think so. I was reading this New Scientist article about

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<v Speaker 1>I think it's called the History of Ice on Earth,

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<v Speaker 1>and they said that there are basically three settings that

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<v Speaker 1>the Earth has. UM greenhouse, which is basically there's no

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<v Speaker 1>ice anywhere on Earth. UH. Ice house which is like

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<v Speaker 1>an ice age glacial period where there is ice even

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<v Speaker 1>like today there's ice on the Arctic and Antarctic caps

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<v Speaker 1>right um. And then there's a snowball um setting the

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<v Speaker 1>most fun of all, which is like the entire planet

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<v Speaker 1>is frozen over the least fun of all. There have

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<v Speaker 1>been periods of Earth's history where the whole thing was

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<v Speaker 1>just a giant ball of ice. Yeah, if we want

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<v Speaker 1>to talk about the you know, the I don't know

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<v Speaker 1>if you want to call it the Big Ice Age.

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<v Speaker 1>But when we think of the term ice age, we

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<v Speaker 1>most people are probably talking about the one that began

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<v Speaker 1>about seventy thousand years ago, uh during the Pleistocene era

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<v Speaker 1>lasted about sixty thousand years UH. And if you're talking

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<v Speaker 1>about the United States, uh, and the four major glaciations

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<v Speaker 1>they hit the Midwest, the Nebraska and the Kanson the

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<v Speaker 1>Illinois and the famous Wisconsin glaciation. Yeah, that's the one

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<v Speaker 1>that just ended that. We just came out of the

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<v Speaker 1>Wisconsin one, that's right. And they call him this because

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<v Speaker 1>that's where they were geographically. Well that's where I think

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<v Speaker 1>the greatest evidence of them has been discovered. Right. So, um,

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<v Speaker 1>and in all this it's kind of confusing, actually, but

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<v Speaker 1>just just the the current ice age that we're in

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<v Speaker 1>started two point five eight million years ago, right, and

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<v Speaker 1>again it's still going two point five eight million years

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<v Speaker 1>to present, the quaternary ice age. Um. And so those

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<v Speaker 1>little other subdivisions have to do with when the ice

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<v Speaker 1>has been relatively scarce or when it's been all over

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<v Speaker 1>the place. And then to make it even more slightly,

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<v Speaker 1>can using during periods of glaciation. There's even periods where

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<v Speaker 1>the glaciers retreat and advance. That's stadial and interstadial periods,

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<v Speaker 1>and those tend to be a little more local. Uh,

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<v Speaker 1>And and happened a lot a lot more quickly, and

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<v Speaker 1>glacial or in an interglacial period, happened on the scale

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<v Speaker 1>of tens of thousands of years. Yes, that's right. And uh,

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<v Speaker 1>this is nothing new, Like you said, this has been

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<v Speaker 1>going on since there was a planet Earth. But um,

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<v Speaker 1>actually recognizing and and what is an ice age just

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<v Speaker 1>sort of on the newer front, because in the old days,

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<v Speaker 1>you know, they would see a big rock and they

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<v Speaker 1>would say, boy, the thing looks like it slid down

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<v Speaker 1>that mountain there, because you can see that mountains all

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<v Speaker 1>carved up and this rock shouldn't be here, and that's weird.

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<v Speaker 1>So that was the Great Flood of Biblical Times. We

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<v Speaker 1>treated an episode on Yeah, that was a good one,

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<v Speaker 1>and um, so that was kind of how things were explained,

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<v Speaker 1>how these things ended up places where they probably did

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<v Speaker 1>not start out. Yeah, people noticed that there was just

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<v Speaker 1>weird stuff going on in the geography around them, right, Um,

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<v Speaker 1>but they didn't they didn't place it correctly. Until it

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<v Speaker 1>turns out the Swiss peasantry and some German peasants as well,

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<v Speaker 1>started to notice that their glaciers were receding. And as

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<v Speaker 1>their glaciers receded up there and say the Alps, it

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<v Speaker 1>left some markings that they noticed also the same kind

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<v Speaker 1>of markings further down the mountain. So the Swiss peasants

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<v Speaker 1>put two and two together and said, you know what,

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<v Speaker 1>I think the glaciers used to be way, way bigger

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<v Speaker 1>than they are today, and that maybe that is what

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<v Speaker 1>explains these boulders that shouldn't be here being here in

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<v Speaker 1>the middle of this field. And I guess from what

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<v Speaker 1>I can gather, it was kind of like common folk

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<v Speaker 1>wisdom in some areas of like the Swiss Alps, long

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<v Speaker 1>before science understood it. And it was actually a Swiss

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<v Speaker 1>geologist who was the first one to advance a genuine

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<v Speaker 1>bona fide hypothesis for ice ages. Yeah, Lewis Uh, I

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<v Speaker 1>guess sees is how I'm gonna pronounce that. And um

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<v Speaker 1>he in seven presented um his ideas about this glacial

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<v Speaker 1>activity at a conference, the science conference, and everyone was like, yeah,

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<v Speaker 1>m I don't know. I don't know about you. I

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<v Speaker 1>don't know about that. Well, they didn't know about him.

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<v Speaker 1>He was he was a smart guy, right, he was established.

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<v Speaker 1>But they're like, you're just go back to your opium

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<v Speaker 1>pretty much. And apparently his his first theory was that

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<v Speaker 1>there there have been an ice age. It happened like

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<v Speaker 1>very quickly. Yeah, he was off basically like night and day. Uh,

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<v Speaker 1>and and that um it had followed a catastrophe, right, Yeah.

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<v Speaker 1>I wonder if he would have that seems like the

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<v Speaker 1>one thing that might have put them off. It was

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<v Speaker 1>how unlikely that sounded right? Because he was wrong? Like

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<v Speaker 1>I won. If you would have said it happened slowly

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<v Speaker 1>over time, let's say, yeah, they may have said like,

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<v Speaker 1>oh well, I'm not buy that he's presenting his finding.

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<v Speaker 1>He's like, what do you guys want to hear? But

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<v Speaker 1>I'll massage it in that way. Yeah, it happened overnight

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<v Speaker 1>and they all just cross their arms. He goes or

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<v Speaker 1>overnight over a very long period of time. Uh so

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<v Speaker 1>before him though, um, quite a few years before him,

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<v Speaker 1>there was a scotsman. Oh yeah, born in Edinburgh, Edinburgh,

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<v Speaker 1>buried at Greyfriars Kirkyard. Wow, which did you ever go there?

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<v Speaker 1>I walked past it. I never made it in Okay,

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<v Speaker 1>well my hotel was right there, so I walked through it. Amazing,

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<v Speaker 1>amazing cemetery. I went to Marry King's close instead, which

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<v Speaker 1>is pretty awesome too. Oh you had to go to

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<v Speaker 1>one or the other. They're close to each other. Um,

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<v Speaker 1>there's only so much time in the day. Off not

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<v Speaker 1>close enough? Uhive a man named James Hutton, uh man,

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<v Speaker 1>this guy was He was a stud the father of geology.

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<v Speaker 1>He had this idea that he he was one of

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<v Speaker 1>the first people to look around and say, you know what,

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<v Speaker 1>the Earth is always changing, Like if you look around

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<v Speaker 1>and pay attention, look at it, that birds just died.

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<v Speaker 1>Like he might sit for days and look and wait

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<v Speaker 1>for something to move. But he said, the Earth is

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<v Speaker 1>constantly changing, and I have an idea that it's probably

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<v Speaker 1>always been this way. So if we look at what's

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<v Speaker 1>going on now and we apply that to the past,

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<v Speaker 1>we might come up with some pretty interesting stuff here, right. Yeah,

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<v Speaker 1>he said that there's basically clues to the past in

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<v Speaker 1>the present. Yeah, just like, look what's going on around you.

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<v Speaker 1>This might have happened ten thousand years ago as well,

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<v Speaker 1>and that might explain something like that boulder being someplace

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<v Speaker 1>different exactly. And we keep going to the boulders. But

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<v Speaker 1>the boulders are actually some really really high quality evidence

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<v Speaker 1>for ice ages in general. Um, there's there. There's actually

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<v Speaker 1>a term for it among people who study ice ages.

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<v Speaker 1>They're called erratics. And an erratic is a very very

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<v Speaker 1>heavy boulder, way too heavy to have been moved by humans.

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<v Speaker 1>Um that is also too far from its point of

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<v Speaker 1>origin to just say rolled downhill it doesn't make any

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<v Speaker 1>sense that it's there, which is why it's called n erratic.

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<v Speaker 1>There's some very famous ones. Um, there's one in the

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<v Speaker 1>Swiss Alps. Uh, well, I'm sure there's many, but there's

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<v Speaker 1>one in particular. This article mentions that's in the Swiss

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<v Speaker 1>Alps that is, um, about fifty miles from its point

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<v Speaker 1>of origin. There's one in Central Park that is many

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<v Speaker 1>miles away from its point of origin. In New Jersey,

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<v Speaker 1>it moved, tried to make it in the big city.

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<v Speaker 1>It was a bridge and tunnel boulder, right. So, and

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<v Speaker 1>that's actually one of the one of the ways the

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<v Speaker 1>Germans figured out that there was such a thing as

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<v Speaker 1>ice age because they said, see that bowler there in

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<v Speaker 1>that field, I'm pretty sure that skinnin Avian rock, and uh,

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<v Speaker 1>sure enough they were correct. And so you start to

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<v Speaker 1>put all this stuff together, huge bowlders being moved, Um,

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<v Speaker 1>valleys between mountains, carved out in a U shape rather

0:13:01.840 --> 0:13:05.840
<v Speaker 1>than that telltale V shape that a river carves out. Um.

0:13:05.880 --> 0:13:08.560
<v Speaker 1>These are clues. They're not well they are erratics, but

0:13:09.040 --> 0:13:11.800
<v Speaker 1>their clues into the past. Yeah that when you start

0:13:11.840 --> 0:13:14.679
<v Speaker 1>to put all of them together. The only thing that

0:13:14.679 --> 0:13:21.080
<v Speaker 1>that really explains them, is huge, massive movements of glaciers.

0:13:21.400 --> 0:13:24.800
<v Speaker 1>Glacial movement. Yeah. And and when you study that stuff

0:13:25.160 --> 0:13:27.640
<v Speaker 1>and you look at these grooves and you study the boulders,

0:13:27.640 --> 0:13:30.880
<v Speaker 1>you can actually make calculations. And it's amazing that way

0:13:30.920 --> 0:13:34.319
<v Speaker 1>back then they were able to make these calculations. Uh.

0:13:34.360 --> 0:13:38.320
<v Speaker 1>Agazz in particular and some other guys got together and

0:13:38.360 --> 0:13:42.480
<v Speaker 1>they said that the present ice age at its peak,

0:13:42.559 --> 0:13:46.560
<v Speaker 1>I guess, um, was about a mile thick of glacier

0:13:47.080 --> 0:13:51.560
<v Speaker 1>A mile of ice. Yes, it's amazing yeah. Um. And

0:13:52.120 --> 0:13:56.280
<v Speaker 1>further studies have concluded that in the last ice age, um,

0:13:56.320 --> 0:14:02.000
<v Speaker 1>I guess there was Wisconsin glaciation. Um. The the about

0:14:02.000 --> 0:14:05.240
<v Speaker 1>a third of the earth was covered in glaciers. Have

0:14:05.400 --> 0:14:08.000
<v Speaker 1>we said that glacier as yet? I mean, it almost

0:14:08.000 --> 0:14:09.960
<v Speaker 1>goes without saying, but just in case. Yeah, it's just

0:14:09.960 --> 0:14:13.559
<v Speaker 1>really densely packed snow it is, and it snow that

0:14:13.559 --> 0:14:16.400
<v Speaker 1>that isn't allowed to melt. It's it's cold enough so

0:14:16.440 --> 0:14:18.920
<v Speaker 1>that it never fully melts. At the base, it forms

0:14:18.960 --> 0:14:22.240
<v Speaker 1>to ice, and on top you've got more and more snow,

0:14:22.280 --> 0:14:24.640
<v Speaker 1>and as more and more snow doesn't melt, the ice

0:14:24.640 --> 0:14:27.560
<v Speaker 1>builds up thicker and thicker and just from the sheer

0:14:27.680 --> 0:14:32.920
<v Speaker 1>force of these things mass encountering gravity, they can actually move.

0:14:33.120 --> 0:14:36.760
<v Speaker 1>They're like very slow most of the time, very slow

0:14:36.840 --> 0:14:41.960
<v Speaker 1>moving rivers of ice on a massive scale. Yeah, and

0:14:41.960 --> 0:14:44.120
<v Speaker 1>and well we'll get to that later. I was gonna

0:14:44.360 --> 0:14:47.400
<v Speaker 1>tease something out. Uh, should we take a quick break?

0:14:48.040 --> 0:14:50.360
<v Speaker 1>All right, we'll take a break and we'll get back

0:14:50.400 --> 0:15:19.160
<v Speaker 1>to a little more amazing glaciers. All right. So we've

0:15:19.160 --> 0:15:23.640
<v Speaker 1>talked about the sheer size a mile a mile thick

0:15:23.680 --> 0:15:25.560
<v Speaker 1>of ice. Yeah, and I said, like a third of

0:15:25.560 --> 0:15:28.760
<v Speaker 1>the Earth. I think it covered seventeen million square miles

0:15:28.760 --> 0:15:31.840
<v Speaker 1>of the planet during the last glaciation cubic miles, my friend,

0:15:31.880 --> 0:15:35.640
<v Speaker 1>cubic miles, right, So junk is deep. Yeah, a mile deep. Man,

0:15:35.640 --> 0:15:39.840
<v Speaker 1>That is nuts. Uh. So Antarctica had about ten percent

0:15:39.880 --> 0:15:42.720
<v Speaker 1>more ice than it does now. And the big change

0:15:42.960 --> 0:15:46.000
<v Speaker 1>with the big difference, Uh, what sets that ice age

0:15:46.000 --> 0:15:49.920
<v Speaker 1>apart was the amount of activity in the northern hemisphere.

0:15:49.920 --> 0:15:52.440
<v Speaker 1>It was very unusual to have the amount of ice

0:15:52.600 --> 0:15:56.720
<v Speaker 1>in North America and Europe extending down like through the

0:15:56.760 --> 0:16:00.120
<v Speaker 1>midwest of the United States. It was it was a

0:16:00.160 --> 0:16:03.160
<v Speaker 1>new scene, a new chili scene. Ye, a whole new

0:16:03.240 --> 0:16:06.480
<v Speaker 1>jam basically, and Chuck. I mean like it was largely

0:16:06.520 --> 0:16:10.840
<v Speaker 1>in North America, but this also, um really covered a

0:16:10.880 --> 0:16:14.120
<v Speaker 1>lot of Europe too. I mean like Ireland was covered,

0:16:14.200 --> 0:16:18.760
<v Speaker 1>Germany was covered, Scandinavia was covered by ice, and basically

0:16:19.040 --> 0:16:22.280
<v Speaker 1>everything that wasn't covered by ice, and Europe was a tundra,

0:16:22.760 --> 0:16:25.720
<v Speaker 1>very much like Siberia is today. I actually I saw

0:16:25.760 --> 0:16:28.040
<v Speaker 1>a documentary on I think it was a History Channel

0:16:28.200 --> 0:16:33.320
<v Speaker 1>show about the Last Ice Age, and um, somebody figured

0:16:33.360 --> 0:16:35.520
<v Speaker 1>out how much all of that ice weight are you

0:16:35.560 --> 0:16:40.360
<v Speaker 1>ready for this? Basilion pounds? This might be more than

0:16:40.400 --> 0:16:45.280
<v Speaker 1>a bazillion sixty eight thousand trillion tons was the total

0:16:45.320 --> 0:16:48.080
<v Speaker 1>weight of the ice of the Earth on the Earth

0:16:48.160 --> 0:16:50.760
<v Speaker 1>during the Last Ice Age, during the last place. How

0:16:50.760 --> 0:16:53.920
<v Speaker 1>many maxes that have no idea? It's like more than

0:16:54.040 --> 0:16:59.320
<v Speaker 1>a hundred uh well a North America loan about thirteen, Um,

0:16:59.520 --> 0:17:02.920
<v Speaker 1>I'm sorry, about ten million square miles of ice. And

0:17:03.400 --> 0:17:05.320
<v Speaker 1>you know this all came from the ocean, which means

0:17:06.040 --> 0:17:08.920
<v Speaker 1>the ocean level was hundreds and hundreds of feet lower

0:17:09.240 --> 0:17:11.560
<v Speaker 1>during this ice age. Yeah, like Canada is used to

0:17:11.720 --> 0:17:14.919
<v Speaker 1>having large parts of it being covered by glacier, the

0:17:14.960 --> 0:17:17.440
<v Speaker 1>United States is not used to this, but it came

0:17:17.480 --> 0:17:21.240
<v Speaker 1>all the way down into the plains in some cases,

0:17:21.720 --> 0:17:26.640
<v Speaker 1>and basically from New York over to Washington State totally

0:17:26.680 --> 0:17:32.679
<v Speaker 1>covered by again a mile thick sheet of ice. Like

0:17:32.680 --> 0:17:35.520
<v Speaker 1>you can ice skate on that without worry. You're not

0:17:35.560 --> 0:17:39.200
<v Speaker 1>gonna fall through, it's still gonna crack. Did you ever

0:17:39.240 --> 0:17:42.480
<v Speaker 1>do that growing up? Did Ohio? Like like you'd skate

0:17:42.520 --> 0:17:45.119
<v Speaker 1>on lakes? Yeah, And we were never allowed to do

0:17:45.200 --> 0:17:47.880
<v Speaker 1>that until my dad went out and stomped on it,

0:17:47.960 --> 0:17:50.680
<v Speaker 1>like jumped up and down, and if he didn't go through,

0:17:50.760 --> 0:17:52.639
<v Speaker 1>then we were allowed to skate. He's like, kids, if

0:17:52.680 --> 0:17:55.359
<v Speaker 1>I die right. It wasn't. It wasn't the most fool

0:17:55.400 --> 0:17:57.959
<v Speaker 1>proof technique, but it was nice and dad to do

0:17:58.040 --> 0:18:00.960
<v Speaker 1>that for us. I don't know, think I'm not much

0:18:00.960 --> 0:18:02.879
<v Speaker 1>of a worry word, but I'm that still would have

0:18:02.880 --> 0:18:04.520
<v Speaker 1>like creeped me out. I've seen enough movies, you know,

0:18:05.160 --> 0:18:08.640
<v Speaker 1>left under ice. So the Mammi River would freeze over,

0:18:08.760 --> 0:18:10.480
<v Speaker 1>but we weren't allowed to skate on the river. Some

0:18:10.520 --> 0:18:12.760
<v Speaker 1>people did, we weren't allowed to. Instead, there was a

0:18:12.800 --> 0:18:16.120
<v Speaker 1>golf course with ponds that would freeze pretty good, pretty good.

0:18:16.560 --> 0:18:18.320
<v Speaker 1>There was your You weren't going to fall through these

0:18:18.320 --> 0:18:22.760
<v Speaker 1>small ponds pretty rough though, right, like skating on it's

0:18:22.760 --> 0:18:25.639
<v Speaker 1>not it depends it depends on and I don't remember

0:18:25.680 --> 0:18:27.800
<v Speaker 1>what it depends on. Yeah, it's it's never like an

0:18:27.800 --> 0:18:32.560
<v Speaker 1>ice drink. But certain type of weather, maybe non windy weather,

0:18:32.600 --> 0:18:35.080
<v Speaker 1>I think is what it was, because then like if

0:18:35.080 --> 0:18:37.359
<v Speaker 1>there was kind of like a choppiness to it from

0:18:37.400 --> 0:18:40.800
<v Speaker 1>the wind, it could freeze like that freeze choppy, Whereas

0:18:40.840 --> 0:18:43.280
<v Speaker 1>if it wasn't windy, I would guess it would it

0:18:43.320 --> 0:18:47.000
<v Speaker 1>would be smoother. So sometimes it was pretty smooth. Other

0:18:47.040 --> 0:18:48.639
<v Speaker 1>times you're like, I can't even skate on, but your

0:18:48.720 --> 0:18:51.240
<v Speaker 1>dad would drive a zambonie out there and fix it

0:18:51.280 --> 0:18:54.320
<v Speaker 1>all up. It over and if the zamboni didn't fall through,

0:18:54.359 --> 0:18:57.520
<v Speaker 1>then we were allowed to skate, right. I just picture

0:18:57.520 --> 0:18:59.640
<v Speaker 1>of the zamboni falling through. But it's a little pond,

0:18:59.680 --> 0:19:04.120
<v Speaker 1>so you're a'd still like just a bove. I feel

0:19:04.119 --> 0:19:06.560
<v Speaker 1>like I missed out, though, I mean not that life

0:19:06.600 --> 0:19:09.160
<v Speaker 1>is over. You can still skate on ponds. I don't

0:19:09.200 --> 0:19:13.440
<v Speaker 1>picture myself going to Minnesota in the in the winter.

0:19:14.000 --> 0:19:17.080
<v Speaker 1>Give it a try. The trade off it wasn't It

0:19:17.119 --> 0:19:19.560
<v Speaker 1>wasn't a very good trade off because the winners are

0:19:19.560 --> 0:19:22.359
<v Speaker 1>pretty brutal. Yeah, like if you have local ponds that

0:19:22.400 --> 0:19:26.280
<v Speaker 1>freeze over, you're cold too. I still feel like I

0:19:26.359 --> 0:19:28.919
<v Speaker 1>missed out. Yeah, I mean you're fine. It wasn't that

0:19:28.920 --> 0:19:30.679
<v Speaker 1>big of it was just teasing when I said, you

0:19:30.720 --> 0:19:35.000
<v Speaker 1>did miss that. Uh all right, So people are skating

0:19:35.040 --> 0:19:37.440
<v Speaker 1>all over the world. A third of the world people

0:19:37.440 --> 0:19:41.040
<v Speaker 1>are ice skating on during during the ice age UM

0:19:41.160 --> 0:19:44.560
<v Speaker 1>and like we mentioned these things, UM they've been described

0:19:44.600 --> 0:19:49.760
<v Speaker 1>as bulldozers just plowing through uh the earth basically um

0:19:49.880 --> 0:19:53.719
<v Speaker 1>leaving large swaths they call it glacial till. This debris

0:19:53.800 --> 0:19:57.200
<v Speaker 1>that they leave behind, and these are you know, once

0:19:57.240 --> 0:20:00.000
<v Speaker 1>you figure out how it works, the evidence is every

0:20:00.080 --> 0:20:03.719
<v Speaker 1>where of exactly what happened. Yeah, Because as these glaciers

0:20:03.800 --> 0:20:06.840
<v Speaker 1>move and that ice that has formed the basis of

0:20:06.880 --> 0:20:10.879
<v Speaker 1>the glacier is in contact with the earth below it,

0:20:10.880 --> 0:20:13.479
<v Speaker 1>it's picking up all sorts of crud that all that

0:20:13.640 --> 0:20:17.199
<v Speaker 1>to breathe that glacial till you said, erratic boulders. And

0:20:17.200 --> 0:20:21.600
<v Speaker 1>as it's doing this, it's actually creating a um a

0:20:21.760 --> 0:20:24.480
<v Speaker 1>scrubbing mechanism. Right. So, like you said, if you look

0:20:24.480 --> 0:20:29.760
<v Speaker 1>around at mountains and and and valleys with exposed rock

0:20:30.280 --> 0:20:34.160
<v Speaker 1>that were um rubbed by glaciers. There's gonna be crazy

0:20:34.240 --> 0:20:38.600
<v Speaker 1>grooves worked into them. Some look like roads almost, yes, um,

0:20:38.680 --> 0:20:42.080
<v Speaker 1>some are kind of polished and rounded, And it's all

0:20:42.119 --> 0:20:45.240
<v Speaker 1>from this glacial activity rubbing stuff over the tops of

0:20:45.280 --> 0:20:48.240
<v Speaker 1>these mountains. It's pretty interesting stuff. And then other things

0:20:48.320 --> 0:20:50.280
<v Speaker 1>like you'll know, you know, you'll see like a movie

0:20:50.320 --> 0:20:56.480
<v Speaker 1>where um, this incredibly beautiful uh like river Valley has

0:20:56.760 --> 0:21:01.040
<v Speaker 1>just gravel everywhere, like just scattered all all throughout, like

0:21:01.119 --> 0:21:04.600
<v Speaker 1>the valley floor. That's not supposed to be there. The

0:21:04.680 --> 0:21:07.800
<v Speaker 1>glacier deposited that. That's right, it's more evidence of the

0:21:07.920 --> 0:21:11.120
<v Speaker 1>ice age. Yeah, that's interesting to think of it. It's

0:21:11.160 --> 0:21:13.280
<v Speaker 1>not supposed to be there. No, and you think of

0:21:13.320 --> 0:21:15.679
<v Speaker 1>that like that's what that's what that looks like. You know,

0:21:15.760 --> 0:21:18.520
<v Speaker 1>of course that's what it's. That's that's that's supposed to

0:21:18.520 --> 0:21:20.800
<v Speaker 1>be there. But no, it's technically not. Had we not

0:21:20.920 --> 0:21:25.360
<v Speaker 1>had um these glaciation events, that stuff wouldn't be there.

0:21:25.640 --> 0:21:30.520
<v Speaker 1>And that fascinating earth science. Uh is that your favorite science?

0:21:31.320 --> 0:21:34.480
<v Speaker 1>I think it's become it. Yeah, yeah, it really does

0:21:35.280 --> 0:21:40.280
<v Speaker 1>get me jazzed, all right. So it wasn't just um,

0:21:41.280 --> 0:21:44.200
<v Speaker 1>the direct path of these glaciers that was affected out

0:21:44.200 --> 0:21:49.800
<v Speaker 1>on the edges of these massive moving sheets of ice. Um,

0:21:50.000 --> 0:21:53.560
<v Speaker 1>you had things like arctic deserts, and you had these

0:21:53.680 --> 0:21:57.320
<v Speaker 1>big areas of dusty wind. Uh. And there's actually a

0:21:57.359 --> 0:21:59.639
<v Speaker 1>few ways to pronounce this l O E s s

0:22:00.160 --> 0:22:05.240
<v Speaker 1>heard everything from lowest to lows to less I like lowest, Yeah,

0:22:05.320 --> 0:22:09.399
<v Speaker 1>like lowest too. Um covering all over the earth basically,

0:22:09.560 --> 0:22:12.720
<v Speaker 1>and this is created by those glaciers just like grinding

0:22:12.760 --> 0:22:16.280
<v Speaker 1>into the earth. Yeah, um, stirn everything up right, and

0:22:16.320 --> 0:22:18.720
<v Speaker 1>then the wind just comes and picks it up, the

0:22:19.160 --> 0:22:22.119
<v Speaker 1>finest of the particles and just deposits them. So in

0:22:22.160 --> 0:22:26.000
<v Speaker 1>some places you had so if if your area wasn't

0:22:26.040 --> 0:22:29.199
<v Speaker 1>covered by glacier, that didn't mean you weren't affected by

0:22:29.200 --> 0:22:32.840
<v Speaker 1>the glaciation, because you would have these lowest deserts are

0:22:33.200 --> 0:22:36.480
<v Speaker 1>glacier glacial deserts that formed. And in some places the

0:22:36.520 --> 0:22:39.760
<v Speaker 1>lowest was like twenty ft thick, and apparently it's still there.

0:22:39.960 --> 0:22:44.000
<v Speaker 1>In much of the Midwest, the sub straight below the

0:22:44.080 --> 0:22:51.359
<v Speaker 1>soil is lowest, deposited from these lowest deserts UM. And

0:22:51.400 --> 0:22:53.560
<v Speaker 1>so you would think when you hear about this kind

0:22:53.560 --> 0:23:00.360
<v Speaker 1>of activity that it had to be like hundred degrees chillier, right,

0:23:00.680 --> 0:23:03.960
<v Speaker 1>or fifty or forty even, but it was only about

0:23:04.000 --> 0:23:08.720
<v Speaker 1>ten degrees fahrenheit about five point six celsius lower uh

0:23:08.720 --> 0:23:12.720
<v Speaker 1>than temperatures now, which it's it wouldn't think that that

0:23:12.760 --> 0:23:15.920
<v Speaker 1>would be enough, right, But it's not all just about

0:23:15.920 --> 0:23:18.920
<v Speaker 1>the temperature. That's kind of the point. No, The point

0:23:18.960 --> 0:23:21.640
<v Speaker 1>that Molly makes is that it's not like, oh, it's

0:23:21.680 --> 0:23:24.280
<v Speaker 1>just so much colder than it was before all the time.

0:23:24.760 --> 0:23:29.199
<v Speaker 1>The key to an ice age um forming glaciers a

0:23:29.200 --> 0:23:33.320
<v Speaker 1>glacial period is that this the time when it's supposed

0:23:33.359 --> 0:23:37.320
<v Speaker 1>to actually melt, is colder than usual, so that there's

0:23:37.440 --> 0:23:41.400
<v Speaker 1>less melt than than before. And the less melt you have,

0:23:41.920 --> 0:23:44.439
<v Speaker 1>the more chance you have for snow to fall and

0:23:44.520 --> 0:23:47.119
<v Speaker 1>make up for whatever melted and actually add to it,

0:23:47.359 --> 0:23:50.360
<v Speaker 1>which means that the glaciers growing. As long as more

0:23:50.400 --> 0:23:52.960
<v Speaker 1>snow is added to the glacier than it loses during

0:23:53.000 --> 0:23:56.159
<v Speaker 1>say the summer months, your glaciers growing. Yeah, and if

0:23:56.200 --> 0:23:58.919
<v Speaker 1>it's not losing much, it doesn't take much snow. And

0:23:59.000 --> 0:24:04.240
<v Speaker 1>this this cycles arts. There's something called albedo or albedo

0:24:04.520 --> 0:24:08.600
<v Speaker 1>albedo and it's uh, it's the real reflectivity of ice.

0:24:08.680 --> 0:24:11.760
<v Speaker 1>And you know once this ice gets going, it's reflecting

0:24:11.880 --> 0:24:14.320
<v Speaker 1>away the sun. So it's while you're hotter in the

0:24:14.359 --> 0:24:16.760
<v Speaker 1>summer wearing a black T shirt than a white T shirt. Yeah,

0:24:16.800 --> 0:24:19.320
<v Speaker 1>and it's just it creates that cycle basically where it's

0:24:19.359 --> 0:24:23.000
<v Speaker 1>all just compounding, all these different elements coming together absolutely

0:24:23.000 --> 0:24:25.399
<v Speaker 1>to make ice super thick. So you have if you

0:24:25.440 --> 0:24:29.280
<v Speaker 1>have a glacier form on planet Earth and it reflects

0:24:29.359 --> 0:24:32.360
<v Speaker 1>a bunch of sunlight and makes it colder, well that's

0:24:32.400 --> 0:24:35.960
<v Speaker 1>gonna create the conditions for other glaciers to form too,

0:24:36.160 --> 0:24:39.360
<v Speaker 1>So it has a compounding effect as well that albedo does.

0:24:39.560 --> 0:24:41.120
<v Speaker 1>All right, well let's take a break and we're gonna

0:24:41.119 --> 0:24:44.640
<v Speaker 1>come back and talk about a very famous Serbian mathematician.

0:25:10.040 --> 0:25:15.439
<v Speaker 1>All right, so I said, famous Serbian mathematician. Had you

0:25:15.440 --> 0:25:18.199
<v Speaker 1>already heard of this guy? Yeah? Really, i'd heard. I

0:25:18.200 --> 0:25:22.160
<v Speaker 1>had heard about the Milankovich cycles. Um. So his name

0:25:22.160 --> 0:25:25.960
<v Speaker 1>was Milutin Milankovic. And it's amazing to me that in

0:25:25.960 --> 0:25:30.200
<v Speaker 1>the nineteen twenties, people like well, i'll just say him,

0:25:30.440 --> 0:25:34.840
<v Speaker 1>was able to figure out with a lot of accuracy, um,

0:25:34.920 --> 0:25:39.359
<v Speaker 1>the Milankovich cycles. Basically, he said, you know what, I

0:25:39.400 --> 0:25:43.000
<v Speaker 1>have a theory on why these these summers are cooler,

0:25:43.280 --> 0:25:47.199
<v Speaker 1>and why this ice age happened, And it's not just

0:25:47.280 --> 0:25:51.280
<v Speaker 1>the temperatures, but it's because of the Sun's relationship to

0:25:51.320 --> 0:25:54.439
<v Speaker 1>the Earth and how much sun the Earth is getting

0:25:55.000 --> 0:25:57.919
<v Speaker 1>UH during the summer months. So he came up with

0:25:57.960 --> 0:26:02.320
<v Speaker 1>three different factors, the tilt UH in the Earth's axis,

0:26:03.000 --> 0:26:05.920
<v Speaker 1>the way the Earth wobbles on that axis, and then

0:26:06.119 --> 0:26:08.639
<v Speaker 1>how close we are to that heat, how close we

0:26:08.680 --> 0:26:11.920
<v Speaker 1>are the sun. He plugged those into a mathematical formula

0:26:12.520 --> 0:26:18.320
<v Speaker 1>and he came up with every one hundred thousand years,

0:26:19.560 --> 0:26:21.720
<v Speaker 1>he's predicting that we're going to get these ice ages.

0:26:22.280 --> 0:26:25.360
<v Speaker 1>Pretty amazing math for back then, it is, especially if

0:26:25.359 --> 0:26:28.200
<v Speaker 1>you go back. So he figured this out, and then

0:26:28.400 --> 0:26:31.480
<v Speaker 1>they went back and looked at the fossil record, the

0:26:31.480 --> 0:26:35.520
<v Speaker 1>geological record, because when he was working, they didn't have

0:26:35.720 --> 0:26:40.239
<v Speaker 1>this understanding. He wasn't like proving that like yes, predicting right.

0:26:40.760 --> 0:26:44.440
<v Speaker 1>So then um about that time and like the well

0:26:44.520 --> 0:26:46.960
<v Speaker 1>after that time, but in like the forties and fifties,

0:26:47.119 --> 0:26:50.280
<v Speaker 1>the US was building army bases all over the world

0:26:50.280 --> 0:26:54.320
<v Speaker 1>in some really crazy places, including the Arctic, and um

0:26:54.480 --> 0:26:58.000
<v Speaker 1>some scientists went along and started taking core samples from

0:26:58.000 --> 0:27:01.640
<v Speaker 1>those places. And they found air bubbles trapped in there

0:27:01.920 --> 0:27:03.840
<v Speaker 1>that were from like a million years ago, Like the

0:27:04.000 --> 0:27:06.920
<v Speaker 1>air was a million years old and it was untouched

0:27:07.080 --> 0:27:10.639
<v Speaker 1>virgin air. And um. They found that they could do

0:27:10.800 --> 0:27:13.120
<v Speaker 1>all sorts of stuff and learn all sorts of things

0:27:13.160 --> 0:27:15.600
<v Speaker 1>from this air. And one of the things they found

0:27:15.800 --> 0:27:21.199
<v Speaker 1>was the basically the time stamp for the ice ages

0:27:21.800 --> 0:27:24.600
<v Speaker 1>during the Quaternary period. And they found out that in

0:27:24.680 --> 0:27:27.840
<v Speaker 1>the first two million years, the first two thirds of

0:27:27.880 --> 0:27:33.360
<v Speaker 1>the Quaternary um ice age, the ice ages, glaciation occurred

0:27:33.359 --> 0:27:38.200
<v Speaker 1>every forty one years. And yeah, yeah, that's what I said.

0:27:38.320 --> 0:27:41.160
<v Speaker 1>He's like, but wait for it, and they said, okay,

0:27:41.160 --> 0:27:44.320
<v Speaker 1>in this this most recent million years, it switched to

0:27:44.480 --> 0:27:47.840
<v Speaker 1>a hundred thousand years. And he just said his arms crossed,

0:27:48.280 --> 0:27:54.280
<v Speaker 1>very smugly. Yeah. Um. And everybody said, that's amazing, that's fantastic. Scientists,

0:27:54.720 --> 0:27:58.560
<v Speaker 1>you guys in the lab coats what causes an ice age,

0:27:58.840 --> 0:28:01.919
<v Speaker 1>And there's just crickets coming back from the scientists, and

0:28:01.960 --> 0:28:05.160
<v Speaker 1>there still is today. Actually, actually, no, that's the opposite,

0:28:05.200 --> 0:28:08.480
<v Speaker 1>is true. Not crickets, but a ton of different answers

0:28:08.480 --> 0:28:12.440
<v Speaker 1>and a ton of different theories. Yeah, lots of crickets,

0:28:13.520 --> 0:28:16.399
<v Speaker 1>but not quite either. What would be the animal that

0:28:16.480 --> 0:28:21.920
<v Speaker 1>would talking crickets, Jimmy crickets everywhere? Man, that I was annoying,

0:28:21.960 --> 0:28:27.280
<v Speaker 1>putting forth, putting forth theories and and as with most things,

0:28:27.320 --> 0:28:30.119
<v Speaker 1>we usually kind of center on. I bet it was

0:28:30.280 --> 0:28:33.200
<v Speaker 1>like most of these things put together, which most scientists

0:28:33.240 --> 0:28:35.679
<v Speaker 1>do well, dude, I was thinking about this, and I

0:28:35.760 --> 0:28:38.960
<v Speaker 1>was like, yes, chaos theory, Like, we have such a

0:28:39.000 --> 0:28:42.360
<v Speaker 1>propensity as humans to be like there's one true explanation,

0:28:42.400 --> 0:28:45.680
<v Speaker 1>there's one factor that explains everything, and that is just

0:28:45.840 --> 0:28:48.760
<v Speaker 1>not the case. This is a perfect example of that.

0:28:48.840 --> 0:28:51.000
<v Speaker 1>I wonder if that's a tendency for humans to want

0:28:51.000 --> 0:28:53.560
<v Speaker 1>to be right. Like the people actually doing the research

0:28:53.960 --> 0:28:57.520
<v Speaker 1>say like, no, this is my ideas. Yeah, I think

0:28:57.600 --> 0:29:00.160
<v Speaker 1>that's part of it, But I think it's more are

0:29:00.160 --> 0:29:03.560
<v Speaker 1>just like our brains are wired to find like the

0:29:03.640 --> 0:29:08.560
<v Speaker 1>least common denominator to find, um, the easiest route. Yeah,

0:29:08.680 --> 0:29:11.720
<v Speaker 1>maybe you know, just for efficiency's sake, that makes sense.

0:29:12.120 --> 0:29:14.440
<v Speaker 1>I kind of like the idea of like, I'm hands

0:29:14.480 --> 0:29:18.080
<v Speaker 1>across America. Did you participate in Hands across America? Not

0:29:18.200 --> 0:29:21.040
<v Speaker 1>hated it back then, but oh man, I get it now.

0:29:21.040 --> 0:29:23.280
<v Speaker 1>I'm just kidding. I think I did actually, yeah, there

0:29:23.320 --> 0:29:25.680
<v Speaker 1>was huge, huge gaps, but it was still pretty great.

0:29:26.360 --> 0:29:28.200
<v Speaker 1>We should do a show on that. I didn't know

0:29:28.200 --> 0:29:31.000
<v Speaker 1>there were gaps, of course there were oh yeah, pretty

0:29:31.000 --> 0:29:33.840
<v Speaker 1>pretty big ones. Yeah, there was at no point complete.

0:29:35.080 --> 0:29:36.720
<v Speaker 1>I think our school did it. Wasn't that the deal?

0:29:37.400 --> 0:29:41.840
<v Speaker 1>Like probably did this church, church, hippie church. I don't

0:29:41.880 --> 0:29:43.840
<v Speaker 1>know if my church might have been like, no, we're

0:29:43.880 --> 0:29:46.360
<v Speaker 1>not holding hands. You could be holding hands with an atheist.

0:29:47.200 --> 0:29:49.800
<v Speaker 1>Probably you wouldn't even know it. That probably would have

0:29:49.840 --> 0:29:53.920
<v Speaker 1>been the case. All right. So another theory is, um,

0:29:54.000 --> 0:29:57.640
<v Speaker 1>we've talked a lot about plate tectonics and our geez

0:29:57.640 --> 0:30:03.000
<v Speaker 1>and the volcano episodes and what else the plate tectonics episode.

0:30:03.000 --> 0:30:07.520
<v Speaker 1>Did we do one on that specifically among the close

0:30:07.560 --> 0:30:11.160
<v Speaker 1>to episodes? Man, I don't remember where it first popped up,

0:30:11.200 --> 0:30:14.520
<v Speaker 1>but it's definitely come up. Clapped up another one of

0:30:14.560 --> 0:30:18.800
<v Speaker 1>your non pun puns. Yes, I hope. I'm like creating

0:30:19.080 --> 0:30:22.800
<v Speaker 1>a pretty a pretty extensive case for the fact that

0:30:22.840 --> 0:30:25.760
<v Speaker 1>all of my puns are accidental. I don't think like

0:30:25.840 --> 0:30:30.200
<v Speaker 1>that accidental puns a good banding too. Ironically, it's okay.

0:30:30.400 --> 0:30:33.760
<v Speaker 1>Uh So plate tectonics is another theory. Basically, you know,

0:30:33.920 --> 0:30:37.640
<v Speaker 1>everyone knows when you get to a higher altitude, it's

0:30:37.640 --> 0:30:39.880
<v Speaker 1>going to be colder, and the conditions are more likely

0:30:39.960 --> 0:30:43.080
<v Speaker 1>to for glaciers to form. And so when these these

0:30:43.560 --> 0:30:47.280
<v Speaker 1>plates on the Earth are smashing together, everyone also knows

0:30:47.320 --> 0:30:49.800
<v Speaker 1>from listening to our show, that's how we get these

0:30:49.840 --> 0:30:54.560
<v Speaker 1>lovely mountain ranges and why there are higher altitudes. So

0:30:54.880 --> 0:30:56.680
<v Speaker 1>that's another theory that that had a lot to do

0:30:56.720 --> 0:31:01.200
<v Speaker 1>with it. Yeahs sense. Some scientists lay um the Quaternary

0:31:01.440 --> 0:31:04.320
<v Speaker 1>ice Age, the whole shebang. That's two point five eight

0:31:04.360 --> 0:31:07.720
<v Speaker 1>million year old ice age that we're in in still

0:31:08.240 --> 0:31:11.520
<v Speaker 1>um basically at the feet of the creation of the Himalayas,

0:31:11.520 --> 0:31:16.040
<v Speaker 1>where Asia and India collide, creating the Himalayas, and most

0:31:16.080 --> 0:31:22.280
<v Speaker 1>importantly the Tibetan Plateau and this rising of land changing

0:31:22.680 --> 0:31:27.120
<v Speaker 1>um the way that air moves across this huge portion

0:31:27.200 --> 0:31:31.800
<v Speaker 1>of land Eurasia UM, and that it had an impact

0:31:32.000 --> 0:31:37.000
<v Speaker 1>on climate, which has an impact on historical climate, which

0:31:37.040 --> 0:31:40.640
<v Speaker 1>can change things, make things cold enough so that glaciers

0:31:40.720 --> 0:31:45.240
<v Speaker 1>can form and really get a foothold. Right. More interesting, Chuck,

0:31:45.480 --> 0:31:49.960
<v Speaker 1>is that it's apparently that's they're like, that's probably kind

0:31:50.000 --> 0:31:53.600
<v Speaker 1>of a factor, but there's an even bigger factor that

0:31:53.680 --> 0:31:56.560
<v Speaker 1>they think that came out of that upwelling of of earth.

0:31:57.560 --> 0:32:02.720
<v Speaker 1>Bear with me. So, when earth meets earth and there's

0:32:02.720 --> 0:32:05.440
<v Speaker 1>an upwelling and they form mountains or something like that, right,

0:32:06.440 --> 0:32:09.720
<v Speaker 1>you know, the process of weathering, it's like breaking in

0:32:09.800 --> 0:32:13.600
<v Speaker 1>genes or a strato various, Right, you break in mountains too. Well,

0:32:13.640 --> 0:32:17.320
<v Speaker 1>that's actually a chemical reaction between like the air and

0:32:17.440 --> 0:32:21.840
<v Speaker 1>the earth. And when rock is exposed, it becomes weathered

0:32:21.920 --> 0:32:26.600
<v Speaker 1>because c O two reacts with the rock to basically

0:32:26.680 --> 0:32:32.200
<v Speaker 1>form some sort of um uh equilibrium that's been interrupted

0:32:32.240 --> 0:32:36.840
<v Speaker 1>or disrupted by the exposure of unweathered rock. Right. Well,

0:32:37.040 --> 0:32:40.120
<v Speaker 1>to carry that out, c O two has to be

0:32:40.240 --> 0:32:44.160
<v Speaker 1>drawn from the atmosphere, which means you're basically removing c

0:32:44.360 --> 0:32:46.719
<v Speaker 1>O two from the atmosphere. When you create a new

0:32:46.760 --> 0:32:49.240
<v Speaker 1>mountain mountain chain, and if you're talking about a mountain

0:32:49.320 --> 0:32:52.520
<v Speaker 1>chain as extensive as the Himalayas, a lot of CEO

0:32:52.640 --> 0:32:55.160
<v Speaker 1>two is going to be removed from the atmosphere. When

0:32:55.200 --> 0:32:58.000
<v Speaker 1>you remove c O two from the atmosphere, you reduce

0:32:58.120 --> 0:33:01.160
<v Speaker 1>the greenhouse effect. And when you deduced the greenhouse effect,

0:33:01.480 --> 0:33:04.720
<v Speaker 1>the earth becomes cooler, possibly enough for an ice age.

0:33:04.920 --> 0:33:08.479
<v Speaker 1>The timings right as well. The Himalayans formed right before

0:33:08.560 --> 0:33:11.920
<v Speaker 1>the Quaternary Ice Age began. Ye aren't that amazing? It

0:33:12.080 --> 0:33:19.080
<v Speaker 1>is or science? Uh. The other thing is dust atmospheric changes. Um,

0:33:19.160 --> 0:33:21.000
<v Speaker 1>A lot of dust in the air is gonna keep

0:33:21.120 --> 0:33:25.120
<v Speaker 1>the sun from shining down its warmth onto the Earth

0:33:25.720 --> 0:33:30.840
<v Speaker 1>and keep temperatures cooler. And since I mentioned volcanoes, Um,

0:33:30.880 --> 0:33:33.960
<v Speaker 1>there were a lot of volcanoes, a lot of activity

0:33:34.320 --> 0:33:39.760
<v Speaker 1>that preceded the glacial ages. Um. But you know, launching

0:33:39.760 --> 0:33:40.959
<v Speaker 1>a lot of dust in the air. I don't think

0:33:40.960 --> 0:33:44.840
<v Speaker 1>it's coincidence. It's probably all tied in together. Yeah, I

0:33:45.080 --> 0:33:48.160
<v Speaker 1>would guess that. Um, it's not just volcanic ash. I mean,

0:33:48.200 --> 0:33:51.520
<v Speaker 1>there was just dust period, but the volcanic ash added

0:33:51.560 --> 0:33:56.200
<v Speaker 1>to it, you know, right. And I think even after um,

0:33:56.280 --> 0:34:01.400
<v Speaker 1>after the volcanoes stopped erupting gases that affect the atmosphere directly,

0:34:01.760 --> 0:34:04.600
<v Speaker 1>they still interact with the water vapor in the atmosphere

0:34:04.680 --> 0:34:08.480
<v Speaker 1>to mess with it in a continued way. UM. Sun

0:34:08.560 --> 0:34:12.080
<v Speaker 1>spots are also another one too, right. Yeah, that's one

0:34:12.120 --> 0:34:17.359
<v Speaker 1>of the main reasons for the little ice age, right. Yeah,

0:34:17.480 --> 0:34:20.799
<v Speaker 1>but we talked about in the strata areas, so the

0:34:20.880 --> 0:34:23.560
<v Speaker 1>little ice age. Um, so did you did you see

0:34:23.560 --> 0:34:27.879
<v Speaker 1>that article I sent you? Yeah, it was pretty pretty interesting. Um,

0:34:27.920 --> 0:34:31.200
<v Speaker 1>but there's a our understanding of the little ice age,

0:34:31.200 --> 0:34:33.279
<v Speaker 1>which is not the best name for it, but there's

0:34:33.280 --> 0:34:37.920
<v Speaker 1>a period should be little ice age. There's the from

0:34:38.840 --> 0:34:43.360
<v Speaker 1>d to eighteen fifty. Europe in particular, well the northern hemisphere,

0:34:43.400 --> 0:34:47.160
<v Speaker 1>but Europe got it pretty bad. Um. It was basically

0:34:47.200 --> 0:34:51.200
<v Speaker 1>what amounts to an ice age for for this area. Um,

0:34:51.360 --> 0:34:54.960
<v Speaker 1>Greenland and Iceland were cut off by ice for months

0:34:54.960 --> 0:34:58.520
<v Speaker 1>at a time. They used to grow wine in England,

0:34:58.960 --> 0:35:04.120
<v Speaker 1>not anymore. Scotland they grew wine, Yeah, like bottles would

0:35:04.120 --> 0:35:07.160
<v Speaker 1>just pop up out of the grounds. The Highlands of

0:35:07.160 --> 0:35:10.759
<v Speaker 1>Scotland would be locked into ice at like and up

0:35:11.080 --> 0:35:14.000
<v Speaker 1>the Baltic Sea froze over. Yeah, the canals and the

0:35:14.040 --> 0:35:17.680
<v Speaker 1>Netherlands routinely froze. It was it was a really rough time. Well,

0:35:17.880 --> 0:35:20.920
<v Speaker 1>it wasn't. It wasn't. It's pretty interesting because this article

0:35:20.960 --> 0:35:23.120
<v Speaker 1>you sent, you know, points out a lot of the

0:35:23.200 --> 0:35:27.320
<v Speaker 1>history that you know, it affected everything from shipping to

0:35:27.600 --> 0:35:31.160
<v Speaker 1>crops to you know, people turning on one another in

0:35:31.239 --> 0:35:35.360
<v Speaker 1>some areas then other areas things flourished, right, So apparently

0:35:36.080 --> 0:35:40.200
<v Speaker 1>areas and groups that had access to extensive trade networks,

0:35:40.280 --> 0:35:45.040
<v Speaker 1>especially with the South or the tropics. Um, they they flourished.

0:35:45.239 --> 0:35:47.520
<v Speaker 1>But if you were in like a marginal area, say

0:35:47.600 --> 0:35:51.160
<v Speaker 1>like the Alps, you were toast like you suffered from famine.

0:35:51.200 --> 0:35:54.719
<v Speaker 1>Apparently glaciers were advancing enough that they were just overrunning

0:35:54.719 --> 0:35:59.040
<v Speaker 1>towns and it sounds it sounds absolutely nuts, but actually

0:35:59.080 --> 0:36:03.000
<v Speaker 1>glaciers can move surprisingly fast. Right. There was a glacier

0:36:03.200 --> 0:36:11.600
<v Speaker 1>in Alaska in that was clocked advancing at ten a day. Yeah,

0:36:11.640 --> 0:36:13.839
<v Speaker 1>I mean that's thirty ft a day. That's you can

0:36:13.880 --> 0:36:16.279
<v Speaker 1>watch that happen. Yeah, or the very least you could

0:36:16.280 --> 0:36:20.919
<v Speaker 1>set up your your inner volometer camera and watch it later.

0:36:22.520 --> 0:36:25.439
<v Speaker 1>Or if you're just super patient, Yeah, I bet what's

0:36:25.480 --> 0:36:29.120
<v Speaker 1>his name? Yeah, the scotsman. I bet James Hutton would

0:36:29.120 --> 0:36:32.359
<v Speaker 1>have sat there and until he's yeah, you know, yeah,

0:36:32.640 --> 0:36:37.480
<v Speaker 1>patient man. Uh what else do we cover the sun spots?

0:36:38.120 --> 0:36:40.399
<v Speaker 1>Well not Yeah, I mentioned that that might have been

0:36:40.400 --> 0:36:42.480
<v Speaker 1>why the little ice age happened. And by the way,

0:36:42.520 --> 0:36:45.520
<v Speaker 1>we on the Strata Areas podcast heard from a lot

0:36:45.520 --> 0:36:49.640
<v Speaker 1>of people about this double blind study that um or

0:36:49.760 --> 0:36:53.719
<v Speaker 1>where they had musicians play um the stratas and uh,

0:36:53.800 --> 0:36:58.160
<v Speaker 1>then against modern violins, and um, they preferred I think

0:36:58.360 --> 0:37:01.640
<v Speaker 1>generally preferred the modern violin or so people are like, oh,

0:37:01.680 --> 0:37:04.160
<v Speaker 1>you're just getting the brand name. That's kind of a

0:37:04.160 --> 0:37:08.360
<v Speaker 1>reductive way to say it. Um. And and then afterwards

0:37:08.440 --> 0:37:12.879
<v Speaker 1>to the violinists they serge them cough, they're like, it's folgers. Well,

0:37:12.920 --> 0:37:15.400
<v Speaker 1>the other thing we heard from other people that said,

0:37:16.040 --> 0:37:20.040
<v Speaker 1>these violinists know what they're testing. They're testing clearly testing

0:37:20.040 --> 0:37:23.080
<v Speaker 1>and strata varius against a modern instrument. They don't just say, like,

0:37:23.120 --> 0:37:26.279
<v Speaker 1>put on this blindfold and you're two violins, which one

0:37:26.320 --> 0:37:28.840
<v Speaker 1>smells neater. So we probably should have included that, But

0:37:29.040 --> 0:37:31.319
<v Speaker 1>I don't think that like settles it in any like

0:37:31.360 --> 0:37:35.240
<v Speaker 1>scientific way or any Yeah, I saw in our research

0:37:35.400 --> 0:37:38.320
<v Speaker 1>that that was not necessarily the case. It's on a

0:37:38.400 --> 0:37:41.799
<v Speaker 1>number of different sources that that they can tell a

0:37:41.840 --> 0:37:45.520
<v Speaker 1>difference that it is actually the best violins, and these

0:37:45.520 --> 0:37:48.919
<v Speaker 1>are people that have, you know, opinions. It's not like

0:37:49.320 --> 0:37:52.759
<v Speaker 1>you can't scientifically prove that because every person you pick

0:37:52.760 --> 0:37:54.959
<v Speaker 1>out is going to have a different take on the matter.

0:37:55.280 --> 0:37:58.239
<v Speaker 1>And we weren't poopooing modern instruments because clearly they're only

0:37:58.280 --> 0:38:00.919
<v Speaker 1>a handful of strads out there being played, and there's

0:38:01.800 --> 0:38:06.920
<v Speaker 1>many many orchestras and they're not playing like pawnshop violins,

0:38:07.719 --> 0:38:10.399
<v Speaker 1>you know. Anyway, I just want to mention that, So

0:38:10.480 --> 0:38:14.640
<v Speaker 1>these sun spots, right, there's actually a cycle that was

0:38:14.960 --> 0:38:19.279
<v Speaker 1>recognized by a British astronomer named E. W. Maunder. It's

0:38:19.320 --> 0:38:22.560
<v Speaker 1>pretty British name, and he was living during the Little

0:38:22.600 --> 0:38:27.480
<v Speaker 1>Ice Age UM and he noticed. Yeah, he was like, well,

0:38:27.560 --> 0:38:31.919
<v Speaker 1>like how it's cold you can ice skate on a pond. Um.

0:38:32.040 --> 0:38:36.439
<v Speaker 1>He noticed that the so the Little Ice Age should

0:38:36.440 --> 0:38:40.360
<v Speaker 1>actually be called the little period where it was pretty

0:38:40.400 --> 0:38:44.160
<v Speaker 1>cold and then really really cold and two different points,

0:38:44.880 --> 0:38:48.120
<v Speaker 1>and those points were between twelve ninety and undred and

0:38:48.160 --> 0:38:51.720
<v Speaker 1>then sixty five and seventeen fifteen. It was really cold,

0:38:51.760 --> 0:38:56.200
<v Speaker 1>like kind of ice ages conditions for real UM. And E. W.

0:38:56.360 --> 0:38:59.640
<v Speaker 1>Maunder noticed that, especially the time when he was alive

0:38:59.719 --> 0:39:04.920
<v Speaker 1>during between the sixteen and seventeen fifty period seventeen fifteen period, UM,

0:39:05.080 --> 0:39:09.040
<v Speaker 1>sun spots were not nearly as active. And he was like,

0:39:09.080 --> 0:39:12.279
<v Speaker 1>I wonder if this correlates to little ice ages, and

0:39:12.320 --> 0:39:14.239
<v Speaker 1>it would make sense, even though it makes sense in

0:39:14.239 --> 0:39:17.839
<v Speaker 1>a really weird way, a roundabout way. Actually, Yeah, sun

0:39:17.840 --> 0:39:20.120
<v Speaker 1>spot I guess we should just say what that is.

0:39:20.160 --> 0:39:23.560
<v Speaker 1>It's a dark spot, a cooler spot on the Sun.

0:39:23.680 --> 0:39:26.919
<v Speaker 1>But the key there is it contains magnetic energy. So

0:39:27.520 --> 0:39:29.719
<v Speaker 1>you would think that sun spots are cooler than the

0:39:29.719 --> 0:39:33.480
<v Speaker 1>rest of the Sun. So how would that well wait,

0:39:33.520 --> 0:39:35.680
<v Speaker 1>now I've got it backwards, No, you got it? Yeah? Yeah,

0:39:35.920 --> 0:39:38.319
<v Speaker 1>so how would that keep it warmer on Earth? But

0:39:38.400 --> 0:39:42.640
<v Speaker 1>it's about that magnetic field cutting through cloud cover or

0:39:42.680 --> 0:39:45.520
<v Speaker 1>cutting the cloud cover, right, So less cloud cover means

0:39:45.560 --> 0:39:48.400
<v Speaker 1>that the heat from the Sun isn't trapped, it just

0:39:48.560 --> 0:39:53.320
<v Speaker 1>escapes into space. Counterintuitive, but it makes sense. Yeah, because

0:39:53.360 --> 0:39:57.160
<v Speaker 1>these sun spots are big enough that when it's facing Earth,

0:39:58.560 --> 0:40:01.879
<v Speaker 1>it's putting out less heat energy. So you would think

0:40:01.920 --> 0:40:06.480
<v Speaker 1>it would it would directly cool it. It indirectly cools it. Right. Weird,

0:40:06.719 --> 0:40:13.600
<v Speaker 1>It is weird, but amazing earth science. Uh So, whether

0:40:13.640 --> 0:40:15.680
<v Speaker 1>or not we're headed for another one is a lot

0:40:16.120 --> 0:40:20.000
<v Speaker 1>There's a lot of debate on that because some people say, well,

0:40:20.040 --> 0:40:23.840
<v Speaker 1>there's no strict definition even what an ice age is,

0:40:23.960 --> 0:40:26.680
<v Speaker 1>so who's to say. Other people say, now you know what,

0:40:26.760 --> 0:40:30.880
<v Speaker 1>humans have cause uh such an impact here that there

0:40:30.880 --> 0:40:34.279
<v Speaker 1>probably won't be another ice age. It's extremely possible that

0:40:34.440 --> 0:40:37.640
<v Speaker 1>we have altered the climate enough that we're not going

0:40:37.680 --> 0:40:40.719
<v Speaker 1>to see like we may have ended on our own

0:40:41.080 --> 0:40:44.640
<v Speaker 1>the Quaternary ice age. It may be over now or

0:40:44.719 --> 0:40:47.040
<v Speaker 1>on the way to being over, in which case we

0:40:47.080 --> 0:40:48.719
<v Speaker 1>have a whole other set of problems to deal with,

0:40:48.840 --> 0:40:53.000
<v Speaker 1>but not an ice age, not glaciers. Um. There was

0:40:53.040 --> 0:40:55.440
<v Speaker 1>actually a study that made the rounds, I think this

0:40:55.560 --> 0:40:59.200
<v Speaker 1>year or last year, that really drummed up a lot

0:40:59.239 --> 0:41:03.000
<v Speaker 1>of media engine because these researchers said that they predicted

0:41:03.040 --> 0:41:06.320
<v Speaker 1>a period of very low sun spot activity in thirty

0:41:06.400 --> 0:41:09.000
<v Speaker 1>years because we're due for one technically, right were a

0:41:09.800 --> 0:41:13.799
<v Speaker 1>year point, Yes, yeah, we're due for another glaciation event.

0:41:14.520 --> 0:41:16.760
<v Speaker 1>And these people said, well, there's gonna be sun spots

0:41:16.760 --> 0:41:18.919
<v Speaker 1>in thirty years, and the media took it and said

0:41:19.040 --> 0:41:22.440
<v Speaker 1>there's gonna be another ice age in thirty years. Um,

0:41:22.719 --> 0:41:26.000
<v Speaker 1>And that's not necessarily the case. It's a pretty big

0:41:26.080 --> 0:41:29.600
<v Speaker 1>leap from saying, yes, there's low sun spot activity, so

0:41:29.640 --> 0:41:33.600
<v Speaker 1>we're gonna have an ice age. But if we hadn't

0:41:33.600 --> 0:41:36.799
<v Speaker 1>burned all those fossil fuels, maybe that would be the case.

0:41:36.880 --> 0:41:40.239
<v Speaker 1>Maybe we would start to see glaciation beginning again in

0:41:40.280 --> 0:41:44.000
<v Speaker 1>about thirty years. Again we're probably not going to because

0:41:44.080 --> 0:41:47.319
<v Speaker 1>we've raised the temperature of the planet by it a

0:41:47.320 --> 0:41:52.520
<v Speaker 1>full degree celsius since night UM, so it's possible we

0:41:52.560 --> 0:41:54.720
<v Speaker 1>won't ever see an ice age again, which is sad

0:41:55.040 --> 0:41:58.680
<v Speaker 1>because some people say that it was this last um,

0:41:59.120 --> 0:42:02.480
<v Speaker 1>this ice age, not just the last glaciation event, but

0:42:02.520 --> 0:42:05.920
<v Speaker 1>the Quaternary ice Age as a whole that pushed humans

0:42:05.960 --> 0:42:11.000
<v Speaker 1>to evolve to the wonderful, amazing specimens we are today. UM.

0:42:11.040 --> 0:42:14.480
<v Speaker 1>A lot of advancements happened because of it. Adaptations and

0:42:14.560 --> 0:42:18.200
<v Speaker 1>animals and early humans there were there was movement among

0:42:18.560 --> 0:42:21.000
<v Speaker 1>around Earth because the sea levels were a lot lower,

0:42:21.080 --> 0:42:23.600
<v Speaker 1>so you could make your way around bigger parts of

0:42:23.600 --> 0:42:25.759
<v Speaker 1>the Earth. They weren't cut off like before like they

0:42:25.760 --> 0:42:30.960
<v Speaker 1>are now. UM. Apparently, our brains grew tremendously in size

0:42:31.880 --> 0:42:34.839
<v Speaker 1>during the Quaternary Ice Age at a in a time

0:42:34.880 --> 0:42:38.719
<v Speaker 1>period that correlates with it, and one hypothesis is that

0:42:39.000 --> 0:42:42.759
<v Speaker 1>the cooler temperatures allowed us to dissipate heat more naturally

0:42:43.120 --> 0:42:47.359
<v Speaker 1>and to save our energy or use more energy, which

0:42:47.360 --> 0:42:50.520
<v Speaker 1>would allow our brains to grow. Interesting and then other

0:42:50.520 --> 0:42:53.440
<v Speaker 1>people say, well, you know what, the chro magnets also

0:42:53.719 --> 0:42:56.759
<v Speaker 1>invented the sewing needle during this time because of the

0:42:56.760 --> 0:42:59.920
<v Speaker 1>ice age, so that they could start sewing and close.

0:43:00.120 --> 0:43:02.799
<v Speaker 1>Is the technology that allowed us to truly spread out

0:43:02.840 --> 0:43:05.560
<v Speaker 1>over the earth. Yeah, because you could go live where

0:43:05.560 --> 0:43:07.719
<v Speaker 1>it was cold, because you could make a big park

0:43:07.840 --> 0:43:11.080
<v Speaker 1>out of a musk ox exactly. The muskox would say

0:43:11.120 --> 0:43:15.000
<v Speaker 1>thank you for using me human. I don't know about that,

0:43:15.040 --> 0:43:20.359
<v Speaker 1>But you got anything else? Nope, I think that's it. Man,

0:43:21.040 --> 0:43:24.600
<v Speaker 1>This is good one, Chuck Uh. If you want to

0:43:24.600 --> 0:43:28.440
<v Speaker 1>know more about ice ages, you can type those words

0:43:28.520 --> 0:43:31.239
<v Speaker 1>into the search bar at how stuff works dot com.

0:43:31.280 --> 0:43:34.000
<v Speaker 1>And since I said search parts, time for a listener. Mayo.

0:43:37.360 --> 0:43:40.800
<v Speaker 1>Remember in the animal testing episode when I wondered aloud

0:43:40.800 --> 0:43:43.239
<v Speaker 1>about the names of pork and beef and swine and

0:43:43.760 --> 0:43:46.120
<v Speaker 1>all that stuff. I'm glad you're covering this. Apparently I'm

0:43:46.160 --> 0:43:48.359
<v Speaker 1>the only person on the planet who did not know this.

0:43:48.560 --> 0:43:50.320
<v Speaker 1>I didn't know it either, because we had a bunch

0:43:50.320 --> 0:43:52.919
<v Speaker 1>of people right in Uh. And it's super interesting. So

0:43:53.440 --> 0:43:57.640
<v Speaker 1>I picked one that was a good explanation from a

0:43:57.680 --> 0:44:02.359
<v Speaker 1>gentleman in Bristol, United Kingdom. He said this before ten

0:44:02.480 --> 0:44:05.279
<v Speaker 1>sixty six, in England, most people spoke a form of

0:44:05.280 --> 0:44:08.120
<v Speaker 1>Germanic English Uh, and he says, by the way, I'm

0:44:08.120 --> 0:44:11.920
<v Speaker 1>glossing over several centuries of linguistic history with that. However,

0:44:11.960 --> 0:44:14.600
<v Speaker 1>after the invasion by William the Conqueror and his eventual coronation,

0:44:14.960 --> 0:44:18.239
<v Speaker 1>Norman became the dominant language. UH. Norman is based on

0:44:18.480 --> 0:44:21.040
<v Speaker 1>Northern French dialects, so would have used words such as

0:44:21.120 --> 0:44:25.319
<v Speaker 1>mutton and booth for sheep and cows. These words were

0:44:25.360 --> 0:44:27.080
<v Speaker 1>used by people who would have been able to afford

0:44:27.719 --> 0:44:31.359
<v Speaker 1>to eat such food, namely the gentry. However, peasants who

0:44:31.360 --> 0:44:34.600
<v Speaker 1>would have raised raise the animals still use the Germanic

0:44:34.600 --> 0:44:38.720
<v Speaker 1>words like sheep and cow, and these words stuck. English

0:44:38.840 --> 0:44:42.440
<v Speaker 1>is full of high and low words gentry or peasantry

0:44:42.760 --> 0:44:45.680
<v Speaker 1>for similar meanings, with the high words being French based

0:44:46.040 --> 0:44:50.120
<v Speaker 1>therefore Latin based. Really interesting. Um. Having stopped myself from

0:44:50.160 --> 0:44:52.759
<v Speaker 1>going on, as is the subject I've always been obsessed with,

0:44:52.800 --> 0:44:55.160
<v Speaker 1>and I hope that I have piqued your interest as well.

0:44:55.880 --> 0:44:58.439
<v Speaker 1>Be warned the subject as a rabbit hole, I will

0:44:58.480 --> 0:45:01.520
<v Speaker 1>also add I was gutted to miss your UK tour,

0:45:02.120 --> 0:45:03.920
<v Speaker 1>and I hope you enjoyed it enough to come back

0:45:03.960 --> 0:45:08.960
<v Speaker 1>one day. UM. I also cheekily plug Bristol as an

0:45:09.000 --> 0:45:11.839
<v Speaker 1>amazing place to live and visit. Yeah, congratulations on your

0:45:11.840 --> 0:45:15.239
<v Speaker 1>new sky pier. I don't heard of that. It's like

0:45:15.280 --> 0:45:19.160
<v Speaker 1>a it's like a huge observation UFO that goes up

0:45:19.560 --> 0:45:23.600
<v Speaker 1>on their coast. You can just see for miles and miles. Interesting.

0:45:24.640 --> 0:45:26.360
<v Speaker 1>Much love to you both and thanks for doing what

0:45:26.400 --> 0:45:29.800
<v Speaker 1>you do. Cheers. That is from Matt Gallaford of Bristol.

0:45:30.080 --> 0:45:33.560
<v Speaker 1>Thanks Matt, We'll definitely be back. And thanks to everyone

0:45:33.560 --> 0:45:36.360
<v Speaker 1>who wrote in with that good information. I wish I

0:45:36.400 --> 0:45:40.600
<v Speaker 1>could have read them all. Uh. If you want to

0:45:40.600 --> 0:45:42.400
<v Speaker 1>get in touch of us to let us know something

0:45:42.480 --> 0:45:44.840
<v Speaker 1>we missed, or to tell us how grey we're doing,

0:45:44.960 --> 0:45:48.279
<v Speaker 1>or well yeah, you can tweet to us at s

0:45:48.400 --> 0:45:50.560
<v Speaker 1>Y s K podcast. You can also hang out with

0:45:50.600 --> 0:45:55.399
<v Speaker 1>me at Josh Underscore, um Underscore Clark at on Twitter two.

0:45:55.920 --> 0:45:58.879
<v Speaker 1>You can hang out with Chuck at Charles W. Chuck

0:45:58.920 --> 0:46:01.400
<v Speaker 1>Brian on Facebook or our Stuff you Should Know page

0:46:01.400 --> 0:46:04.120
<v Speaker 1>at Facebook dot com, slash stuff you Should Know. You

0:46:04.120 --> 0:46:06.439
<v Speaker 1>can hang out with us on Instagram. You can send

0:46:06.480 --> 0:46:08.879
<v Speaker 1>us an email to Stuff podcast at how Stuff Works

0:46:08.880 --> 0:46:10.759
<v Speaker 1>dot com and has always joined us at our home

0:46:10.760 --> 0:46:18.120
<v Speaker 1>on the web. Stuff you Should Know dot com For

0:46:18.200 --> 0:46:20.520
<v Speaker 1>more on this and thousands of other topics. Is It

0:46:20.600 --> 0:46:28.960
<v Speaker 1>How stuff Works dot com