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Plates moving due to convection in mantle

Plates Moving Due to Convection in Mantle. Created by Sal Khan.

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  • female robot ada style avatar for user Sophie Schallock
    How many plates are in the world today? Were there fewer, more or the same amount of plates when the dinosaurs were around? Will there be more plates in the future in 500 years?
    (8 votes)
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  • purple pi purple style avatar for user nicole valentine
    But after time dose the water start to doile when going thow the sistum or will it just go one time and then stop.
    (6 votes)
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  • male robot donald style avatar for user TheDeathviper90
    what happen to pangea ?
    (2 votes)
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  • leafers seed style avatar for user Cassidy Clark
    I understand what convection is and how the mantle is heated, but where does the mantle receive its heat from? The core?
    (3 votes)
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  • aqualine ultimate style avatar for user Deadpool
    i heard that the atlantic ocean is growing bigger, every year, so does that push the continents farther apart? And also what is causing the continents to move apart
    (3 votes)
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    • piceratops ultimate style avatar for user AegonTargaryen
      Yes, the Atlantic ocean is getting bigger and the pacific ocean is getting smaller due to the continental drift. This is caused by the natural moments of the plates as they glide on the semi-liquid mantle. This mantle often has currents caused by the subducting fluid and this force pushed the plates in many directions.
      (2 votes)
  • blobby green style avatar for user Abhiram Bitla
    When you say the convection current heats up and then say it cools and shifts to the right, do you mean it is shifting the magma to the right, or the new oceanic crust to the right?
    (3 votes)
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  • male robot hal style avatar for user Filipe Ronzani
    the movement of the manto have an unique direction? like counterclockwise or clockwise ?
    (3 votes)
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  • female robot grace style avatar for user yamaha
    why are there spots hotter than others in the mantle?
    (3 votes)
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    • aqualine ultimate style avatar for user brian.li.101
      Heat is unevenly distributed throughout the mantle. You can't pin it to any single specific reason, but some examples include abundance of certain elements, level of radioactive decay, overlying material (oceanic crust vs. continental crust because they have different heat capacities), etc.
      (2 votes)
  • spunky sam blue style avatar for user Paul Kang
    Sal mentions around that the convection currents would be slow, and says earlier that the asthenosphere is part-solid. If this is the case, have scientists estimated the viscosity of such material, and are they able to use that information to predict movements?
    (2 votes)
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    • leaf green style avatar for user Florent Figon
      First thing just to be clear, the asthenosphere is completely solid (except some places where there is magma, but it is a tiny percentage of its volume). The Earth is not a molten ball or something like that, only the outer core is fully liquid (as we know by studying seismic S-waves).

      Then yes, scientists actually have measured the viscosity of the asthenosphere. It is estimated to be 10^(20) Pa.s (= Pascal times second, this is the unit of viscosity). In comparison, water at 20°C is 0.001 Pa.s and olive oil is 1 Pa.s. They have been able to measure it thanks to the so-called "Post-glacial rebound" in Denmark. There was a glacier on Denmark 20,000 years ago. The lithosphere below it lowered in the more fluid asthenosphere because of the glacier's weight. Once the glacier had disappeared, the fluid asthenosphere (which had been moved by the lithosphere) has slowly come back and regularly pushed the lithosphere to the top. So, since 20,000 years, the Danish lake's beaches have slowly risen and we can see it today. Then, by measuring the speed of this rise, we can estimate the viscosity of the asthenosphere.

      Predicting movement is something more complicated (and I do not have much information about it), but the viscosity of the asthenosphere constrains the speed of mantle convection. So we know that convection through the whole asthenosphere (and not only right beneath a glacier) is dynamic, but lasts several million years.
      (3 votes)
  • starky tree style avatar for user imamulhaq
    In the cycle mentioned at can water ever escape the cycle through evaporation or anything else?
    (2 votes)
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Video transcript

What I want to do in this video is talk a little bit about maybe why the plates are actually moving in the first place. And nothing I'm talking about in this video has been definitively proved. This is just kind of the current thinking, the leading thinking, on why plates are actually moving. Although we haven't seen the definitive evidence yet, and it's probably a combination of a bunch of things. Now, before we even talk about plates, let's just talk about convection. And you might already be familiar with the term, but just in case you're not, let's do a little bit of review of convection. So let's say I have a pot over here. So that is my pot. And it contains some water. So I have water in my pot. And let's say I only heat one end of the pot. So I put a flame right over at that end of the pot. So what's going to happen? Well, the water that's right over the flame is going to be warmed up more than any of the other water. So this water is going to get warm. But when it gets warm, it also becomes less dense. When you have a fluid, if you warm it up, the molecules are vibrating more. They have more kinetic energy. They're going to a bounce further distances away from each other. They will become less dense. And if you have something that's less dense, and it's surrounded by things that are more dense, and we're dealing in kind of a fluid state right here, that warm, less dense water is going to move upwards. It's going to move upwards. Well, when it moves upwards something has to replace it. So you're going to have cooler water from this side of the container kind of replacing where that water was. Now, this water, as it rises, what's going to happen to it? Well, it's going to cool down. It's going to get further from the flame. It's going to mix with maybe some of the other water, or transfer some of its kinetic energy to the neighboring water. So it'll cool down. But once it cools down, what's it going to want to do? Remember, in general, the closer you are to the flame. So the water closer to the flame in general is going to be warmer. So all of this stuff is going to be warmer, and all of this stuff up here, like the coldest water, is always going to be furthest from the flame. And so the coldest water is going to be over here. But remember, the coldest water is also the densest water. So this water over here is dense. And so it will sink. It's denser than the water around it. And it also helps replace the water that's going here to get warmed up again. And so what you do is you have this cycle here. Warm water rises, moves over to the right down here, and then goes back down as it cools down, and it's dense, and then it gets warmed up again. And so this process, essentially what it's doing is it's transferring the heat. It's allowing the heat to be transferred from this one spot throughout the fluid. And so we call this process, this is convection. Now, the reason why we think the plates are moving is because we think that there are similar types of convection currents in the asthenosphere, in the mantle, in the more fluid part of the mantle. Remember, most of the mantle you can kind of view it as this mooshy, spongy, not quite liquid, but not quite solid state, kind of plastic. It can kind of moosh past. It can kind of flow like super, super, super thick, like super viscous fluid. So not quite solid, not quite liquid. But the same thing could be happening. You have certain areas in the mantle that are hotter than others, and this particular in the asthenosphere. And those areas, that's where you're going to have the material in the mantle move up, because it's hotter, it's less dense, and it will move up. And maybe it'll cause one of these divergent rifts where kind of plate material and crustal material is forming. And then as it moves up, it cools down, and eventually sinks, only to get heated up again. So it has this kind of circular motion just like we saw with the boiling water. And so that process, remember this isn't completely liquid. It is rocky. So it's going to potentially be able to take other things with it. It could maybe drag the crust along with it. Or I should say it could drag the lithosphere along with it, not just the crust. It could drag all this rigid rock up here along with it, causing it to move in that general direction. So you have the drag there. You could also imagine this kind of a suction effect, where, if you view it as a fluid, you have a bunch of fluid coming down here. So it would kind of pull the lithosphere down at those points, and it would kind of push the lithosphere up at those points. So you have these convection currents that are essentially driving it. These aren't going to be super fast moving fluid convection currents, like you would expect with boiling water or with heated water. These would be slow moving convection currents, but they're moving enough, and they're able to kind of put enough drag on the lithosphere to take the lithosphere along with it. And so that's kind of at a high level the dominant theory as to why they're moving. There's other ones that talk about maybe these lithospheric plates, they kind of thicken as they move further away from this area where the ridge is forming. And if we look at this oceanic crust right over here. And so over time, they're denser over here, because there's more cooled down material at these points. And it's already a little bit lower because this is where a lot of the land is being created. And so there's maybe some gravitational effects. But the dominant effect, we think, is due to this convection in the upper mantle.