Isostatic equilibrium

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  • เผยแพร่เมื่อ 24 ก.ย. 2024
  • An explanation of why the Earth has high-elevation continents versus low-elevation ocean basins

ความคิดเห็น • 26

  • @gouraviyerankollu525
    @gouraviyerankollu525 3 ปีที่แล้ว +4

    I am watching this video in 2020.after 4 years too. This video seems so new. Very informative and practically understandable. Thank you and thanks to granite too..(lol)....Your passion and energy for earth science can be seen in every video of yours by which I am so inspired .-love.

  • @scarletybegonias3
    @scarletybegonias3 4 ปีที่แล้ว

    We give a presentation to Montessori elementary children that is similar to this, though simplified, and this helped me understand. I liked the element of gratitude. Thank you!

  • @MRBMN-zp4cd
    @MRBMN-zp4cd 3 ปีที่แล้ว

    the way he explains everything so well is impressive

  • @gg8840
    @gg8840 ปีที่แล้ว

    Beautifully explained.

  • @bharatpanwar6257
    @bharatpanwar6257 3 ปีที่แล้ว +1

    soo informative i am all over with my doubts!!!thx u would definitely be the best teacher

  • @MikeHawkNetwork
    @MikeHawkNetwork 7 ปีที่แล้ว +2

    I have a theory.
    What if the reason for denser oceanic crust is due to compression from the wait of water, and the reason that continental crust is less dense is because it is not being compressed by such pressure (water).
    We already know that Earth's internal volume is not uniform, nor is it's surface a perfect sphere.
    When water formed, is it possible that it condensed in specific pockets of the Earth (what we know as ocean basins), thus compressing these regions?
    As for the continental regions, consider their low density formation a result of "convection", so to speak.
    If a load (pressure) is applied to any object, there will be a tendency for that object to deform in the direction of such load.
    But with out a load, the object in question will stay at rest, that is of course if that object was already at rest to begin with, which it was not (kinetic energy).
    I am NOT a geologist, I am an engineering student at UTA and this is my first geology course.
    That being said, don't rip me a new one for this, what may be a misguided theory, as I intended this to be a sort of thought provoking statement.
    Good video.

    • @majidshaib461
      @majidshaib461 5 ปีที่แล้ว +1

      Which theory you have?

  • @Chandra-e1k
    @Chandra-e1k ปีที่แล้ว

    you are so good in explaining it with ease & clarity Sir

  • @stinkybhole
    @stinkybhole ปีที่แล้ว

    wow you explain it better than my college professor. crazy

  • @gundichapradhan1469
    @gundichapradhan1469 5 ปีที่แล้ว

    It is an interesting article to know the scientific reasoning .

  • @altayebofficial
    @altayebofficial 3 ปีที่แล้ว

    Amazing explanation, sir. Thanks a lot!

  • @sara-jy7hx
    @sara-jy7hx 3 ปีที่แล้ว +1

    Gorgeous🔥

  • @learningvideos6689
    @learningvideos6689 3 ปีที่แล้ว

    Well explained dear

  • @Грусть-ц2к
    @Грусть-ц2к ปีที่แล้ว

    спасибо за перевод

  • @cath198
    @cath198 4 ปีที่แล้ว

    The oceanic crust is 5 km (3 mi) continental crust is typically 30 km (20 mi)

  • @monojitsaha3071
    @monojitsaha3071 6 ปีที่แล้ว

    Amazing! Want more videos

  • @pradipdarbar9799
    @pradipdarbar9799 ปีที่แล้ว

    It's amazing but I don't get info. What actually I was comes to find

  •  4 ปีที่แล้ว +1

    I shall start thanking granite regularly for swimming on the mantle.I already thank water for ice swimming on it.

  • @ephraimdikel7663
    @ephraimdikel7663 5 ปีที่แล้ว

    Thank you 🙏🏻

  • @nununu05
    @nununu05 3 ปีที่แล้ว

    Nice vid my guy

  • @mahmoudmaher00
    @mahmoudmaher00 4 ปีที่แล้ว

    you're amazing!

  • @10act37
    @10act37 5 ปีที่แล้ว

    Granite rocks!!

  • @richardguy279
    @richardguy279 6 ปีที่แล้ว

    Post Glacial Rebound is a lot of bunkum from day one Get real

  • @alexanderduee
    @alexanderduee 6 ปีที่แล้ว

    handsome

  • @zulakingyt1230
    @zulakingyt1230 10 หลายเดือนก่อน

    cachame