Natural Hazards and Disasters – Chapter 7 Geography NCERT class 11

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Key notes, lectures and summary of Class 11 NCERT Chapter 7 – Natural Hazards and Disasters. In this chapter we will understand:

1. Whats causes Natural Hazards and Disasters?
2. What are the consequences of it?
3. Classification of Natural Disasters.
4. Natural Hazards and Disasters in India.
5. Some locations on maps for better understanding.

This video is an elearning instructional design which is a web based e learning technique through which concepts become easier to understand. Its a revolutionary move, as the internet is flooding with many online learning classes, online education degrees, online education programs only to boost learning capability. Subscribe to my channel for more, as i will be developing elearning courses only to make you understand concepts in a crisp and clear manner.

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— You can also view playlists of other NCERT Geography videos:-
Class 6 – https://www.youtube.com/watch?v=gAZP9…
Class 7 – https://www.youtube.com/watch?v=Whz0l…
Class 8 – https://www.youtube.com/watch?v=PIrwd…
Class 9 – https://www.youtube.com/watch?v=VuDbi…
Class 10 – https://www.youtube.com/watch?v=hTT_d…
Class 11 – https://www.youtube.com/watch?v=Nntks…

Class 11th Geography is important from examination stand point. It covers all the nuances and basic concepts of India’s Geographical and Physical Environment. Competitive exams like UPSC Civil Services Exam, National Defence Academy NDA, Combined Defence Services CDS, Bank (PO, Clerk, Specialist), RBI (PO, Clerk, Specialist), Combined Graduate Level CGL, Central Armed Police Force CAPF (Assistant Commandant), Intelligence Bureau IB and many more exams have put major emphasis on Class 11th Geography. Questions appear in thoughtful, opinionated and factual manner. You can easily score, if you watch these videos without having to read the entire book full of textual data.

Happy new year, I really hope your academic and career pursuits take a massive boost this year. Peace!

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27 Comments

  1. The movement of plates at the Earth's surface is driven by the convection of material in the mantle, which is the layer of the Earth between the crust and the core. Convection occurs when heat is transferred from one place to another by the movement of a fluid, in this case, the semi-solid mantle rock.

    The mantle is heated by the core at the bottom, and this heat causes the mantle rock to become less dense and rise towards the Earth's surface. As the mantle rock rises, it cools and becomes more dense, causing it to sink back down into the mantle. This cycle of rising and sinking creates a continuous flow of material in the mantle, which drives the convection of the mantle.

    The movement of the mantle causes the plates at the Earth's surface to move as well. The plates are rigid and float on top of the mantle, so as the mantle moves, it carries the plates with it. The movement of the plates is influenced by several factors, including the shape and size of the plates, the presence of ridges and trenches, and the forces generated by the mantle convection.

    In the case of plate tectonics and the theory of seafloor spreading, the mantle convection drives the movement of the oceanic plates away from the mid-ocean ridges, causing the ocean floor to expand and the ocean basins to grow. This process has been ongoing for millions of years, and it is one of the key mechanisms by which the Earth's crust has changed and evolved over time

  2. Seafloor spreading is a key concept in the theory of plate tectonics, which explains how the Earth's crust is composed of large plates that move and interact with each other. The theory of seafloor spreading states that new oceanic crust is formed at mid-ocean ridges and is then moved away from the ridge in opposite directions.

    Here's how the process of seafloor spreading works in detail:

    Formation of magma: Magma rises to the Earth's surface at mid-ocean ridges, which are long, underwater mountain ranges that run along the ocean floor. The magma cools and solidifies to form new oceanic crust.

    Movement of plates: As the new oceanic crust is formed at the mid-ocean ridge, the existing crust on either side of the ridge is pulled away from the ridge and moves in opposite directions. This movement of the plates is driven by the convection of material in the mantle beneath the Earth's crust.

    Expansion of the ocean floor: As the plates move away from the mid-ocean ridge, the ocean floor expands, causing the ocean basin to grow. This process of ocean floor expansion has been going on for millions of years, and has resulted in the ocean basins that we see today.

    Evidence for seafloor spreading: The theory of seafloor spreading has been supported by a variety of geological and geophysical evidence, including the presence of magnetic stripes on the ocean floor, the shape and structure of mid-ocean ridges, and the ages of oceanic crust as determined from radiometric dating.

    In summary, the theory of seafloor spreading explains how new oceanic crust is formed at mid-ocean ridges and is then moved away from the ridge in opposite directions, causing the ocean floor to expand. This process is a key part of the plate tectonic theory, which explains how the Earth's crust is composed of large plates that move and interact with each other.

  3. Bro ended this chapter in 17min my teacher took 5days to complete this chapter without knowing that nobody is understanding him >:( Thanks sir lot of love 💕❤️ may god fulfill your desire or wishes

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