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Q.What could be the reason for the disintegration of Gondwana? (Journey to the end of the Earth)

CBSECBSE Class XII Board 2025Subjective· 2mImportance★★★★★
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Gondwana disintegrated due to the fundamental geological process of plate tectonics, where convection currents in Earth's mantle caused the supercontinent to rift apart, leading to the formation and slow drift of the modern continents.

Gondwana was a colossal supercontinent that existed hundreds of millions of years ago, comprising what are now South America, Africa, Antarctica, Australia, and India. Its breakup is a classic example of continental drift, a key aspect of plate tectonics. The Earth's outermost layer, the lithosphere, is not a single, solid shell but is broken into several large plates. These plates are in constant, albeit extremely slow, motion, driven by powerful forces originating deep within the Earth. This dynamic nature of our planet's surface is the fundamental reason why Gondwana could not remain intact.

Here is a step-by-step explanation of the process:

  1. The Supercontinent Gondwana: For a significant period, roughly from 500 to 180 million years ago, the landmasses that now form the southern continents were joined together as a single supercontinent called Gondwana. It was situated primarily in the Southern Hemisphere and supported a unique ecosystem, including early forms of life.

  2. The Driving Force: Plate Tectonics: The primary reason for Gondwana's disintegration is the phenomenon of plate tectonics. Deep within the Earth's mantle, intense heat from the core generates slow but powerful convection currents. Hot, less dense material rises towards the surface, spreads laterally beneath the lithospheric plates, and then cools and sinks back down. This continuous circulation creates a dragging force on the overlying tectonic plates, causing them to move, collide, or pull apart.

    The movement of tectonic plates (vv) is typically on the order of a few centimeters per year, driven by mantle convection.

    v≈1 to 10 cm/yearv \approx 1 \text{ to } 10 \text{ cm/year}

  3. Initial Rifting and Separation: Over millions of years, these immense forces caused significant stress within the vast Gondwana supercontinent. Around 180 million years ago, rifting began. This process involves the crust stretching and thinning, eventually leading to the formation of deep valleys and, ultimately, new ocean basins as the landmasses pull apart. The first major splits occurred, separating Africa and South America from the rest of Gondwana. …

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