🌍Continental Drift Theory🌍

The Continental Drift Theory, proposed by Alfred Wegener in 1912, explains that the continents we see today were once joined together in a single supercontinent called Pangaea. Over millions of years, this massive landmass slowly broke apart, and the pieces drifted to their current positions. This theory revolutionized our understanding of Earth’s geology and laid the foundation for the modern theory of plate tectonics.


Evidence for continental drift includes the “jigsaw puzzle fit” of continents like South America and Africa, the discovery of similar fossils across distant continents, matching rock formations, and evidence of past climates such as glacial deposits found in now-tropical areas.


The movement of continents continues even today, reshaping Earth’s surface gradually through earthquakes, volcanic activity, and the formation of mountains. Continental drift not only explains the past but also helps predict the future changes in our planet’s geography. 🌏✨

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