Continental Drift Theory – Groundbreaking Theory
Continental Drift theory is also called the Groundbreaking Theory of Moving Continents, as according to this theory the major landmass of earth moved with a very slow rate and with time it broke down into smaller landmass that we see in the present day. Earthquake – Definition, Causes, Effects, Protection
- The major land mass Pangea broke into lauresia and gondwana land and futher boke into the present day continents.
- Due to the drift and movement we observe a lot of similarities in the structure and biological creatures in different continents.
- After observing we can see that there are jig-saw attachment in the shapes of different contents.
- India was previously a part of African continent with time it moved towards Asia and merged with it.
Continental Drift Theory: Definition, Evidence, Limitations
The Continental Drift Theory proposes that Earth’s continents were once part of a single supercontinent called Pangaea, which later fragmented and drifted to their current positions over millions of years. This theory, initially proposed by Alfred Wegener, is supported by evidence such as matching coastlines, geological similarities, and fossil distribution across continents. The concept laid the foundation for the modern understanding of plate tectonics.
In this article, We have discussed the Continental Drift Theory and supporting evidence for the Drift Theory, and limitations of the theory, and many more.
Let’s dive right in.