What drives the continued India-Asia convergence since the collision at 55 Ma?

Continent-Continent Convergent Plate BoundariesThe Earth's surface is made up of large, moving sections called tectonic plates. Sometimes, two continental plates push toward each other. When this happens, neither plate sinks because both are made of thick, low-density rock. Instead, the edges of the plates crumple and fold, creating high mountain ranges. One of the best examples of this is the Himalayas, where the Indian plate and the Eurasian plate continue to collide. This movement creates...

Wegener and the Continental Drift HypothesisIn the early 1900s, Alfred Wegener, a German scientist, proposed the Continental Drift Hypothesis, the idea that Earth’s continents were once joined together in a supercontinent called Pangaea and slowly drifted apart over millions of years. Although his ideas were not widely accepted then, later discoveries provided evidence supporting continental movement, leading to the modern theory of plate tectonics. Understanding Wegener’s hypothesis helps...

Supercontinent Cycle and PangaeaThe supercontinent cycle is the process where Earth's landmasses come together to form a supercontinent and then break apart over millions of years. This cycle has repeated several times in Earth’s history. The most well-known supercontinent was Pangaea, which existed about 300 million years ago. It included all the land on Earth in one large mass. Over time, Pangaea split apart due to the movement of tectonic plates, creating the continents we see today.

Ocean-Continent Convergent Plate BoundariesThe Earth's surface is made up of large pieces of rock called tectonic plates. These plates are always moving, but very slowly. Sometimes, an oceanic plate and a continental plate move toward each other. This is called an ocean-continent convergent boundary. When this happens, the heavier oceanic plate sinks under the lighter continental plate in a process called subduction. This movement causes earthquakes, volcanoes, and the formation of mountains...

Cenozoic Plate TectonicsThe Earth's surface is always changing. The Cenozoic Era, which began about 66 million years ago and continues today, has been a time of major changes in Earth's land and oceans. Large pieces of Earth's crust, called tectonic plates, have moved to form mountains, shifting continents and opening new ocean basins. These movements have shaped the world as we know it.During the Cenozoic, the continents moved into their current positions. Mountain ranges like the Himalayas...

Mesozoic Plate TectonicsImagine Earth’s land as one giant puzzle piece. A long time ago, during the Mesozoic Era, all the land on Earth was connected to one big supercontinent called Pangaea. Over millions of years, the pieces of this giant puzzle slowly drifted apart, forming the continents we see today. This movement happened because of plate tectonics, the slow shifting of vast sections of Earth’s crust. As these plates moved, they caused earthquakes, created mountains, and even changed...