The plate boundary between the Eurasian Plate and the Indian Plate is primarily a convergent boundary. This is where the two tectonic plates are moving toward each other.
At this boundary, the Indian Plate is pushing northward into the Eurasian Plate. This collision is responsible for the formation of the Himalayas, one of the highest mountain ranges in the world. As the Indian Plate subducts beneath the Eurasian Plate, it leads to significant geological activity, including earthquakes and volcanic activity.
The intense pressure and friction at this boundary cause the rocks in the Earth’s crust to deform, resulting in the rising of mountain ranges and the creation of deep valleys. Understanding this boundary helps geologists comprehend the dynamic nature of the Earth’s surface and the processes that shape our planet.