Final answer:
The boundary between the Indian and Eurasian Plates is a continent-continent convergent boundary, forming the Himalayas as the plates collide and push upward.
Step-by-step explanation:
The boundary between the Indian and Eurasian Plates that leads to the formation of the Himalayan mountain range is a continent-continent convergent boundary. This type of boundary is characterized by the collision of two continental plates, which pushes up the earth to create mountain chains. The Indian Plate is still pushing northward into the Eurasian Plate, and this tectonic action is responsible for both the rise of the Himalayas and the seismic activity in the region. In fact, the pressure from tectonic action against these plates causes the Himalayas to rise in elevation by as much as one to five millimeters per year.