The Himalayas, a mountain range at the northern edge of the India plate
convergent plate boundaries
At convergent continental tectonic plate boundaries, the most likely feature formed is a mountain range. This occurs due to the collision and compression of two continental plates, leading to the uplift of the Earth's crust. An example of this is the Himalayas, which were formed by the collision of the Indian and Eurasian plates. Additionally, intense geological activity such as earthquakes is common in these regions.
Most of the volcanoes at convergent boundaries are stratovolcanoes.
Convergent boundary
The Pontic Mountains are formed by convergent boundaries, where the Eurasian plate subducts beneath the Anatolian plate. This collision causes uplift and deformation of the Earth's crust, resulting in the formation of mountain ranges like the Pontic Mountains.
The Earth's tallest mountain ranges are formed at convergent plate boundaries.
They were formed by deposition and by convergent boundaries
Mountains are formed at convergent plate boundaries or also known as fault lines.
Mountain ranges are normally formed at convergent plate boundaries.
They were all formed at convergent boundaries
Convergent boundaries are where two tectonic plates hit each other. This can cause earthquakes, but can also create mountains.
They were all formed at convergent boundaries