Which type of plate movement can lead to the formation of mountains?

The formation of mountains is predominantly associated with convergent movement. This type of plate boundary occurs when two tectonic plates collide or move towards each other. The immense pressure generated from this collision forces the Earth's crust to buckle and fold, leading to the uplift of land and the creation of mountain ranges.

An example of this process can be observed in the Himalayas, where the Indo-Australian plate is colliding with the Eurasian plate. The continuous compression results in the rise of one of the world’s highest mountain ranges.

Unlike convergent movement, divergent movement involves tectonic plates pulling apart from each other, which typically leads to the creation of new oceanic crust and features such as mid-ocean ridges rather than mountains. Transform movement involves plates sliding past each other and does not create significant vertical features like mountains. Rotational movement is not a recognized mode of plate tectonics in this context and is not generally associated with the formation of geological structures like mountains.