Convergent plate tectonics creates mountain ranges with foliated metamorphic rocks?

Convergent plate tectonics occurs when tectonic plates collide, leading to intense pressure and heat that transform existing rocks into metamorphic rocks. This process often results in the formation of mountain ranges, such as the Himalayas, where the collision of the Indian and Eurasian plates has produced significant uplift. Foliated metamorphic rocks, characterized by their parallel layers or bands, form under the directional pressure associated with these tectonic forces, allowing minerals to realign and create distinct textures. Thus, mountain-building through convergent tectonics is closely linked to the formation of foliated metamorphic rocks.