How do shifting tectonic plates influence the formation of mountain ranges worldwide?

Tectonic plates are massive sections of Earth's crust that float on the semi-fluid layer beneath, and their interactions are crucial in shaping the planet's topography. When these plates collide, pull apart, or slide past each other, they cause significant geological activity, including the creation of mountain ranges. For instance, the Himalayas, the world's tallest mountain range, formed as a result of the Indian subcontinent colliding with the Eurasian plate. Similarly, the Andes in South America illustrate the dynamics along a convergent boundary where the oceanic Nazca plate subducts beneath the continental South American plate. Understanding these tectonic interactions not only explains the formation of mountains but also offers insights into the seismic risks and geological history of regions around the globe.