Final answer:
The Himalayas, formed by the collision between the Indian and Eurasian Plates, and the Ural Mountains, a result of an ancient orogeny, are both real-life examples of convergent plate boundaries.
Step-by-step explanation:
Real-Life Example of Convergent Plate Boundaries
One real-life example of a convergent plate boundary is the region where the Indian Plate is colliding with the Eurasian Plate. This interaction is responsible for the formation of the Himalayas, which including me of the world's highest peaks, such as Mount Everest. The Himalayas are a result of the intense compressional forces at the convergent boundary where the denser Indian Plate subducts beneath the lighter Eurasian Plate, leading to the uplift of the mountain range.
Moreover, the Ural Mountains in Russia are also a classic example of an ancient convergent boundary between two continental plates. These mountains formed hundreds of millions of years ago during the Ural orogeny and still stand today as a defining topographical feature of the region.