Which mountain range is an example of converging plate boundaries?

The Himalayas Mountain Range is an exemplary formation resulting from converging plate boundaries. This mountain range was formed when the Indian tectonic plate collided with the Eurasian tectonic plate. This collision began approximately 50 million years ago and is still continuing today, causing the Himalayas to rise even higher.

Converging plate boundaries occur when two tectonic plates move towards each other, leading to geological phenomena such as mountain building, volcanic activity, or earthquakes. In the case of the Himalayas, the immense pressure from the collision of the two plates has molded the landscape, giving rise to some of the tallest peaks in the world.

In addition to the Himalayas, other mountain ranges have different origins. The Appalachian Mountains, for example, are much older and were formed primarily through the compression of the Earth's crust when continental plates collided, but they are not currently active like the Himalayas. The Ural Mountains and the Rocky Mountains also have distinct histories and were formed through different geological processes, such as continental collision at different plate boundaries or volcanic activity.