Here's why:

* India and Eurasia Collision: The Himalayan Mountains are indeed formed due to the collision of the Indian tectonic plate with the Eurasian tectonic plate. This collision began in the Eocene epoch, roughly 56 million years ago.

* Ongoing Collision: This collision is still happening today. The Indian plate is still moving northward and colliding with the Eurasian plate. This continuous movement is what drives the uplift and growth of the Himalayas.

Important Notes:

* Rate of Collision: The rate of collision is relatively slow, about 5 cm per year, but it has been going on for a very long time.

* Ongoing Uplift: This ongoing collision means the Himalayas are still growing taller.

* Future of the Himalayas: The Himalayas are expected to continue growing for millions of years to come.

So, while the statement accurately describes the formation and ongoing nature of the Himalayan Mountains, it's important to understand the details of this process and its implications for the future.