Mountains on Earth are limited in height due to the strength of rocks and the processes that form them, such as volcanism and plate tectonics. As mountains grow taller, their weight can cause them to collapse, and erosion counteracts their growth. The Earth's crust floats on a partially molten layer called the asthenosphere, which can lead to sinking if mountains exceed a certain height. While there is no theoretical limit to mountain height, factors like buoyancy and geological processes impose practical constraints. Continuous tectonic activity, like the movement of the Indian plate, can contribute to mountain growth, but overall, the combination of these factors restricts heights beyond approximately 10 kilometers.