The life cycle of mountains typically involves several stages, including formation, erosion, and eventual decay. Mountains are formed primarily through tectonic processes, such as the collision of tectonic plates, which can create ranges like the Himalayas. Over time, weathering and erosion wear down these peaks, reshaping the landscape and contributing to sediment deposition in valleys and plains. Eventually, as mountains continue to erode, they may become more subdued, transitioning into hills or plateaus in a process that can take millions of years.
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