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In geology, rejuvenation refers to the process where a landform, typically in its "old age" stage, is renewed by a new period of uplift. This uplift can interrupt the natural progression of the geomorphic cycle, returning the landform to a more youthful state with steeper slopes and more vigorous erosion. This concept was central to William M. Davis's theory of landform evolution, which proposed that landforms progress through stages of youth, maturity, and old age, eventually being reduced to a peneplain near sea level. Rejuvenation can occur at any point in this cycle, effectively restarting the process. While Davis emphasized time as the primary factor, modern understanding suggests a dynamic equilibrium between landforms and the processes acting upon them.1

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  1. uplift
  2. geomorphic cycle

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