: A matureland is marked by well-developed drainage systems and rounded, softened topography. The sharp features of a "young" landscape have been eroded away, but the land has not yet reached the extreme flatness of a peneplain.
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Abundant rainfall promotes thick vegetation and deep chemical weathering, resulting in rounded, soil-covered mature ridges and dense drainage networks.
If left undisturbed by further tectonic movement, a matureland will eventually degrade into a peneplain —a featureless, low-relief plain sitting just slightly above sea level, occasionally punctuated by isolated, erosion-resistant rock hills called monadnocks. Defining Characteristics of a Matureland
How are used to map drainage density
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