: The extreme aridity of the Atacama Desert has essentially "frozen" these maturelands in time. Because there is so little rainfall to cause further erosion, the ancient rolling hills remain visible today, providing a rare "mosaic" of different geological ages.
: Rivers no longer cut straight down; they begin to meander, creating wide floodplains. matureland
One of the most scientifically significant examples is the . Geologists have used this specific landscape to understand the timing of the uplift of the Andes . : The extreme aridity of the Atacama Desert
To understand a matureland, one must look at the "Geographical Cycle" proposed by Davis, which categorizes landscape evolution into three primary stages: One of the most scientifically significant examples is the
A matureland is distinct from other landforms due to several defining features:
: Eventually, the hills disappear almost entirely, leaving a low-relief plain called a peneplain . Case Study: The Matureland of Northern Chile