3 main geomorphological processes king theory
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The most popular theory of landform development was given by American geomorphologist William Morris Davis. His concept of geographical cycle (or commonly known as cycle of erosion) provided a genetic classification and systematic description of landforms.
According to Davis, geographical cycle is a period of time during which an uplifted landmass undergoes its transformation by the process of land sculpture ending into low featureless plain or peneplain (which Davis called peneplane), Davis’s theory was the outcome of a set of theories and models presented by him during the 1880s and 1890s.
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