Analyse the sequential development of landforms in either karst or coastal region
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Karst topography - sequential development It is a simple geomorphic cycle as it involves one surface (limestone) and one process (solution). It is fluvial transformation on limestone INITIAL CONDITIONS: - faulted folded limestone surface - surface drainage - water table is the base level Process includes Surface drainage , disappearance of surface drainage , reappearance of subterranean drainage as surface drainage YOUTH
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