- Peneplain
A peneplain is the final stage in
fluvial or streamerosion .After the streams in an area have reached "
base level ", lateral erosion is dominant - as the streams erode the highland areas between them. Finally, the upland is almost gone: the streamfloodplain s merge in an area of very low to no topographic relief. The resulting flat plain is the ultimate stage in the "cycle of erosion " or "geographical cycle".The streams within a peneplained region show extensive
meander ing and braiding. If the area is subsequently uplifted due to adjacent orogenic processes, without internal deformation within the peneplain, the streams will again begin downward erosion - creating incisedmeander s,water gap s, and other unique geomorphic features.A peneplain can be mistaken for a depositional plain. However, the rocks beneath a peneplain have been folded and tilted by tectonic forces, while the rocks beneath a depositional plain lie in horizontal layers.
The peneplain concept was developed early in the 1900s by the geomorphologists,
William Morris Davis andWalther Penck .
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