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A peneplain is defined as a more or less level land surface produced by erosion over a long period, undisturbed by crustal movement. They are formed as a result of extensive fluvial erosion following extended relative tectonic stability.

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Flat areas on continents that are eraded?

Flat areas on continents that have been eroded are known as peneplains. These are vast regions of low relief that form due to extensive erosion over millions of years. Peneplains often develop in regions with relatively uniform geological characteristics and are commonly found in old mountain ranges or shield areas.


Are low rolling hills and example of a peneplain?

Yes, low rolling hills can be considered an example of a peneplain, which is a landform that has been eroded to a nearly flat surface but still retains some subtle topographic features. Peneplains are typically the result of prolonged erosion and weathering, leading to a landscape that is relatively smooth and gentle in relief. While peneplains are often associated with extensive geological timeframes, low rolling hills can represent the remnants of such processes.


What has the author Harald Svensson written?

Harald Svensson has written: 'Method for exact characterizing of denudation surfaces, especially peneplains, as to the position in space' -- subject(s): Peneplains, Plains 'Distribution and chronology of relict polygon patterns of the Laholm Plain, the Swedish West Coast' -- subject(s): Ice-wedge polygons 'The use of stress situations in vegetation for detecting ground conditions on aerial photographs' 'Distribution and chronology of relict polygon patterns on the Laholm plain, the Swedish West coast' -- subject(s): Ice-wedge polygons, Patterned ground 'Glaciation och morfologi' -- subject(s): Glacial epoch, Glaciers, Physical geography


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