What is Peneplain and Monadnock: Peneplain/Monadnock
Автор: Geotourism and Modern Geotechniques
Загружено: 2022-02-15
Просмотров: 17674
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A peneplain is a low-relief plain which is formed as a result of stream erosion. It is produced by fluvial erosion that would occur, in the course of geologic time. Peneplains are sometimes associated with the cycle of erosion also.
The term "peneplain" refers to an area that resembles a plain. It is created by river erosion and continues until all of the elevated sections are eroded. When a peneplain is raised, it becomes a Plateau.
A Monadnock is an isolated mountain representing an erosional residual peak or knob.
Monadnock" is formed from the exposure of a harder rock as a result of the erosion of a softer one once surrounding it. Some time Monadnocks also called "Inselberg.
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