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Summary Of: Peneplain

the same elevation represent the remnants of a peneplain that was uplifted to form the Allegheny Plateau... the same elevation represent the remnants of a peneplain that was uplifted to form the Allegheny Plateau... the same elevation represent the remnants of a peneplain that was uplifted to form the... A peneplain can be mistaken for a depositional plain... the rocks beneath a peneplain have been folded and tilted by tectonic forces... The peneplain concept was developed early in the 1900s by the geomorphologists...

Encyclodia Page On: Peneplain

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| cite | references or sources | reliable sources | Unverifiable | Canisteo River Valley from Pinnacle State Park, New York. The distant peaks at the same elevation represent the remnants of a peneplain that was uplifted to form the Allegheny Plateau, which is a dissected plateau in southwestern New York. In this area, the sharp relief that is seen on some of the Allegheny Plateau has been rounded by glaciation | | Pinnacle State Park | New York | Allegheny Plateau | dissected plateau | New York | glaciation | fluvial | erosion | base level | floodplains | topographic relief | cycle of erosion | meandering | braiding | orogenic | meanders | water gaps | geomorphic | William Morris Davis | Walther Penck | | topographical term | stub | help | Categories | Topography stubs | Geomorphology | Erosion landforms | Articles lacking sources from December 2007 | All articles lacking sources |
This article is licensed under the GNU Free Documentation License. It uses material from the Wikipedia article "Peneplain".