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Encyclopedia > Peneplain

Canisteo River Valley from Pinnacle State Park 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 NY. In this area, the sharp relief that is seen on some of the Allegheny Plateau has been rounded by glaciation
Canisteo River Valley from Pinnacle State Park 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 NY. In this area, the sharp relief that is seen on some of the Allegheny Plateau has been rounded by glaciation

A peneplain is final stage in fluvial or stream erosion. After the streams in an area have reached base level, lateral erosion is dominant as the streams erode the highland areas between them. Finally, virtually all of the upland is gone and the stream floodplains merge in an area of very low to no topographic relief. Essentially the result is a flat plain which is the ultimate stage in the cycle of erosion or geographical cycle. The streams within a peneplained region show extensive meandering 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 and create incised meanders, water gaps, and other unique geomorphic features. The concept was developed by the early geomorphologists William Morris Davis and Walther Penck in the early 1900s. Image File history File linksMetadata Download high-resolution version (2000x1333, 2122 KB) Summary Canisteo River Valley from Pinnacle State Park, Addison, NY Licensing File history Legend: (cur) = this is the current file, (del) = delete this old version, (rev) = revert to this old version. ... Image File history File linksMetadata Download high-resolution version (2000x1333, 2122 KB) Summary Canisteo River Valley from Pinnacle State Park, Addison, NY Licensing File history Legend: (cur) = this is the current file, (del) = delete this old version, (rev) = revert to this old version. ... Pinnacle State Park and Golf Course is located in Steuben County, New York in the USA. The park is southwest of Corning, New York in the Town of Addison, east of Village of Addison. ... The Allegheny Plateau is a large, dissected plateau area in southern New York, western Pennsylvania, West Virginia, and eastern Ohio. ... Shaded relief map of Cumberland Plateau and Ridge and Valley Appalachians on the Virginia/West Virginia border A dissected plateau is an area that has been uplifted, then severely eroded so that the relief is sharp. ... Austrias longest glacier, the Pasterze, winds its 8 km (5 mile) route at the foot of Austrias highest mountain, the Grossglockner A glacier is a large, long-lasting river of ice that is formed on land and moves in response to gravity. ... The word fluvial is used in geography and earth science to refer to all topics related to flowing water. ... Severe soil erosion in a wheat field near Washington State University, USA. Erosion is the displacement of solids (soil, mud, rock and other particles) by the agents of wind, water or ice, by downward or down-slope movement in response to gravity or by living organisms (in the case of... The base level of a river or stream is the lowest point to which it can flow, often referred to as the mouth of the river. ... It has been suggested that this article or section be merged with Flood plain. ... Surface of the Earth Topography, a term in geography, has come to refer to the lay of the land, or the physiogeographic characteristics of land in terms of elevation, slope, and orientation. ... The complete series of changes or stages through which a landmass passes from the inception of erosion on a newly uplifted or exposed surface through its dissection into mountains and valleys to the final stage when it is worn down to the level of the sea or to some other... To meet Wikipedias quality standards, this article or section may require cleanup. ... A braided river channel consists of a network of small channels separated by small islands called braid bars. ... Orogeny is the process of mountain building, and as such is both a tectonic structural event, a geographical event and a chronological event, in that orogenic events happen within a time frame, affect certain regions of rocks and crust, and cause distinctive structural phenomena and related tectonic activity. ... To meet Wikipedias quality standards, this article or section may require cleanup. ... Water gap is a term geologists use to describe a notch which flowing water has carved into a mountain. ... Surface of the Earth Geomorphology is the study of landforms, including their origin and evolution, and the processes that shape them. ... William Morris Davis (February 12, 1850 - February 5, 1934) was an American geographer, geologist and meteorologist, often called the father of American geography. He was born into a Quaker family in Philadelphia, Pennsylvania, son of Edward M. Davis and Maria Mott Davis (a daughter of the womens advocate Lucretia... Walther Penck (August 30, 1888 - September 29, 1923) Born in Vienna as son of Albrecht Penck. ...


  Results from FactBites:
 
Peneplain - Wikipedia, the free encyclopedia (238 words)
Canisteo River Valley from Pinnacle State Park 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 NY.
A peneplain is final stage in fluvial or stream erosion.
The streams within a peneplained region show extensive meandering and braiding.
Geology of the Appalachians - Biocrawler (5316 words)
The pattern of the folded strata on the low lying Cretaceous peneplain must have resembled the pattern of the curved grain of wood on a planed board.
When the peneplain was uplifted the weaker strata were worn down almost to a lowland of a second generation, while the resistant sandstones, of which there are three chief members, retained a great part of their new-gained altitude in the form of long narrow even-crested ridges with an occasional sharp bending in peculiar zigzags.
Certain districts within the mountains, apparently consisting of less resistant crystalline rocks, have been reduced to basin-like peneplains in the same amount of time that served only to grade the slopes and subdue the summits of the neighboring mountains of more resistant rocks.
  More results at FactBites »

 

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