FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2150076109> ?p ?o ?g. }

• W2150076109 endingPage "1166" @default.
• W2150076109 startingPage "1153" @default.
• W2150076109 abstract "ABSTRACT Landscape evolution and surface morphology in mountainous settings are a function of the relative importance between sediment transport processes acting on hillslopes and in channels, modulated by climate variables. The Niesen nappe in the Swiss Penninic Prealps presents a unique setting in which opposite facing flanks host basins underlain by identical lithologies, but contrasting litho‐tectonic architectures where lithologies either dip parallel to the topographic slope or in the opposite direction (i.e. dip slope and non‐dip slope). The north‐western facing Diemtigen flank represents such a dip slope situation and is characterized by a gentle topography, low hillslope gradients, poorly dissected channels, and it hosts large landslides. In contrast, the south‐eastern facing Frutigen side can be described as non‐dip slope flank with deeply incised bedrock channels, high mean hillslope gradients and high relief topography. Results from morphometric analysis reveal that noticeable differences in morphometric parameters can be related to the contrasts in the relative importance of the internal hillslope‐channel system between both valley flanks. While the contrasting dip‐orientations of the underlying flysch bedrock has promoted hillslope and channelized processes to contrasting extents and particularly the occurrence of large landslides on the dip slope flank, the flank averaged beryllium‐10 ( 10 Be)‐derived denudation rates are very similar and range between 0.20 and 0.26 mm yr −1 . In addition, our denudation rates offer no direct relationship to basin's slope, area, steepness or concavity index, but reveal a positive correlation to mean basin elevation that we interpret as having been controlled by climatically driven factors such as frost‐induced processes and orographic precipitation. Our findings illustrate that while the landscape properties in this part of the northern Alpine border can mainly be related to the tectonic architecture of the underlying bedrock, the denudation rates have a strong orographic control through elevation dependent mean annual temperature and precipitation. Copyright © 2013 John Wiley & Sons, Ltd." @default.
• W2150076109 created "2016-06-24" @default.
• W2150076109 creator A5006175692 @default.
• W2150076109 creator A5015132884 @default.
• W2150076109 creator A5038729621 @default.
• W2150076109 creator A5064576442 @default.
• W2150076109 creator A5084656266 @default.
• W2150076109 date "2013-12-18" @default.
• W2150076109 modified "2023-10-16" @default.
• W2150076109 title "The influence of bedrock orientation on the landscape evolution, surface morphology and denudation (¹⁰Be) at the Niesen, Switzerland" @default.
• W2150076109 cites W1502832271 @default.
• W2150076109 cites W1526822975 @default.
• W2150076109 cites W1567384947 @default.
• W2150076109 cites W1576404872 @default.
• W2150076109 cites W1913649990 @default.
• W2150076109 cites W1964010981 @default.
• W2150076109 cites W1964834558 @default.
• W2150076109 cites W1968920596 @default.
• W2150076109 cites W1969970441 @default.
• W2150076109 cites W1972793009 @default.
• W2150076109 cites W1977900147 @default.
• W2150076109 cites W1990613401 @default.
• W2150076109 cites W1999043798 @default.
• W2150076109 cites W1999704161 @default.
• W2150076109 cites W2002473398 @default.
• W2150076109 cites W2005035365 @default.
• W2150076109 cites W2006133689 @default.
• W2150076109 cites W2006659777 @default.
• W2150076109 cites W2009425598 @default.
• W2150076109 cites W2021373812 @default.
• W2150076109 cites W2025383682 @default.
• W2150076109 cites W2027718670 @default.
• W2150076109 cites W2027909499 @default.
• W2150076109 cites W2029488558 @default.
• W2150076109 cites W2032744251 @default.
• W2150076109 cites W2034686087 @default.
• W2150076109 cites W2037971711 @default.
• W2150076109 cites W2038265449 @default.
• W2150076109 cites W2038340088 @default.
• W2150076109 cites W2044136956 @default.
• W2150076109 cites W2046655889 @default.
• W2150076109 cites W2047338649 @default.
• W2150076109 cites W2048535129 @default.
• W2150076109 cites W2050639907 @default.
• W2150076109 cites W2051271933 @default.
• W2150076109 cites W2054321110 @default.
• W2150076109 cites W2062691332 @default.
• W2150076109 cites W2063155650 @default.
• W2150076109 cites W2072789416 @default.
• W2150076109 cites W2074297072 @default.
• W2150076109 cites W2082334370 @default.
• W2150076109 cites W2088030399 @default.
• W2150076109 cites W2090004785 @default.
• W2150076109 cites W2090279538 @default.
• W2150076109 cites W2092850099 @default.
• W2150076109 cites W2093905602 @default.
• W2150076109 cites W2104555680 @default.
• W2150076109 cites W2107656651 @default.
• W2150076109 cites W2112815562 @default.
• W2150076109 cites W2113828320 @default.
• W2150076109 cites W2116123160 @default.
• W2150076109 cites W2131052540 @default.
• W2150076109 cites W2131642202 @default.
• W2150076109 cites W2135955237 @default.
• W2150076109 cites W2144168304 @default.
• W2150076109 cites W2144501045 @default.
• W2150076109 cites W2156202476 @default.
• W2150076109 cites W2160329343 @default.
• W2150076109 cites W2169620131 @default.
• W2150076109 cites W2225905194 @default.
• W2150076109 cites W2329120260 @default.
• W2150076109 cites W2399900627 @default.
• W2150076109 cites W561505314 @default.
• W2150076109 doi "https://doi.org/10.1002/esp.3511" @default.
• W2150076109 hasPublicationYear "2013" @default.
• W2150076109 type Work @default.
• W2150076109 sameAs 2150076109 @default.
• W2150076109 citedByCount "21" @default.
• W2150076109 countsByYear W21500761092015 @default.
• W2150076109 countsByYear W21500761092016 @default.
• W2150076109 countsByYear W21500761092017 @default.
• W2150076109 countsByYear W21500761092018 @default.
• W2150076109 countsByYear W21500761092019 @default.
• W2150076109 countsByYear W21500761092020 @default.
• W2150076109 countsByYear W21500761092021 @default.
• W2150076109 countsByYear W21500761092022 @default.
• W2150076109 crossrefType "journal-article" @default.
• W2150076109 hasAuthorship W2150076109A5006175692 @default.
• W2150076109 hasAuthorship W2150076109A5015132884 @default.
• W2150076109 hasAuthorship W2150076109A5038729621 @default.
• W2150076109 hasAuthorship W2150076109A5064576442 @default.
• W2150076109 hasAuthorship W2150076109A5084656266 @default.
• W2150076109 hasBestOaLocation W21500761092 @default.
• W2150076109 hasConcept C109007969 @default.
• W2150076109 hasConcept C114793014 @default.
• W2150076109 hasConcept C122792734 @default.
• W2150076109 hasConcept C127313418 @default.
• W2150076109 hasConcept C137527640 @default.

• next