FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2022340042> ?p ?o ?g. }

• W2022340042 endingPage "30" @default.
• W2022340042 startingPage "12" @default.
• W2022340042 abstract "Large areas of the Norwegian fjord landscapes are covered by hillslopes that reflect the influence of glacial inheritance from the Last Glacial Maximum (LGM). The focus of this paper is two-fold: (1) analyze the spatio-temporal variability of relevant denudational slope processes and process intensities over the Holocene; and (2) detect Holocene modification of the glacial valley morphometry. Research was performed on hillslope systems within two steep, parabolic-shaped and glacier-fed tributary valleys, Erdalen and Bødalen located on the western side of the Jostedalsbreen ice cap in western Norway. Orthophoto delineation, high resolution mapping (TLS), detailed geomorphological information and spatial data analysis were combined with dating techniques and geophysical investigations. Calculated Holocene rockwall retreat rates at selected slope test sites range from 0.38 to 0.67 mm yr− 1, with a mean value of 0.53 mm yr− 1. Slightly higher values were found in Erdalen, with a mean rockwall retreat rate of 0.57 mm yr− 1 compared to 0.50 mm yr− 1 in Bødalen. Valley-wide Holocene rockwall retreat rates of 0.38–0.50 mm yr− 1 are consistent with other estimates of Holocene rockwall retreat rates in cold mountain environments. It is shown that the glacial inheritance of topography is the most important factor controlling valley development since the LGM and that sediment storage capacity is primarily conditioned by valley morphometry. Compared to contemporary rates, the results indicate enhanced denudation activity and intensity immediately following deglaciation and during the ‘Little Ice Age’. The overall tendency of landscape development is postglacial widening of the parabolic-shaped valley morphometry through rockwall retreat with associated debris accumulation beneath rockwalls. As a result, the glacially sculpted topography has not yet adapted to denudational processes acting under Holocene environmental conditions." @default.
• W2022340042 created "2016-06-24" @default.
• W2022340042 creator A5033568516 @default.
• W2022340042 creator A5034902305 @default.
• W2022340042 date "2013-04-01" @default.
• W2022340042 modified "2023-10-16" @default.
• W2022340042 title "Holocene hillslope development in glacially formed valley systems in Nordfjord, western Norway" @default.
• W2022340042 cites W1964815140 @default.
• W2022340042 cites W1968993853 @default.
• W2022340042 cites W1970575928 @default.
• W2022340042 cites W1973552644 @default.
• W2022340042 cites W1988196896 @default.
• W2022340042 cites W1988336745 @default.
• W2022340042 cites W1990921543 @default.
• W2022340042 cites W2003639363 @default.
• W2022340042 cites W2008659909 @default.
• W2022340042 cites W2015306729 @default.
• W2022340042 cites W2044156036 @default.
• W2022340042 cites W2044802409 @default.
• W2022340042 cites W2046815103 @default.
• W2022340042 cites W2053017959 @default.
• W2022340042 cites W2056481109 @default.
• W2022340042 cites W2062470311 @default.
• W2022340042 cites W2079548035 @default.
• W2022340042 cites W2080042998 @default.
• W2022340042 cites W2081069745 @default.
• W2022340042 cites W2083264254 @default.
• W2022340042 cites W2083293775 @default.
• W2022340042 cites W2083949358 @default.
• W2022340042 cites W2084455550 @default.
• W2022340042 cites W2086607760 @default.
• W2022340042 cites W2089549717 @default.
• W2022340042 cites W2095126466 @default.
• W2022340042 cites W2116321811 @default.
• W2022340042 cites W2126799351 @default.
• W2022340042 cites W2142369945 @default.
• W2022340042 cites W2154388005 @default.
• W2022340042 cites W2158733184 @default.
• W2022340042 cites W2797540839 @default.
• W2022340042 cites W4232783867 @default.
• W2022340042 cites W4235476556 @default.
• W2022340042 cites W4238576860 @default.
• W2022340042 doi "https://doi.org/10.1016/j.geomorph.2012.11.021" @default.
• W2022340042 hasPublicationYear "2013" @default.
• W2022340042 type Work @default.
• W2022340042 sameAs 2022340042 @default.
• W2022340042 citedByCount "19" @default.
• W2022340042 countsByYear W20223400422014 @default.
• W2022340042 countsByYear W20223400422015 @default.
• W2022340042 countsByYear W20223400422016 @default.
• W2022340042 countsByYear W20223400422017 @default.
• W2022340042 countsByYear W20223400422018 @default.
• W2022340042 countsByYear W20223400422019 @default.
• W2022340042 countsByYear W20223400422020 @default.
• W2022340042 countsByYear W20223400422021 @default.
• W2022340042 crossrefType "journal-article" @default.
• W2022340042 hasAuthorship W2022340042A5033568516 @default.
• W2022340042 hasAuthorship W2022340042A5034902305 @default.
• W2022340042 hasConcept C100834320 @default.
• W2022340042 hasConcept C100970517 @default.
• W2022340042 hasConcept C114793014 @default.
• W2022340042 hasConcept C127313418 @default.
• W2022340042 hasConcept C140345934 @default.
• W2022340042 hasConcept C151730666 @default.
• W2022340042 hasConcept C15739521 @default.
• W2022340042 hasConcept C15785411 @default.
• W2022340042 hasConcept C180705331 @default.
• W2022340042 hasConcept C188291805 @default.
• W2022340042 hasConcept C20116678 @default.
• W2022340042 hasConcept C205649164 @default.
• W2022340042 hasConcept C77928131 @default.
• W2022340042 hasConcept C87432785 @default.
• W2022340042 hasConceptScore W2022340042C100834320 @default.
• W2022340042 hasConceptScore W2022340042C100970517 @default.
• W2022340042 hasConceptScore W2022340042C114793014 @default.
• W2022340042 hasConceptScore W2022340042C127313418 @default.
• W2022340042 hasConceptScore W2022340042C140345934 @default.
• W2022340042 hasConceptScore W2022340042C151730666 @default.
• W2022340042 hasConceptScore W2022340042C15739521 @default.
• W2022340042 hasConceptScore W2022340042C15785411 @default.
• W2022340042 hasConceptScore W2022340042C180705331 @default.
• W2022340042 hasConceptScore W2022340042C188291805 @default.
• W2022340042 hasConceptScore W2022340042C20116678 @default.
• W2022340042 hasConceptScore W2022340042C205649164 @default.
• W2022340042 hasConceptScore W2022340042C77928131 @default.
• W2022340042 hasConceptScore W2022340042C87432785 @default.
• W2022340042 hasLocation W20223400421 @default.
• W2022340042 hasOpenAccess W2022340042 @default.
• W2022340042 hasPrimaryLocation W20223400421 @default.
• W2022340042 hasRelatedWork W2052320602 @default.
• W2022340042 hasRelatedWork W2053096958 @default.
• W2022340042 hasRelatedWork W2071818709 @default.
• W2022340042 hasRelatedWork W2114579658 @default.
• W2022340042 hasRelatedWork W2510472800 @default.
• W2022340042 hasRelatedWork W2901133170 @default.
• W2022340042 hasRelatedWork W3147398677 @default.
• W2022340042 hasRelatedWork W4220723266 @default.
• W2022340042 hasRelatedWork W4251501809 @default.

• next