FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2097616268> ?p ?o ?g. }

• W2097616268 endingPage "205" @default.
• W2097616268 startingPage "189" @default.
• W2097616268 abstract "Despite the importance of landsliding in routing sediment through mountainous drainage basins, few studies have documented landsliding rates over extended time and space scales. We have investigated landsliding in surficial material in the Queen Charlotte Islands using a large inventory of events, derived from aerial photography, covering an area of 166.7 km 2 . The mean erosion rate for shallow landsliding is 0.10 mm·a –1 , which is at the upper end of shallow landsliding rates observed in the Pacific Northwest and coastal British Columbia, but several orders of magnitude lower than rock-based landsliding rates reported in the literature. Probability distributions for landslide area and volume are somewhat convex in form. Flattening of the curve found at low magnitudes may be due to sampling bias or physical mechanisms inhibiting failure, and the steepening for high values may exist because the sampling period is not long enough to adequately represent large events. Landslides generally initiate on hillslope gradients greater than 0.50–0.60. The largest numbers of landslides occur on south- to southwest-facing slopes and east- to northeast-facing slopes. Most events occur on concave and straight hillslopes in upper-slope positions. Landsliding rates were found not to be affected by rock type. Hillslopes in the Queen Charlotte Islands are often mantled by weathered Quaternary deposits and, hence, landsliding events are not directly controlled by weathering of bedrock. About 31% of landslides identified in this study deposited material in stream reaches, with about 83% of these landslides deposited in reaches with gradients between 3% and 10%." @default.
• W2097616268 created "2016-06-24" @default.
• W2097616268 creator A5027688472 @default.
• W2097616268 creator A5058182500 @default.
• W2097616268 creator A5081841238 @default.
• W2097616268 creator A5087037554 @default.
• W2097616268 date "2002-02-01" @default.
• W2097616268 modified "2023-10-05" @default.
• W2097616268 title "Sediment transfer by shallow landsliding in the Queen Charlotte Islands, British Columbia" @default.
• W2097616268 cites W1480646436 @default.
• W2097616268 cites W2004260341 @default.
• W2097616268 cites W2004841941 @default.
• W2097616268 cites W2025099067 @default.
• W2097616268 cites W2041004134 @default.
• W2097616268 cites W2046940001 @default.
• W2097616268 cites W2050114269 @default.
• W2097616268 cites W2073154176 @default.
• W2097616268 cites W2078441470 @default.
• W2097616268 cites W2080371153 @default.
• W2097616268 cites W2096717450 @default.
• W2097616268 cites W2129067208 @default.
• W2097616268 cites W2131755739 @default.
• W2097616268 cites W2159027331 @default.
• W2097616268 cites W2316411706 @default.
• W2097616268 cites W4237067774 @default.
• W2097616268 cites W4247267616 @default.
• W2097616268 cites W4376848342 @default.
• W2097616268 doi "https://doi.org/10.1139/e01-068" @default.
• W2097616268 hasPublicationYear "2002" @default.
• W2097616268 type Work @default.
• W2097616268 sameAs 2097616268 @default.
• W2097616268 citedByCount "124" @default.
• W2097616268 countsByYear W20976162682012 @default.
• W2097616268 countsByYear W20976162682013 @default.
• W2097616268 countsByYear W20976162682014 @default.
• W2097616268 countsByYear W20976162682016 @default.
• W2097616268 countsByYear W20976162682017 @default.
• W2097616268 countsByYear W20976162682018 @default.
• W2097616268 countsByYear W20976162682019 @default.
• W2097616268 countsByYear W20976162682020 @default.
• W2097616268 countsByYear W20976162682021 @default.
• W2097616268 countsByYear W20976162682022 @default.
• W2097616268 countsByYear W20976162682023 @default.
• W2097616268 crossrefType "journal-article" @default.
• W2097616268 hasAuthorship W2097616268A5027688472 @default.
• W2097616268 hasAuthorship W2097616268A5058182500 @default.
• W2097616268 hasAuthorship W2097616268A5081841238 @default.
• W2097616268 hasAuthorship W2097616268A5087037554 @default.
• W2097616268 hasConcept C111368507 @default.
• W2097616268 hasConcept C113541313 @default.
• W2097616268 hasConcept C114793014 @default.
• W2097616268 hasConcept C123157820 @default.
• W2097616268 hasConcept C127313418 @default.
• W2097616268 hasConcept C137527640 @default.
• W2097616268 hasConcept C186295008 @default.
• W2097616268 hasConcept C187320778 @default.
• W2097616268 hasConcept C2776023875 @default.
• W2097616268 hasConcept C2816523 @default.
• W2097616268 hasConcept C40724407 @default.
• W2097616268 hasConcept C69823785 @default.
• W2097616268 hasConcept C76886044 @default.
• W2097616268 hasConceptScore W2097616268C111368507 @default.
• W2097616268 hasConceptScore W2097616268C113541313 @default.
• W2097616268 hasConceptScore W2097616268C114793014 @default.
• W2097616268 hasConceptScore W2097616268C123157820 @default.
• W2097616268 hasConceptScore W2097616268C127313418 @default.
• W2097616268 hasConceptScore W2097616268C137527640 @default.
• W2097616268 hasConceptScore W2097616268C186295008 @default.
• W2097616268 hasConceptScore W2097616268C187320778 @default.
• W2097616268 hasConceptScore W2097616268C2776023875 @default.
• W2097616268 hasConceptScore W2097616268C2816523 @default.
• W2097616268 hasConceptScore W2097616268C40724407 @default.
• W2097616268 hasConceptScore W2097616268C69823785 @default.
• W2097616268 hasConceptScore W2097616268C76886044 @default.
• W2097616268 hasIssue "2" @default.
• W2097616268 hasLocation W20976162681 @default.
• W2097616268 hasOpenAccess W2097616268 @default.
• W2097616268 hasPrimaryLocation W20976162681 @default.
• W2097616268 hasRelatedWork W1980755777 @default.
• W2097616268 hasRelatedWork W2004301820 @default.
• W2097616268 hasRelatedWork W2004912142 @default.
• W2097616268 hasRelatedWork W2023965594 @default.
• W2097616268 hasRelatedWork W2036520723 @default.
• W2097616268 hasRelatedWork W2264006446 @default.
• W2097616268 hasRelatedWork W2342682623 @default.
• W2097616268 hasRelatedWork W2494306156 @default.
• W2097616268 hasRelatedWork W33518744 @default.
• W2097616268 hasRelatedWork W4211209040 @default.
• W2097616268 hasVolume "39" @default.
• W2097616268 isParatext "false" @default.
• W2097616268 isRetracted "false" @default.
• W2097616268 magId "2097616268" @default.
• W2097616268 workType "article" @default.