Matches in SemOpenAlex for { <https://semopenalex.org/work/W2089651025> ?p ?o ?g. }
Showing items 1 to 92 of
92
with 100 items per page.
- W2089651025 endingPage "204" @default.
- W2089651025 startingPage "195" @default.
- W2089651025 abstract "Geological mapping in Assynt, NW Scotland, has identified three areas of large-scale, linear, bedrock grooving. These closely spaced, subparallel, megagrooves occur predominantly on Cambrian quartzite, are not structurally controlled, and trend generally in the direction of palaeo-ice flow. On the basis of geomorphological evidence, most notably erosional relationships and s-forms, it is proposed that the megagrooves formed at the base of the last (Main Late Devensian) ice sheet and are chiefly the result of high-energy subglacial meltwater erosion. The unusual concentration of bedrock-cut Nye channels in Assynt indicates the presence of large volumes of meltwater beneath the last ice sheet in this region of NW Scotland. This high discharge of meltwater was probably accompanied by localized fast ice-sheet flow, akin to present-day ice streams. It is suggested that bedrock megagrooves may be the geomorphological signature of ice-stream onset zones." @default.
- W2089651025 created "2016-06-24" @default.
- W2089651025 creator A5056085650 @default.
- W2089651025 date "2005-02-01" @default.
- W2089651025 modified "2023-09-30" @default.
- W2089651025 title "Bedrock megagrooves in Assynt, NW Scotland" @default.
- W2089651025 cites W130258813 @default.
- W2089651025 cites W1492862160 @default.
- W2089651025 cites W1668160995 @default.
- W2089651025 cites W1969797890 @default.
- W2089651025 cites W1977786326 @default.
- W2089651025 cites W1998855729 @default.
- W2089651025 cites W2014685035 @default.
- W2089651025 cites W2029373128 @default.
- W2089651025 cites W2034964464 @default.
- W2089651025 cites W2045458576 @default.
- W2089651025 cites W2055187238 @default.
- W2089651025 cites W2074832795 @default.
- W2089651025 cites W2095480887 @default.
- W2089651025 cites W2123416608 @default.
- W2089651025 cites W2149061491 @default.
- W2089651025 cites W2320936205 @default.
- W2089651025 cites W4205230436 @default.
- W2089651025 doi "https://doi.org/10.1016/j.geomorph.2004.09.002" @default.
- W2089651025 hasPublicationYear "2005" @default.
- W2089651025 type Work @default.
- W2089651025 sameAs 2089651025 @default.
- W2089651025 citedByCount "40" @default.
- W2089651025 countsByYear W20896510252012 @default.
- W2089651025 countsByYear W20896510252015 @default.
- W2089651025 countsByYear W20896510252016 @default.
- W2089651025 countsByYear W20896510252017 @default.
- W2089651025 countsByYear W20896510252018 @default.
- W2089651025 countsByYear W20896510252019 @default.
- W2089651025 countsByYear W20896510252020 @default.
- W2089651025 countsByYear W20896510252021 @default.
- W2089651025 countsByYear W20896510252023 @default.
- W2089651025 crossrefType "journal-article" @default.
- W2089651025 hasAuthorship W2089651025A5056085650 @default.
- W2089651025 hasConcept C100834320 @default.
- W2089651025 hasConcept C111368507 @default.
- W2089651025 hasConcept C114793014 @default.
- W2089651025 hasConcept C123157820 @default.
- W2089651025 hasConcept C123750103 @default.
- W2089651025 hasConcept C127313418 @default.
- W2089651025 hasConcept C136894858 @default.
- W2089651025 hasConcept C137527640 @default.
- W2089651025 hasConcept C151730666 @default.
- W2089651025 hasConcept C17409809 @default.
- W2089651025 hasConcept C197435368 @default.
- W2089651025 hasConcept C207318512 @default.
- W2089651025 hasConcept C31258907 @default.
- W2089651025 hasConcept C41008148 @default.
- W2089651025 hasConcept C42090638 @default.
- W2089651025 hasConcept C81820708 @default.
- W2089651025 hasConceptScore W2089651025C100834320 @default.
- W2089651025 hasConceptScore W2089651025C111368507 @default.
- W2089651025 hasConceptScore W2089651025C114793014 @default.
- W2089651025 hasConceptScore W2089651025C123157820 @default.
- W2089651025 hasConceptScore W2089651025C123750103 @default.
- W2089651025 hasConceptScore W2089651025C127313418 @default.
- W2089651025 hasConceptScore W2089651025C136894858 @default.
- W2089651025 hasConceptScore W2089651025C137527640 @default.
- W2089651025 hasConceptScore W2089651025C151730666 @default.
- W2089651025 hasConceptScore W2089651025C17409809 @default.
- W2089651025 hasConceptScore W2089651025C197435368 @default.
- W2089651025 hasConceptScore W2089651025C207318512 @default.
- W2089651025 hasConceptScore W2089651025C31258907 @default.
- W2089651025 hasConceptScore W2089651025C41008148 @default.
- W2089651025 hasConceptScore W2089651025C42090638 @default.
- W2089651025 hasConceptScore W2089651025C81820708 @default.
- W2089651025 hasIssue "3-4" @default.
- W2089651025 hasLocation W20896510251 @default.
- W2089651025 hasOpenAccess W2089651025 @default.
- W2089651025 hasPrimaryLocation W20896510251 @default.
- W2089651025 hasRelatedWork W1979458090 @default.
- W2089651025 hasRelatedWork W1983162852 @default.
- W2089651025 hasRelatedWork W2006125956 @default.
- W2089651025 hasRelatedWork W2008590108 @default.
- W2089651025 hasRelatedWork W2013690481 @default.
- W2089651025 hasRelatedWork W2117642839 @default.
- W2089651025 hasRelatedWork W2135827512 @default.
- W2089651025 hasRelatedWork W2314337543 @default.
- W2089651025 hasRelatedWork W2772489487 @default.
- W2089651025 hasRelatedWork W4231358795 @default.
- W2089651025 hasVolume "65" @default.
- W2089651025 isParatext "false" @default.
- W2089651025 isRetracted "false" @default.
- W2089651025 magId "2089651025" @default.
- W2089651025 workType "article" @default.