FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2099346111> ?p ?o ?g. }

• W2099346111 endingPage "494" @default.
• W2099346111 startingPage "477" @default.
• W2099346111 abstract "Denudation mechanisms differ fundamentally between limestone and silicate rock types, which are subject to very different rate thresholds and enhancers/inhibitors. Silicates are removed largely by erosion, the mechanical entrainment and transport of particles. This is a relatively high energy, and highly episodic, process which occurs only when a minimum threshold flow velocity is exceeded; it is inhibited by vegetation cover and favoured by strongly seasonal runoff. Limestone is removed largely by chemical dissolution at a rate directly proportional to runoff. Dissolution is a relatively low energy process that can occur at any flow velocity or in static water; in general it is enhanced by vegetation cover and non-seasonality of runoff. These contrasting factors in the denudation of silicates versus limestone can produce strikingly uneven rates of surface lowering across a landscape, sometimes akin to the well known ‘tortoise and hare race’, where the slow and steady denudation of limestones may in the long term exceed the sometimes rapid, but often localized and episodic, erosion of silicates. Prolonged exposure of limestone to a humid temperate climate in a tectonically stable environment produces low-relief corrosion plains in which limestone uplands are anomalous and, in most instances, due to recent unroofing from beneath a siliciclastic cover. In a highly seasonal or semi-arid climate almost the exact inverse may develop, with ‘flashy’ runoff and sparse vegetation favouring erosion rather than dissolution. Even under a constant humid climate progressive unroofing of a thick limestone unit within folded siliciclastics may lead to a topographic inversion over time, with the limestone outcrop always forming a topographic low flanked by siliciclastic uplands. Valleys will be initiated on anticlinal crests, where the limestone is first unroofed, but progressive lowering of the limestone causes these valleys to migrate to their final position in the synclinal troughs. In humid climates isostatic compensation in response to slow, but continuous, denudation of extensive limestone outcrops may be a significant factor in the development of relief on adjacent, more slowly eroding, silicate outcrops. Copyright © 2004 John Wiley & Sons, Ltd." @default.
• W2099346111 created "2016-06-24" @default.
• W2099346111 creator A5022945325 @default.
• W2099346111 date "2004-02-11" @default.
• W2099346111 modified "2023-09-30" @default.
• W2099346111 title "Tortoises and hares: dissolution, erosion and isostasy in landscape evolution" @default.
• W2099346111 cites W1519476993 @default.
• W2099346111 cites W1965699878 @default.
• W2099346111 cites W1970130975 @default.
• W2099346111 cites W1988290474 @default.
• W2099346111 cites W2008248704 @default.
• W2099346111 cites W2010436562 @default.
• W2099346111 cites W2017277567 @default.
• W2099346111 cites W2042980435 @default.
• W2099346111 cites W2066416007 @default.
• W2099346111 cites W2066546656 @default.
• W2099346111 cites W2067093186 @default.
• W2099346111 cites W2072712492 @default.
• W2099346111 cites W2076904246 @default.
• W2099346111 cites W2083343669 @default.
• W2099346111 cites W2090926216 @default.
• W2099346111 cites W2093001750 @default.
• W2099346111 cites W2101313655 @default.
• W2099346111 cites W2101466506 @default.
• W2099346111 cites W2120864630 @default.
• W2099346111 cites W2132394621 @default.
• W2099346111 cites W2142408179 @default.
• W2099346111 cites W2144411479 @default.
• W2099346111 cites W2150803244 @default.
• W2099346111 cites W2151357448 @default.
• W2099346111 cites W2161430494 @default.
• W2099346111 cites W2577996715 @default.
• W2099346111 cites W3604062 @default.
• W2099346111 cites W4300840576 @default.
• W2099346111 cites W657397921 @default.
• W2099346111 doi "https://doi.org/10.1002/esp.1047" @default.
• W2099346111 hasPublicationYear "2004" @default.
• W2099346111 type Work @default.
• W2099346111 sameAs 2099346111 @default.
• W2099346111 citedByCount "47" @default.
• W2099346111 countsByYear W20993461112012 @default.
• W2099346111 countsByYear W20993461112014 @default.
• W2099346111 countsByYear W20993461112015 @default.
• W2099346111 countsByYear W20993461112016 @default.
• W2099346111 countsByYear W20993461112017 @default.
• W2099346111 countsByYear W20993461112018 @default.
• W2099346111 countsByYear W20993461112019 @default.
• W2099346111 countsByYear W20993461112020 @default.
• W2099346111 countsByYear W20993461112021 @default.
• W2099346111 countsByYear W20993461112022 @default.
• W2099346111 countsByYear W20993461112023 @default.
• W2099346111 crossrefType "journal-article" @default.
• W2099346111 hasAuthorship W2099346111A5022945325 @default.
• W2099346111 hasBestOaLocation W20993461112 @default.
• W2099346111 hasConcept C114793014 @default.
• W2099346111 hasConcept C123157820 @default.
• W2099346111 hasConcept C127313418 @default.
• W2099346111 hasConcept C151730666 @default.
• W2099346111 hasConcept C187320778 @default.
• W2099346111 hasConcept C18903297 @default.
• W2099346111 hasConcept C1965285 @default.
• W2099346111 hasConcept C50477045 @default.
• W2099346111 hasConcept C76886044 @default.
• W2099346111 hasConcept C77928131 @default.
• W2099346111 hasConcept C81461190 @default.
• W2099346111 hasConcept C86803240 @default.
• W2099346111 hasConcept C87432785 @default.
• W2099346111 hasConceptScore W2099346111C114793014 @default.
• W2099346111 hasConceptScore W2099346111C123157820 @default.
• W2099346111 hasConceptScore W2099346111C127313418 @default.
• W2099346111 hasConceptScore W2099346111C151730666 @default.
• W2099346111 hasConceptScore W2099346111C187320778 @default.
• W2099346111 hasConceptScore W2099346111C18903297 @default.
• W2099346111 hasConceptScore W2099346111C1965285 @default.
• W2099346111 hasConceptScore W2099346111C50477045 @default.
• W2099346111 hasConceptScore W2099346111C76886044 @default.
• W2099346111 hasConceptScore W2099346111C77928131 @default.
• W2099346111 hasConceptScore W2099346111C81461190 @default.
• W2099346111 hasConceptScore W2099346111C86803240 @default.
• W2099346111 hasConceptScore W2099346111C87432785 @default.
• W2099346111 hasIssue "4" @default.
• W2099346111 hasLocation W20993461111 @default.
• W2099346111 hasLocation W20993461112 @default.
• W2099346111 hasOpenAccess W2099346111 @default.
• W2099346111 hasPrimaryLocation W20993461111 @default.
• W2099346111 hasRelatedWork W1744977351 @default.
• W2099346111 hasRelatedWork W1851726814 @default.
• W2099346111 hasRelatedWork W1988290474 @default.
• W2099346111 hasRelatedWork W1997580997 @default.
• W2099346111 hasRelatedWork W2348087381 @default.
• W2099346111 hasRelatedWork W2371149085 @default.
• W2099346111 hasRelatedWork W2391363624 @default.
• W2099346111 hasRelatedWork W286878504 @default.
• W2099346111 hasRelatedWork W4295677999 @default.
• W2099346111 hasRelatedWork W816694438 @default.
• W2099346111 hasVolume "29" @default.
• W2099346111 isParatext "false" @default.
• W2099346111 isRetracted "false" @default.

• next