FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2077807218> ?p ?o ?g. }

• W2077807218 endingPage "184" @default.
• W2077807218 startingPage "157" @default.
• W2077807218 abstract "The shore of the former tidal wetland northeast of Cardiff, called the Wentlooge Level and reclaimed during the Roman period, exposes a series of late Flandrian lithostratigraphic units dominated by estuarine clays. Chief among these are the (upper) Wentlooge Formation (up to 2.5 m thick) and the Rumney Formation (up to 2.7 m thick). The (upper) Wentlooge Formation consists of greenish grey slightly silty clays and is capped by an immature palaeosol yielding signs of clay illuviation. Extending down from a level within the palaeosol is a reticulate system of deep drainage ditches, some of which are locally filled with Romano-British cultural debris, regarded as dating their excavation. Such fills are sealed by the soil. Marine erosion after the Roman period but before late mediaeval times destroyed much of the upper Wentlooge Formation together with a presumed Roman sea defence. The then unprotected drainage ditches were invaded during this episode of coastal retreat and widened out to form a series of large embayments that defined flat-topped headlands on which the palaeosol formed a capping. The overlying Rumney Formation is a series of pink estuarine silty clays with some sands and gravels. It infills the embayments of the coastline cut in the Wentlooge beds and smothers its headlands to a thickness of about 1.4 m. Deposition in the embayments began in the 15th century, but on the headlands was delayed for a further 100-200 years. The outward movement of the shore recorded by the mudflat and marsh deposits of the earlier part of the Rumney Formation was eventually reversed with the formation of a bold mud cliff that has continued to retreat inland to its present position. On the upper part of this cliff are exposed sand sheets which record sand bodies formed during the retreat, at the heads of inlets, as pocket beaches, and as landward-facing bars cast up on to the salt marsh during high tides and storms. Two younger lithostratigraphic units of recent date, the Awre Formation and the Northwick Formation, have stratigraphical relations similar to the Rumney Formation and record further movements of the strand. The coastal oscillations recorded by the lithostratigraphy are attributable to fluctuations in the role and strength of waves at the shore, as governed by either medium-term weather changes or the positions of offshore shoals, or by the morphology of the shore itself." @default.
• W2077807218 created "2016-06-24" @default.
• W2077807218 creator A5005277423 @default.
• W2077807218 date "1987-04-14" @default.
• W2077807218 modified "2023-10-02" @default.
• W2077807218 title "Late Flandrian shoreline oscillations in the Severn Estuary: the Rumney formation at its typesite (Cardiff area)" @default.
• W2077807218 cites W1991596164 @default.
• W2077807218 cites W2009946541 @default.
• W2077807218 cites W2010654040 @default.
• W2077807218 cites W2016709223 @default.
• W2077807218 cites W2034816464 @default.
• W2077807218 cites W2074901625 @default.
• W2077807218 cites W2081916452 @default.
• W2077807218 cites W2086448319 @default.
• W2077807218 cites W2086622232 @default.
• W2077807218 cites W2097726912 @default.
• W2077807218 cites W2122433968 @default.
• W2077807218 cites W2125097190 @default.
• W2077807218 cites W2139685614 @default.
• W2077807218 cites W2325972299 @default.
• W2077807218 cites W2326815333 @default.
• W2077807218 cites W2477550510 @default.
• W2077807218 cites W320138108 @default.
• W2077807218 cites W610027560 @default.
• W2077807218 cites W2482306520 @default.
• W2077807218 doi "https://doi.org/10.1098/rstb.1987.0006" @default.
• W2077807218 hasPublicationYear "1987" @default.
• W2077807218 type Work @default.
• W2077807218 sameAs 2077807218 @default.
• W2077807218 citedByCount "50" @default.
• W2077807218 countsByYear W20778072182014 @default.
• W2077807218 countsByYear W20778072182015 @default.
• W2077807218 countsByYear W20778072182017 @default.
• W2077807218 countsByYear W20778072182018 @default.
• W2077807218 countsByYear W20778072182023 @default.
• W2077807218 crossrefType "journal-article" @default.
• W2077807218 hasAuthorship W2077807218A5005277423 @default.
• W2077807218 hasConcept C111368507 @default.
• W2077807218 hasConcept C114793014 @default.
• W2077807218 hasConcept C121332964 @default.
• W2077807218 hasConcept C127313418 @default.
• W2077807218 hasConcept C151730666 @default.
• W2077807218 hasConcept C152382732 @default.
• W2077807218 hasConcept C166957645 @default.
• W2077807218 hasConcept C17409809 @default.
• W2077807218 hasConcept C185515318 @default.
• W2077807218 hasConcept C205649164 @default.
• W2077807218 hasConcept C24890656 @default.
• W2077807218 hasConcept C2776023875 @default.
• W2077807218 hasConcept C2781291010 @default.
• W2077807218 hasConcept C2816523 @default.
• W2077807218 hasConcept C64297162 @default.
• W2077807218 hasConcept C76123530 @default.
• W2077807218 hasConceptScore W2077807218C111368507 @default.
• W2077807218 hasConceptScore W2077807218C114793014 @default.
• W2077807218 hasConceptScore W2077807218C121332964 @default.
• W2077807218 hasConceptScore W2077807218C127313418 @default.
• W2077807218 hasConceptScore W2077807218C151730666 @default.
• W2077807218 hasConceptScore W2077807218C152382732 @default.
• W2077807218 hasConceptScore W2077807218C166957645 @default.
• W2077807218 hasConceptScore W2077807218C17409809 @default.
• W2077807218 hasConceptScore W2077807218C185515318 @default.
• W2077807218 hasConceptScore W2077807218C205649164 @default.
• W2077807218 hasConceptScore W2077807218C24890656 @default.
• W2077807218 hasConceptScore W2077807218C2776023875 @default.
• W2077807218 hasConceptScore W2077807218C2781291010 @default.
• W2077807218 hasConceptScore W2077807218C2816523 @default.
• W2077807218 hasConceptScore W2077807218C64297162 @default.
• W2077807218 hasConceptScore W2077807218C76123530 @default.
• W2077807218 hasIssue "1171" @default.
• W2077807218 hasLocation W20778072181 @default.
• W2077807218 hasOpenAccess W2077807218 @default.
• W2077807218 hasPrimaryLocation W20778072181 @default.
• W2077807218 hasRelatedWork W128811910 @default.
• W2077807218 hasRelatedWork W1971308625 @default.
• W2077807218 hasRelatedWork W1972506182 @default.
• W2077807218 hasRelatedWork W2010758201 @default.
• W2077807218 hasRelatedWork W2070113985 @default.
• W2077807218 hasRelatedWork W2268442924 @default.
• W2077807218 hasRelatedWork W2333348788 @default.
• W2077807218 hasRelatedWork W2494306156 @default.
• W2077807218 hasRelatedWork W2970679797 @default.
• W2077807218 hasRelatedWork W4210429390 @default.
• W2077807218 hasVolume "315" @default.
• W2077807218 isParatext "false" @default.
• W2077807218 isRetracted "false" @default.
• W2077807218 magId "2077807218" @default.
• W2077807218 workType "article" @default.