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About: Severn bore     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : yago:TidalFlow107404114, within Data Space : dbpedia.demo.openlinksw.com associated with source document(s)

Type: Thingyago:WikicatTidalBoresyago:WikicatVisitorAttractionsInGloucestershiregeo:SpatialThingyago:Abstraction100002137yago:Attraction106615561yago:ChangeOfLocation107311115yago:Current107406765yago:Event100029378yago:Flow107405893yago:Happening107283608yago:Movement107309781yago:PsychologicalFeature100023100yago:YagoPermanentlyLocatedEntityyago:Show106619065yago:SocialEvent107288639yago:TidalBore107403920yago:TidalFlow107404114 New Facet based on Instances of this Class

The Severn bore is a tidal bore seen on the tidal reaches of the River Severn in south western England. It is formed when the rising tide moves into the funnel-shaped Bristol Channel and Severn Estuary and the surging water forces its way upstream in a series of waves, as far as Gloucester and beyond. The bore behaves differently in different stretches of the river; in the lower, wider parts it is more noticeable in the deep channels as a slight roller, while the water creeps across the sand and mudflats. In the narrower, upper reaches, the river occupies the whole area between its banks and the bore advances in a series of waves that move upstream. Near Gloucester, the advancing water overcomes two weirs, and sometimes one in Tewkesbury, before finally petering out.