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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.
Claims for its origins include a 1955 ride of 2.4 km (1.5 mi) along the tidal bore of the River Severn. [ 1 ] River surfing on standing waves has been documented as far back as 1972 on an artificial wave created on a section of the Eisbach man-made river , a side arm of the Isar River , near Haus der Kunst in the Englischer Garten park in ...
The site (Severn Estuary and Upper Severn Estuary) is listed in the 'Forest of Dean Local Plan Review' as a Key Wildlife Site (KWS). [ 22 ] Both SSSI citations provide detail of the geological and biological interest and of particular note is the international importance for wintering and wading birds of passage, [ 1 ] and of estuarine habits ...
A bore in Morecambe Bay, in the United Kingdom Video of the Arnside Bore, in the United Kingdom The tidal bore in Upper Cook Inlet, in Alaska. A tidal bore, [1] often simply given as bore in context, is a tidal phenomenon in which the leading edge of the incoming tide forms a wave (or waves) of water that travels up a river or narrow bay, reversing the direction of the river or bay's current.
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Maisemore Bridge connects the village to Alney Island, and provides a viewpoint for the Severn bore.Maisemore Weir and Lock were built in about 1870. [3] The weir is at the upper limit of the tides on the Severn.
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