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The River Severn (Welsh: Afon Hafren, pronounced [ˈavɔn ˈhavrɛn]), at 220 miles (354 km) long, is the longest river in Great Britain. [4] [5] It is also the river with the most voluminous flow of water by far in all of England and Wales, with an average flow rate of 107 m 3 /s (3,800 cu ft/s) at Apperley, Gloucestershire.
The Severn River is crossed by two bridges. One, known as the Severn River Bridge or Pearl Harbor Memorial Bridge, carries US 50/US 301/MD 2 and was first built in 1886. The other carries MD 450, and is now officially named the "US Naval Academy Bridge" because its south end traverses the academy. The latter bridge was built as a drawbridge in ...
Horsbere Brook is a tributary of the River Severn. It begins at Great Witcombe and flows in a northwesternly direction towards Longford, it's mouth being the Severn. Part of the brook forms a section of the boundary between the villages of Longford and Longlevens. Horsbere is culverted as it passes under the A40, A38, A417, and A46 roads.
Motorway crossings over the River Severn Prince of Wales Bridge (M4 motorway) Severn Bridge (M48 motorway) Queenhill Viaduct (M50 motorway) This is a list of crossings of the River Severn in Great Britain (including bridges, tunnels, ferries and fords), in order from source to mouth. The Severn has historically been a very important and busy river, and has been bridged throughout history. The ...
The Severn Estuary (Welsh: Aber Hafren) is the estuary of the River Severn, flowing into the Bristol Channel between South West England (from North Somerset, Bristol and South Gloucestershire) and South Wales (from Cardiff, Newport to Monmouthshire).
Hafren (or Sabre, Sabren, or Sabrina; Welsh: Hafren; Old Welsh: Habren) is a legendary British princess who was drowned in the River Severn by her repudiated stepmother Gwendolen. The legend appears in Geoffrey of Monmouth's pseudohistorical chronicle Historia Regum Britanniae (c. 1136).
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.
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