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The Bedford Level Corporation (or alternatively the Corporation of the Bedford Level) was founded in England in 1663 to manage the draining of the Fens of East Central England. It formalised the legal status of the Company of Adventurers previously formed by the Duke of Bedford to reclaim 95,000 acres of the Bedford Level.
The Fens or Fenlands in eastern England are a naturally marshy region supporting a rich ecology and numerous species. Most of the fens were drained centuries ago, resulting in a flat, dry, low-lying agricultural region supported by a system of drainage channels and man-made rivers ( dykes and drains) and automated pumping stations .
Bogs of England (30 P) The Broads (2 C, 3 P) F. Fens of England (23 P) M. Marshes of England (1 C, 18 P) O. Otmoor (12 P) R. Ramsar sites in England (1 C, 131 P) S ...
Wicken Fen, England. Grasses in the foreground are typical of a fen. A fen is a type of peat-accumulating wetland fed by mineral-rich ground or surface water. [1] [2] It is one of the main types of wetland along with marshes, swamps, and bogs. Bogs and fens, both peat-forming ecosystems, are also known as mires. [2]
Alfred Bog - a dome bog in eastern Ontario, Canada sphagnum bog east of Ottawa in eastern Ontario; The Bog - a putrescent lowland in Saint-Henri, Quebec known for its diverse array of toads and squires; Burns Bog - in British Columbia, the largest domed peat bog in North America; Eagle Hill Bog - A small spaghnum bog on Campobello Island, New ...
Fenn's, Whixall and Bettisfield Mosses straddle the border between England and Wales. Fenn's Moss is on the Welsh side of the border and is in Wrexham County Borough, while Whixall Moss is in north Shropshire, on the English side of the border, and is only separated from Fenn's Moss by the Border Drain, a ditch similar to many others on the mosses, [1] which was dug in 1826. [2]
The Lincolnshire Fens are an area of low-lying land which have been subject to flooding and attempts to prevent it for centuries. In medieval times, the Midfen Dyke was built to drain the area, but by 1500, this was regarded less as a drain for the land than as a boundary marker between the Parts of Holland and the Parts of Kesteven, two of the three medieval subdivisions of Lincolnshire which ...
The Middle Levels of the Fens are a low-lying area of approximately 270 square miles (700 km 2), much of which is at or below sea level. [1] Attempts to protect them from inundation and to make them suitable for agriculture began in 1480, when the Bishop of Ely, John Morton, constructed a 12-mile (19 km) straight cut from Stanground to Guyhirne.