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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 ...
This is a list of bogs, wetland mires that accumulate peat from dead plant material, usually sphagnum moss. [1] Bogs are sometimes called quagmires (technically all bogs are quagmires while not all quagmires are necessarily bogs) and the soil which composes them is sometimes referred to as muskeg ; alkaline mires are called fens rather than bogs.
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 ...
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]
The Lincolnshire Wolds which also includes the Lincolnshire Wolds National Landscape are a range of low hills in the county of Lincolnshire, England which runs roughly parallel with the North Sea coast, from the Humber Estuary just west of the town of Barton-upon-Humber in North Lincolnshire down in a south easterly direction towards the flat Lincolnshire Fens in the south-east of the county ...
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