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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.
This is a list of bog bodies grouped by location of discovery. Bog bodies, or bog people, are the naturally preserved corpses of humans and some animals recovered from peat bogs . The bodies have been most commonly found in the Northern European countries of Denmark, Germany, The Netherlands, the United Kingdom, and Ireland.
Ireland's Bord na Móna ("peat board") was one of the first companies to mechanically harvest peat, which is being phased out. [31] The other major use of dried peat is as a soil amendment (sold as moss peat or sphagnum peat) to increase the soil's capacity to retain moisture and enrich the soil. [4] It is also used as a mulch.
A lump of peat Peat stacks in Südmoslesfehn (district of Oldenburg, Germany) in 2013 Peat gatherers at Westhay, Somerset Levels in 1905 Peat extraction in East Frisia, Germany. Peat is an accumulation of partially decayed vegetation or organic matter. It is unique to natural areas called peatlands, bogs, mires, moors, or muskegs.
Tollund Man, Denmark, 4th century BC Gallagh Man, Ireland, c. 470–120 BC. A bog body is a human cadaver that has been naturally mummified in a peat bog.Such bodies, sometimes known as bog people, are both geographically and chronologically widespread, having been dated to between 8000 BC and the Second World War. [1]
Lindow Moss peat workings in 2005. Lindow Moss, also known as Saltersley Common, is a raised mire peat bog on the edge of Wilmslow in Cheshire, England.It has been used as common land since the medieval period and is best known for the discovery of the preserved bog body of Lindow Man in 1984 as well as Lindow Woman the year before.
The Irish Peatland Conservation Council describes the bog as "an important area of peatland, as much a part of Irish natural heritage as the Book of Kells." [2] The bog is much reduced after centuries of industrial exploitation and recent encroachments by development. [citation needed] Efforts are underway to preserve sections of it. [citation ...
On western moors, the peat layer may be several metres thick. Scottish "muirs" are generally heather moors, but also have extensive covering of grass, cotton-grass, mosses, bracken and under-shrubs such as crowberry, with the wetter moorland having sphagnum moss merging into bog-land. [1]
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