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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.
The bog continues to form peat, and over time a shallow dome of bog peat develops into a raised bog. The dome is typically a few meters high in the center and is often surrounded by strips of fen or other wetland vegetation at the edges or along streamsides where groundwater can percolate into the wetland.
All mires are initially fens when the peat starts to form, and may turn into bogs once the height of the peat layer reaches above the surrounding land. A quagmire is a floating (quaking) mire, bog, or any peatland being in a stage of hydrosere or hydrarch (hydroseral) succession, resulting in pond-filling yields underfoot (floating mats).
Luhasoo bog in Estonia.The mire has tussocks of heather, and is being colonised by pine trees.. This is a list of bogs, wetland mires that accumulate peat from dead plant material, usually sphagnum moss. [1]
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]
(See bog.) The main constituents of the peat are rootless peat mosses that grow slowly in height whilst at the same time the lower layer becomes peat as the air is excluded. Depending on the geographical location, various species of peat moss are involved in making a raised bog. The growth rate of the peat layer is only about a millimetre per year.
Sphagnum peat moss is a frequently used growth medium for the cultivation of houseplants and forest plants, is obtained by harvesting peat bogs in the circumboreal area and then distributed across the globe. [65] Peat moss is a crucial substrate for forest plant nursery production, as it significantly enhances the quality and survival of ...
Thorne and Hatfield Moors Re-flooded peat workings on Thorne Moors form part of the Humberhead Peatlands National Nature Reserve The Moors within South Yorkshire Location North-east and east of Doncaster, South Yorkshire, England OS grid SE723151 Coordinates 53°38′N 0°55′W / 53.63°N 0.91°W / 53.63; -0.91 Area 8,201 acres (33.19 km 2) Thorne and Hatfield Moors form the ...