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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]
A bog in Lauhanvuori National Park, Isojoki, Finland Tourbière du Lac-à-la-Tortue (fr), ombrotrophic, Quebec, Canada Peat bog and peat to dry, L'Isle-aux-Coudres, Quebec, Canada, 1976 Drone video of Kakerdaja bog in Estonia (September 2021) Precipitation accumulates in many bogs, forming bog pools, such as Koitjärve bog in Estonia.
Peat provides around 4% of Finland's annual energy production. [91] Also, agricultural and forestry-drained peat bogs actively release more CO 2 annually than is released in peat energy production in Finland. The average regrowth rate of a single peat bog, however, is indeed slow, from 1,000 up to 5,000 years. Furthermore, it is a common ...
Blanket bog on the Yell, Shetland Islands, with some peat working. Blanket bog or blanket mire, also known as featherbed bog, is an area of peatland, forming where there is a climate of high rainfall and a low level of evapotranspiration, allowing peat to develop not only in wet hollows but over large expanses of undulating ground.
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 ...
Muskeg consists of non-living organic material in various states of decomposition (as peat), ranging from fairly intact sphagnum moss, to sedge peat, to highly decomposed humus. Pieces of wood can make up five to fifteen percent of the peat soil. The water table tends to be near the surface.
(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.
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).