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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 quaking bog, schwingmoor, or swingmoor is a form of floating bog occurring in wetter parts of valley bogs and raised bogs and sometimes around the edges of acidic lakes. The bog vegetation, mostly sphagnum moss anchored by sedges (such as Carex lasiocarpa ), forms a floating mat approximately half a meter thick on the surface of water or ...
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.
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 practice to forest used peat bogs instead of giving them a chance to renew ...
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).
Store Vildmose (lit.: Large Wild-bog) is bogland located in northern Jutland, Vendsyssel, about 20 km north-west of Aalborg. It is the remnant of an extensive raised peat bog, in large part drained by constructed canals in the early 20th century. Some areas are still relatively untouched and give an impression of the original nature of this bog.
A raised bog of this type develops from a lake or flat marshy area, over either non-acidic or acidic substrates. Over centuries there is a progression from open lake, to marsh and then fen (or on acidic substrates, valley bog), as silt or peat fill the lake. Eventually, peat builds up to a level where the land surface is too flat for ground or ...
Fleet Moss, which is 2.5 miles (4 km) north of the village of Oughtershaw, [4] is an important peatland that stores carbon, filters water and provides a habitat for wildlife and fauna. [5] A road extends over the hill from Oughtershaw to Gayle, then Hawes , which passes Fleet Moss, but attains a slightly higher altitude than the bog of 1,932 ft ...