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Poor fens are, in many ways, an intermediate between rich fens and bogs. Hydrologically, they are more similar to rich fens than to bogs, but regarding vegetation composition and chemistry, they are more similar to bogs than rich fens. [30] They are much more acidic than their rich counterparts, with a pH of approximately 5.5 to 4. [12]
There are two types of mire: bog and fen. [2] A bog is a mire that, due to its raised location relative to the surrounding landscape, obtains all its water solely from precipitation (ombrotrophic). [7] A fen is located on a slope, flat, or in a depression and gets most of its water from the surrounding mineral soil or from groundwater ...
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 ...
Niitvälja Bog - is a fen in Harju County; ... Differences between bogs and other wetlands. Muskeg; Fen; Bog body; Bog iron; Bog snorkelling; List of bog bodies ...
There are four main kinds of wetlands – marsh, swamp, bog, and fen (bogs and fens being types of peatlands or mires). Some experts also recognize wet meadows and aquatic ecosystems as additional wetland types. [1] Sub-types include mangrove forests, carrs, pocosins, floodplains, [1] peatlands, vernal pools, sinks, and many others. [22]
There are two types of mire – fens and bogs. A bog is a domed-shaped land form, is higher than the surrounding landscape, and obtains most of its water from rainfall (i.e., is ombrotrophic) while a fen is located on a slope, flat, or depression and gets its water from both rainfall and surface water.
Muskeg is approximately synonymous with bog or peatland, and is a standard term in Canada and Alaska. The term became common in these areas because it is of Cree origin; maskek ( ᒪᐢᑫᐠ ) meaning "low-lying marsh".
This water has flowed over or through rocks often acquiring dissolved chemicals which raise the nutrient levels and reduce the acidity, which leads to different vegetation such as fen or poor fen. In most cases, ombrotrophic bogs are extremely nutrient deficient, relying solely on precipitation and atmospheric dust for nutrient supply. This ...