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A fen is a type of peat-accumulating wetland fed by mineral-rich ground or surface water. [1] [2] It is one of the main types of wetland along with marshes, swamps ...
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 (minerotrophic). Thus, while a bog is always acidic and nutrient-poor, a fen may be slightly acidic, neutral, or alkaline, and either nutrient-poor or nutrient-rich. [ 8 ]
A biome (/ ˈ b aɪ. oʊ m /) is a ... Fen, and Moor; Temperate Deserts and Semi-Deserts; Coniferous Forests; Temperate Deciduous Forests; Natural Grasslands ...
A fen is another wetland form, which is created by a seep from below. The fen is affected by the calcium included in the seepage. It is usually associated with glacial moraines. Vegetation can be either herbaceous plants or heavily forested. The best known fen in the dunes is mistakenly called Cowles Bog, rather than more appropriately, Cowles ...
England population density and low elevation coastal zones. The Fens are particularly vulnerable to sea level rise.. The Fens or Fenlands in eastern England is a area of former marshland of low lying land supporting a rich ecology and numerous species.
A fen-meadow is a type of peatland, common in North America and Europe, that receives water from precipitation and groundwater. Habitat The ...
Poplar growing on muskeg. Muskeg (Ojibwe: mashkiig; Cree: maskīk; French: fondrière de mousse, lit. moss bog) is a peat-forming ecosystem found in several northern climates, most commonly in Arctic and boreal areas.
As this progression continues, riparian trees and bushes appear and a carr landscape is created – in effect a wooded fen in a waterlogged terrain. At this stage, overall, unlike the overwhelming acidity of decaying reeds, the pH is not too acidic and the soil is not too deficient in minerals, making a habitat for endemic and other wildlife.