Downholland Moss

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Downholland Moss SSSI
Site of Special Scientific Interest
Lancashire UK location map.svg
Red pog.svg
Location within Lancashire
Location Lancashire
Grid reference SD327079
Coordinates 53°34′04″N3°01′20″W / 53.567834°N 3.0221956°W / 53.567834; -3.0221956
Area52.4 acres (0.2121 km2; 0.08187 sq mi)
Notification 1990

Downholland Moss is a Site of Special Scientific Interest, notified in 1990. [1] It is located near the town of Formby in Lancashire, England. Geological deposits at the site have been used to reconstruct palaeoenvironments and past sea-level change. [2]

Downholland Moss was one of several raised mires in Lancashire formed where glacial deposits allowed raised bogs to develop. [3]

Part of the land area designated as Downholland Moss Site of Special Scientific Interest is owned by the Church Commissioners [4]

Related Research Articles

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Peat is an accumulation of partially decayed vegetation or organic matter. It is unique to natural areas called peatlands, bogs, mires, moors, or muskegs. Sphagnum moss, also called peat moss, is one of the most common components in peat, although many other plants can contribute. The biological features of sphagnum mosses act to create a habitat aiding peat formation, a phenomenon termed 'habitat manipulation'. Soils consisting primarily of peat are known as histosols. Peat forms in wetland conditions, where flooding or stagnant water obstructs the flow of oxygen from the atmosphere, slowing the rate of decomposition. Peat properties such as organic matter content and saturated hydraulic conductivity can exhibit high spatial heterogeneity.

<span class="mw-page-title-main">Bog</span> Type of wetland with peat-rich soil

A bog or bogland is a wetland that accumulates peat as a deposit of dead plant materials – often mosses, typically sphagnum moss. It is one of the four main types of wetlands. Other names for bogs include mire, mosses, quagmire, and muskeg; alkaline mires are called fens. A bayhead is another type of bog found in the forest of the Gulf Coast states in the United States. They are often covered in heath or heather shrubs rooted in the sphagnum moss and peat. The gradual accumulation of decayed plant material in a bog functions as a carbon sink.

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References

  1. "SSSI detail". designatedsites.naturalengland.org.uk. Retrieved 2024-09-29.
  2. Huddart, D. (1992-01-01). "Coastal environmental changes and morphostratigraphy in southwest Lancashire, England". Proceedings of the Geologists' Association. 103: 217–236. doi:10.1016/S0016-7878(08)80231-3. ISSN   0016-7878.
  3. "Lancashire Mosslands | IUCN UK Peatland Programme". IUCN Peatland Programme. Retrieved 2024-09-29.
  4. "Mapping the habitats of England's ten largest institutional landowners". Who owns England?. 2020-10-06. Retrieved 2024-09-29.
Downholland Moss