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Sphagnum magellanicum, commonly called Magellanic bogmoss, [2] Magellan's sphagnum, [3] Magellan's peatmoss or midway peat moss, is a widespread species of moss found in wet boreal forest in the far south and southwest of South America and in northern North America and Eurasia.
Ard or plough-marks on a boulder in a clearance cairn Ard-marks on a boulder in a clearance cairn at Eglinton Country Park A clearance cairn formed using mechanised extraction A recent clearance cairn devoid of lichen and moss growth. Cairns may be discrete, in large groups (cairnfields) or as linear formations—linear cairns.
Sphagnum is a genus of approximately 380 accepted species [2] [3] of mosses, commonly known as sphagnum moss, also bog moss and quacker moss (although that term is also sometimes used for peat). Accumulations of Sphagnum can store water, since both living and dead plants can hold large quantities of water inside their cells; plants may hold 16 ...
Peat is an accumulation of partially decayed vegetation or organic matter. It is unique to natural areas called peatlands, bogs, mires, moors, or muskegs. [1] [2] Sphagnum moss, also called peat moss, is one of the most common components in
moss bog) is a peat-forming ecosystem found in several northern climates, most commonly in Arctic and boreal areas. 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". [1]
Sphagnum girgensohnii, commonly known as Girgensohn's bogmoss, [4] Girgensohn's sphagnum [5] or common green peat moss, is a species of peat moss with a Holarctic and Indo-Malesian distribution. First described by Edmund Russow in 1865, it is a relatively robust moss species characterised by its green to straw-coloured appearance and ...