Peat can be formed from different materials, but a large percentage of the peat harvested is composed of sphagnum moss. Peat is a type of soil that is made up of partially decomposed plant matter. Peat formation is the result of incomplete decomposition of the remains of plants growing in waterlogged conditions. Hence, from the above, we can say that peat humus is a subcategory of peat humus.

Peat formed in very wet conditions accumulates faster, and is less decomposed, than that in drier places. In certain circumstances, peat can be an early stage in coal formation.

The peatland ecosystem is the most efficient carbon sink on the planet, because peatland plants capture CO 2 naturally released from the peat, maintaining an equilibrium. Peat is the "forgotten fossil fuel. This abundant resource (often mixed with wood at an average of 2.6%) is burned to produce heat and electricity. Different combined conditions of water and temperature decide the balance between accumulation and decomposition of peat, i.e. Peat, an organic fuel consisting of spongy material formed by the partial decomposition of organic matter, primarily plant material, in wetlands. Peat is a type of soil that is made up of partially decomposed plant matter.It is found in areas with very high moisture and low oxygen. Meanwhile, sphagnum moss is a plant grown on the surface layer above of the peatland, soil or a swamp. Peat provides around 6.2% of Finland's annual energy production, second only to Ireland. The contribution of peat to greenhouse gasemissions of Finland can exceed 10 million metric tonnes of carbon dioxide per year – equal to the total emissions of all passeng… And hence the name peat moss. Peat forms in bogs.

According to this theory the presence of either aerobic or anaerobic conditions decides whether any biomass will accumulate and in what form. The composition of peat can also be used to reconstruct ancient ecologies by examining the types and quantities of … Peat is found in wetlands and bogs across many countries. Peat is formed by the slow decay of successive layers of aquatic and semiaquatic plants, e.g., sedges, reeds, rushes, and mosses, and is the earliest stage of transition from compressed plant growth to the formation of coal coal, Bogs are a type of wetland with a high acid content. The composition of peat can also be used to reconstruct ancient ecologies by examining the types and quantities of its organic constituents. Most of the peat bogs that exist today formed since the retreat of the glaciers after the last ice age around 12,000 years ago.

As the peat which is formed in the peat-producing layer becomes subjected to anaerobic conditions in the deeper layers of the deposit, it is preserved and shows comparatively little change with time”. The large amount of water prevents and slows decomposition. Peat is only a minor contributor to the world energy supply. Peatlands cover about 3% of the earth’s land mass; they are found in the temperate (Northern Europe and America) and tropical regions (South East Asia, South America, South Africa and the Caribbean) 1.

Peat (/ p iː t /), also known as turf (/ t ɜːr f /), is an accumulation of partially decayed vegetation or organic matter.It is unique to natural areas called peatlands, bogs, mires, moors, or muskegs. They are found in peatlands (also called bogs or mires).

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