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Luhasoo bog in Estonia.The mire has tussocks of heather, and is being colonised by pine trees.. This is a list of bogs, wetland mires that accumulate peat from dead plant material, usually sphagnum moss. [1]
Bog iron is a form of impure iron deposit that develops in bogs or swamps by the chemical or biochemical oxidation of iron carried in solution. In general, bog ores consist primarily of iron oxyhydroxides , commonly goethite (FeO(OH)).
A cataract bog is a rare ecological community, formed where a permanent stream flows over a granite outcropping. The sheeting of water keeps the edges of the rock wet without eroding the soil, but in this precarious location no tree or large shrub can maintain a roothold. The result is a narrow, permanently wet, sunny habitat.
Reports of bog bodies surfaced during the early 18th century. [1] In 1965, the German scientist Alfred Dieck catalogued more than 1,850 bog bodies, but later scholarship revealed much of Dieck's work was erroneous. [2] Hundreds of bog bodies have been recovered and studied, [3] although it is believed that only around 45 remain intact today. [4]
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After bog iron was made redundant by the increasing availability of iron ore, Allaire closed the Howell Works and eventually retired there with his family. The property remained in private hands until being bequeathed to the state in 1941. Today, the Howell Works is a registered historic site known as Allaire Village.
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Volo Bog State Natural Area is a nature reserve in Illinois, United States, preserving Volo Bog. The bog was designated a National Natural Landmark in 1973 as the only remaining open-water quaking bog in Illinois. [1] The site also contains woodlands, savanna, marshes, prairie restoration areas, shrubland and old fields.