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A raised bog in Ķemeri National Park, Jūrmala, Latvia, formed approximately 10,000 years ago in the postglacial period and now a tourist attraction. A bog or bogland is a wetland that accumulates peat as a deposit of dead plant materials – often mosses, typically sphagnum moss. [ 1]
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.
The Big Dig was a megaproject in Boston that rerouted the then elevated Central Artery of Interstate 93 that cut across Boston into the O'Neill Tunnel and built the Ted Williams Tunnel to extend Interstate 90 to Logan International Airport. Those two projects were the origin of the official name, the Central Artery/Tunnel Project ( CA/T Project ).
This is a list of bog bodies in order of country in which they were first discovered. Bog bodies, or bog people, are the naturally preserved corpses of humans and some animals recovered from peat bogs. The bodies have been most commonly found in the Northern European countries of Denmark, Germany, The Netherlands, the United Kingdom and Ireland.
1972. 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.
Zurich Bog. Categories: Bogs by country. Wetlands of the United States. Bogs of North America.
Big O notation is a mathematical notation that describes the limiting behavior of a function when the argument tends towards a particular value or infinity. Big O is a member of a family of notations invented by German mathematicians Paul Bachmann, [1] Edmund Landau, [2] and others, collectively called Bachmann–Landau notation or asymptotic ...
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)). Iron-bearing groundwater typically emerges as a spring and the iron in it forms ferric hydroxide upon ...