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  2. List of bogs - Wikipedia

    en.wikipedia.org/wiki/List_of_bogs

    Alfred Bog - a dome bog in eastern Ontario, Canada sphagnum bog east of Ottawa in eastern Ontario; The Bog - a putrescent lowland in Saint-Henri, Quebec known for its diverse array of toads and squires; Burns Bog - in British Columbia, the largest domed peat bog in North America; Eagle Hill Bog - A small spaghnum bog on Campobello Island, New ...

  3. Bog - Wikipedia

    en.wikipedia.org/wiki/Bog

    Bogs contain species of vulnerable reptilians such as the bog turtle. [20] Bogs even have distinctive insects; English bogs give a home to a yellow fly called the hairy canary fly (Phaonia jaroschewskii), and bogs in North America are habitat for a butterfly called the bog copper (Lycaena epixanthe).

  4. Category:Bogs of the United States by state - Wikipedia

    en.wikipedia.org/wiki/Category:Bogs_of_the...

    W. Bogs of Washington (state) ‎ (2 P) Bogs of West Virginia ‎ (3 P) Bogs of Wisconsin ‎ (6 P) Categories: Bogs of the United States. Wetlands of the United States by state. Hidden category: Container categories.

  5. Appalachian bogs - Wikipedia

    en.wikipedia.org/wiki/Appalachian_bogs

    Appalachian bogs. Cranberry Glades, a bog preserve in West Virginia. Appalachian bogs are boreal or hemiboreal ecosystems, which occur in many places in the Appalachian Mountains, particularly the Allegheny and Blue Ridge subranges. [1][2] Though popularly called bogs, many of them are technically fens. [3]

  6. Bog iron - Wikipedia

    en.wikipedia.org/wiki/Bog_iron

    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 ...

  7. Raised bog - Wikipedia

    en.wikipedia.org/wiki/Raised_bog

    The term raised bog derives from the fact that this type of bog rises in height over time as a result of peat formation. They are like sponges of peat moss, full of water, that form a more or less dome shape in the landscape. In Germany, the term Hochmoor (lit. ' high bog ') strictly refers only to the classical, lens-shaped bogs of northwest ...

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