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      • A bog or bogland is a wetland that accumulates peat as a deposit of dead plant materials – often mosses, typically sphagnum moss. It is one of the four main types of wetlands.
      en.wikipedia.org/wiki/Bog
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  2. Oct 3, 2024 · Bog, type of wetland ecosystem characterized by wet, spongy, poorly drained peat-rich soil. Typical bogs are highly acidic and only occur in areas where the water is very low in minerals. They cover vast areas in the tundra and boreal forest regions of Canada, northern Europe, and Russia.

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  3. en.wikipedia.org › wiki › BogBog - Wikipedia

    A bog or bogland is a wetland that accumulates peat as a deposit of dead plant materials – often mosses, typically sphagnum moss. [1] It is one of the four main types of wetlands . Other names for bogs include mire , mosses, quagmire, and muskeg ; alkaline mires are called fens .

  4. Bogs are unique wetland ecosystems characterized by their waterlogged, acidic, and nutrient-poor conditions. They are typically found in areas with high rainfall and poor drainage, such as depressions or old glacial lakes. Bog formation begins when vegetation, primarily mosses, start to grow in water-saturated environments.

  5. www.nationalgeographic.org › encyclopedia › bogBog

    Oct 19, 2023 · A bog is a freshwater wetland of soft, spongy ground consisting mainly of partially decayed plant matter called peat. Bogs are generally found in cool, northern climates. They often develop in poorly draining lake basins created by glaciers during the most recent ice age.

  6. What is a Bog? Bogs are acidic, peat-accumulating wetlands defined by three main characteristics: Sky-Water: Rain & snow (rather than ground water and runoff) are the main water sources in true bogs.

  7. bog has been forming for a shorter period of time (often 5-6,000 years) and also because the sloping nature of much ground prevents effective water-logging and results in greater nutrient through-flow.

  8. Bogs, also known as ombrogenous mires, are higher than their surrounding landscapes and receive water only from precipitation. Fens, or geogenous mires, are located in depressions and receive water that has been in contact with mineral bedrock or soil.

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