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Another bog-like wetland is called a fen. Bogs and Fens Peatlands are generally divided into two categories: bogs and fens. Bogs and fens are wetlands. Bogs receive water and nutrients only from the … Grasses and sedges are common plants in fens and fens often look like meadows. Bogs are characterized by their poor soil and high peat content, while fens have less peat and more plant life than a bog. At least they are if you can call a wet place with nothing but peat, or sphagnum moss, underfoot “land.” Such features, not quite land and not quite water, dot the Adirondack landscape. Vegetation in boreal peatlands are primarily in bogs and fens. They are like bogs because they have peat deposits in them, but unlike bogs some of their … Usually, they are covered with sphagnum moss, sedges and shrubs that can grow in low alkaline conditions, like leather leaf and other plants from the heather family. The bogs, due to high acidity, do not provide high levels of nutrients like nitrogen and phosphorous for plant life. Like bogs, fens formed when glaciers retreated. Both are permanently saturated wetlands. Fens typically are fed by a steady source of ground water whereas bogs are usually enclosed depressions filled by rain water. Their saturated, acidic soils are low in nutrients. Because of their water and soil conditions, bogs and fens are home to rare and specialized plants. These unusual wetlands are home to a variety of plants and animals including unique bog lemmings, pitcher plants, and sundews. Bogs receive their water from rainfall and snowmelt. Bogs and fens are uncommon wetland communities with water chemistry (pH) at the extremes: bogs are acidic and fens are basic or alkaline. Whenever and wherever we hike, we march around and over them, sometimes on boardwalks, planks, or corduroy.