Bayhead in the context of "Peat bog"

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⭐ Core Definition: Bayhead

A bayhead or baygall is a specific type of wetland or swamp habitat. The name baygall is derived from sweetbay magnolia (Magnolia virginiana) and sweet gallberry holly (Ilex coriacea). Baygalls are recognized as a discrete ecosystem by ecologists and the swamps have been described as "distinct wetland communities in the Natural Communities of Louisiana". Baygall swamps are most often found in the low lying margins of floodplains and bottomlands with little or poor drainage to the main creek, bayou, or river channel. Baygall or bayhead swamps found on slopes and hillsides are sometimes referred to as a forest seep or hanging bogs. Hanging bogs are typically found in hardwood-pine forests. Most baygall swamps are semi-permanently saturated, or flooded.

The characteristics of a bayhead swamp are mostly broad, shallow drains, which can be found near margins of bottomlands and floodplains with little or no drainage. They most often receive a slow, but steady supply of water from seepage at the base of slopes and bluffs. Baygalls are relatively shallow wetlands, ranging from wet and saturated soils and leaf litter, to a few inches of stagnate or very slowly moving water, although some may occasionally be deeper depending on topography and rainfall. Most are also under closed or nearly closed canopies. Occasionally, larger and deeper baygalls may have open water at the center with floating vegetation such as the fragrant water-lily (Nymphaea odorata).

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👉 Bayhead in the context of Peat bog

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. Other names for bogs include mire, mosses, quagmire, and muskeg; alkaline mires are called fens. A bayhead is another type of bog found in the forest of the Gulf Coast states in the United States. They are often covered in heath or heather shrubs rooted in the sphagnum moss and peat. The gradual accumulation of decayed plant material in a bog functions as a carbon sink.

Bogs occur where the water at the ground surface is acidic and low in nutrients. A bog usually is found at a freshwater soft spongy ground that is made up of decayed plant matter which is known as peat. They are generally found in cooler northern climates and are formed in poorly draining lake basins. In contrast to fens, they derive most of their water from precipitation rather than mineral-rich ground or surface water. Water flowing out of bogs has a characteristic brown colour, which comes from dissolved peat tannins. In general, the low fertility and cool climate result in relatively slow plant growth, but decay is even slower due to low oxygen levels in saturated bog soils. Hence, peat accumulates. Large areas of the landscape can be covered many meters deep in peat.

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