Mire

A mire or quagmire, sometimes called a peatland, is a wetland terrain without forest cover, dominated by living, peat-forming plants. For botanists and ecologists, the term peatland is a more general term for any terrain dominated by peat to a depth of at least 30 cm (12 in), even if it has been completely drained (i.e., a peatland can be dry, but a mire by definition must be wet).

There are two types of mire: bogs and fens. A bog is a dome-shaped landform that protrudes above the surrounding landscape and obtains most of its water from rainfall (i.e., is ombrotrophic), while a fen is located on a slope, flat, or depression and gets its water from both rainfall and surface water. Also, while a bog is always acidic and nutrient-poor, a fen may be slightly acidic, neutral, or alkaline, and either nutrient-poor or nutrient-rich.

A mire is distinguished from a swamp by its lack of a forest canopy; although some bogs may support limited tree or bush growth, mires are dominated by grass and mosses. A mire is distinguished from a marsh by its water nutrients and distribution: marshes are characterized by nutrient-rich stagnant or slow-moving waters while mire waters are located mostly below the soil surface level. A mire is also distinguished from a marsh by its plant life: marsh plants are generally submerged or floating-leaved while those in a mire are not.

Relying on rainwater for nutrient input, mires are usually deficient in both nitrogen and phosphorus and may vary widely with regard to nitrogen. These characteristics mean that mires are a kind of "...living relic... [A] living skin on an ancient body" in which successive layers of regular plant growth and decay are preserved stratigraphically with a quality of preservation unknown in other wetland environments.