A blanket bog is a very acidpeatbog, low in nutrients and extending widely over a flat terrain. They are found in cold wet climates. Research Blanket Bog
Bog is the name given to a piece of wet, soft, and spongy ground, where the soil is composed mainly of decaying and decayed vegetable matter. Such ground is valueless for agriculture until reclaimed, but often yields abundance of peat for fuel.
A bog seems usually to be formed as follows: A shallow pool induces the formation of aquatic plants, which gradually creep in from the borders to the deeper centre. Mud accumulates round their roots and stalks, and a semi-fluid mass is formed, well suited for the growth of moss, particularly Sphagnum, which now begins to luxuriate, continually absorbing water, and shooting out new plants above as the old decay beneath; these are consequently rotted, and compressed into a solid substance, gradually replacing the water by a mass of vegetable matter. A layer of clay, frequently found over gravel, assists the formation of bog by its power of retaining moisture. When the subsoil is very retentive, and the quantity of water becomes excessive, the superincumbent peat sometimes bursts forth and floats over adjacent lands.
Bogs are generally divided into two classes: red bogs, or peat-mosses, and black bogs, or mountain mosses. The former class are found in extensive plains frequently running through several counties, such as the Chatmoss in Lancashire, and the Bog of Alien in Ireland, the depth varying from 3.6 to 13 metres. Their texture is light and full of filaments, and is formed by the slow decay of mosses and plants of different kinds. The lower parts, being more entirely decayed, approach nearer to the nature of the humus than the upper portion, and, as being more carbonaceous, are more valuable for fuel. Black bog is formed by a more rapid decomposition of plants. It is heavier and more homogeneous in quality, but is usually found in limited and detached portions, and at high elevations where its reclamation is difficult.
In Ireland bogs frequently rest on a calcareous subsoil, which is of great value in reclaiming them. In the reclamation of bog land a permanent system of drainage must be established; the loose and spongy soil must be mixed with a sufficient quantity of mineral matter to give firmness to its texture and fertilize its superabundant humus; proper manures must be provided to facilitate the extraction of nutriment from the new soil, and a rotation of crops adopted suitable for bringing it into permanent condition. The materials best adapted for reclaiming peat are calcareousearths, limestonegravel, shell-marl, and shell-sand. Thoroughly reclaimed bogs are not liable to revert to their former condition. Trunks of trees are often found in bogs as are also bones of extinct animals. Research Bog
Andromeda is a genus of plants belonging to the heaths. One species, Andromeda polifolia, found in peat-bogs in Britain and elsewhere in Europe, is an acrid narcotic hurtful to sheep. Research Andromeda
The Beautiful Snout (Hypena crassalis) is a moth of the family Noctuidae with a wing span of between 25 and 30 mm distributed through northern and central Europe in wetlands, peat bogs and coniferous forests, flying from May to July. Research Beautiful Snout
The Beautiful Yellow Underwing (Anarta myrtilli) is a small moth of the family Noctuidae with a wing span of about 20 mm found mainly in peat-bogs in Europe and flies during the day. Research Beautiful Yellow Underwing
The Chevron moth (Eulithis testata) is a moth of the family Geometridae with a wing span of between 25 and 35 mm found in Europe, Asia and North America flying from July to September in damp meadows, peat-bogs and forests on peaty soil. Research Chevron Moth
Cranberry (Vacciniumoxycoccus) is a prostrate evergreen shrub of the natural order Vacciniaceae (whortleberry group) with oval leaves, red wheel-shaped corolla and red berries. It is native to Europe, north Asia and North America where it is extensively cultivated for its fruit. It is also called Moss-berry or Moor-berry, as it grows only on peat-bogs or swampy land, usually among masses of sphagnum. The berry, when ripe, is globose and dark red, and a little more than six millimetres in diameter. These berries form a sauce of exquisite flavour, and were originally used for tarts, before being used for an accompaniment to turkey and as a juice drink. The American cranberry, a native of Canada and the United States, has larger berries than the European species, and is extensively cultivated in some localities. Vaccinium vitis-idaea, the cowberry, is often called the cranberry in Scotland. Research Cranberry