Alluvium is river transported deposits of mud, sand and gravel that accumulate to form distinctive features such as levees, flood plains and deltas. Research Alluvium
A bar was a British baker's unit of measurement equivalent to 196 lbs.
In law, a bar is the railing that encloses the place which council occupy in courts of justice; hence the phrase, at the bar of the court, that is, in open court. Hence also persons duly admitted as pleaders or advocates before the courts of England are denominated barristers , and the whole body of such barristers or advocates are called the bar. The enclosed place or dock in which persons accused of crimes stand in court is also called the bar. Near the door of both houses of Parliament there is also a bar, beyond which none but the members and clerks are admitted, and at which counsel, witnesses, offenders against privilege, etc, are heard.
Bath is the immersion of the body in water, or an apparatus for this purpose. The use of the bath as an institution apart from occasional immersion in rivers or the sea, is, as might be anticipated, an exceedingly old custom. Homer mentions the bath as one of the first refreshments offered to a guest; thus, when Ulysses enters the palace of Circe, a bath is prepared for him, and he is anointed after it with costly perfumes. No representation, however, of a bath as we understand it is given upon the Greek vases, bathers being represented either simply washing at an elevated basin, or having water poured over them from above. In later times, rooms, both public and private, were built expressly for bathing, the public baths of the Greeks being mostly connected with the gymnasia. Apparently, by an inversion of the later practice, it was customary in the Homeric epoch to take first a cold and then a hot bath; but the Lacedemonians substituted the hot-air sudorific bath, as less enervating than warm water, and in Athens at the time of Demosthenes and Socrates the warm bath was considered by the more rigorous as an effeminate custom.
The fullest details we have with respect to the bathing of the ancients apply to its luxurious development under the Romans. Their bathing establishments consisted of four main sections: the undressing room, with an adjoining chamber in which the bathers were anointed; a cold room with provision for a cold bath; a room heated moderately to serve as a preparation for the highest and lowest temperatures; and the sweating-room, at one extremity of which was a vapour-bath and at the other an ordinary hot bath. After going through the entire course both the Greeks and Romans made use of strigils or scrapers, either of horn or metal, to remove perspiration, oil, and impurities from the skin. Connected with the bath were walks, covered race-grounds, tennis-courts, and gardens, the whole, both in the external and internal decorations, being frequently on a palatial scale. The group of the Laocoon and the Parnese Hercules were both found in the ruins of Roman baths.
With respect to modern baths, that commonly in use in Russia consists of a single hall, built of wood, in the midst of which is a powerful metal oven, covered with heated stones, and surrounded with broad benches, on which the bathers take their places. Cold water is then poured upon the heated stones, and a thick, hot steam rises, which causes the sweat to issue from the whole body. The bather is then gently whipped with wet birch rods, rubbed with soap, and washed with lukewarm and cold water; of the latter, some pailfuls are poured over his head; or else he leaps, immediately after this sweating-bath, into a river or pond, or rolls in the snow.
The Turks, by their religion, are obliged to make repeated ablutions daily, and for this purpose there is, in every city, a public bath connected with a mosque. A favourite bath among them, however, is a modification of the hot-air sudorific-bath of the ancients introduced under the name of Turkish Bath into other than Islamic countries. A regular accompaniment of this bath, when properly given, is the operation known as 'kneading,' or massage, generally performed at the close of the sweating process, after the final rubbing of the bather with soap, and consisting in a systematic pressing and squeezing of the whole body, stretching the limbs, and manipulating all the joints as well as the fleshy and muscular parts.
Public baths were common in Europe during the late 19th century, but the first English public baths and wash-houses of the kind common in all cities during the late 19th century were established in Liverpool and near the London docks in 1844. In 1846 an act was passed for their encouragement, and a Baths and Wash-houses Act of 1878 authorized the establishment of cheap swimming-baths.
The principal natural warm baths in England are at Bath in Somersetshire (the hottest), and Brixton and Matlock in Derbyshire. The temperature of the Bath springs ranges from 109 to 117 degrees, while that of the Buxton and Matlockwaters scarcely exceeds 82 degrees. The baths of Harrogate, which are strongly impregnated with sulphuretted hydrogen gas, are also of great repute for the cure of obstinate cutaneous diseases, indurations of the glands, etc. The most celebrated natural hot baths in Europe are those of Aix-la-Chapelle, and the various Baden in Germany; Toeplitz, in Bohemia; Bagnieres, Bareges, and Dax, in the south of France; and Spa, in Belgium. Besides the various kinds of water-bath with or without medication or natural mineral ingredients, there are also milk, oil, wine, earth, sand, mud, and electric baths, smoke-baths and gas-baths; but these are as a rule only indulged after specific prescription.
The practice of bathing as a method of cure in cases of disease falls under the head of hydrotherapathy; in the 19th century it was advised that even when bathing was employed simply for pleasure or purification due regard should be paid to the physiological condition of the bather. During the Victorian era in Britain writers were concerned about the potential dangers of bathing, and one warned:
'in many cases cold bathing should be avoided altogether, especially by those who have any tendency to spitting of blood or consumption, by gouty people, or by those who have any latent visceral disease or apoplectic tendency. Wherever the bath is followed by shivering instead of by a healthy reactionary glow, it is undesirable; and a cold bath in the morning after any debauchery or excess in eating or drinking on the previous evening is exceedingly imprudent. Delicate persons and children ought not to bathe in the sea before ten or eleven o'clock in the morning, and in no case should bathing be indulged after a long fast. In cold streams and rivers additional precautions should be taken, the cold plunge, when heated or fatigued, being frequently attended with fatal results. Even warm baths are not wholly free from danger; apoplexy and death having been known to follow a hot bath when entered with a full stomach. As a rule the temperature should not exceed 105 degrees, and they should not be too long continued. Frequent indulgence in them has an enervating effect, though the majority of people need as yet no renewal of Hadrian's prohibitive legislation in this matter.'
The eminent author, George Black, in 1892, while generally encouraging bathing, and describing bathing as 'likely to be of excellent use and efficacy both in the prevention and cure of disease.' Also went on to warn:
'Baths should never be taken immediately after a meal, nor when the body is very much exhausted by fatigue or excitement of any kind, nor during nor just before menstruation; and they should be sparingly and guardedly used by pregnant women.' Research Bath
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
Dredging is a term applied to the operation of removing mud, silt, and other deposits from the bottom of harbours, canals, rivers, docks, etc. The most simple dredging apparatus is the spoon apparatus, which consists of a strong iron ring or hoop, properly formed for making an impression upon the soft matter at the bottom, so as to scoop it into a large bag attached to the ring and perforated with a number of small holes. The means for working it is a long handle, a suspending rope, and a crane or sweep-pole planted in a boat.
Much more effective was the steam dredging-machine that became common during the 19th century. It had a succession of strong iron buckets on an endless chain, which traversed on a frame whose lower end was vertically adjustable so as to regulate the depth at which it worked. It was worked by steam, and the buckets tore up the matter at the bottom, raised it, and discharge it into punts or hoppers close to the dredging vessel. Various forms of steam - pump dredgers, in which suction-pipes were the chief features, were also used.
The river Clyde, from being a shallow stream, was converted, mainly by dredging, into a waterway carrying large vessels up to Glasgow.
Dredging rivers for gold has been largely carried on since the 19th century; and the gold-dredge may even be floated in water artificially supplied.
Dredging is also the operation of dragging the bottom of the sea for molluscs, plants, and other objects, it may be for scientific observation. The oyster-dredge is a light iron frame with a scraper like a narrow hoe on one side, and a bag attached to receive the oysters. The dredges used by naturalists are mostly modifications of or somewhat similar to the oyster-dredge. Scientific dredging assumed a high importance at the end of the 19th century for research into the life of deep-sea areas, before the invention of deep-sea diving equipment and cameras. Research Dredging
A floating island is an island formed in a lake or other inland water, consisting generally of a mass of earth held together by interlacing roots. Sometimes such islands are large enough to serve as pasture grounds. Artificial floating islands have been formed by placing lakemud on rafts of wicker-work covered with reeds. Research Floating Island
Warping is a mode of increasing the fertility of land along the banks of rivers liable to overflow by allowing them to deposit their mud, called ' warp', upon the surface overflown. Research Warping
An alligator is a genus of crocodilian reptile of the family Alligatoridae. They differ from the true crocodiles in having a shorter and flatter head, in having cavities or pits in the upper jaw, into which the long canine teeth of the under jaw fit, and in having the feet much less webbed. Their habits are less perfectly aquatic. They are confined to the warmer parts of America, where they frequent swamps and marshes, and may be seen basking on the dry ground during the day in the heat of the sun. They are most active during the night, when they make a loud bellowing. The largest of these animals grow to the length of about six metres. They are covered by a dense armour of horny scales, and have a huge mouth, armed with strong, conical teeth. They swim with wonderful celerity, impelled by their long, laterally-compressed, and powerful tails. On land their motions are proportionally slow and embarrassed because of the length and un-wieldiness of their bodies and the shortness of their limbs.
Alligators feed on fish, and any small animals or carrion, and sometimes catch pigs on the shore, or dogs which are swimming. They even sometimes make man their prey. In winter they burrow in the mud of swamps and marshes, lying torpid until the warm weather. The female lays a great number of eggs, which are deposited in the sand or mud, and left to be hatched by the heat of the sun, but the mother alligator is very attentive to her young. The most fierce and dangerous species is that found in the southern parts of the United States Alligator Lucius, having the snout a little turned up, slightly resembling that of the pike. The alligators of South America are there very often called Caymans. Alligator sclerops is known also as the Spectacled Cayman, from the prominent bony rim surrounding the orbit of each eye. The flesh of the alligator is sometimes eaten. Among the fossils of the south of England are remains of a true alligator Alligator Hantoniensis in the Eocene beds of the Hampshire basin. Research Alligator More pictures of Alligator
Angler is any of an order of fishes Lophiiformes, with flattened body and broad head and jaws. Many species have small, plant-like tufts on their skin. These act as camouflage for the fish as it waits, either floating among seaweed or lying on the sea bottom, twitching the enlarged tip of the threadlike first ray of its dorsal fin to entice prey. There are over 200 species of angler fish, living in both deep and shallow water in temperate and tropical seas. The males of some species have become so small that they live as parasites on the females.
The British species, Lophius piscatorius is also from its habits and appearance called the Fishing-frog and Sea-devil. It is a remarkable fish often coasts. It is from 1 to 1.5 metres long; the head is very wide, depressed, with protuberances, and bearing long separate movable tendrils; the mouth is capacious, and armed with formidable teeth. Its voracity is extreme, and it is said to lie concealed in the mud, and attract the smaller fishes within its reach by gently waving the filamentous appendages on its head. Research Angler
The Probert Encyclopaedia was designed, edited and programed by
Matt and Leela Probert
Abbreviations
Research Alluvium
