OpenLLM-France/wikimedia huggingface dataset:
# 1911 Encyclopædia Britannica/Lappenberg, Johann Martin

See also Johann Martin Lappenberg on Wikipedia; and our 1911 Encyclopædia Britannica disclaimer.
​LAPPENBERG, JOHANN MARTIN (1794–1865), German historian, was born on the 30th of July 1794 at Hamburg, where his father, Valentin Anton Lappenberg (1759–1819), held an official position. He studied medicine, and afterwards history, at Edinburgh. He continued to study history in London, and at Berlin and Göttingen, graduating as doctor of laws at Göttingen in 1816. In 1820 he was sent by the Hamburg senate as resident minister to the Prussian court. In 1823 he became keeper of the Hamburg archives; an office in which he had the fullest opportunities for the laborious and critical research work upon which his reputation as an historian rests. He retained this post until 1863, when a serious affection of the eyes compelled him to resign. In 1850 he represented Hamburg in the German parliament at Frankfort, and his death took place at Hamburg on the 28th of November 1865. Lappenberg’s most important work is his Geschichte von England, which deals with the history of England from the earliest times to 1154, and was published in two volumes at Hamburg in 1834–1837. It has been translated into English by B. Thorpe as History of England under the Anglo-Saxon Kings (London 1845, and again 1881), and History of England under the Norman Kings (Oxford, 1857), and has been continued in three additional volumes from 1154 to 1509 by R. Pauli. His other works deal mainly with the history of Hamburg, and include Hamburgische Chroniken in Niedersächsischer Sprache (Hamburg, 1852–1861); Geschichtsquellen des Erzstiftes und der Stadt Bremen (Bremen, 1841); Hamburgisches Urkundenbuch (Hamburg, 1842); Urkundliche Geschichte des Hansischen Stahlhofes zu London (Hamburg, 1851); Hamburgische Rechtsalterthümer (Hamburg, 1845); and Urkundliche Geschichte des Ursprunges der deutschen Hanse (Hamburg, 1830), a continuation of the work of G. F. Sartorius. For the Monumenta Germaniae historica he edited the Chronicon of Thietmar of Merseburg, the Gesta Hammenburgensis ecclesiae pontificum of Adam of Bremen and the Chronica Slavorum of Helmold, with its continuation by Arnold of Lübeck. Lappenberg, who was a member of numerous learned societies in Europe, wrote many other historical works.
See E. H. Meyer, Johann Martin Lappenberg (Hamburg, 1867); and R. Pauli in the Allgemeine deutsche Biographie, Band xvii. (Leipzig, 1883).
# 1911 Encyclopædia Britannica/Lapparent, Albert Auguste Cochon de

See also Albert Auguste Cochon de Lapparent on Wikipedia; and our 1911 Encyclopædia Britannica disclaimer.
​LAPPARENT, ALBERT AUGUSTE COCHON DE (1839–1908), French geologist, was born at Bourges on the 30th of December 1839. After studying at the École Polytechnique from 1858 to 1860 he became ingénieur au corps des mines, and took part in drawing up the geological map of France; and in 1875 he was appointed professor of geology and mineralogy at the Catholic Institute, Paris. In 1879 he prepared an important memoir for the geological survey of France on Le Pays de Bray, a subject on which he had already published several memoirs, and in 1880 he served as president of the French Geological Society. In 1881–1883 he published his Traité de géologie (5th ed., 1905), the best European text-book of stratigraphical geology. His other works include Cours de minéralogie (1884, 3rd ed., 1899), La Formation des combustibles minéraux (1886), Le Niveau de la mer et ses variations (1886), Les Tremblements de terre (1887), La Géologie en chemin de fer (1888), Précis de minéralogie (1888), Le Siècle du fer (1890), Les Anciens Glaciers (1893), Leçons de géographie physique (1896), Notions générales sur l’écorce terrestre (1897), Le Globe terrestre (1899), and Science et apologétique (1905). With Achille Delesse he was for many years editor of the Révue de géologie and contributed to the Extraits de géologie, and he joined with A. Potier in the geological surveys undertaken in connexion with the Channel Tunnel proposals. He died in Paris on the 5th of May 1908.
# 1911 Encyclopædia Britannica/Lappa

See also Lapa Island on Wikipedia; and our 1911 Encyclopædia Britannica disclaimer.
​LAPPA, an island directly opposite the inner harbour of Macao, the distance across being from 1 to 11/2 m. It is a station of the Chinese imperial maritime customs which collects duties on vessels trading between China and the Portuguese colony ​of Macao. The arrangement is altogether abnormal, and was consented to by the Portuguese government in 1887 to assist the Chinese authorities in the suppression of opium smuggling. A similar arrangement prevails at the British colony of Hong-Kong, where the Chinese customs station is Kowloon. In both cases the customs stations levy duties on vessels entering and leaving the foreign port in lieu of levying them, as ought to be done, on entering or leaving a Chinese port.
# 1911 Encyclopædia Britannica/Lar

See also Lar, Iran on Wikipedia; and our 1911 Encyclopædia Britannica disclaimer.
​LAR, a city of Persia, capital of Laristan, in 27° 30′ N., 53° 58′ E., 180 m. from Shiraz and 75 from the coast at Bander Lingah. It stands at the foot of a mountain range in an extensive plain covered with palm trees, and was once a flourishing place, but a large portion is in ruins, and the population which early in the 18th century numbered 50,000 is reduced to 8000. There are still some good buildings, of which the most prominent are the old bazaar consisting of four arcades each 180 ft. long, 14 broad and 22 high, radiating from a domed centre 30 ft. high, an old stone mosque and many cisterns. The crest of a steep limestone hill immediately behind the town and rising 150 ft. above the plain is crowned by the ruins of a castle formerly deemed impregnable. Just below the castle is a well sunk 200 ft. in the ​rock. The tower-flanked mud wall which surrounds the town is for the most part in ruins.
# 1911 Encyclopædia Britannica/Lapse

See also Lapse and anti-lapse on Wikipedia; and our 1911 Encyclopædia Britannica disclaimer.
​LAPSE (Lat. lapsus, a slip or departure), in law, a term used in several senses. (1) In ecclesiastical law, when a patron has neglected to present to a void benefice within six months next after the avoidance, the right of presentation is said to lapse. In such case the patronage or right of presentation devolves from the neglectful patron to the bishop as ordinary, to the metropolitan as superior and to the sovereign as patron paramount. (2) The failure of a testamentary disposition in favour of any person, by reason of the decease of its object in the testator’s lifetime, is termed a lapse. See Legacy, Will.
# 1911 Encyclopædia Britannica/Lapworth, Charles

See also Charles Lapworth on Wikipedia; and our 1911 Encyclopædia Britannica disclaimer.
​LAPWORTH, CHARLES (1842– ), English geologist, was born at Faringdon in Berkshire on the 30th of September 1842. He was educated partly in the village of Buckland in the same county, and afterwards in the training college at Culham, near Oxford (1862–1864). He was then appointed master in a school connected with the Episcopal church at Galashiels, where he remained eleven years. Geology came to absorb all his leisure time, and he commenced to investigate the Silurian rocks of the Southern Uplands, and to study the graptolites and other fossils which mark horizons in the great series of Lower Palaeozoic rocks. His first paper on the Lower Silurian rocks of Galashiels was published in 1870, and from that date onwards he continued to enrich our knowledge of the southern uplands of Scotland until the publication by the Geological Society of his masterly papers on The Moffat Series (1878) and The Girvan Succession (1882). Meanwhile in 1875 he became an assistant master in the Madras College, St Andrews, and in 1881 professor of geology and mineralogy (afterwards geology and physiography) in the Mason College, now University of Birmingham. In 1882 he started work in the Durness-Eriboll district of the Scottish Highlands, and made out the true succession of the rocks, and interpreted the complicated structure which had baffled most of the previous observers. His results were published in “The Secret of the Highlands” (Geol. Mag., 1883). His subsequent work includes papers on the Cambrian rocks of Nuneaton and the Ordovician rocks of Shropshire. The term Ordovician was introduced by him in 1879 for the strata between the base of the Lower Llandovery formation and that of the Lower Arenig; and it was intended to settle the confusion arising from the use by some writers of Lower Silurian and by others of Upper Cambrian for the same set of rocks. The term Ordovician is now generally adopted. Professor Lapworth was elected F.R.S. in 1888, he received a royal medal in 1891, and was awarded the Wollaston medal by the Geological Society in 1899. He was president of the Geological Society, 1902–1904. His Intermediate Text-book of Geology was published in 1899.
See article, with portrait and bibliography, in Geol. Mag. (July 1901).
# 1911 Encyclopædia Britannica/Float

See also Float on Wikipedia; and our 1911 Encyclopædia Britannica disclaimer.
​FLOAT (in O. Eng. flot and flota, in the verbal form fléotan; the Teutonic root is flut-, another form of flu-, seen in “flow,” cf. “fleet”; the root is seen in Gr. πλέειν, to sail, Lat. pluere, to rain; the Lat. fluere and fluctus, wave, is not connected), the action of moving on the surface of water, or through the air. The word is used also of a wave, or the flood of the tide, river, backwater or stream, and of any object floating in water, as a mass of ice or weeds; a movable landing-stage, a flat-bottomed boat, or a raft, or, in fishing, of the cork or quill used to support a baited line or fishing-net. It is also applied to the hollow or inflated organ by means of which certain animals, such as the “Portuguese man-of-war,” swim, to a hollow metal ball or piece of whinstone, &c., used to regulate the level of water in a tank or boiler, and to a piece of ivory in the cistern of a barometer. “Float” is also the name of one of the boards of a paddle-wheel or water-wheel. In a theatrical sense, it is used to denote the footlights. The word is also applied to something broad, level and shallow, as a wooden frame attached to a cart or wagon for the purpose of increasing the carrying capacity; and to a special kind of low, broad cart for carrying heavy weights, and to a platform on wheels used for shows in a procession. The term is applied also to various tools, especially to many kinds of trowels used in plastering. It is also used of a dock where vessels may float, as at Bristol, and of the trenches used in “floating” land. In geology and mining, loose rock or ore brought down by water is known as “float,” and in tin-mining it is applied to a large trough used for the smelted tin. In weaving the word is used of the passing of weft threads over part of the warp without being woven in with it, also of the threads so passed. In the United States a voter not attached to any particular party and open to bribery is called a “float” or “floater.”
# 1911 Encyclopædia Britannica/Flood

See also Flood on Wikipedia; and our 1911 Encyclopædia Britannica disclaimer.
​FLOOD (in O. Eng. flód, a word common to Teutonic languages, cf. Ger. Flut, Dutch vloed, from the same root as is seen in “flow,” “float”), an overflow of water, an expanse of water submerging land, a deluge, hence “the flood,” specifically, the Noachian deluge of Genesis, but also any other catastrophic submersion recorded in the mythology of other nations than the Hebrew (see Deluge, The). In the sense of “flowing water,” the word is applied to the inflow of the tide, as opposed to “ebb.”
# 1911 Encyclopædia Britannica/Floor

See also floor on Wiktionary; and our 1911 Encyclopædia Britannica disclaimer.
​FLOOR (from O. Eng. flor, a word common to many Teutonic languages, cf. Dutch vloer, and Ger. Flur, a field, in the feminine, and a floor, masculine), generally the lower horizontal surface of a room, but specially employed for one covered with boarding or parquetry. The various levels of rooms in a house are designated as “ground-floor,” “first-floor,” “mezzanine-floor,” &c. The principal floor is the storey which contains the chief apartments whether on the ground- or first-floor; in Italy they are always on the latter and known as the “piano nobile.” The storey below the ground-floor is called the “basement-floor,&rdqrdquo; even if only a little below the level of the pavement outside; the storey in a roof is known as the “attic-floor.” The expressions one pair, two pair, &c., apply to the storeys above the first flight of stairs from the ground (see also Carpentry).
# 1911 Encyclopædia Britannica/Flock

See also Flock on Wikipedia; and our 1911 Encyclopædia Britannica disclaimer.
​FLOCK. 1. (A word found in Old English and Old Norwegian, from which come the Danish and Swedish words, and not in other Teutonic languages), originally a company of people, now mainly, except in figurative usages, of certain animals when gathered together for feeding or moving from place to place. For birds it is chiefly used of geese; and for other animals most generally of sheep and goats. It is from the particular application of the word to sheep that “flock” is used of the Christian Church in its relation to the “Good Shepherd,” and also of a congregation of worshippers in its relation to its spiritual head.
2. (Probably from the Lat. floccus, but many Teutonic languages have the same word in various forms), a tuft of wool, cotton or similar substance. The name “flock” is given to a material formed of wool or cotton refuse, or of shreds of old woollen or cotton rags, torn by a machine known as a “devil.” This material is used for stuffing mattresses or pillows, and also in upholstery. The name is also applied to a special kind of wall-paper, which has an appearance almost like cloth, or, in the more expensive kinds, of velvet. It is made by dusting on a specially prepared adhesive surface finely powdered fibres of cotton or silk. The word “flocculent” is used of many substances which have a fleecy or “flock”-like appearance, such as a precipitate of ferric hydrate.
# 1911 Encyclopædia Britannica/Flodoard

See also Flodoard on Wikipedia; and our 1911 Encyclopædia Britannica disclaimer.
​FLODOARD (894–966), French chronicler, was born at Epernay, and educated at Reims in the cathedral school which had been established by Archbishop Fulcon (822–900). As canon of Reims, and favourite of the archbishops Herivaeus (d. 922) and Seulfus (d. 925), he occupied while still young an important position at the archiepiscopal court, but was twice deprived of his benefices by Heribert, count of Vermandois, on account of his steady opposition to the election of the count’s infant son to the archbishopric. Upon the final triumph of Archbishop Artold in 947, Flodoard became for a time his chief adviser, but withdrew to a monastery in 952, and spent the remaining years of his life in literary and devotional work. His history of the cathedral church at Reims (Historia Remensis Ecclesiae) is one of the most remarkable productions of the 10th century. Flodoard had been given charge of the episcopal archives, and constructed his history out of the original texts, which he generally reproduces in full; the documents for the period of Hincmar being especially valuable. The Annales which Flodoard wrote year by year from 919 to 966 are doubly important, by reason of the author’s honesty and the central position of Reims in European affairs in his time. Flodoard’s poetical works are of hardly less historical interest. The long poem celebrating the triumph of Christ and His saints was called forth by the favour shown him by Pope Leo VII., during whose pontificate he visited Rome, and he devotes fourteen books to the history of the popes.
Flodoard’s works were published in full by J. P. Migne (Patrologia Latina, vol. 135); a modern edition of the Annales is the one edited by P. Lauer (Paris, 1906). For bibliography see A. Molinier, Sources de l’histoire de France (No. 932).
# 1911 Encyclopædia Britannica/Floe

See also Floe on Wikipedia; and our 1911 Encyclopædia Britannica disclaimer.
​FLOE (of uncertain derivation; cf. Norse flo, layer, level plain), a sheet of floating ice detached from the main body of polar ice. It is of less extent than the field of “pack” ice, which is a compacted mass of greater depth drifting frequently under the influence of deep currents, while the floating floe is driven by the wind.
# 1911 Encyclopædia Britannica/Flodden

See also Battle of Flodden on Wikipedia; and our 1911 Encyclopædia Britannica disclaimer.
​FLODDEN, or Flodden Field, near the village of Branxton, in Northumberland, England (10 m. N.W. of Wooler), the scene of a famous battle fought on the 9th of September 1513 between the English and the Scots. On the 22nd of August a great Scottish army under King James IV. had crossed the border. For the moment the earl of Surrey (who in King Henry VIII.’s absence was charged with the defence of the realm) had no organized force in the north of England, but James wasted much precious time among the border castles, and when Surrey appeared at Wooler, with an army equal in strength to his own, which was now greatly weakened by privations and desertion, he had not advanced beyond Ford Castle. The English commander promptly sent in a challenge to a pitched battle, which the king, in spite of the advice of his most trusted counsellors, accepted. On the 6th of September, however, he left Ford and took up a strong position facing south, on Flodden Edge. Surrey’s reproaches for the alleged breach of faith, and a second challenge to fight on Millfield Plain were this time disregarded. The English commander, thus foiled, executed a daring and skilful march round the enemy’s flank, and on the 9th drew up for battle in rear of the hostile army. It is evident that Surrey was confident of victory, for he placed his own army, not less than the enemy, in a position where defeat would involve utter ruin. On his appearance the Scots hastily changed front and took post on Branxton Hill, facing north. The battle began at 4 p.m. Surrey’s archers and cannon soon gained the upper hand, and the Scots, unable quietly to endure their losses, rushed to close quarters. Their left wing drove the English back, but Lord Dacre’s reserve corps restored the fight on this side. In all other parts of the field, save where James and Surrey were personally opposed, the English gradually gained ground. The king’s corps was then attacked by Surrey in front, and by Sir Edward Stanley in flank. As the Scots were forced back, a part of Dacre’s force closed upon the other flank, and finally Dacre himself, boldly neglecting an almost intact Scottish division in front of him, charged in upon the rear of King James’s corps. Surrounded and attacked on all sides, this, the remnant of the invading army, was doomed. The circle of spearmen around the king grew less and less, and in the end James and a few of his nobles were alone left standing. Soon they too died, fighting to the last man. Among the ten thousand Scottish dead were all the leading men in the kingdom of Scotland, and there was no family of importance that had not lost a member in this great disaster. The “King’s Stone,” said to mark the spot where James was killed, is at some distance from the actual battlefield. “Sybil’s Well,” in Scott’s Marmion, is imaginary.
# 1911 Encyclopædia Britannica/Floorcloth

See also Floorcloth, Kamptulicon, Oilcloth and Linoleum on Wikipedia; and our 1911 Encyclopædia Britannica disclaimer.
​FLOORCLOTH, a rough flannel cloth used for domestic cleaning; also a generic term applied to a variety of materials used in place of carpets for covering floors, and known by such trade names as kamptulicon, oil-cloth, linoleum, corticine, cork-carpet, &c. Kamptulicon (καμπτός, flexible, οὐλος, thick) was patented in 1844 by E. Galloway, but did not attract much attention till about 1862. It was essentially a preparation of india-rubber masticated up with ground cork, and rolled out into sheets between heavy steam-heated rollers, sometimes over a backing of canvas. Owing to its expensiveness, it has given place to cheaper materials serving the same purpose. Oil-cloth is a coarse canvas which has received a number of coats of thick oil paint, each coat being rubbed smooth with pumice stone before the application of the next. Its surface is ornamented with patterns printed in oil colours by means of wooden blocks. Linoleum (linum, flax, oleum, oil), patented by F. Walton in 1860 and 1863, consists of oxidized linseed oil and ground cork. These ingredients, thoroughly incorporated with the addition of certain gummy and resinous matters, and of pigments such as ochre and oxide of iron as required, are pressed on to a rough canvas backing between steam-heated rollers. Patterns may be printed on its surface with oil paint, or by an improved method may be inlaid with coloured composition so that the colours are continuous through the thickness of the linoleum, instead of being on the surface only, and thus do not disappear with wear. Lincrusta-Walton is a similar material to linoleum, also having oxidized linseed oil as its base, which is stamped out in embossed patterns and used as a covering for walls.