was as fond of acting as Goethe, and like him began with a puppet | exceptional circumstances, to put duty before inclination and to stage, succeeded by amateur theatricals, the chief entertainment provided for her guests at Nohant. Undaunted by many failures, she dramatized several of her novels with moderate successFrançois le champi, played at the Odéon in 1849, and Les Beaux Messieurs de Bois-Doré (1862) were the best;.Claudie, produced in 1851, is a charming pastoral play, and Le Marquis de Villemer (1864) (in which she was helped by Dumas fils) was a genuine triumph. Her statue by Clésinger was placed in the foyer of the Théâtre Français in 1877. Of George Sand's style a foreigner can be but an imperfect judge, but French critics, from Sainte-Beuve, Nisard and Caro down to Jules Lemaître and Faguet, have agreed to praise her spontaneity, her correctness of diction, her easy opulence-the lactea uberlas that Quintilian attributes to Livy. The language of her country novels is the genuine patois of middle France rendered in a literary form. Thus in La Petite Fadette, by the happy device of making the hemp dresser the narrator, she speaks (to quote Sainte-Beuve) as though she had on her right the unlettered rustic and on her left a member of the Académie, and made herself the interpreter between the two. She hits the happy mean between the studied archaism of Courier's Daphnis et Cloe and the realistic patois of the later kailyard novel which for Southerners requires a glossary. Of her style generally the characteristic quality is fluidity. She has all the abandon of an Italian improvisatore, the simplicity of a Bernardin de St Pierre without his mawkishness, the sentimentality of a Rousseau without his. egotism, the rhythmic eloquence of a Chateaubriand without his grandiloquence. uphold the reign of law and order. Both passed through phases of faith, but while even Positivism did not cool George Eliot's innate religious fervour, with George Sand religion was a passing experience, no deeper than her republicanism and less lasting than her socialism, and she lived and died a gentle savage. Rousseau's Confessions was the favourite book of both (as it was of Emerson), but George Eliot was never converted by the high priest of sentimentalism into a belief in human perfectibility and a return to nature. As a thinker George Eliot is vastly superior; her knowledge is more profound and her psychological analysis subtler and more scientific. But as an artist, in unity of design, in harmony of treatment, in purity and simplicity of language, so felicitous and yet so unstudied, in those qualities which make the best of George Sand's novels masterpieces of art, she is as much her inferior. Mr Francis Gribble has summed up her character in" a scornful, insular way" as a light woman. A truer estimate is that of Sainte-Beuve, her intimate friend for more than thirty years, but never her lover. "In the great crises of action her intellect, her heart and her temperament are at one. She is a thorough woman, but with none of the pettinesses, subterfuges, and mental reservations of her sex; she loves wide vistas and boundless horizons and instinctively seeks them out; she is concerned for universal happiness and takes thought for the improvement of mankind-the last infirmity and most innocent mania of generous souls. Her works are in very deed the echo of our times. Wherever we were wounded and stricken her heart bled in sympathy, and all our maladies and miseries evoked from her a lyric wail." plus de calme," was her last prayer, and her dying words, " Ne détruisez pas la verdure." As a painter of nature she has much in common with Words- George Sand died at Nohant on the 8th of June 1876. To worth. She keeps her eye on the object, but adds, like Words- a youth and womanhood of storm and stress had succeeded an worth, the visionary gleam, and receives from nature but what old age of serene activity and then of calm decay. Her nights she herself gives. Like Wordsworth she lays us on the lap of were spent in writing, which seemed in her case a relaxation from earth and sheds the freshness of the early world. She, too, had the real business of the day, playing with her grandchildren, found love in huts where poor men dwell, and her miller, her gardening, conversing with her visitors-it might be Balzac bagpipers, her workers in mosaic are as faithful renderings in or Dumas, or Octave Feuillet or Matthew Arnold-or writing prose of peasant life and sentiment as Wordsworth's leech-long letters to Sainte-Beuve and Flaubert. "Calme, toujours gatherer and wagoners and gleaners are in verse. Her psychology is not subtle or profound, but her leading characters are clearly conceived and drawn in broad, bold outlines. No one has better understood or more skilfully portrayed the artistic temperament-the musician, the actor, the poet-and no French writer before her had so divined and laid bare the heart of a girl. She works from within outwards, touches first the mainspring and then sets it to play. As Mr Henry James puts it, she interviews herself. Rarely losing touch of earth, and sometimes of the earth earthy, she is still at heart a spiritualist. Her final word on herself rings true, "Toujours tourmentée des choses divines." Unlike Victor Hugo and Balzac, she founded no school, though Fromentin, Theuriet, Cherbuliez, Fabre and Bazin might be claimed as her collateral descendants. In Russia her influence has been greater. She directly inspired Dostoievski, and Turgenieff owes much to her. In England she has found her warmest admirers. Elizabeth Barrett Browning wrote sonnets to "the large-brained woman and large-hearted man, self-named George Sand." To Thackeray her diction recalled the sound of village bells falling sweetly and softly on the ear, and it sent a shiver through John Stuart Mill, like a symphony of Haydn or Mozart. Leslie Stephen advised Thomas Hardy, then an aspiring contributor to the Cornhill, to read George Sand, whose country stories seemed to him perfect. The harmony and grace, even if strictly inimitable, are good to aim at." He pronounced the Histoire de ma vie about the best biography he had ever read. F. W. H. Myers claimed her as anima naturaliter Christiana and the inspired exponent of the religion of the future. George Eliot by her very name invites and challenges com. parison with George Sand. But it was as a humble follower, not as a rival, that she took George Sand as sponsor. Both women broke with social conventions, but while George Sand (if the expression may be allowed) kicked over the traces, George Eliot was impelled all the more emphatically, because of her BIBLIOGRAPHY.-The collected edition of George Sand's works was published in Paris (1862-1883) in 96 volumes, with supplement 109 volumes; the Histoire de ma vie appeared in 20 volumes in 1854-1855. The Etude bibliographique sur les œuvres de George Sand by "le bibliophile Isaac" (vicomte de Spoelberck) (Brussels, 1868) gives the most complete bibliography. Of Vladimir Karenin's (pseudonym of Mme Komarova) George Sand, the most complete life, the first two volumes (1899-1901) carry the life down to 1839. There is much new material in George Sand et sa fille, by S. Rocheblaye (1905), Correspondance de G. Sand et d'Alfred de Musset (Brussels, 1904). Correspondance entre George Sand et Gustave Flaubert (1904), and Lettres à Alfred de Musset et à Sainte-Beuve (1897). E. M. Caro's George Sand (1887) is rather a critique than a life. Lives by Mire court (1855) and by Haussonville (1878) may also be consulted. Of the numerous shorter studies may be mentioned those of SainteBeuve in the Causeries du lundi and in Portraits contemporains; Jules Lemaitre in Les Contemporains, vol. iv.; E. Faguet, XIX Siècle; F. W. H. Myers, Essays Ancient and Modern (1883); Henry James in North American Review (April 1902); Matthew Arnold, Mixed Essays (1879). See also René Doumic's George Sand (1909), which has been translated into English by Alys Hallard as George (F. S.) Sand: Some Aspects of her Life and Writings (1910). SAND. When rocks or minerals are pulverized by any agencies, natural or artificial, the products may be classified as gravels, sands and muds or clays, according to the size of the individual particles. If the grains are so fine as to be impalpable (about in. in diameter) the deposit may be regarded as a mud or clay; if many of them are as large as peas the rock is a gravel. Sands may be uniform when they have been sorted out by some agency such as a gentle current of water or the wind blowing steadily across smooth arid lands, but usually they vary much both in the coarseness of their grains and in their mineral composition. The great source of natural sands is the action of the atmosphere, frost, rain, plants and other agencies in breaking up the surfaces of rocks and reducing them to the condition of fine powder; in other words sands are ordinarily the product of the agencies of denudation operating on the rocks of the earth's crust. Not all, however, are of this kind, for a few are artificial, like the crushed tailings produced in the extractions of metals from their ores; there are also volcanic sands which have originated by explosions of steam in the craters of active volcanoes. A great part of the surface of the globe is covered by sand. In fertile regions the soil is very often of a sandy nature; though most soils are mixtures of sand with clay or stones, and may be described as loams rather than as sands. Pure sandy soils are found principally near sea-coasts where the sand has been blown inwards from the shore, or on formations of soft and friable sandstone like the Greensand. The soil of deserts also is often arenaceous, but there the finer particles have been lifted and borne away by the wind. Accumulations of sand are found also in some parts of the courses of our rivers, very often over wide stretches of the seashore, and more particularly on the sea bottom, where the water is not very deep, at no great distance from the land. Of the rock-making minerals which are common on the earth's crust only a limited number occur at all frequently in sand deposits. For several reasons quartz is by far the commonest ingredient of sands. It is a very abundant mineral in rocks and is comparatively hard, so that it is not readily worn down to a very fine muddy paste. It also possesses practically no cleavage, and does not split up naturally into thin fragments. If we add to this that it is nearly insoluble in water and that it does not decompose, but preserves its freshness unaltered after long ages of exposure to weathering, we can see that it has all the properties necessary for furnishing a large portion of the sandy material produced by the detrition of rock masses. With quartz there is often a small amount of felspar (principally microcline, orthoclase and oligoclase), but this mineral, though almost as common as quartz in rocks, splits up readily on account of its cleavage, and decomposes into fine, soft, scaly aggregates of mica and kaolin, which are removed by the sifting action of water and are deposited as muds or clays. Small plates of white mica, which, though soft and very fissile, decompose very slowly, are often mingled with the quartz and felspar. In addition to these, all sands contain such minerals as garnet, tourmaline, zircon, rutile and anatase, which are common rock-forming minerals, both hard and resistant to decomposition. Among the less common ingredients are topaz, staurolite, kyanite, andalusite, chlorite, iron oxides, biotite, hornblende and augite, while small particles of chert, felsite and other fine-grained rocks appear frequently in the coarser sand deposits, Shore sands and river sands, which have not been transported for any great distance from their parent rocks, often contain minerals that are too soft or too readily decomposed to persist. In the Lizard district of Cornwall the sands at the base of cliffs of serpentine are rich in olivine, augite, enstatite, tremolite and chromite. Near volcanic islands such minerals as biotite, hornblende, augite and zeolites may form a large portion of the local sand deposits. In marine sands also organic substances are almost universally present, either fragments of plants or the debris of calcareous shells, in fact many sands consist almost entirely of such fragments (shell sands). Around coral islands there are often extensive deposits of comminuted coral (coral sands), mixed with which there is a varying proportion of broken skeletons of calcareous algae, sponge-spicules and other debris of organic origin. The Greensands which are widely distributed over the floor of the oceans, in places where the continental shelf merges into the greater depths, owe their colour to small rounded lumps of glauconite. Among the accessory ingredients of sands which are of great value and interest are the precious metals, especially gold and platinum. These are found usually in the lower parts of the sand deposits resting on the bed-rock, because of their high specific gravity, and have been derived from the destruction of the rocks in which they originally occurred either in quartzose veins or as disseminated particles. Tinstone occurs also in this way ("stream-tin "), and in Ceylon, Burma, Brazil, South Africa, &c., precious stones such as the diamond, ruby, spinel, chrysoberyl and tourmaline are found in beds of sand and gravel (gem sands). In general the sand grains have a rounded or oviform shape due to mutual attrition during transport. Those which have been carried farthest are most rounded; sands deposited at no great distance from their parent rock often consist largely of angular grains. The smaller fragments may be carried along in suspension In water, and may travel for many miles without being sensibly worn; but coarse sands and fine gravels are swept along the bottom and are subjected to an intense grinding action. Something depends also on the hardness of the minerals present in the sands, yet even the diamonds and other gems found in sand deposits have often their corners worn and smoothed. Minerals with very perfect cleavage, such as mica, split up into thin plates under the shock of impact with adjacent grains, and are never rounded like quartz or tourmaline. In deserts the transport of the sands is effected by the wind, and owing to the low viscosity of air even the smallest grains are not held in suspension but are rolled along the ground: hence very fine quartzose sands are sometimes met with in arid regions with every particle smoothed and polished. These sands flow almost like a liquid and are used in hour-glasses. Similar "desert sands occur among the sandstones of the Trias and were doubtless formed in the manner described. In addition to river sands, shore sands, marine sand deposits and desert sands, there are many other types of sand deposits. Blown sands are usually found near the seashore, but occur also at the margin of some great lakes like those of N. America; desert sands belong in great part to this category. These sands have been blown into their present position by the wind, and unless fixed by vege tation are constantly though slowly in movement, being in consequence a menace to agricultural land on their leeward sides. They may be shell sands, quartz sands or mixed sands, and often show very marked oblique stratification or current bedding." The surface of blown sand deposits is generally marked by dunes. Glacial sands are common in districts like Britain and those parts of N. America which have been covered by an ice-sheet. They are really water-borne and have been deposited by streams, though they occur in situations where rivers no longer flow. The waters produced by the melting of the ice-sheets flooded extensive tracts of country, laying down sand and mud deposits in temporary lakes. These sands are usually angular, because they have not been transported to any great distance. The old high-level terraces which border the lower courses of many rivers, though usually consisting of gravel, are often accompanied by considerable sand deposits. Many of the Tertiary and some of the Secondary sandstone rocks are so incompletely consolidated by cementation that they are essentially sand rocks, and especially when weathered may be used as sources of sand. Thus in Britain there are Pliocene sands (St Erth, Cornwall, &c.), Eocene sands (Bagshot sands and Thanet sands); and the Lower and Upper Greensand (Cretaceous) are often dug in pits, though sometimes firmly coherent and more properly described as sandstones (q.v.). The economic uses of sands are very numerous. They are largely employed for polishing and scouring both for domestic and manu facturing purposes. "Bath bricks" are made from the sand of the river Parrett near Bridgwater. Sand for glass-making was formerly obtained at Alum Bay in the Isle of Wight and at Lynn in Norfolk, but must be very pure for the best kinds of glass, and crushed quartz or flint is often preferred on this account. One of the principal uses of sand is for making mortar and cement: for this any good clean quartzose sand free from salts is suitable; it may be washed to remove impurities and sifted to secure uniformity in the size of the individual grains. Moulding sands, adapted for foundry purposes, generally contain a small admixture of clay. Sands are also em ployed in brick-making, in filtering, and for etching glass and other substances by means of the sand blast. (J. S. F.) SANDAL (from the Latinized form of Gr. σavôáλov or gárdaλov: this probably represents the Persian sandal, slipper; it is not to be referred to Gr. oavis, board), the foot-covering which consists of a sole of leather or other material attached to the sole of the foot by a thong of leather passing between the great and second toe, crossed over the instep and fastened round the ankle (see SHOE and COSTUME, section Greek and Roman). Sandals are only worn regularly among the peoples of Western civilization by friars, though forms of them are found among the peasants in Spain and the Balkans. They have in recent times been adopted by the extreme advocates of hygienic dress, especially for young children. In the early part of the 19th century a form of low, light slipper fastened by a ribbon crossed over the instep and round the ankle, and worn by women, was known as a sandal. SANDALWOOD (from Fr. sandal, santal, Gr. σávraλov, σávdaλov, Pers. sandal, chandan, Skt. chandana, the sandal tree; the form "sanders" is probably an English corruption), a fragrant wood obtained from various trees of the natural order Santalaceae, and principally from Santalum album, a native of India. The use of sandalwood dates as far back at least as the 5th century B.C. It is still extensively used in India and China, wherever Buddhism prevails, being employed in funeral rites and religious ceremonies. Until the middle of the 18th century India was the only source of sandalwood. The discovery of a sandalwood in the islands of the Pacific led to difficulties with the natives, often ending in bloodshed, the celebrated missionary John Williams (1796-1839), amongst others, having fallen a victim to an indiscriminate retaliation by the natives on white men visiting the islands. The loss of life in this trade was at one time even greater than in that of whaling, with which it ranked as one of the most adventurous of callings. In India sandalwood is largely used in the manufacture of boxes, fans and other ornamental articles of inlaid work, and to a limited extent in medicine as a domestic remedy for all kinds of pains and aches. The oil, obtained by distilling the wood in chips, is largely used as a perfume, few native Indian attars or essential oils being free from admixture with it. In the form of powder or paste the wood is employed in the pigments used by the Brahmans for their distinguishing caste-marks. Red sandalwood, known also as red sanders wood, is the product of a small leguminous tree, Pterocarpus santalinus, native of S. India, Ceylon and the Philippine Islands. A fresh surface of the wood has a rich deep red colour, which on exposure, however, assumes a dark brownish tint. In medieval times red sandalwood possessed a high reputation in medicine, and it was valued as a colouring ingredient in many dishes. It is pharmacologically quite inert Now it is little used as a colouring agent in pharmacy, its principal application being in wool-dyeing. Several other species of Pterocarpus, notably P. indicus, contain the same dyeing principle and can be used as substitutes for red sandalwood. The barwood and camwood of the Guinea Coast of Africa, from Baphia nitida or an allied species, called santal rouge d'Afrique by the French, are also in all respects closely allied to the red sandalwood of Oriental countries. As a substitute for copaiba (qv), sandalwood oil, distilled from the wood of Santalum album, is more expensive and pleasanter to take, but it is less efficient, as it does not contain any analogue to the valuable resin in copaiba. SANDARACH (Fr. sandaraque, Lat. sandaraca, Gr. oavdapákn, realgar or red sulphide of arsenic, cf. Pers. sandarus, Skt sindura, realgar), in mineralogy realgar or native arsenic disulphide, but generally (a use found in Dioscorides) a resinous body obtained from the small coniferous tree Callitris quadrivalvis, native of the north-west regions of Africa, and especially characteristic of the Atlas mountains. The resin, which is procured as a natural exudation on the stems, and also obtained by making incisions in the bark of the trees, comes into commerce in the form of small round balls or elongated tears, transparent, and having a delicate yellow tinge. It is a little harder than mastic, for which it is sometimes substituted. It is also used as incense, and by the Arabs medicinally as a remedy for diarrhoea. It has no medicinal advantages over many of the resins employed in modern therapeutics. An analogous resin is procured in China from Callitris sinensis, and in S. Australia, under the name of pine gum, from C. Reissii. SANDBACH, a market town in the Crewe parliamentary division of Cheshire, England, 5 m. N.E. of Crewe, on the London & North-Western and North Staffordshire railways. Pop. of urban district (1901) 5558. It lies on a headstream of the small river Wheelock, a tributary of the Weaver. The parish church of St Mary is Perpendicular, with a fine carved roof of the 17th century. A few old timbered houses, of the same period, remain. In the market-place are two remarkable crosses covered with rude carvings, and assigned by some to the 7th century, being similar to those at Monasterboice and elsewhere in Ireland. There are boot and shoe factories, chemical works and a manufactory of fustians, with salt-works and iron-works in the adjacent township of Wheelock. SANDBERGER, KARL LUDWIG FRIDOLIN VON (1826-1898), German palaeontologist and geologist, was born at Dillenburg, Nassau, on the 22nd of November 1826. He was educated at the universities of Bonn, Heidelberg and Giessen, at the last of which he graduated Ph.D. in 1846. He then studied at the university of Marburg, where he wrote his first essay, Übersicht der geologischen Verhältnisse des Herzogtums Nassau (1847) In 1849 he became curator of the Natural History Museum at Wiesbaden, and began to study the Tertiary strata of the Mayence Basin, and also the Devonian fossils of the Rhenish provinces, on which he published elaborate memoirs. In 1855 he was appointed professor of mineralogy and geology at the Polytechnic Institute at Karlsruhe, and he took part in the geological survey of Baden. From 1863 to 1896 he was professor of mineralogy and geology at the university of Würzburg His great work Die Land- und Süsswasser-Conchylien der Vorwelt was published in 1870-1875. Later he issued an authoritative work on mineral veins, Untersuchungen über Erzgänge (1882-1885). He died at Würzburg on the 11th of April 1898. His brother GUIDO SANDBERGER (1821-1869) was an authority on fossil cephalopoda, and together they published Die Versteinerungen des rheinischen Schichtensystems in Nassau (1850–1856). SANDBY, PAUL (1725-1809), English water-colour painter, was born at Nottingham in 1725. In 1746 he was appointed by the duke of Cumberland draughtsman to the survey of the Highlands. In 1752 he quitted this post and retired to Windsor, where he occupied himself with the production of water-colour drawings of scenery and architecture. Sir Joseph Banks commissioned him to bring out in aquatint (a method of engraving then peculiar to Sandby) forty-eight plates drawn during a tour in Wales. Sandby displayed considerable power as a caricaturist in his attempt to ridicule the opposition of Hogarth he was chosen a foundation-member of the Royal Academy and to the plan for creating a public academy for the arts. In 1768 appointed chief drawing-master to the Royal Military Academy at Woolwich. He held this situation till 1799. Sandby is best remembered, however, by his water-colour paintings. They are topographical in character, and, while they want the richness and brilliancy of modern water-colour, he nevertheless impressed upon them the originality of his mind. His etchings, such as the Cries of London and the illustrations to Ramsay's Gentle Shepherd, and his plates, such as those to Tasso's Jerusalem Delivered, are numerous and carefully executed. He died in London on the 9th of November 1809. SANDEAU, LÉONARD SYLVAIN JULIEN [JULES] (18111883), French novelist, was born at Aubusson (Creuse) on the 19th of February 1811. He was sent to Paris to study law, but spent much of his time with unruly students. He met Madame Dudevant (George Sand) at Le Coudray in the house of a friend, and when she came to Paris in 1831 she joined Sandeau. The intimacy did not last long, but it produced Rose et Blanche (1831), a novel written in common under the pseudonym Jules Sand, from which George Sand took the idea of her famous nom de guerre. Sandeau continued for nearly fifty years to produce novels and to collaborate in plays. His best works are Marianna (1839), in which he draws a portrait of George Sand; Le Docteur Herbeau (1841); Catherine (1845); Mademoiselle de la Seiglière (1848), a successful picture of society under Louis Philippe, dramatized in 1851; Madeleine (1848); La Chasse au roman (1849); Sacs et parchemins (1851); La Maison de Penarvan (1858); La Roche aux mouettes (1871). The famous play of Le Gendre de M.Poirier is one of several which he wrote with Emile Augier-the novelist usually contributing the story had been made conservateur of the Mazarin library in 1853, elected and the dramatist the theatrical working up. Meanwhile Sandeau to the Academy in 1858, and next year appointed librarian of St Cloud At the suppression of this latter office, after the fall of the empire. he was pensioned. He died on the 24th of April 1883. style, and his refusal to pander to the popular taste in the morals and He was never a very popular novelist, and the quiet grace of his incidents of his novels, may have disqualified him for popularity. See G Planche, Portraits littéraires (1849), vol i';]. Clarétie, J Sandeau (1883); F. Brunetière in the Revue des deux mondes (1887). SAND-EEL, or SAND-LAUNCE. The fishes known under these names form a small family (Ammodytidae) now included with the Scombresocidae in the sub-order Percesoces. They were formerly placed in the Anacanthini and supposed to be allied to the Gadidae, but a fossil form Cobitopsis has recently been described in which the pelvic fins are present, and are abdominal in position as in Belone and Scombresox. The Their body is of an elongate-cylindrical shape, with the head terminating in a long conical snout, the projecting lower jaw forming the pointed end A low long dorsal fin, in which no distinction between spines and rays can be observed, occupies nearly the whole length of the back, and a long anal, composed of similar short and delicate rays, commences immediately behind the vent, which is caudal is forked and the pectorals are short placed about midway between the head and caudal fin The total absence of ventral fins indicates the burrowing habits of these fishes. The scales, when present, are very small, but generally the development of scales has only proceeded to the formation of oblique folds of the integuments. The eyes are lateral and of moderate size; the dentition is quite rudimentary Sand-eels are small littoral marine fishes, only one species attaining a length of 18 in. (Ammodytes lanceolatus). They live in shoals at various depths on a sandy bottom, and bury themselves in the sand on the slightest alarm. Other shoals live in deeper water. When they are surprised by fish of prey or porpoises they are frequently driven to the surface in such dense masses that numbers of them can be scooped out of the water with a bucket or hand-net. Sand eels destroy a great quantity of fry and other small creatures, such as the lancelet (Amphioxus), which lives in similar localities. They are excellent eating, and are much sought after for bait. They are captured by small meshed seines, as well as by digging in the sand. The eggs of sand-eels are small, heavier than sea-water and slightly adhesive. they are scattered among the grains of sand in which the fishes live, and the larvae and young at various stages of growth may be taken with the row-net in sandy bays in summer. Orthographie (1856; 4th ed., 1878), and was an active member of the See Friedrich Düsel, Daniel Sanders (1886; 2nd ed., 1890); A. SANDERS, NICHOLAS (c. 1530-1581), Roman Catholic agent owed much to the generosity of Sir Francis Englefield (qv). Sand-eels are common in the N. Atlantic, a species scarcely under a handsome tomb. See T. H. Thornton, Sir Robert Sandeman (1895); and R. I. Bruce, The Forward Policy (1900). SANDERS, DANIEL (1819-1896), German lexicographer, was born on the 12th of November 1819 at Altstrelitz in Mecklenburg, of Jewish parentage. He was educated at the " Gymnasium Carolinum" in the neighbouring capital Neustrelitz, and the universities of Berlin and Halle, where he took the degree of doctor philosophiae. From 1842 to 1852 he conducted with success the school at Altstrelitz. In 1852 he subjected Grimm's Deutsches Wörterbuch to a rigorous examination, and as a result published his dictionary of the German language, Wörterbuch der deutschen Sprache (3 vols., 1859-1865). This was followed by his Ergänzungswörterbuch der deutschen Sprache (1878-1885). Among others of his works in the same field are Fremdwörterbuch (Leipzig, 1871: 2nd ed., 1891), Wörterbuch der Hauptschwierigkeiten in der deutschen Sprache (1872; 22nd ed., 1892) and Lehrbuch der deutschen Sprache für Schulen (8th ed., 1888). Sanders laid down his views in his Katechismus der deutschen dependeth upon the stout assailing of England." His ardent zeal SANDERSON, ROBERT (1587-1663), English divine, was born to several benefices. On the recommendation of Laud he was appointed one of the royal chaplains in 1631, and was a favourite preacher with the king, who made him regius professor of divinity at Oxford in 1642. The Civil War kept him from entering the office till 1646; and in 1648 he was ejected by the Parliamentary visitors. He recovered his position at the Restoration, was moderator at the Savoy Conference, 1661, and was promoted to the bishopric of Lincoln. He died two years later on the 29th of January 1663. His most celebrated work is his Cases of Conscience, deliberate judgments upon points of morality submitted to him. They are distinguished by moral integrity, good sense and learning. His practice as a college lecturer in logic is better evidenced by than by his Compendium of Logic, first published in 1618. A complete edition of Sanderson's works (6 vols.) was edited by William Jacobson in 1854. It includes the Life by Izaak Walton, revised and enlarged. these cases SANDFORD, JOHN DE (d. 1294), archbishop of Dublin, was probably an illegitimate son of the baronial leader, Gilbert Basset (d. 1241), or of his brother Fulk Basset, bishop of London from 1241 until his death in 1259, a prelate who was prominent during the troubles of Henry III.'s reign. John was a nephew of Sir Philip Basset (d. 1271), the justiciar. He first appears as an official of Henry III. in Ireland and of Edward I. in both England and Ireland; he was appointed dean of St Patrick's, Dublin, in 1275. In 1284 he was chosen archbishop of Dublin in succession to John of Darlington; some, however, objected to this choice and Sandford resigned his claim; but was elected a second time while he was in Rome, and returning to Ireland was allowed to take up the office. In 1288, during a time of great confusion, the archbishop acted as governor of Ireland. In 1290 he resigned and returned to England. Sandford served Edward I. in the great case over the succession to the Scottish throne in 1292 and also as an envoy to the German king, Adolph of Nassau, and the princes of the Empire. On his return from Germany he died at Yarmouth on the 2nd of October 1294. Sandford's elder brother, Fulk (d. 1271), was also archbishop of Dublin. He is called Fulk de Sandford and also Fulk Basset owing to his relationship to the Bassets. Having been archdeacon of Middlesex and treasurer and chancellor of St Paul's Cathedral, London, he was appointed archbishop of Dublin by Pope Alexander IV. in 1256. He took some slight part in the government of Ireland under Henry III. and died at Finglas on the 4th of May 1271. SANDGATE, a watering-place of Kent, England, on the S.E. coast, 1 m. W. of Folkestone, on the South-Eastern & Chatham railway. Pop. of urban district (1901) 2023. It is connected with Hythe, 3 m. W., by a tramway belonging to the railway company. It is included in the parliamentary borough of Hythe. Sandgate Castle was built by Henry VIII., but on the formation of a camp here in 1806 it was considerably altered. The camp of Shorncliffe lies N. of the town on a plateau. SAND-GROUSE, the name by which are commonly known the members of a small group of birds frequenting sandy tracts, and having their feet more or less clothed with feathers after the fashion of grouse (q.v.), to which they were originally thought to be closely allied; the species first described were by the earlier Their systematists invariably referred to the genus Tetrao. separation therefrom is due to C. J. Temminck, who made for them a distinct genus which he called Pterocles. Further investigation of the osteology and pterylosis of the sand-grouse revealed still greater divergence from the normal Gallinae (to which the true grouse belong), as well as several curious resemblances to the pigeons; and in the Zoological Society's Proceedings for 1868 (p. 303) T. H. Huxley proposed to regard them, under the name of Pteroclomorphae, as forming a group equivalent to the Alectoromorphae and Peristeromorphae. They are now 1 It seems to have been first used by J. Latham in 1783 (Synopsis, iv. p. 751) as the direct translation of the name Tetrao arenarius given by Pallas. He states that he published this name in 1809; but hitherto research has failed to find it used until 1815. ་་ generally regarded as forming a separate sub-order Pterocles SANDHURST, a town in the Wokingham parliamentary division of Berkshire, England, 9 m. N. of Aldershot. Pop. (1901) 2386. Two miles south-east of the town, near the villages of Cambridge Town and York Town, and the railway stations of Blackwater and Camberley on the South-Eastern and Chatham and South-Western lines, is the Sandhurst Royal Military College. It was settled here in 1812, having been already removed by its founder, the duke of York, from High Wycombe, where it was opened in 1799, to Great Marlow in 1802. It stands in beautiful grounds, which contain a large lake. Wellington College station on the South-Eastern branch line to Reading, near Sandhurst itself, serves Wellington College, one of the principal modern public schools of England, founded in memory These were separated by Bonaparte (Comptes rendus, xlii. p. 880) as a distinct genus, Pteroclurus, which later authors have justly seen no reason to adopt. |