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106 furnished by inscriptions are to follow. Being formed by scholars actuated by no aesthetic principles of selection, but solely intent on preserving everything they could find, the Latin anthology is much more heterogeneous than the Greek, and unspeakably inferior. The really beautiful poems of Petronius and Apuleius are more properly in serted in the collected editions of their writings, and more than half the remainder consists of the frigid conceits or pedantic professional exercises of grammarians of a very late period of the empire, relieved by an occasional gem, such as the apostrophe of the dying Hadrian to his spirit, or the epithalamium of Gallienus. The collection is also, for the most part, too recent in date, and too exclusively literary in character, to add much to our knowledge of classical antiquity. The epitaphs are interesting, but the genuine ness of many of them is very questionable.  ANTHON,, an American philologist and professor of classics, was born in New York city in 1797, and died there 29th July 1867. After graduating with honours at Columbia College in 1815, he commenced the study of law, and in 1819 was admitted to the bar. But in 1820 he was appointed assistant professor of languages in his alma- mater, and he thenceforth devoted himself solely to classical literature. Soon after he commenced his well-known editions of the classics, the best known being that of the Poems of Horace, with extensive notes and comments, pub lished in 1830. In the latter year he was made rector of the grammar school attached to his college, and in 1835 he succeeded to the chair of Professor Morse.  ANTHONY,, the founder of, was at the of  in   Inheriting a large fortune, he thought it his duty to distribute it among his neighbours and the poor, and to live a rigidly. He spent several in solitude, where according to tradition he was sorely tempted by the. Many disciples flocked to his retreat at, and built their cells around his, thus forming the earliest. (See .) Anthony visited when upwards of a hundred  old, and took an important part in the controversy with the, a fact to which we are probably indebted for the record of the life of the saint written by Athanasius. Soon after returning to his cell he died, his last injunction being that the place of his should be kept secret. Seven translations of his letters are extant in the Bibliotheca Patrum. Many were believed to have been wrought by his intervention, among others, the cure of what was called the “sacred fire,” and afterwards &quot;Anthony’s fire&rdquo;. For this reason he is usually represented with a by his side, as typical of the   which he was supposed to relieve. The of  Anthony is observed on the 17th of, under which date the Acta Sanctorum of the  contains a  translation of Athanasius’s life of the saint, and other documents giving an account of his. The events of his life—in particular his temptation by the and his meeting with —form the subjects of celebrated  by, , , and others. For further details of Anthony’s connection with the, see.  ANTHRACITE,,, or , is a variety of coal differing from the common or bituminous kind in containing a larger proportion of carbon in its composition ; that element being present in anthracite to the extent of from 90 to 95 per cent, of its entire mass, while the carbon in bituminous coal usually varies from 75 to 90 per cent. Anthracite is further distinguished by its compactness, high specific gravity, bright lustre, which is frequently iridescent on the natural surfaces, and its conchoidal fracture. It does not soil the fingers when handled, like ordinary coal ; it ignites with difficulty, and burns with a feeble, smokeless flame, giving out an intense heat. No sharply defined line of demarcation can be drawn between anthracite and the bituminous varieties of coal, as the one series merges by imperceptible degrees into the other. This gradation is observable in the coal deposits themselves, anthracite and bituminous coal being frequently found not far removed in different parts of the same seam, and the gradual transformation from a flaming coal to a compact, lustrous, non-flaming kind, being easily traceable. Anthracite has been defined as &quot; the ultimate product of the conversion of vegetable matter into coal;&quot; and the following table, drawn up by Dr Percy (Manual of Metallurgy], may be taken as indicating the successive stages in the process. In this table the carbon is stated at a constant standard of 1 00, in order better to exhibit the comparative quantities of the other elements which enter into the composition of the bodies named:—

Carbon. Hydrogen. Oxygen. 1. Wood (mean of 26 analyses) 100 1218 83 07 2. Peat .1 100 9 85 55 67 3. Lignite (average of 15 varieties) 100 8 37 42 42 4. Ten Yard Coal, South Staffordshire 100 6-12 21 23 5. Steam Coal, from the Tyne 100. 5 91 18 32 6. Peiitrefelin Coal of South Wales ...100 4 75 5 "28 7. Anthracite of Pennsylvania, U.S. ...100 2 84 174

The chief deposits of anthracite in Great Britain exist in the great coal-field of South Wales. They extend principally along the north side of the coal basin ; and on its western limit, in Pembrokeshire, the coal is entirely anthracitic. Professor Warrington Smyth remarks, on the disposition of the deposits in South Wales : " Even within the distance of a few hundred yards the Llanelly beds are seen to be bituminous where they rise to the south, and anthracitic in the opposite side of the trough." In the neighbourhood of Bideford, in North Devonshire, a series of thin seams of an impure, clayey anthracite are worked, to which properly the name culm ought to be restricted, although the whole of the anthracite exported from this country appears under that designation in the Board of Trade returns. The very meagre coal-bearing strata of Ireland yield anthracite almost exclusively. The name Kilkenny coal is given to anthracite, because that county is the centre of the South Irish coal-field, which yields no bituminous coal whatever. In the limited patches of coal found in the north of Ireland, however, some bituminous seams occur associated with anthracite. On the European continent anthracite is generally found accompanying the deposits of bituminous coal. In Belgium and Westphalia the lowest or oldest deposits of the series are anthracitic, while in Rhenish Bavaria it is the upper beds which are " dry," or least bituminous. In North America, where enormous stores of coal exist, anthracite is found in due proportion, the deposits in Pennsylvania being the richest known. The late Professor H. D. Rogers pointed out an interesting relation between the contortion or disturbance of strata in the Appalachian coal-field and the amount of bituminous matter the coal contains. In the western extension of the coal-field, where the beds are horizontal and undisturbed, the seams are highly bituminous ; and in propertion as disturbance increases, the volatile compounds decrease, till on its eastern limit, in the Appalachian chain, normous seams of a compact, pure anthracite are developed. Anthracite is used for iron-smelting and in other metallurgical operations, for lime-burning, for heating kilns, and other purposes requiring a steady, smokeless leat. As it burns with an intense concentrated heat, it is not so suitable for steam boilers as ordinary flaming coal ; and the difliculty with which it ignites, as well as its disagreeable decrepitation, renders it less eligible for household purposes. 