Always put the best interpretation on a tenet. Why not on Christianity, wholesome, sweet, and poetic? It is the record of a pure and holy soul, humble, absolutely disinterested, a truth-speaker, and bent on serving, teaching, and uplifting men. Christianity taught the capacity, the element, to love the All-perfect without a stingy bargain for personal happiness. It taught that to love him was happiness,--to love him in others' virtues.--_Emerson._
Look upon your chastenings, then, no matter how grievous they may be for the present, as God's chariots, sent to carry your souls into the "high places" of spiritual achievement and uplifting, and you will find that they are, after all, "paved with love."--_Smith._
Radiate an energy of serenity and peace so that you have an uplifting effect on those you come into contact with. Your presence will make others feel calm and assured.
So Nestor. They, inscribing each his lot, Into the helmet cast it of the son Of Atreus, Agamemnon. Then the host Pray'd all, their hands uplifting, and with eyes To the wide heavens directed, many said--
He spake, and drawing nigh, with his rais'd foot, Insolent as he was and brutish, smote Ulysses' haunch, yet shook not from his path The firm-set Chief, who, doubtful, mused awhile Whether to rush on him, and with his staff To slay him, or uplifting him on high, Downward to dash him headlong; but his wrath Restraining, calm he suffer'd the affront. Him then Eumæus with indignant look Rebuking, rais'd his hands, and fervent pray'd.
As Enjolras walked towards this place, he passed the whole situation in review in his own mind. The gravity of events was self-evident. When facts, the premonitory symptoms of latent social malady, move heavily, the slightest complication stops and entangles them. A phenomenon whence arises ruin and new births. Enjolras descried a luminous uplifting beneath the gloomy skirts of the future. Who knows? Perhaps the moment was at hand. The people were again taking possession of right, and what a fine spectacle! The revolution was again majestically taking possession of France and saying to the world: "The sequel to-morrow!" Enjolras was content. The furnace was being heated. He had at that moment a powder train of friends scattered all over Paris. He composed, in his own mind, with Combeferre's philosophical and penetrating eloquence, Feuilly's cosmopolitan enthusiasm, Courfeyrac's dash, Bahorel's smile, Jean Prouvaire's melancholy, Joly's science, Bossuet's sarcasms, a sort of electric spark which took fire nearly everywhere at once. All hands to work. Surely, the result would answer to the effort. This was well. This made him think of Grantaire.
The mountain zone is towards the south of the island, and covers an area of about 4212 sq. m. The uplifting force seems to have been exerted from south-west to north-east, and although there is much confusion in many of the intersecting ridges, and spurs of great size and extent are sent off in many directions, the lower ranges manifest a remarkable tendency to run in parallel ridges in a direction from south-east to north-west. Towards the north the offsets of the mountain system radiate to short distances and speedily sink to the level of the plain. Detached hills are rare; the most celebrated of these are Mihintale (anc. _Missïaka_), which overlooks the sacred city of Anuradhapura, and Sigiri. The latter is the only example in Ceylon of those solitary acclivities which form so remarkable a feature in the tableland of the Deccan--which, starting abruptly from the plain, with scarped and perpendicular sides, are frequently converted into strongholds accessible only by precipitous pathways or by steps hewn in the solid rock. Entry: CEYLON
Arnold's poetic activity almost ceased after he left the chair of poetry at Oxford. He was several times sent by government to make inquiries into the state of education in France, Germany, Holland and other countries; and his reports, with their thorough-going and searching criticism of continental methods, as contrasted with English methods, showed how conscientiously he had devoted some of his best energies to the work. His fame as a poet and a literary critic has somewhat overshadowed the fact that he was during thirty-five years of his life--from 1851 to 1836--employed in the Education Department as one of H.M. inspectors of schools, while his literary work was achieved in such intervals of leisure as could be spared from the public service. At the time of his appointment the government, by arrangement with the religious bodies, entrusted the inspection of schools connected with the Church of England to clergymen, and agreed also to send Roman Catholic inspectors to schools managed by members of that communion. Other schools--those of the British and Foreign Society, the Wesleyans, and undenominational schools generally--were inspected by laymen, of whom Arnold was one. There were only three or four of these officers at first, and their districts were necessarily large. It is to the experience gained in intercourse with Nonconformist school managers that we may attribute the curiously intimate knowledge of religious sects which furnished the material for some of his keen though good-humoured sarcasms. The Education Act of 1870, which simplified the administrative system, abolished denominational inspection, and thus greatly reduced the area assigned to a single inspector. Arnold took charge of the district of Westminster, and remained in that office until his resignation, taking also an occasional share in the inspection of training colleges for teachers, and in conferences at the central office. His letters, _passim_, show that some of the routine which devolved upon him was distasteful, and that he was glad to entrust to a skilled assistant much of the duty of individual examination and the making up of schedules and returns. But the influence he exerted on schools, on the department, and on the primary education of the whole country, was indirectly far greater than is generally supposed. His annual reports, of which more than twenty were collected into a volume by his friend and official chief, Sir Francis (afterwards Lord) Sandford, attracted, by reason of their freshness of style and thought, much more of public attention than is usually accorded to blue-book literature; and his high aims, and his sympathetic appreciation of the efforts and difficulties of the teachers, had a remarkable effect in raising the tone of elementary education, and in indicating the way to improvement. In particular, he insisted on the formative elements of school education, on literature and the "humanities," as distinguished from the collection of scraps of information and "useful knowledge"; and he sought to impress all the young teachers with the necessity of broader mental cultivation than was absolutely required to obtain the government certificate. In his reports also he dwelt often and forcibly on the place which the study of the Bible, not the distinctive formularies of the churches, ought to hold in English schools. He urged that besides the religious and moral purposes of Scriptural teaching, it had a literary value of its own, and was the best instrument in the hands even of the elementary teacher for uplifting the soul and refining and enlarging the thoughts of young children. Entry: ARNOLD
With modern orchestral conditions the text seems positively to demand an unecclesiastical, not to say sensational, style, and probably the only instrumental Requiem Masses which can be said to be great church music are the sublime unfinished work of Mozart (the antecedents of which would be a very interesting subject) and the two beautiful works by Cherubini. These latter, however, tend to be funereal rather than uplifting. The only other artistic solution of the problem is to follow Berlioz, Verdi and Dvorák in the complete renunciation of all ecclesiastical style. Entry: 5
The volcanic origin of the Andes and their comparatively recent elevation still subject Chile, in common with other parts of the western coast region, to frequent volcanic and seismic disturbances. In some instances since European occupation, violent earthquake shocks have resulted in considerable elevations of certain parts of the coast. After the great earthquake of 1835 Captain Robert FitzRoy (1805-1865) of H.M.S. "Beagle" found putrid mussel-shells still adhering to the rocks 10 ft. above high water on the island of Santa Maria, 30 m. from Concepción, and Charles Darwin declares, in describing that disaster, that "there can be no doubt that the land round the bay of Concepción was upraised two or three feet." These upheavals, however, are not always permanent, the upraised land sometimes settling back to its former position. This happened on the island of Santa Maria after 1835. The existence of sea-shells at elevations of 350 to 1300 ft. in other parts of the republic shows that these forces, supplemented by a gradual uplifting of the coast, have been in operation through long periods of time and that the greater part of central and southern Chile has been raised from the sea in this way. These earthquake shocks have two distinct characteristics, a slight vibration, sometimes almost imperceptible, called a _temblor_, generally occurring at frequent intervals, and a violent horizontal or rotary vibration, or motion, also repeated at frequent intervals, called a _terremoto_, which is caused by a fracture or displacement of the earth's strata at some particular point, and often results in considerable damage. When the earthquake occurs on the coast, or beneath the sea in its vicinity, tidal waves are sometimes formed, which cause even greater damage than the earthquake itself. Arica has been three times destroyed by tidal waves, and other small towns of the north Chilean coast have suffered similar disasters. Coquimbo was swept by a tidal wave in 1849, and Concepción and Talcahuano were similarly destroyed in 1835. The great earthquake which partially destroyed Valparaiso in 1906, however, was not followed by a tidal wave. These violent shocks are usually limited to comparatively small districts, though the vibrations may be felt at long distances from the centre of disturbance. In this respect Chile may be divided into at least four great earthquake areas, two in the desert region, the third enclosing Valparaiso, and the fourth extending from Concepción to Chiloé. A study of Chilean earthquake phenomena, however, would probably lead to a division of southern Chile into two or more distinct earthquake areas. Entry: CHILE
_Earth Movements and Vulcanicity._--During the greater part of the Cretaceous period crustal movements had been small and local in effect, but towards the close a series of great deformative movements was inaugurated and continued into the next period. These movements make it possible to discriminate between the Cretaceous and Tertiary rocks, because the conditions of sedimentation were profoundly modified by them, and in most parts of the world there resulted a distinct break in the sequence of fossil remains. Great tracts of our modern continental land areas gradually emerged, and several mountainous tracts began to be elevated, such as the Appalachians, parts of the Cordilleras, and the Rocky Mountains, and their northern continuation, and indeed the greater part of the western N. American continent was intensely affected; the uplifting was associated with extensive faulting. Volcanic activity was in abeyance in Europe and in much of Asia, but in America there were many eruptions and intrusions of igneous rock towards the close of the period. Diabases and peridotites had been formed during the Lower Cretaceous in the San Luis Obispo region. Great masses of ash and conglomerate occur in the Crow's Nest Pass in Canada; porphyries and porphyritic tuffs of later Cretaceous age are important in the Andes; while similar rocks are found in the Lower Cretaceous of New Zealand. It is, however, in the Deccan lava flows of India that we find eruptions on a scale more vast than any that have been recorded either before or since. These outpourings of lava cover 200,000 sq. m. and are from 4000 to 6000 ft. thick. They lie upon an eroded Cenomanian surface and are to some extent interbedded with Upper Cretaceous sediments. Entry: CRETACEOUS
_Progress of Geological Conceptions in the Middle Ages._--During the centuries that succeeded the fall of the Western empire little progress was made in natural science. The schoolmen in the monasteries and other seminaries were content to take their science from the literature of Greece and Rome. The Arabs, however, not only collected and translated that literature, but in some departments made original observations themselves. To one of the most illustrious of their number, Avicenna, the translator of Aristotle, a treatise has been ascribed, in which singularly modern ideas are expressed regarding mountains, some of which are there stated to have been produced by an uplifting of the ground, while others have been left prominent, owing to the wearing away of the softer rocks around them. In either case, it is confessed that the process would demand long tracts of time for its completion. Entry: 2