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t appear to be mourning robes. I was often reminded of those wicked lines of BYRON'S on the gondola: 'For sometimes they contain a deal of fun, Like mourning-coaches when the funeral's done.' But let us turn from the animate to the inanimate, and visit the famous AEtna, called by the Sicilians _Mongibello_. From the silence of Homer on the subject, it is supposed that in his remote age the fires of the mountain were unknown; but geologists have proof that they have a far more ancient date. The Grecian poet Pindar is the first who mentions its eruptions. He died four hundred and thirty-five years before CHRIST; from that time to this, at irregular intervals, it has vomited forth its destructive lavas. It is computed to be eleven thousand feet high. Its base, more than an hundred miles in circumference, is interspersed with numerous conical hills, each of which is an extinct crater, whose sides, now shaded by the vine, the fig tree, and the habitations of man, once glowed with the fiery torrent. Some of them are yet almost destitute of vegetation; mere heaps of scoriae and ashes; but the more ancient ones are richly clad with verdure. Let the reader imagine a mountain whose base is as broad as the whole range of the Catskills, as seen from Catskill village, rising to nearly three times their height; its lower parts are of gentle ascent, but as it rises it becomes more and more steep, until it terminates in a broken summit. Imagine it divided, as the eye ascends, into three regions or belts: the first and lowest is covered with villages, gardens, vineyards, olive-groves, oranges, and fields of grain and flax, and the date-bearing palm. The second region, which commences about four thousand feet above the sea, is called the _Regione Sylvosa_, or woody region. Here chestnuts, hexes, and on the north pines of great size flourish. This belt reaches to the elevation of about seven thousand feet, where the _Regione Scoperta_, or bare region, commences. The lower part of this is intermingled lava, rocks, volcanic sands, and snow; still higher are vast fields of spotless snow, which centuries have seen unwasted, with here and there a ridgy crag of black lava, too steep for the snows to lodge upon; and toward the summit of the cone, dark patches of scoriae and ashes, which, heated by the slumbering fires, defy the icy blasts of these upper realms of air. It will readily be supposed that, when viewed from a distance, Mount AEt
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