mutual antagonism. The twin chains, the Lebanon and the Anti-Lebanon, which divide the country down the centre, are composed of the same kind of calcareous rocks and sandstone, while the same sort of reddish clay has been deposited on their slopes by the glaciers of the same geological period.*

Arid and bare on the northern side, they sent out towards the south featureless monotonous ridges, furrowed here and there by short narrow valleys, hollowed out in places into basins or funnel-shaped ravines, which are widened year by year by the down-rush of torrents. These ridges, as they proceed southwards, become clothed with verdure and offer a more varied outline, the ravines being more thickly wooded, and the summits less uniform in contour and colouring. Lebanon becomes white and ice-crowned in winter, but none of its peaks rises to the altitude of perpetual snows: the highest of them, Mount Timarun, reaches 10,526 feet, while only three others exceed 9000.* Anti-Lebanon is, speaking generally, 1000 or 1300 feet lower than its neighbour: it becomes higher, however, towards the south, where the triple peak of Mount Hermon rises to a height of 9184 feet. The Orontes and the Litâny drain the intermediate space. The Orontes rising on the west side of the Anti-Lebanon, near the ruins of Baalbek, rushes northwards in such a violent manner, that the dwellers on its banks call it the rebel—Nahr el-Asi.** About a third of the way towards its mouth it enters a depression, which ancient dykes help to transform into a lake; it flows thence, almost parallel to the sea-coast, as far as the 36th degree of latitude. There it meets the last spurs of the Amanos, but, failing to cut its way through them, it turns abruptly to the west, and then to the south, falling into the Mediterranean after having received an increase to its volume from the waters of the Afrîn.

The Litâny rises a short distance from the Orontes; it flows at first through a wide and fertile plain, which soon contracts, however, and forces it into a channel between the spurs of the Lebanon and the Galilæan hills. The water thence makes its way between two cliffs of perpendicular rock, the ravine being in several places so narrow that the branches of the trees on the opposite sides interlace, and an active man could readily leap across it. Near Yakhmur some detached rocks appear to have been arrested in their fall, and, leaning like flying buttresses against the mountain face, constitute a natural bridge over the torrent. The basins of the two rivers lie in one valley, extending eighty leagues in length, divided by an almost imperceptible watershed into two beds of unequal slope. The central part of the valley is given up to marshes. It is only towards the south that we find cornfields, vineyards, plantations of mulberry and olive trees, spread out over the plain, or disposed in terraces on the hillsides. Towards the north, the alluvial deposits of, the Orontes have gradually formed a black and fertile soil, upon which grow luxuriant crops of cereals and other produce. Cole-Syria, after having generously nourished the Oriental empires which had preyed upon her, became one of the granaries of the Roman world, under the capable rule of the Cæsars.

Syria is surrounded on all sides by countries of varying aspect and soil. That to the north, flanked by the Amanos, is a gloomy mountainous region, with its greatest elevation on the seaboard: it slopes gradually towards the interior, spreading out into chalky table-lands, dotted over with bare and rounded hills, and seamed with tortuous valleys which open out to the Euphrates, the Orontes, or the desert. Vast, slightly undulating plains succeed the table-lands: the soil is dry and stony, the streams are few in number and contain but little water. The Sajur flows into the Euphrates, the Afrîn and the Karasu when united yield their tribute to the Orontes, while the others for the most part pour their waters into enclosed basins. The Khalus of the Greeks sluggishly pursues its course southward, and after reluctantly leaving the gardens of Aleppo, finally loses itself on the borders of the desert in a small salt lake full of islets: about halfway between the Khalus and the Euphrates a second salt lake receives the Nahr ed-Dahab, the "golden river." The climate is mild, and the temperature tolerably uniform. The sea-breeze which rises every afternoon tempers the summer heat: the cold in winter is never piercing, except when the south wind blows which comes from the mountains, and the snow rarely lies on the ground for more than twenty-four hours. It seldom rains during the autumn and winter months, but frequent showers fall in the early days of spring. Vegetation then awakes again, and the soil lends itself to cultivation in the hollows of the valleys and on the table-lands wherever irrigation is possible. The ancients dotted these now all but desert spaces with wells and cisterns; they intersected them with canals, and covered them with farms and villages, with fortresses and populous cities. Primæval forests clothed the slopes of the Amanos, and pinewood from this region was famous both at Babylon and in the towns of Lower Chaldæa. The plains produced barley and wheat in enormous quantities, the vine throve there, the gardens teemed with flowers and fruit, and pistachio and olive trees grew on every slope. The desert was always threatening to invade the plain, and gained rapidly upon it whenever a prolonged war disturbed cultivation, or when the negligence of the inhabitants slackened the work of defence: beyond the lakes and salt marshes it had obtained a secure hold. At the present time the greater part of the country between the Orontes and the Euphrates is nothing but a rocky table-land, ridged with low hills and dotted over with some impoverished oases, excepting at the foot of Anti-Lebanon, where two