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rate dominion at the distance of a short journey from one another. As an instance of this, we may mention, that on the road from Jerusalem to Sannour, by way of Nablous, there are no fewer than three governors of cities, all of whom claim the honours of independent sovereigns; for, although they acknowledge a nominal superiority in the Pasha of Damascus, they exclude his jurisdiction in all cases where he does not enforce his authority at the head of his troops. The same affectation of independence descends to the sheiks of villages, who, aware of the precarious tenure by which their masters remain in office, are disposed to treat their orders with contempt. Like them, too, they turn to their personal advantage the power of imposition and extortion which belongs to every one who is clothed with official rank in Syria. They sell justice and protection; and in this market, as in all others, he who offers the best price is certain to obtain the largest share of the commodity.*

This chapter would not be complete were we to omit all allusion to the Jews, the ancient inhabitants of Palestine. Their number, according to a statement lately published in Germany, amounts to between three and four millions, scattered over the face of the whole earth, but still maintaining the same laws which their ancestors received from their inspired legislator more than three thousand years ago. In Europe there are nearly two millions, enjoying different privileges according to the spirit of the several governments; in Asia, the estimate exceeds seven hundred thousand; in Africa, more than half a million; and in America, about ten thousand. It is supposed, however, on good grounds, that the Jewish population on both sides of Mount Taurus is considerably greater than is here given, and that their gross number does not fall much short of five millions.†

In Palestine of late years they have greatly increased. It is said that not fewer than ten thousand inhabit Saphet and Jerusalem, and that in their worship they still sing those pathetic hymns which their manifold tribulations have inspired; bewailing, amid the ruins of their ancient capital, the fallen city and the desolate tribes. In Persia, one of them addressed a Christian missionary in these affecting

p. 315.

See Jowett's Christian Researches in Syria and the Holy Land, † Weimar, Geographical Ephemerides; and History of the Jews, vol. . p. 332.

words:"I have travelled far; the Jews are everywhere princes in comparison with those in the land of Iran. Heavy is our captivity, heavy is our burden, heavy is our slavery; anxiously we wait for redemption."

History, says an eloquent writer, is the record of the past; it presumes not to raise the mysterious veil which the Almighty has spread over the future. The destinies of this wonderful people, as of all mankind, are in the hands of the all-wise Ruler of the universe; his decrees will certainly be accomplished; his truth, his goodness, and his wisdom will be clearly vindicated. This, however, we may venture to assert, that true religion will advance with the dissemination of sound and useful knowledge. The more enlightened the Jew becomes, the more incredible will it appear to him that the gracious Father of the whole human race intended an exclusive faith, a creed confined to one family, to be permanent; and the more evident also will it appear to him, that a religion which embraces within the sphere of its benevolence all the kindreds and languages of the earth is alone adapted to an improved and civilized age.*

We presume not to expound the signs of the times, nor to see farther than we are necessarily led by the course of events; but it is impossible not to be struck with the aspect of that grandest of all moral phenomena which is suspended upon the history and actual condition of the sons of Jacob. At this moment they are nearly as numerous as when David swayed the sceptre of the Twelve Tribes; their expectations are the same, their longings are the same; and on whatever part of the earth's surface they have their abode, their eyes and their faith are all pointed in the same direction, to the land of their fathers and the holy city where they worshipped. Though rejected by God and persecuted by man, they have not once, during eighteen hundred long years, ceased to repose confidence in the promises made by Jehovah to the founders of their nation; and although the heart has often been sick and the spirit faint, they have never relinquished the hope of that bright reversion in the latter days which is once more to establish the Lord's house on the top of the mountains, and to make Jerusalem the glory of the whole world.

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CHAPTER IX.

The Natural History of Palestine.

Travellers too much neglect Natural History-Maundrell, Hasselquist, Clarke-GEOLOGY-Syrian Chain -Libanus-Calcareous RocksGranite-Trap-Volcanic Remains-Chalk-Marine Exuvia-Precious Stones-METEOROLOGY-Climate of Palestine-Winds-Thun

der-Clouds-Waterspouts--Ignis Fatuus-ZOOLOGY-Scripture Animals-The Hart-The Roebuck-Fallow-deer-Wild Goat-Pygarg -Wild Ox-Chamois-Unicorn-Wild Ass-Wild Goats of the Rock -Saphan, or Coney-Mouse-Porcupine-Jerboa-Mole-Bat-BIRDS -Eagle-Ossifrage-Ospray-Vulture-Kite-Raven-Owl-Nighthawk-Cuckoo-Hawk-Little Owl-Cormorant-Great Owl-Swan -Pelican-Gier Eagle-Stork-Heron-Lapwing-Hoopoe-AMPHIBIA AND REPTILES-Serpents known to the Hebrews-Ephe-Chephir --Acshub-Pethen -Tzeboa-Tzimmaon -Tzepho-Kippos — Shephiphon-Shachal--Saraph, the Flying Serpent--Cockatrice' Eggs -The Scorpion-Sea monsters, or Seals-FRUITS AND PLANTS-Vegetable Productions of Palestine-The Fig-tree-Palm-Olive--Cedars of Libanus-Wild Grapes-Balsam of Aaron-Thorn of Christ.

EVERY one who writes on the Holy Land has occasion to regret that travellers in general have paid so little attention to its geological structure and natural productions. Maundrell, it is true, was not entirely destitute of physical science; but the few remarks which he makes are extremely vague and unconnected, and, not being expressed in the language of system, throw very little light on the researches of the natural philosopher or the geologist. Hasselquist had more professional learning, and has accordingly contributed more than any of his predecessors to our acquaintance with Palestine, viewed in its relations to the animal, the vegetable, and the mineral kingdoms. Still the reader of his Voyages and Travels in the Levant cannot fail to perceive, that some of the branches of natural knowledge, which are now cultivated with the greatest care, were in his day very little improved; and more especially, that they were deficient in accuracy of description and distinctness of arrangement. Dr. Clarke's observations are perhaps more scientific than those of the Swedish naturalist just named, and particularly in the departments of mineralogy and geology

to which he had devoted a large share of his attention. But even in his works we look in vain for a satisfactory treatise on the mountain-rocks of Palestine, on the geognostic formation of that interesting part of Western Asia, or on the fossil treasures which its strata are understood to envelop. We are therefore reduced to the necessity of collecting from various authors, belonging to different countries and successive ages, the scattered notices which appear in their works, and of arranging them according to a plan most likely to suit the comprehension of the common reader.

SECTION 1.-GEOLOGY.

At first view it would appear that the ridges of Palestine are all a ramification of Mount Taurus. But the proper Syrian chain begins on the south of Antioch, at the huge peak of Casius, which shoots up to the heavens its tapering summit, covered with thick forests. The same chain, under various names, follows the direction of the eastern shore of the Mediterranean, at no greater distance, generally speaking, than twenty-four miles from its waters. Mount Libanus forms its most elevated summit. At length it is divided into two branches, of which the one looks westward to the sea, the other, which bounds the Plain of Damascus, verges in the direction of the desert and the banks of the Euphrates. Hermon, whose lofty top condenses the moisture of the atmosphere, and gives rise to the dews so much celebrated in the Sacred Writings, stands between Heliopolis and the capital of Syria. The latter ridge received from the Greeks the denomination of AntiLibanus, a name unknown among the natives, and which, being employed somewhat arbitrarily by historians and topographers, has occasioned considerable obscurity in their writings.

The hills in this part of Syria are composed of a calca reous rock having a whitish colour, is extremely hard, and which rings in the ear when smartly struck with a hammer. The same description applies to the masses that surround Jerusalem, which on the one hand stretch to the River Jordan, and on the other extend to the Plain of Acre and

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Jaffa. Like all limestone strata, they present a great num. ber of caverns, to which, as places of retreat, frequent allusion is made in the books of Samuel and of the Kings. There is one near Damascus, capable of containing four thousand men; and it must have been in a similar recess that David and his men encountered the ill-fated Saul when pursued by him on the hills of the wild goats.

The mountains that skirt the Valley of the Dead Sea present granite and those other rocks which, according to the system of Werner, characterize the oldest or primitive formation. Mount Sinai is a member of the same group, and exhibits mineral qualities of a similar nature, extending to a certain distance on both sides of the Arabian Gulf. It is probable that this region, at a remote epoch, was the theatre of immense volcanoes, the effects of which may still be traced along the banks of the Lower Jordan, and more especially in the lake itself. The warm baths at Tabaria show that the same cause still exists, although much restricted in its operation,—an inference which is amply confirmed by the lavas, the bitumen, and pumice which continue to be thrown ashore by the waves of Asphaltites.

Dr. Clarke remarks, that in the neighbourhood of Cana there are several basaltic appearances. The extremities of columns, prismatically formed, penetrated the surface of the soil, so as to render the path very rough and unpleasant. These marks of regular or of irregular crystallization generally denote, according to his opinion, the vicinity of water lying beneath their level. The traveller, having passed over a series of successive plains, resembling in their gradation the order of a staircase, observes, as he descends to the inferior stratum upon which the water rests, that where rocks are disclosed the symptoms of crystallization have taken place, and then the prismatic configuration is commonly denoted basaltic. Such an appearance, therefore, in the approach to the Lake of Tiberias is only a parallel to similar phenomena exhibited by rocks near the Lakes of Locarno and Bolsenna in Italy, by those of the Wenner Lake in Sweden, by the bed of the Rhine near Cologne in Germany, by the Valley of Ronca in the territory of Verona, by the Pont de Bridon in the state of Venice, and by numerous other examples in the same country. A corresponding effect is produced on a small scale on the southern declivity

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