History of the Jews, Vol. 1 (of 6). Graetz Heinrich

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СКАЧАТЬ living object. The atmosphere of this region is likewise impregnated with salt, and, as the adjacent land is covered with lime-pits, it forms a dreary desert. The oval-shaped border of the Dead Sea rises, in some parts, to a height of more than 1,300 feet above the water level, and being totally bare and barren, the entire district presents a most dismal aspect.

      Between the water-line and the mountain walls there are, however, some oases in which the balsam shrub thrives, and which, in regard to fertility, are not inferior to any spot on earth. Being situated near the centre of the western seaboard, this strip of land is exceedingly fruitful. But luxuriant as the vegetation of this place is, it is even surpassed by that of the oasis on the south-east corner of the Dead Sea. Here stood at one time the town of Zoar, which was noted as the city of palm-trees (Tamarah). This locality likewise favoured in former ages the growth of the balsam shrub. At a distance of five miles to the north-east, near the town of Beth-Haran, the famous balm of Gilead was found; but by the side of the Dead Sea miasmatic salt-marshes extend for a length of several miles. The shores of this sea and also of the sea of Galilee send forth thermal springs impregnated with sulphur, and these serve to cure various maladies.

      The essentially mountainous configuration of Palestine was of great benefit to the Israelites. Two long and imposing mountain ranges, separated by a deep valley, raise their heads in the north, like two snow-capped giants. One of them is Mount Lebanon, the tallest peak of which has a height of more than 10,000 feet, and is named Dhor el-Khedib. The other mountain is Hermon (the Anti-Lebanon), the highest point of which, the Sheikh, has an elevation of 9,300 feet. The Lebanon was never included in the land of Israel; it remained in the possession of the Phœnicians, the Aramæans, and the people who succeeded the latter. This mountain range was of practical utility to the Israelites, who derived from its celebrated cedar forests the material for their edifices. Besides this, its lofty and odoriferous crests formed a favourite theme in the imagery of the Hebrew poets. Mount Hermon, with its snow-covered head, touches the north side of the ancient territory of Israel. This mountain, if not hidden by intervening hills, forms a charming object of admiration even at a distance of a hundred miles.

      The spurs of these two ranges were continued in the northern mountains of Israel (Mount Naphtali, subsequently named the mountains of Galilee), the highest peak of which rises to 4,000 feet. These heights have a gradual slope towards the great and fertile plain of Jezreel, which is only 500 feet above the level of the sea. Several mountain ranges intersect this plain and divide it into smaller plains. Mount Tabor (1,865 feet high) is not so much distinguished for its height as for its cupola shape. Mount Moreh (1,830 feet), now called Ed-Duhy, seems to lean against Mount Tabor. Not far from there, somewhat towards the east, run the hill-tops of Gilboa (2,000 feet). On the west side of the great plain lies the extensive tree-crested range of Carmel, which forms a wall close to the sea. The great plain of Jezreel has the shape of an irregular triangle, with a length of twenty miles from north to south, and a breadth of from six to fifteen miles from east to west, having the mountain border of Carmel on the one side and that of Gilboa on the other. This plain divides the land into two unequal parts. The northern half, which is the smaller, received at a later time the name of Galilee. On the south of this plain, the ground gradually rises, and, at one point, attains an elevation of 2,000 feet. This district was called Mount Ephraim. From Jerusalem, southwards to Hebron, the land again ascends to a height of 3,000 feet, forming the land of Judah. Here there is a gradual descent, and at the old frontier town of Beersheba the level does not rise above 700 feet. At this point begins the table-land of Mount Paran. This district was not included in the actual territory of Israel. Both Mount Ephraim and Mount Judah have a slope from east to west. Between the mountain-side and the Mediterranean Sea, from north to south, that is, from Carmel to the southern steppe, extends a plain of increasing breadth, which is called "the Plain of Sharon," or the "low country" (shefelah). In the east the mountain declines towards the Jordan. Some peaks of this mountain acquired a special significance. Such were the two hills by the side of Shechem, Gerizim, "the mountain of the blessing" (2,650 feet), and Ebal, "the mountain of the curse" (2,700 feet); Bethel, in the east (2,400 feet); Mizpeh, some hours' journey from the subsequent capital; Mount Zion (2,610 feet); and the Mount of Olives (2,700 feet). This peculiar and greatly varied configuration of the land had its effect not only upon the productions of the soil, but also upon the character of the people. From north to south, Palestine is divided into three belts. The broad mountainous tract occupies the centre; the low land (shefelah) extends from the west to the sea, and the meadows (kikkar, araboth) from the east to the Jordan. In the lowland the climate is mild; in the mountains, it is severe during the rainy season, but temperate in the summer. In the district of the Jordan the heat continues during the greater part of the year.

      With the exception of the Jordan, the land has no rivers which retain their waters throughout the year; but even this river, owing to its precipitous course, is not navigable. The Jordan rises from three sources in the slopes of Hermon. At first it runs sluggishly, and before entering the Lake of Merom it divides into small streams. On emerging from the lake, its waters are united in a narrow basalt bed, and flow into the Lake of Galilee. On issuing thence, the Jordan widens, rushes over rocks, and, after forming many rapids in its swift course, empties itself and disappears in the Dead Sea. During spring-time, when the melting snow of Hermon swells the waters, this river fertilises the adjoining low-lying plains, especially those on its eastern bank.

      The other streams, including the Jarmuk and Jabbok, become dry in the hot summer season. Such winter streams (nechalim), nevertheless, enhance the productiveness of the district through which they flow, and the cultivated lands are situated on the banks of these intermittent streams. The fertility of the soil is also favoured by the small springs which flow down the hills without being collected into rivulets. The districts devoid of springs are supplied with drinking-water by the rain, which is gathered in cisterns excavated in the rocks.

      The greater portion of Palestine is blessed with an abundant yield of produce. This is due to the nature of the soil, and to the copious drainage from the highlands of Lebanon, Hermon (Anti-Lebanon), with their spurs, as well as to the rain which falls twice a year. The land flowed "with milk and honey," and has retained this characteristic even to the present day, wherever the industry of man is active. It is decidedly a beautiful land "of brooks of water, of fountains and depths that spring out of valleys and hills; a land of wheat, and barley, and vines, and fig-trees, and pomegranates; a land of the oil-olive, and of honey; a land wherein thou shalt eat bread without scarceness, thou shalt not want anything in it; a land whose stones are iron, and out of whose hills thou mayest dig brass."7 The plains are especially fruitful, and yield to the laborious cultivator two crops a year. But also the land lying to the north of the plain of Jezreel is by no means sterile. In olden times it had such an abundance of olive trees as to give rise to the saying that the husbandman "dips his foot in oil."

      The central district to the south of the great plain, which belonged to Ephraim and Manasseh, rewarded its toilers with rich harvests. On all sides springs gush forth from the rocky fissures; and as their waters gather together, they attain sufficient force to drive the mills, besides supplying the soil with ample moisture. The land of the sons of Joseph was blessed,

      "With the fruit of the heavens above,

      And of the deep that coucheth beneath;

      And with precious fruit brought forth by the sun,

      And with the precious things put forth by the moon."8

      The hill-sides were adorned with blooming gardens, and with vineyards exuberantly laden with grapes. The mountains, overshadowed by forests of terebinths, oaks and yew trees, favoured the fertility of the valleys.

      In favourable situations the palm-tree produced a superabundance of sweet fruit, the juicy contents of which sometimes even trickled to the ground. There was less fruitfulness in the southern tracts, owing to the numerous chalk hills and the small number of valleys. But even here good pastures were found for the herds. Below Hebron the extreme south, СКАЧАТЬ