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Waves Complete v9.6 (2016.03.23) OS X [dada]

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The ESV text may be quoted (in written, visual, or electronic form) up to and inclusive of five hundred (500) verses without express written permission of the publisher, providing that the verses quoted do not amount to a complete book of the Bible nor do the verses quoted account for twenty-five (25%) percent or more of the total text of the work in which they are quoted.

When quotations from the ESV text are used in non-saleable media, such as church bulletins, orders of services, posters, transparencies, or similar media, a complete copyright notice is not required, but the initials (ESV) must appear at the end of a quotation.

The shoreline runs for nearly three miles southward along the base of Jebel Usdum, and then sweeps sharply round to the east, leaving on the south a naked, miry plain called Sabkah, ten miles long from north to south by about six wide. It is in summer coated with a saline crust, but is so low that when the water is high a large section of it is flooded. Numerous torrent beds from the salt range on the west, and from the higher ground of the Arabah on the south, run across it, converting large portions into impassable swamps. On its southern border the old diluvium terrace rises like a white wall to a height of more than two hundred feet. It is only on getting close to it that the sides are seen to be rent and torn into a thousand fantastic forms by winter torrents and the wearing away of the softer deposits. The Sabkah is bounded on the east by Wady Tufeileh, one of the principal drains of the Arabah, and containing a brackish, perennial stream.

Beyond it the character of the surface completely changes. The ground rises in an easy slope to the foot of the Moab Mountains, and is covered with dense thickets of reeds, tamarisk, acacia, retem, zyziphus, and other shrubs, intermixed with fertile fields, cultivated by the Ghawarineh Arabs (as the inhabitants of the Ghor are called, here the worst representatives of their race), and producing abundant crops of wheat, maize, indigo, melons, and cucumbers. Tristram says: "The place positively swarmed with birds in countless myriads. There were doves by the score on every bush, large and small (Turtur risorius and T. Aegyptius), bulbuls, the hopping-thrush, shrikes, the gorgeous little sun-bird resplendent in the light, and, once more, our new sparrow. The Abyssinian lark, pipits, and wagtails luxuriated in the moist rills at our feet, which were fringed by drooping tufts of caper (Capparis Aegyptiaca) in full flower. All teemed with a prodigality of life" (p. 336).

The Peninsula of el-Lisan, "the Tongue" SEE BAY, is the most remarkable feature on the eastern shore. It juts out opposite the great ravine of Kerak. The neck connecting it with the mainland is a strip of low, bare sand, measuring five miles across. In outline the peninsula bears some resemblance to the human foot, the toe projecting northward and forming a sharp promontory. Its length is about nine miles, and from the heel or southwestern point to the southern shoreline is seven miles. The main body is a Post-tertiary deposit composed of layers of marl, gypsum, and sandy conglomerate, manifestly coeval with the great diluvial terrace, and corresponding with it in elevation. The top is a table land, broad towards the south, but gradually narrowing to a serried ridge at the northern end. It is white and almost entirely destitute of vegetation. The surface is all rent and torn by torrent beds; and the sides are worn away into pyramidal masses resembling lines and groups of white tents. It is worthy of special note that in the wadys and along the shores pieces of sulphur, bitumen, rock salt, and pumice stone are found in great profusion. Probably, if examined with care, geological phenomena similar to those in Wady Mahawat might be found on this peninsula, and some additional light thus thrown upon the destruction of the cities of the plain. Poole says "the soil appeared sulphurous" (Journal R.G.S. 26, 62-64).

The plain between the mountains and the mouth of the Jordan is in general well watered, and covered with luxuriant vegetation and occasional thickets of tamarisk, retem, and acacia. At the ruins of Suweimeh, De Saulcy found a copious hot spring with a ruinous aqueduct (Voyage en Terre-Sainte, 1, 317). Along the shore pieces of pumice stone, lava, and bitumen are found imbedded in the sand and mud as if washed up by the waves; and at this point are more distinct traces of volcanic action than elsewhere around the sea.


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