Читать книгу Harper's New Monthly Magazine, No. XXVII, August 1852, Vol. V - Various - Страница 6

MEMOIRS OF THE HOLY LAND
BAY OF ACRE

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At length the great plain of Acre, with the bay, and the broad expanse of the Mediterranean in the distance, opens before him. The town of Acre, surrounded with its white walls, stands just on the margin of the water, at the northern extremity of the bay; while at the southern point of it stands Haïfa, sheltered by the mountain, and adorned by the consular flags of the several nations who have commercial agents there. In former times the principal harbor for shipping was at Acre, but from some change which the course of time has effected in the conformation of the coast or in the deposit of sand, the only deep water is now found at the southern extremity of the bay, where the Kishon finds its outlet – and Haïfa has consequently become the port. It is not improbable, in fact, that the greater depth of water at this point is to be attributed to the effect produced by the outflow of the river in impeding the accumulation of deposits from the sea.

The river, as will be seen from the map, in flowing into the bay passes across the beach of sand. Its depth and the quantity of water which issues from it vary very much, according to the season of the year, and thus the accounts of travelers who ford it at different periods differ extremely. In its ordinary condition it is very easily forded, but sometimes, when swollen with rains, it overflows the meadows that line its banks, up the valley, and becomes wholly impassable near its mouth. In the summer the stream often becomes so low that the sea, incessantly rolling in from the offing, fills up the outlet entirely with sand, and then smoothing over the dyke which it has made, it forms a beach on the outer slope of it, and thus the sandy shore of the bay is carried continuously across the mouth of the river, and the water is shut back as by a dam.

The next rain, however, and perhaps even the ordinary flow of the river, causes the water to accumulate and rise behind this barrier until it surmounts it. A small stream then begins to flow over the beach – rapidly increasing in force and volume as the sand is washed away – and thus the river regains once more its accustomed channel. This alternate closing and opening of the outlet of a river is a phenomenon often witnessed in cases where the river, at its mouth, traverses a sandy beach on a coast exposed to winds and storms.[3]

The distance from Haïfa to Acre along the shore of the bay is about eight miles. Acre itself has always been a very celebrated fortress, having figured as the central point of almost all great military operations in Syria for nearly two thousand years. It has experienced every possible form and phase of the fortune of war, having been assaulted, defended, besieged, destroyed, and rebuilt again and again, in an endless succession of changes, and in the experience of every possible fortune and misfortune which twenty centuries of uninterrupted military vicissitude could bring. Within the knowledge of the present generation it has been the scene of two terrific conflicts. Perhaps the most important of these events, in a historical point of view, was the struggle for the possession of the place between Napoleon and its English defenders, and the consequent check which was placed upon Napoleon's career, on his advance from Egypt into Syria. On his arrival at Acre, the young general found the port in possession of an English force under the command of Sir Sydney Smith, and though he made the most desperate and determined efforts to dislodge them, he was unable to succeed. He planted his batteries on the declivities of the hills behind the town, and cannonaded the walls from that position; while the English supported the garrison in their defense of the place, by firing upon the batteries of the besiegers from ships which they had anchored in the bay.

3

A striking example of this occurs at Long Branch in New Jersey, where a stream crosses the beach in entering the sea, at a point about half a mile to the southward of the hotels resorted to on that coast in summer by bathers. The visitor who walks along the shore in that direction, sometimes at a certain point finds himself upon an elevated sandy ridge, with the surf of the sea rolling in upon one side of it, and what appears to be a large inland pond lying quietly on the other. A few days afterward, on visiting the spot, he observes, perhaps, that the pond has disappeared; and a wide chasm has been made across the ridge of sand that he walked over before in safety, through the centre of which a small stream is flowing quietly into the sea. Neither of these views are of a nature to awaken any very special interest, except when they are considered in connection with each other: but if the observer should chance to come upon the ground when the pond is nearly full, he may witness a very extraordinary spectacle in the rushing out of the torrent by which the barrier is carried away. The boys of the vicinity often find amusement in hastening the catastrophe, by digging a little channel in the sand with their hands, when the water has risen nearly to the proper level. The stream that flows through this opening is at first extremely small, but it grows wider, deeper, and more rapid every moment, as the opening enlarges, and soon becomes a roaring torrent, spreading to a great width, and tossing itself into surges and crests as it rushes down the slope into the sea, in the most wild and tumultuous manner.

The spectacle is almost equally imposing when, after the pond has emptied itself, and the tide begins to rise, the surf of the sea engages in its work of reconstructing the dam.

Harper's New Monthly Magazine, No. XXVII, August 1852, Vol. V

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