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Legends of Babylon and Egypt in Relation to Hebrew Tradition.pdf

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eighteen milliards <strong>of</strong> <strong>to</strong>ns <strong>of</strong> water. See his work /The Irrigations <strong>of</strong> Mesopotamia/ (E. <strong>and</strong> F. N. Spon, 1911),<br />

/Geographical Journal/, Vol. XL, No. 2 (Aug., 1912), pp. 129 ff., <strong>and</strong> the articles <strong>in</strong> /The Near East/ cited on p. 97, n. 1,<br />

<strong>and</strong> p. 98, n. 2. Sir William Willcocks's volume <strong>and</strong> subsequent papers form the best <strong>in</strong>troduction <strong>to</strong> the study <strong>of</strong><br />

<strong>Babylon</strong>ian Deluge tradition on its material side.<br />

[3] Their works carried out on the Tigris were effective for irrigation; but the <strong>Babylon</strong>ians never succeeded <strong>in</strong><br />

controll<strong>in</strong>g its floods as they did those <strong>of</strong> the Euphrates. A massive earthen dam, the rema<strong>in</strong>s <strong>of</strong> which are still known<br />

as "Nimrod's Dam", was thrown across the Tigris above the po<strong>in</strong>t where it entered its delta; this served <strong>to</strong> turn the river<br />

over hard conglomerate rock <strong>and</strong> kept it at a high level so that it could irrigate the country on both banks. Above the<br />

dam were the heads <strong>of</strong> the later Nahrwân Canal, a great stream 400 ft. wide <strong>and</strong> 17 ft. deep, which supplied the<br />

country east <strong>of</strong> the river. The Nâr Sharri or "K<strong>in</strong>g's Canal", the Nahar Malkha <strong>of</strong> the Greeks <strong>and</strong> the Nahr el-Malik <strong>of</strong><br />

the Arabs, protected the right bank <strong>of</strong> the Tigris by its own high artificial banks, which can still be traced for hundreds<br />

<strong>of</strong> miles; but it <strong>to</strong>ok its supply from the Euphrates at Sippar, where the ground is some 25 ft. higher than on the Tigris.<br />

The Tigris usually flooded its left bank; it was the right bank which was protected, <strong>and</strong> a breach here meant disaster.<br />

Cf. Willcocks, op. cit., <strong>and</strong> /The Near East/, Sept. 29, 1916 (Vol. XI, No. 282), p. 522.<br />

It was only by constant <strong>and</strong> unremitt<strong>in</strong>g attention that disaster from flood could be averted; <strong>and</strong> the difficulties <strong>of</strong> the<br />

problem were <strong>and</strong> are <strong>in</strong>creased by the fact that the flood-water <strong>of</strong> the Mesopotamian rivers conta<strong>in</strong>s five times as<br />

much sediment as the Nile. In fact, one <strong>of</strong> the most press<strong>in</strong>g <strong>of</strong> the problems the Sumerian <strong>and</strong> early <strong>Babylon</strong>ian<br />

eng<strong>in</strong>eers had <strong>to</strong> solve was the keep<strong>in</strong>g <strong>of</strong> the canals free from silt.[1] What the floods, if left unchecked, may do <strong>in</strong><br />

Mesopotamia, is well illustrated by the decay <strong>of</strong> the ancient canal-system, which has been the immediate cause <strong>of</strong> the<br />

country's present state <strong>of</strong> sordid desolation. That the decay was gradual was not the fault <strong>of</strong> the rivers, but was due <strong>to</strong><br />

the sound pr<strong>in</strong>ciples on which the old system <strong>of</strong> control had been evolved through many centuries <strong>of</strong> labour. At the<br />

time <strong>of</strong> the Moslem conquest the system had already begun <strong>to</strong> fail. In the fifth century there had been bad floods; but<br />

worse came <strong>in</strong> A.D. 629, when both rivers burst their banks <strong>and</strong> played havoc with the dikes <strong>and</strong> embankments. It is<br />

related that the Sassanian k<strong>in</strong>g Parwiz, the contemporary <strong>of</strong> Mohammed, crucified <strong>in</strong> one day forty canal-workers at a<br />

certa<strong>in</strong> breach, <strong>and</strong> yet was unable <strong>to</strong> master the flood.[2] All repairs were suspended dur<strong>in</strong>g the anarchy <strong>of</strong> the<br />

Moslem <strong>in</strong>vasion. As a consequence the Tigris left its old bed for the Shatt el-Hai at Kût, <strong>and</strong> pour<strong>in</strong>g its own <strong>and</strong> its<br />

tributaries' waters <strong>in</strong><strong>to</strong> the Euphrates formed the Great Euphrates Swamp, two hundred miles long <strong>and</strong> fifty broad. But<br />

even then what was left <strong>of</strong> the old system was sufficient <strong>to</strong> support the splendour <strong>of</strong> the Eastern Caliphate.<br />

[1] Cf. /Letters <strong>of</strong> Hammurabi/, Vol. III, pp. xxxvi ff.; it was the duty <strong>of</strong> every village or <strong>to</strong>wn upon the banks <strong>of</strong> the<br />

ma<strong>in</strong> canals <strong>in</strong> <strong>Babylon</strong>ia <strong>to</strong> keep its own section clear <strong>of</strong> silt, <strong>and</strong> <strong>of</strong> course it was also responsible for its own smaller<br />

irrigation-channels. While the <strong>in</strong>vention <strong>of</strong> the system <strong>of</strong> bas<strong>in</strong>-irrigation was practically forced on <strong>Egypt</strong>, the<br />

extraord<strong>in</strong>ary fertility <strong>of</strong> <strong>Babylon</strong>ia was won <strong>in</strong> the teeth <strong>of</strong> nature by the system <strong>of</strong> perennial irrigation, or irrigation all<br />

the year round. In <strong>Babylon</strong>ia the water was led <strong>in</strong><strong>to</strong> small fields <strong>of</strong> two or three acres, while the Nile valley was<br />

irrigated <strong>in</strong> great bas<strong>in</strong>s each conta<strong>in</strong><strong>in</strong>g some thirty <strong>to</strong> forty thous<strong>and</strong> acres. The <strong>Babylon</strong>ian method gives far more<br />

pr<strong>of</strong>itable results, <strong>and</strong> Sir William Willcocks po<strong>in</strong>ts out that <strong>Egypt</strong> <strong>to</strong>-day is gradually ab<strong>and</strong>on<strong>in</strong>g its own system <strong>and</strong><br />

adopt<strong>in</strong>g that <strong>of</strong> its ancient rival; see /The Near East/, Sept. 29, 1916, p. 521.<br />

[2] See Le Strange, /The L<strong>and</strong>s <strong>of</strong> the Eastern Caliphate/, p. 27.<br />

The second great blow <strong>to</strong> the system followed the Mongol conquest, when the Nahrwân Canal, <strong>to</strong> the east <strong>of</strong> the Tigris,<br />

had its head swept away by flood <strong>and</strong> the area it had irrigated became desert. Then, <strong>in</strong> about the fifteenth century, the<br />

Tigris returned <strong>to</strong> its old course; the Shatt el-Hai shrank, <strong>and</strong> much <strong>of</strong> the Great Swamp dried up <strong>in</strong><strong>to</strong> the desert it is<br />

<strong>to</strong>-day.[1] Th<strong>in</strong>gs became worse dur<strong>in</strong>g the centuries <strong>of</strong> Turkish misrule. But the silt<strong>in</strong>g up <strong>of</strong> the Hillah, or ma<strong>in</strong>,<br />

branch <strong>of</strong> the Euphrates about 1865, <strong>and</strong> the transference <strong>of</strong> a great part <strong>of</strong> its stream <strong>in</strong><strong>to</strong> the H<strong>in</strong>dîyah Canal, caused<br />

even the Turks <strong>to</strong> take action. They constructed the old H<strong>in</strong>dîyah Barrage <strong>in</strong> 1890, but it gave way <strong>in</strong> 1903 <strong>and</strong> the<br />

state <strong>of</strong> th<strong>in</strong>gs was even worse than before; for the Hillah branch then dried entirely.[2]<br />

[1] This illustrates the damage the Tigris itself is capable <strong>of</strong> <strong>in</strong>flict<strong>in</strong>g on the country. It may be added that Sir William<br />

Willcocks proposes <strong>to</strong> control the Tigris floods by an escape <strong>in</strong><strong>to</strong> the Tharthâr depression, a great salt pan at the tail <strong>of</strong><br />

Wadi Tharthâr, which lies 14 ft. below sea level <strong>and</strong> is 200 ft. lower than the flood-level <strong>of</strong> the Tigris some thirty-two<br />

miles away. The escape would leave the Tigris <strong>to</strong> the S. <strong>of</strong> Sâmarra, the proposed Beled Barrage be<strong>in</strong>g built below it

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