Mesopotamian Archaeology: An introduction to the archaeology of Mesopotamia and AssyriaHandcock, Percy S. P. (Percy Stuart Peache)
History
Mesopotamian Archaeology: An introduction to the archaeology of Mesopotamia and Assyria
Handcock, Percy S. P. (Percy Stuart Peache)
Iraq -- Antiquities
Thus the physical characteristics of the country in which Babylonian
civilization was developed, if it was not actually the place of its
origin, form a close parallel to those of Lower Egypt; in Egypt however
such evidence as there is, would indicate the South, or Upper Egypt as
the earliest scene of civilization, the North being conquered by the
Mesniu (Metal-users) of the South, not only in the battle-field but also
in culture and civilization. Both countries have but a small sea-board
where their rivers find an outlet, the Nile into the Mediterranean, and
the Tigris and Euphrates into the Persian Gulf; both countries had
emerged and were yearly emerging out of the sea, for it is certain that
at one time the Mediterranean penetrated as far south as Esneh, while as
already mentioned, the Persian Gulf extended at least as far as Babylon;
we are accordingly not surprised to find in both the Babylonian and
Egyptian cosmologies a tradition which told of the creation of the world
out of a primæval mass of water, though this idea looms less
conspicuously in the Egyptian than in the Babylonian and Hebrew
cosmologies. Both countries also were visited by a yearly inundation
which, while it brought no small amount of devastation in its train, at
the same time deposited the mud so essential to the enrichment of the
soil, the desolation being checked or at least mitigated in either
country by an elaborate system of irrigation canals, which same canals
were in the summer-time the means of conveying the life-giving water to
the dry and thirsty land. Both Babylonia and Egypt enjoy a warm climate,
though Egypt is much more dry and therefore healthier, and the
corresponding dryness of its soil has preserved the tangible evidences
of its ancient history in a far more perfect condition than the
marsh-country of Lower Mesopotamia; and lastly the climate of Egypt is
not subject to the same violent changes of temperature incidental to
the seasons in the Valley of the Euphrates.
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