History Of Egypt, Chaldæa, Syria, Babylonia, and Assyria, Volume 1 (of 12) — John Shaqi
History Of Egypt, Chaldæa, Syria, Babylonia, and Assyria, Volume 1 (of 12)Maspero, G. (Gaston)
History
History Of Egypt, Chaldæa, Syria, Babylonia, and Assyria, Volume 1 (of 12)
Maspero, G. (Gaston)
Civilization, Ancient; Egypt -- History -- To 640 A.D.; History, Ancient; Middle East -- History
The White Nile is indebted to the Great Lakes for the greater
persistence of its waters, which feed the river as far as the
Mediterranean, and save the valley from utter drought in winter. But,
even with this resource, the level of the water falls daily, and its
volume is diminished. Long-hidden sandbanks reappear, and are again
linked into continuous line. Islands expand by the rise of shingly
beaches, which gradually reconnect them with each other and with the
shore. Smaller branches of the river cease to flow, and form a mere
network of stagnant pools and muddy ponds, which fast dry up. The main
channel itself is only intermittently navigable; after March boats run
aground in it, and are forced to await the return of the inundation for
their release. From the middle of April to the middle of June, Egypt is
only half alive, awaiting the new Nile.
[Illustration: 034.jpg ASSIOUT]
Those ruddy and heavily charged waters, rising and retiring with almost
mathematical regularity, bring and leave the spoils of the countries
they have traversed: sand from Nubia, whitish clay from the regions
of the Lakes, ferruginous mud, and the various rock-formations of
Abyssinia. These materials are not uniformly disseminated in the
deposits; their precipitation being regulated both by their specific
gravity and the velocity of the current. Flattened stones and rounded
pebbles are left behind at the cataract between Syene and Keneh, while
coarser particles of sand are suspended in the undercurrents and serve
to raise the bed of the river, or are carried out to sea and form the
sandbanks which are slowly rising at the Damietta and Rosetta mouths of
the Nile. The mud and finer particles rise towards the surface, and are
deposited upon the land after the opening of the dykes. Soil which is
entirely dependent on the deposit of a river, and periodically invaded
by it, necessarily maintains but a scanty flora; and though it is well
known that, as a general rule, a flora is rich in proportion to its
distance from the poles and its approach to the equator, it is also
admitted that Egypt offers an exception to this rule. At the most, she
has not more than a thousand species, while, with equal area, England,
for instance, possesses more than fifteen hundred; and of this thousand,
the greater number are not indigenous. Many of them have been brought
From Central Africa by the river: birds and winds have continued
the work, and man himself has contributed his part in making it more
complete. From Asia he has at different times brought wheat barley
the olive, the apple, the white or pink almond, and some twenty
other species now acclimatized on the banks of the Nile. Marsh plants
predominate in the Delta; but the papyrus, and the three varieties of
blue, white, and pink lotus which once flourished there, being no longer
cultivated, have now almost entirely disappeared, and reverted to their
original habitats.
[Illustration: 036.jpg ENTRANCE OF THE MUDIRIYEH OF ASYUT.]
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