The
River Nile
There is no better way to trace the course of Egyptian
history than to follow the course of the Nile. The river
has been Egypt's lifeline for millenniums, fertilizing
the narrow strip of land along its bank with a deposit of
silt after each annual inundation - now controlled by the
High Dam at Aswan. Along its length Pharaohs, nobles and
lesser mortals have all built monuments and tombs to
immortalize themselves.
The
Nile is Associated with Life
"Egypt is the gift of the River Nile", said
Herodotus, the great Greek historian, on his only visit
to Egypt. Egyptians would still agree wholeheartedly with
his words today. At the end of every year, they are eager
to hear good news about the water level in the River Nile.
In 1994 the volume of inlet water was considered high. In
the High Dam Lake, water reached its highest ever level.

boats
on Nile
|
Since
time immemorial, Egyptians have associated the
River Nile with life, fertility and development.
They care about it, and it, in turn, runs in
their blood. It has always been their source of
prosperity, and was the main factor in building
their great civilization. It is from the River
Nile that Egyptians draw their friendly character.
They have gained generosity, sincerity and
fidelity from its flow, flood and purity. Every
day, its banks witness thousands of true love
stories, as lovers meet on its banks. It provides
them with hope and promises them happiness. It
had always been a source of inspiration and
creativity for all kinds of arts. Many songs are
dedicated to the River Nile. And in ancient times,
Egyptians made sacrifices for its sake and
transmitted its legends through successive
generations. |
Nile
river:
From its major source, Lake Victoria in east Central
Africa, the Nile flows generally north through Uganda,
Sudan, and Egypt to the Mediterranean Sea, for 5584 km (3470
mi). From its remotest headstream , the Ruvyironza River
in Burundi, the river is 6671 km (4145 mi) long . The
river basin has an area of more than 3,349,000 sq km (1,293,049
sq mi). The Ruvyironza, regarded as the ultimate source
of the Nile, is one of the upper branches of the Kagera
River in Tanzania. The Kagera follows the boundary of
Rwanda northward, turns along the boundary of Uganda, and
drains into Lake Victoria.
On leaving Lake Victoria at the site of the now-submerged
Ripon Falls, the Nile rushes for 483 km (300 mi) between
high rocky walls and over rapids and cataracts, at first
northwest and then west, until it enters Lake Albert. The
section between the two lakes is called the Victoria Nile.
The river leaves the northern end of Lake Albert as the
Albert Nile, flows through northern Uganda, and at the
Sudan border becomes the Bahr al Jabal. At its junction
with the Bahr al Ghazal, the river becomes the Bahr al
Abyad, or the White Nile. At Khartoum the White Nile is
joined by the Blue Nile, or Bahr al Azraq, so named
because of the color of the water. The Blue Nile, 1529 km
(950 mi) long, gathers its volume mainly from Lake T'ana,
in the Ethiopian Highlands; it is known here as the Abbai.
From Khartoum the Nile flows northeast; 322 km (200 mi)
below that city, it is joined by the 'Atbarah River.
During its course from the confluence of the 'Atbarah
through the Nubian Desert, the river makes two deep bends.
The Nile enters the Mediterranean Sea by a delta that
separates into the Rosetta and Damietta distributaries.
The Nile river valley is home to a host of wildlife,
including Nile crocodile, hippopotamuses, more than 300
species of birds, and numerous fish species.
The first dam on the Nile, the High Dam, was built in
1902 and heightened in 1936. The Makwar Dam, now called
the Sennar Dam, was built across the Blue Nile south of
Khartoum following World War I (1914-1918) to provide
storage water for cotton plantations in the Sudan. A dam
at Jabal Awliya was constructed on the White Nile south
of Khartoum in 1937. But the Aswân High Dam, which
opened in the early 1970s, has most dramatically
transformed the ecology and economic role of the Nile. It
created one of the world's largest reservoirs, Lake
Nasser, allowed the Egyptian government to produce
hydroelectric power, control flooding, and minimize
droughts. But it has severely reduced sedimentation
deposits that the floodwaters once brought to the delta
and increased the river's salinity. Consequently , the
Nile delta has become less fertile, forcing Egyptian
farmers to increase the use of chemical fertilizers.
|