Geology -- Egypt; Nile River; Water-supply -- Egypt
9. =Lake Victoria Nyanza.=--Lake Victoria, the true source of the Nile,
lies on the Equator, and fed by abundant rains and numerous streams,
discharges its surplus waters over the Ripon Falls, and gives birth to
the Victoria Nile. Its most important feeder, the Kagera, whose
southernmost tributary rises in the Kangosi hills 2000 metres above sea
level in south latitude 4°, has a length of some 600 kilometres. The
direct line across the lake from the mouth of the Kagera to the Ripon
Falls is 220 kilometres, so that in academical language the length of
the Nile at the Ripon Falls is already 820 kilometres. Lake Victoria
lies 1129 metres above sea level, and has an area of 60,000 square
kilometres; though until the parallels of longitudes are definitely
settled, the lake may be credited with an area of between 60,000 and
65,000 square kilometres, constituting it the largest fresh water lake
in the old world. Its waters are beautifully clear and perfectly sweet.
The depth of the lake is not great and it is covered with many islands.
The greatest depth found by Commander Whitehouse in the northern half of
the lake has been 73 metres, while the bays are shallow. The northern,
southern and eastern shores of the lake, as described by Sir William
Garstin, are generally clear, while the western shore, especially at the
mouth of the Kagera, is flat, marshy and covered with papyrus. The
country surrounding the lake is undulating or hilly and rises to a
height of 700 metres above the lake at the south-east corner. The rocks
are generally granites, chrystalline schists and quartzites, etc. The
hills are covered with red clay and marl on the higher lands, while the
valleys consist of a rich black loam.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account