Lake Victoria
- This page is about the African lake. For the Australian lake, see Lake Victoria (New South Wales).
Lake Victoria or Victoria Nyanza (also known as Ukerewe and Nalubaale) is one of the Great Lakes of Africa.
Lake Victoria is 68,800 square kilometres (26,560 mi²) in size, making it the continent's largest lake, the largest tropical lake in the world, and the second largest fresh water lake in the world in terms of surface area. Being relatively shallow for its size, with a maximum depth of 84 m (276 ft) and a mean depth of 40 m (131 ft), Lake Victoria ranks as the seventh largest freshwater lake by volume, containing 2,750 cubic kilometres (2.2 million acre-feet) of water. It is the source of the longest branch of the Nile River, the White Nile, and has a catchment area of 184,000 square kilometres (71,040 mi²). The lake lies within an elevated plateau in the western part of Africa's Great Rift Valley and is subject to territorial administration by Tanzania, Uganda and Kenya. The lake has a shoreline of 3,440 km (2138 miles), and has more than 3,000 islands, many of which are inhabited. These include the Ssese Islands in Uganda, a large group of islands in the northwest of the Lake that are becoming a popular destination for tourists.
Exploration history
The first recorded information about Lake Victoria comes from Arab traders plying the inland routes in search of gold, ivory, slaves and other precious commodities. An excellent map known as the Al Adrisi map dated from the 1160s, clearly depicts an accurate representation of Lake Victoria, and attributes it as being the source of the Nile.
The lake was first sighted by Europeans in 1858 when the British explorer John Hanning Speke reached its southern shore whilst on his journey with Richard Francis Burton to explore central Africa and locate the great Lakes. Believing he had found the source of the Nile on seeing this vast expanse of open water for the first time, Speke named the lake after the then Queen of the United Kingdom. Burton, who had been recovering from illness at the time and resting further south on the shores of Lake Tanganyika, was outraged that Speke claimed to have proved his discovery to have been the true source of the Nile when Burton regarded this as still unsettled. A very public quarrel ensued, which not only sparked a great deal of intense debate within the scientific community of the day, but much interest by other explorers keen to either confirm or refute Speke's discovery.
The well known British explorer and missionary David Livingstone failed in his attempt to verify Speke's discovery, instead pushing too far west and entering the Congo River system instead. It was ultimately the American explorer Henry Morton Stanley who confirmed the truth of Speke's discovery, circumnavigating the Lake and reporting the great outflow at Rippon Falls on the Lake's northern shore. It was on this journey that Stanley was said to have greeted the British explorer with the famous words Dr. Livingstone, I presume?, upon discovering the Scotsman ill and despondent in his camp on the shores of Lake Tanganyika. Lake Victoria also has many sea monsters.
Ecology and social impacts
Lake Victoria plays a vital role in supporting the millions of people living around its shores, in one of the most densely populated regions on earth.
The ecosystem of Lake Victoria and its surroundings have been badly affected by human influence. During the 1950s, the nile perch (Lates niloticus) was introduced into the lake's ecosystem in an attempt to improve the yields of fishing in the lake. The nile perch proved totally devastating to the local ecosystem – of the hundreds of endemic species, many are now extinct. Further, the initial good returns on nile perch catches has diminished dramatically. Currently, the nile perch is being overfished. It is reported that some populations of endemic species have increased again.
An eco-problem with a happier outcome was the fight against the huge increase of Water Hyacinth (Eichhornia crassipes), a native of the tropical Americas, which forms thick mats of plant causing difficulties to transportation, fishing, hydroelectic power generation and drinking water supply. By 1995, 90% of the Ugandan coastline was covered by the plant. With mechanical and chemical control of the problem seeming unlikely, the mottled water hyacinth weevil, (Neochetina eichhorniae) was bred and released into the lake with very good results.
Nalubaale dam
The only outflow for Lake Victoria is at Jinja, Uganda where it forms the Victoria Nile. The water originally drained over a natural rock weir. In 1954 British colonial engineers blasted out the weir and replaced it with the Owens Falls dam, now renamed the Nalubaale dam, turning the entire lake into a giant hydroelectric reservoir. A standard for mimicking the old rate of outflow called the "agreed curve" was established, setting the maximum flow rate at 300 to 1700 cubic meters per second (392 - 2224 yd³/sec) depending on the lake's water level.
In 2002 Uganda completed a second hydroelectric complex in the area. By 2006 the water levels in Lake Victoria had reached an 80-year low, and Daniel Kull, a hydrologist with the UN's International Strategy for Disaster Reduction in Nairobi, Kenya, calculated that Uganda was exceeding the agreed curve by 55% [1].
At 3500 cubic meters per second (4578 yd³), more than double the maximum agreed curve, it would take a year to drain 110.4 cubic km (89,500 acre-feet) from the lake. That is approximately 4% of the lake's volume.
Transportation
Since the 1900s Lake Victoria ferries have been an important means of transport between Uganda, Tanzania and Kenya. The main ports on the lake are Kisumu, Mwanza, Bukoba, Entebbe, Port Bell and Jinja.
See also
External links
- Lake Database: Data summary for Lake Victoria
- LakeNet
- Trouble in the Tropics
- Darwin's Nightmare, an award winning documentary film by Hubert Sauper on the global political economy of the Nile perch trade at Lake Victoria and its social consequences for the region.
- New Scientist article on Uganda's violation of the agreed curve for hydroelectric water flow.