Lake Victoria

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This page is about the African lake. For the Australian lake, see Lake Victoria (New South Wales).

Lake Victoria
Lake Victoria, as seen from space
Coordinates	2°3′S 33°4′E,
Lake type	Rift Valley Lake
Primary sources	Kagera River
Primary outflows	White Nile River
Catchment area	184,000 km² 238,900 km² basin
Basin countries	Tanzania Uganda Kenya
Max-length	337 km
Max-width	240 km
Surface area	68,800 km²
Average depth	40 m
Max-depth	84 m
Water volume	2,750 km³
Shore length1	3,440 km
Surface elevation	1,133 m
Islands	3,000 Ssese Islands, Uganda
Settlements	Bukoba, Tanzania Mwanza, Tanzania Kisumu, Kenya Kampala, Uganda Entebbe, Uganda
1 Shore length is an imprecise measure which may not be standardized for this article.

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.

[edit] Geology

Lake Victoria is relatively young; its current basin formed only 400,000 years ago, when westward-flowing rivers were dammed by an upthrown crustal block.^[1] The lake's shallowness, limited river inflow, and large surface area relative to its volume make it vulnerable to climate changes; cores taken from its bottom show that Lake Victoria has dried up completely three times since it formed.^[2] These drying cycles are probably related to past ice ages, which are times when precipitation declined globally.^[3] The lake last dried out 17,300 years ago, and filled again beginning 14,700 years ago; the fantastic adaptive radiation of its native cichlids has taken place in the short period of time since then.^[4]

[edit] Exploration history

The first recorded information about Lake Victoria comes from Arab traders plying the inland routes in search of gold, ivory, other precious commodities and slaves. 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 lake as seen from space, looking west, with other members of the African Great Lakes forming an arc in the middle distance. The cloud-covered forests of the Congo can be made out in the distance.

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.

[edit] 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. In 1954, the Nile perch (Lates niloticus) was first introduced into the lake's ecosystem in an attempt to improve fishery yields of in the lake. Introduction efforts intensified during the very early 1960's. The species was present in small numbers until the early to mid 1980's, when it underwent a massive population expansion and came to dominate the fish community and ecology of the world's largest tropical lake. Also introduced was Nile tilapia (Oreochromis niloticus), now an important food fish for local consumption. The Nile perch proved ecologically and socioeconomically devastating. Together with pollution born of deforestation and overpopulation (of both people and domestic animals), the Nile perch has brought about a massive transformation in the lake ecosystem and to the disappearance of hundreds of endemic haplochromine cichlid species. Many of these are now presumed to be extinct.

Also vanished from Lake Victoria is one of two native species of tilapia (another kind of cichlid fish), known as the ngege, Oreochromis esculentus. The ngege is superior in taste and texture to Nile tilapia, but it does not grow as fast or as large and produces fewer young. Ngege and some representatives of haplochromine diversity survive in minute swamp ponds and lakes that dot the Lake Victoria Basin. The initial good returns on Nile perch catches, at their peak delivering export revenues of several hundred million dollars a year, have diminished dramatically due to poor enforcement of fisheries regulations. The proceeds from Nile perch sales remain an important economic engine in the region, but the resulting wealth is very poorly distributed and the overall balance sheet on the Nile perch introduction to Lake Victoria is well into the red despite the enormous value of the perch landings as an export commodity.

The three countries bordering Lake Victoria- Uganda, Kenya and Tanzania- have agreed in principle to the idea of a tax on Nile perch exports, proceeds to be applied to various measures to benefit local communities and sustain the fishery. However, this tax has not been put into force, enforcement of fisheries and environmental laws generally are lax, and the Nile perch fishery remains in essence a mining operation. Currently, the Nile perch is being overfished. Populations of a few endemic cichlid species have increased again, particularly two or three species of zooplankton-eating, herring-like cichlids (Yssichromis) that school with an abundant native minnow known locally as dagaa (Tanzania), omena (Kenya), or mukene (Uganda). In 1996 The World Bank funded a project to restore and sustain the ecology of Lake Victoria and its fisheries, called LVEMP (Lake Victoria Environmental Management Project).

Meanwhile, the EU invested another large sum in fisheries infrastructure and monitoring. Few of the excellent intentions of these projects have been actualized despite massive expenditures, but the potential for things to be set aright is still great and through it all the ecology of Lake Victoria, in its new incarnation, has proven amazingly resilient. One beneficial product of these foreign aid programs has been the training of a new generation of east African aquatic ecologists, conservation professionals, and fisheries scientists. There has also been a renaissance in the fishery research institutes of the lake. Unfortunately, few of the new professionals find jobs, and fewer still find jobs that allow them to apply what they have learned to solving, rather than perpetuating, the deep problems that still beset the relationship between people and the lake.

An annual migration of blue wildebeest and other bovids arrives at Lake Victoria to find dry season forage. this is one of the largest bovid migrations on the African continent.

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 with very good results.

[edit] Nalubaale dam

An Island on the Lake

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.

[edit] 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. The steamer MV Bukoba sank in the lake on May 21, 1996, killing nearly 1,000 people in one of Africa's worst maritime disasters.

[edit] See also

• Great Lakes
• Rift Valley lakes

[edit] References

1. ^ Reader, John. Africa. Washington, D.C.: National Geographic Society, 2001. p. 227
2. ^ Reader, p. 228
3. ^ Reader, p. 228
4. ^ Reader, p. 228

[edit] External links

• Bibliography on Water Resources and International Law See Lake Victoria. Peace Palace Libray
• 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.