Lake Naivasha
| Lake Naivasha | |
|---|---|
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| Coordinates | Lua error in package.lua at line 80: module 'strict' not found. |
| Basin countries | Kenya |
| Surface area | 139 km² |
| Average depth | 6 m (20 ft) |
| Max. depth | 30 m (100 ft) |
| Surface elevation | 1,884 m (6,180 ft) |
Lake Naivasha is a freshwater lake in Kenya, outside the town of Naivasha in Nakuru County, which lies north west of Nairobi. It is part of the Great Rift Valley. The name derives from the local Maasai name Nai'posha, meaning "rough water" because of the sudden storms which can arise.
Contents
Location
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Lake Naivasha is at the highest elevation of the Kenyan Rift valley at 1,884 metres (6,181 ft) in a complex geological combination of volcanic rocks and sedimentary deposits from a larger Pleistocene era lake. Apart from transient streams, the lake is fed by the perennial Malewa and Gilgil rivers. There is no visible outlet, but since the lake water is relatively fresh it is assumed to have an underground outflow.[1]
The lake has a surface area of 139 km², [2] and is surrounded by a swamp which covers an area of 64 square km, but this can vary largely depending on rainfall. It is situated at an altitude of 1,884 metres (6,180 ft).[2] The lake has an average depth of 6 m (20 ft), with the deepest area being at Crescent Island, at a maximum depth of 30 m (100 ft).[2] Njorowa Gorge used to form the lake's outlet, but it is now high above the lake and forms the entrance to Hell's Gate National Park. The town of Naivasha (formerly East Nakuru) lies on the north-east edge of the lake.
Ecology
The lake is home to a variety of types of wildlife including over 400 different species of bird and a sizeable population of hippos. The fish community in the lake has been highly variable over time, influenced by changes in climate, fishing effort and the introduction of invasive species. The most recent shift in the fish population followed the accidental introduction of common carp in 2001.[3] Nine years later, in 2010, common carp accounted for over 90% of the mass of fish caught in the lake.[4]
There are two smaller lakes in the vicinity of Lake Naivasaha: Lake Oloiden and Lake Sonachi (a green crater lake). The Crater Lake Game Sanctuary lies nearby, while the lake shore is known for its population of European immigrants and settlers.
History
Between 1937 and 1950, the lake was used as a landing place for flying boats on the Imperial Airways passenger and mail route from Southampton in Britain to South Africa. It linked Kisumu and Nairobi. Joy Adamson, the author of Born Free, lived on the shores of the lake in the mid-1960s. On the shores of the lake is Oserian ("Djinn Palace"), which gained notoriety in the Happy Valley days between the two world wars. It now forms part of the Oserian flower farm. In 1999, the Lake Naivasha Riparian Association received the Ramsar Wetland Conservation Award for its conservation efforts regarding the Lake Naivasha Ramsar site.
Agriculture and Industry
Floriculture forms the main industry around the lake. However, the largely unregulated use of lake water for irrigation is reducing the level of the lake and is the subject of concern in Kenya. [5] Fishing in the lake is also another source of employment and income for the local population. The lake varies in level greatly and almost dried up entirely in the 1890s. Lake levels in general follow the rainfall pattern in the catchment area.
In 1981, the first geothermal plant for Lake Naivasha was commissioned and by 1985, a total of 45 MW of electricity was being generated in the area.[2]
The water level for Lake Naivasha reached a low level of 0.6 m depth in 1945, but the water level rose again, with minor drops, to reach a maximum depth nearly 6 m in 1968.[2] There was another major decline of the water level in 1987, when the depth reached 2.25 m above the lake bottom.[2] The decline of the lake water level in 1987 increased concern in the future of geothermal industry, and it was speculated that Lake Naivasha underground water might be feeding the geothermal reservoir at Olkaria.[2] Hence, the decline in the lake water would affect the future of the geothermal industry.
References
- ↑ Harper 2003, p. 1.
- ↑ 2.0 2.1 2.2 2.3 2.4 2.5 2.6 "THE OUTFLOW OF LAKE NAIVASHA BASED ON THE STABLE ISOTOPE COMPOSITION" (characteristics), M.K. Arusei, J. K Sanga, M.P Tole, Department of Chemistry, School of Environmental Studies, Moi University, P.O Box 3900 Eldoret, Kenya, webpage: UNEP-Moi-Arusei-PDF.
- ↑ [ Becht, R., Odada, E. O., & Higgins, S. (2005). Lake Naivasha: Experience and Lessons Learned Brief. Managing lakes and basins for sustainable use, a report for lake basin managers and stakeholders (pp. 277-298). Kusatsu: International Lake Environment Committee Foundation (ILEC).]
- ↑ [Lake Naivasha Annual Fisheries Report, 2010]
- ↑ Lua error in package.lua at line 80: module 'strict' not found.
Sources
- Lua error in package.lua at line 80: module 'strict' not found.
