The Bangweulu swampsare formed by the flooding of the lower Chambeshi River. After much court-wrangling and lengthy hearings on the project, the plan was disposed of by the European company as they built a detour for their pipeline in the surrounding province. The lake is approximately 80 km long and 40 km wide. Bangweulu is one of the world’s great wetland systems, comprising Lake Bangweulu, the Bangweulu Swamps and the Bangweulu Flats or floodplain. The southern floodplains are famous for large herds of the near-endemic Water temperatures at the surface of the Bangweulu system ranged from 25.8 to 28.3°C in November 1993 and from 23.7 to 27.1°C in February 1994.The lake was known to Europeans from reports by chiefs such as It was a desire for the riches of Bangweulu's fisheries and game-rich floodplain which motivated King In early 2004 a private European natural gas company finished preliminary plans to lay a pipeline which would cut directly through the Southeast portion of the Lake. ), 1997. This plan was met with harsh opposition from the local people as well as environmental activists. The Bangweulu is renowned for its vast population of endemic black Lechwe antelope that occur in herds of up to several thousands. It is shallow and friendly with an average depth of 4 metres while the deepest point is 9 metres. These are particularly striking in satellite photographs and are easily seen along the north-western shore, the Lifunge Peninsula There are numerous bays, inlets, smaller lakes and lagoons around Lake Bangweulu, connected by open water, narrow channels or swamps. The basin is fed by 17 principle rivers from a catchment area of 190 000 kms2 , … The lake has an average depth of only 4 m. The Bangweulu system is fed by about seventeen rivers of which the Chambeshi (the source of the Congo River) is the largest, and is drained by the Luapula River. The combined area of the lake and wetlands reaches 15,000 km². The Bangweulu swamps are fed mainly from the north-east by the There are numerous lagoons in the swamps, the more prominent ones are: On the northern side there are several wide swampy estuaries where rivers enter the lake or swamps, going from north-west to north-east they are: Lupososhi Estuary On the eastern and south-eastern sides the swamps are fed by the Munikashi, Luitikila, Lumbatwa, Lukulu and Lulimala rivers.In the main part of the swamps, just south of Chilubi Island, is a large area which is very shallow in the flood season and may become fairly dry at the end of the dry season, called the Lunga Bank The lake is commonly assumed to be a prime habitat for Large grassy floodplains with an area of about 3,000 km² lie mainly south of the swamps, but also in the north-north-east, acting as an extension of the region in the wet season. The lake is drained in the South by the Luapula River, a tributary of the Congo River. The flooded area reaches 15,000 km². Volume: 5.00 km 3: Surface Area: 9,840.00 km 2: Depth: Mean depth: 4.0 m Maximum depth: 10.0 m Type: Fresh Permanent Lua error in Module:Citation/CS1 at line 3738: attempt to index field 'punct_skip' (a nil value). It is a breathtakingly beautiful place to visit.But the area is so incredibly vast it is largely left to the multitudes of wildlife that dwell on the rich resources. With a long axis of 75 km and a width of up to 40 km, Lake Bangweulu’s permanent open water surface is about 3,000 km², which expands when its swamps and floodplains are in flood during the wet season between November and March. Bangweulu — 'where the water sky meets the sky' — is one of the world's great wetland systems, comprising Lake Bangweulu, the Bangweulu Swamps and the Bangweulu Flats or floodplain. Lake Bangweulu: Inland lake - See 14 traveler reviews, 19 candid photos, and great deals for Samfya, Zambia, at Tripadvisor.