Topography and drainage Lake Edward lies at an elevation of , is long by wide at its maximum points, and covers a total surface area of , making it the 15th-largest on the continent. The lake is fed by the Nyamugasani River, the Ishasha River, the
Rutshuru River, the Ntungwe River, and the Rwindi River.
Lake George to the northeast empties into it via the
Kazinga Channel. Lake Edward empties to the north via the
Semliki River into
Lake Albert, where is joins the
White Nile, ultimately flowing to the
Nile. The western
escarpment of the Great Rift Valley towers up to above the western shore of the lake. The southern and eastern shores are flat
lava plains. The
Ruwenzori Mountains are north of the lake. ]
Volcanism The region shows much evidence of volcanic activity over the last 5000 years. The Katwe-Kikorongo and Bunyaruguru Volcanic Fields, with extensive cones and craters, lie either side of the
Kazinga Channel on the northwest shore of the lake. It is thought that Lakes George and Edward used to be joined as one larger lake, but lava from these fields flowed in and divided it, leaving only the Kazinga Channel as the remnant of the past union. To the south lies the May-ya-Moto thermally active volcano away, and the
Nyamuragira volcano in the western
Virunga Mountains lies south, but its lava flows have reached the lake in the past. High-resolution analyses of the elemental composition of calcite and biogenic silica (BSi) content in piston cores from Lake Edward, equatorial Africa, document complex interactions between climate variability and lacustrine geochemistry over the past 5400 years. The similarly sized
Bunyaruguru field on the other side of the Kazinga Channel contains about 30 crater lakes, some of which are larger than Lake Katwe.
Settlements Lake Edward lies completely within the Virunga National Park (DRC) and the
Queen Elizabeth National Park (Uganda) and does not have extensive human habitation on its shores, except at
Ishango (DRC) in the north, home to a park ranger training facility. About two-thirds of its waters are in the DRC and one third in Uganda. Apart from Ishango, the main Congolese settlement in the south is Vitshumbi, while the Ugandan settlements are Mweya and Katwe in the northeast, near the crater lake of that name, which is the chief producer of salt for Uganda. The nearest cities are
Kasese in Uganda to the northeast and
Butembo in the DRC to the northwest, which are respectively about and distant by road. ==Ecology==