Title: Zambezi River Authority
Content:  The Zambezi originates in northwestern Zambia, and runs west and then southwest through Angola before reentering Zambia. It flows south and forms part of the border between Zambia and Namibia. After picking up the waters of the Chobe River at the quadripoint where Zambia, Namibia, Botswana and Zimbabwe meet, the river flows east along the border between Zambia and Zimbabwe, powering the shared Kariba Dam hydroelectric station, before entering Mozambique and flowing to the Indian Ocean. The Zambezi basin also includes parts of Malawi and Tanzania. The Zambezi is the fourth largest river in Africa after the Nile, Congo and Niger.
Title: Zambezi Watercourse Commission
Content:   The Zambezi originates in northwestern Zambia, and runs west and then southwest through Angola before reentering Zambia. It flows south and forms part of the border between Zambia and Namibia. After picking up the waters of the Chobe River at the quadripoint where Zambia, Namibia, Botswana and Zimbabwe meet, the river flows east along the border between Zambia and Zimbabwe, powering the shared Kariba Dam hydroelectric station, before entering Mozambique and flowing to the Indian Ocean. The Zambezi basin also includes parts of Malawi and Tanzania. The Zambezi is the fourth largest river in Africa after the Nile, Congo and Niger.
Title: Zambia
Content:  in Tanzania. In the Zambezi basin, there are a number of major rivers flowing wholly or partially through Zambia: the Kabompo, Lungwebungu, Kafue, Luangwa, and the Zambezi itself, which flows through the country in the west and then forms its southern border with Namibia, Botswana and Zimbabwe. Its source is in Zambia but it diverts into Angola, and a number of its tributaries rise in Angola's central highlands. The edge of the Cuando River floodplain (not its main channel) forms Zambia's southwestern border, and via the Chobe River that river contributes very little water to the Zambezi because most are lost by evaporation. Two of the Zambezi's longest 
Title: Zambezi
Content:  The Zambezi River (also spelled Zambeze and Zambesi) is the fourth-longest river in Africa, the longest east-flowing river in Africa and the largest flowing into the Indian Ocean from Africa. The area of its basin is 1390000 km2, slightly less than half of the Nile's. The 2574 km rises in Zambia and flows through eastern Angola, along the north-eastern border of Namibia and the northern border of Botswana, then along the border between Zambia and Zimbabwe to Mozambique, where it crosses the country to empty into the Indian Ocean. The Zambezi's most noted feature is Victoria Falls. Other notable falls include the Chavuma Falls at the border between Zambia and Angola, and Ngonye Falls, near Sioma in Western Zambia. There are two main sources of hydroelectric power on the river, the Kariba Dam, which provides power to Zambia and Zimbabwe, and the Cahora Bassa Dam in Mozambique, which provides power to Mozambique and South Africa. There are additionally two smaller power stations along the Zambezi River in Zambia, one at Victoria Falls and the other one near Kalene Hill in Ikelenge District.
Title: Zambezi
Content:  The river flows to the southwest into Angola for about 240 km, then is joined by sizeable tributaries such as the Luena and the Chifumage flowing from highlands to the north-west. It turns south and develops a floodplain, with extreme width variation between the dry and rainy seasons. It enters dense evergreen Cryptosepalum dry forest, though on its western side, Western Zambezian grasslands also occur. Where it re-enters Zambia it is nearly 400 m wide in the rainy season and flows rapidly, with rapids ending in the Chavuma Falls, where the river flows through a rocky fissure. The river drops about 400 m in elevation from its source at 1500 m 
Title: Zambezi
Content:  About 160 km from the sea the Zambezi receives the drainage of Lake Malawi through the Shire River. On approaching the Indian Ocean, the river splits up into a delta. Each of the four primary distributaries, Kongone, Luabo and Timbwe, is obstructed by a sand bar. A more northerly branch, called the Chinde mouth, has a minimum depth at low water of 2 m at the entrance and 4 m further in, and is the branch used for navigation. 100 km further north is a river called the Quelimane, after the town at its mouth. This stream, which is silting up, receives the overflow of the Zambezi in the rainy season.
Title: Zambezi
Content:   The river rises in a black marshy dambo in dense undulating miombo woodland 50 km north of Mwinilunga and 20 km south of Ikelenge in the Ikelenge District of North-Western Province, Zambia at about 1524 m above sea level. The area around the source is a national monument, forest reserve and Important Bird Area. Eastward of the source, the watershed between the Congo and Zambezi basins is a well-marked belt of high ground, running nearly east–west and falling abruptly to the north and south. This distinctly cuts off the basin of the Lualaba (the main branch of the upper Congo) from that of the Zambezi. In the neighborhood of the 
Title: Zambezi Basin
Content:  of a rich ecosystem of savannas and humid forests that surround it. Its main navigable course is through the Zambezi River, being the stretch of the mouth in the Indian Ocean (more precisely in the Mozambique Channel) until it surrounds the city of Tete, in the northwest of Mozambique. There are also navigable courses in the Cahora Bassa and Kariba lakes, and in the plains of the Mana Pools, Caprivi Strip, Liuwa-Luena-Baroste-Siloana, Shire, Luangwa and Lake Nyassa, the latter three of which are navigable within two its thirteen sub-basins. Two major sub-basins in the Zambezi basin are interconnected with other major African systems, namely: (a) the Lake Nyassa/Shire River sub-basin, which connects with the Great Rift Valley, and; (b) the perennial river bifurcation in the Selinda Spillway (or Magwegana river), in the Cuando River sub-basin, which connects the Zambezi Basin to the Kalahari Basin.
Title: Geography of Africa
Content:  Of the rivers flowing to the Indian Ocean, the only one draining any large part of the interior plateaus is the Zambezi, whose western branches rise in the western coastal highlands. The main stream has its rise in 11°21′3″ S 24°22′ E, at an elevation of 1500 m. It flows to the west and south for a considerable distance before turning eastward. All the largest tributaries, including the Shire, the outflow of Lake Nyasa, flow down the southern slopes of the band of high ground stretching across the continent from 10° to 12° S. In the southwest, the Zambezi system interlaces with that of the Taukhe (or Tioghe), from which it at times receives surplus water. The rest of the water of the Taukhe, known in its middle course as the Okavango, is lost in a system 
Title: Zambezi
Content:  west is without major tributaries for 240 km. Before this, the Ngonye Falls and subsequent rapids interrupt navigation. South of Ngonye Falls, the river briefly borders Namibia's Caprivi Strip. The strip projects from the main body of Namibia, and results from the colonial era: it was added to German South-West Africa expressly to give Germany access to the Zambezi. Below the junction of the Cuando River and the Zambezi the river bends almost due east. Here, the river is broad and shallow, and flows slowly, but as it flows eastward towards the border of the great central plateau of Africa it reaches a chasm into which the Victoria Falls plunge.

Question: which ocean does the zambezi river flow into?
Answer: Indian Ocean.