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NASA satellite photograph showing the Barotse Floodplain as the bright green to dark blue central region.1 The Zambezi flowing north to south through the middle of the floodplain; 2 confluence of (left to right) the Lungwebungu, Southern Kashiji, Zambezi and Kabompo Rivers, marking the start of the floodplain; 3 end of the floodplain south of Senanga; 4 Ngonye Falls on the Zambezi; 5 Mongu ...
The Zambezian flooded grasslands can be found on seasonally- or permanently-flooded lowlands in the basin of the Zambezi and neighboring river basins. These enclaves lie in the Zambezian region, a broad belt of seasonally-dry miombo and mopane savannas and woodlands that extend east and west across Africa, from northern Botswana, Namibia, and Angola in the west to Tanzania and Mozambique in ...
The lower Zambezi experienced a small flood surge early in the dry season as rain in the Gwembe catchment and north-eastern Zimbabwe rushed through while rain in the upper Zambezi, Kafue, and Lake Malawi basins, and Luangwa to a lesser extent, is held back by swamps and floodplains.
They Zambezian coastal flooded savannas cover an area of 19,346 km². The Zambezi flooded savannas cover the largest area, extending nearly 200 km along the Indian Ocean coast and extending up to 120 km inland. To the south are the adjoining floodplains of the Pungwe and Buzi, which create a flooded savanna of 4500 km².
This floodplain is inundated from December to June, and is fed by other rivers with their own floodplains, and serves as a vast reservoir storing the waters of the Zambezi. The seasonal flooding is very important to agriculture in the province, providing natural irrigation for the grasslands on which huge herds of cattle depend, and bringing ...
The Zambezian and mopane woodlands is a tropical and subtropical grasslands, savannas, and shrublands ecoregion of southeastern Africa.. The ecoregion is characterized by the mopane tree (Colophospermum mopane), and extends across portions of Botswana, Malawi, Mozambique, Namibia, South Africa, Eswatini, Zambia, and Zimbabwe, including the lower basins of the Zambezi and Limpopo rivers.
After only 20 kilometres (12 mi) it emerges from the hills into the broad valley of the Zambezi and meanders over sandy flats about 1.5 kilometres (0.93 mi) wide in a floodplain 3 to 5 kilometres (1.9 to 3.1 mi) in width. It merges with the deeper Zambezi at Luangwa town.
The edges of the floodplain are a white sandy soil covered in thin forest. The main river channel grows from 50 m (160 ft) wide to 200 m (660 ft) wide near the Zambezi, and its floodplain suddenly broadens as it merges with the Zambezi, at the beginning of the Barotse Floodplain, which is 25 km (16 mi) wide at that point. [citation needed]
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