Key Biodiversity Areas

Batoka Gorge (7218)
Zimbabwe, Africa

Site overview


KBA status: confirmed
Year of last assessment: 2001
National site name: Batoka Gorge
Central coordinates: Latitude: -17.9833, Longitude: 25.8667
System: terrestrial
Elevation (m): 500 to 900
Area of KBA (km2): 112.60826
Protected area coverage (%): 74.97
KBA classification: Global/Regional TBD
Legacy site: Yes

Site details


Site description: After crashing over the spectacular Victoria Falls, one of the natural wonders of the world, the Zambezi river hurtles through many gorges on its way to the quieter waters of Lake Kariba. From the falls at 17°56’S 25°52’E, the Batoka Gorge system is about 120 km long, reaching to Sidinda Island (just west of the Matetsi river mouth) at 18°00’S 26°34’E, where the plateau drops below 600 m. The river has carved through the basalt rock here, to make a gorge up to 140 m deep, characterized by cliffs and screes. The landscape and the views are stunning. The Batoka Gorge system lies within the Hwange Communal Land, apart from the first c.12 km below the falls which lies within the Victoria Falls National Park. The flat plain on top supports mopane Colophospermum woodland. Riparian forest occurs in parts along the Zambezi and some of the gorges formed by tributaries, with trees of Diospyros, Trichilia and Rhus among others. The screes are clothed in thick mixed woodland (Commiphora, Entandrophragma, Sterculia, etc., often dominated by Triplochiton), interspersed with grassland. There is virtually no usage of the gorge itself, except for white-water rafting and kayaking along the river.
Rationale for qualifying as KBA: This site qualifies as a Key Biodiversity Area of international significance because it meets one or more previously established criteria and thresholds for identifying sites of biodiversity importance (including Important Bird and Biodiversity Areas, Alliance for Zero Extinction sites, and Key Biodiversity Areas)
Additional biodiversity: See Box for key species. The Batoka Gorge is a haven for cliff-nesting birds, in particular Falco fasciinucha. A pair can usually be seen in the fifth gorge. In the 1990s, it was estimated that Batoka Gorge hosted up to 10 pairs of this small falcon. In addition, there are about 18 pairs of Falco peregrinus, and another 34 species of raptor occur or have been seen there (including owls). At least four pairs of Ciconia nigra nest in the gorge. A rafting survey counted 103 Glareola nuchalis. No other threatened or restricted-range species occur in the Gorge. No checklist of birds exists for this section of the Zambezi river, except for a list of raptors. Non-bird biodiversity: None known to BirdLife International.

Habitats


Land use: nature conservation and research | tourism/recreation
IUCN HabitatCoverage %Habitat detail
Grassland2
Forest5
Shrubland20
Rocky Areas(e.g., inland cliffs, mountain peaks)5
Artificial - Terrestrial67

Threats


Summary of threats to biodiversity at KBA: The area around Victoria Falls was declared a World Heritage Site in 1989. The overriding issue is the proposed Batoka Dam, with the wall being built below the Moemba Falls, at 17°56’S 26°06’E. The dam wall would be 196 m in height, and produce a lake of about 50 km in length and entirely within the gorge. The lake would severely constrain the breeding opportunities for cliff-nesting raptors, and given the reduced space (upstream) and the competitive dominance shown by Falco peregrinus, it is debatable whether F. fasciinucha would survive there. In addition, if Batoka Gorge held a lake rather than a rushing river, then tourism to the site would be bound to increase, with the consequence of greater disturbance (upstream) to the remaining raptors. In the meantime, the lip of the gorge from the falls to its end, on the Zimbabwe side, is a minefield, though this is being cleared.
Threat level 1Threat level 2Threat level 3Timing
Human intrusions & disturbanceRecreational activitiesOngoing

Additional information


References: Du Toit (1982), Hartley (1993), Hartley et al. (1996), Pollard (no date), Williams et al. (1989).