Tropical West Southern Africa (964 – 1107…
964 CE to 1107 CE
Tropical West Southern Africa (964 – 1107 CE): Growing Chiefdoms in Wetland–Savanna Frontiers
Geographic and Environmental Context
Tropical West Southern Africa includes far-northern Botswana and Namibia — the Caprivi Strip, the Okavango Delta, the Etosha Pan, and the Skeleton Coast.
-
Anchors: the Okavango inland delta, the Zambezi–Caprivi wetlands, the Etosha Pan basin, and the Namib’s Skeleton Coast.
Climate and Environmental Shifts
-
Climate remained favorable with high water tables in Okavango Delta and Caprivi wetlands.
-
Etosha alternated between water abundance and dry pan years, shaping mobility.
-
The Skeleton Coast remained marginal but provided marine protein.
Societies and Political Developments
-
Chiefdom-level societies consolidated around Caprivi wetlands, with cattle herds as status markers.
-
San bands in Etosha and Skeleton Coast maintained flexible mobility and exchange with settled groups.
-
Early elite centers emerged along Zambezi–Okavango corridors, connected to broader southern African trade webs.
Economy and Trade
-
Okavango: irrigated gardens and cattle pastures.
-
Caprivi: grain surpluses, ivory, and hides.
-
Etosha: salt and grazing.
-
Exchange of ivory and copper extended toward interior and Indian Ocean networks.
Belief and Symbolism
-
Cattle rituals affirmed chiefly authority.
-
San rock art and trance dances visualized water, rain, and animal spirits.
Long-Term Significance
By 1107, Tropical West Southern Africa supported chiefdoms linked by cattle and trade, while foraging societies remained strong in arid Etosha–Skeleton landscapes.