Interior East Africa (49,293–28,578 BCE) Upper Pleistocene…
49293 BCE to 28578 BCE
Interior East Africa (49,293–28,578 BCE) Upper Pleistocene I — Rift Foragers, Highland Refugia, and Wetland Routes
Geographic and Environmental Context
The inland core of East Africa, covering:
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Eritrea and Djibouti,
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the Ethiopian Highlands,
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South Sudan,
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the Great Lakes region (Uganda, Rwanda, Burundi),
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inland Kenya and Tanzania (Rift Valley belts),
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Zambia, northern Zimbabwe, northern Malawi, and northwestern Mozambique.
Anchors: Lake Tana & Blue Nile headwaters, Axum/Yeha uplands, Upper Nile–Sudd wetlands, Lake Victoria, Lake Tanganyika, Lake Malawi, Rift Valley escarpments (Kenya–Tanzania), Rwenzori–Virunga highlands, Zambezi corridor.
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Rift lakes (Victoria, Tanganyika, Malawi) lower than present but still extensive.
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Ethiopian Highlands offered perennial springs and montane refugia.
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Upper Nile Sudd wetlands fluctuated seasonally.
Climate & Environmental Shifts
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LGM aridity: reduced rainfall, grassland expansion, glaciers present on Rwenzori.
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Rift lakes contracted but remained productive.
Subsistence & Settlement
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Foragers exploited fish, mollusks, hippo, and crocodile in lake margins.
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Hunting of antelope, zebra, buffalo on savannas.
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Highland refugia in Ethiopia sustained small hunter groups.
Technology & Material Culture
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Flake-based industries; bone harpoons for fishing; ground ochre.
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Ostrich eggshell beads show symbolic life.
Movement & Interaction Corridors
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Nile corridor linked Ethiopian Highlands to Sudan and Egypt.
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Rift lakes provided canoe/raft driftways.
Cultural & Symbolic Expressions
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Beads, ochre use; symbolic rock shelters.
Environmental Adaptation & Resilience
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Mobility between wetland and savanna zones buffered drought stress.
Transition
By 28,578 BCE, Interior East Africans had stabilized a lacustrine–savanna dual adaptation.