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This subsidence creates a "graben" (a depressed block of land) over time. The Kafu Crack does not grow continuously. It grows in sudden, violent bursts during seismic events. Uganda experiences moderate seismic activity (typically magnitude 4.0 to 5.5), and each earthquake triggers a cascading collapse: This means you miss out on new features,
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The belongs to the northern extension of the Western Branch . While the Eastern Branch is more volcanically active, the Western Branch is mechanically deeper. This means the crust is thinning faster in the west, creating deep rift valleys that will eventually fill with seawater.
The crack runs roughly parallel to the Kafu River, which flows through western Uganda before emptying into Lake Kyoga. The river itself is a key tributary of the Nile. The proximity to this vital waterway means that the Kafu Crack has direct hydrological consequences, affecting groundwater tables, river courses, and sediment transport.
