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The Windhoek area in Namibia is characterized primarily by normal faults, which are associated with tectonic extension. These faults are part of the larger geological framework of the region, influenced by the East African Rift system. The presence of these faults can lead to significant geological features, such as rift valleys and associated sedimentary basins. Additionally, some areas may exhibit minor strike-slip faults due to lateral tectonic movements.

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8mo ago

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