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Watch the Namibian margin evolving over 300 Mio years after backstacking the denuded section onto the crust. We adjusted for isostasy with an effective thickness of 25 km. This animation is experimental. If you use this animation please cite:
Raab, Matthias (2001). The Geomorphic Response of the Passive Continental Margin of Northern Namibia to Gondwana Break-Up and Global Scale Tectonics, PhD Thesis, Georg-August-Universität Göttingen.