1a). We then compute the corresponding changes in convection-driven dynamic topography (rock uplift/subsidence) of the African continent and evaluate their compatibility with geological constraints.

For example, dynamic topography can explain most of the observed uplift of the East African plateau. The remainder of the high topography can be attributed to uplift of rift shoulders surrounding ...

Much of the Ethiopian landmass is part of the East African Rift Plateau ... impression of the country's topography when Ethiopians refer to the landform as a plateau. Few of these peaks' surfaces ...

Impacts of the Himalayas’ topographic complexity on the moisture transport and precipitation across the Tibetan Plateau during summer, compared to the smooth estimated topography from coarse ...