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A research team including GFZ scientists has tackled one of the most puzzling questions in plate tectonics: how and why ‘stable’ parts of continents gradually rise to form some of the planet’s greatest topographic features. |
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The new research addresses the effects of tectonic forces on the formation of 'Great Escarpments' over hundreds of millions of years. The researchers found that when tectonic plates break apart, strong wave-like processes deep inside the Earth are triggered that can lift the continental surface by more than a kilometre. Their findings help to explain why parts of the continents that were previously considered ‘stable’ experience significant uplift and erosion hundreds or even thousands of kilometres inland, such as the Central Plateau in South Africa. The results have now been published in the scientific journal Nature.
Plateaus are part of the oldest structures of the continents, the so-called cratons, which are several billion years old. These ancient continental structures are considered to be tectonically extremely stable. The vertical movements of these continental core areas are still among the least understood aspects of plate tectonics. Many of the cratonic continental fragments are bounded by steep landforms. One such immense and striking landform is the 'Great Escarpment', which runs along almost the entire coast of southern Africa and surrounds the plateaus there - in some cases at great distance. It was formed more than 120 million years ago with the break-up of the ancient continent Gondwana. Until now, it was assumed that the formation of cratonic plateaus and escarpments took place independently, as they are often spatially separated from each other - sometimes by more than thousand kilometres.
In the newly published study, the team of scientists discovered that escarpments and plateaus are formed when instabilities in the Earth's mantle erode cratonic keels, causing the interior of the craton to rise. The instabilities in the Earth's mantle initially form where the continents break apart, near a rift valley. From there, the instabilities "migrate" along the lithospheric root at a rate of around 15-20 kilometres per million years towards the stable area of the continents (cratons), thereby gradually eroding the cratonic keels.
The team's study provides a new explanation for the puzzling vertical movements of cratons far from the edges of the continents. The deep levels of the Earth's plates can have a major influence on the development of Earth’s surface. The scientists were able to show that a single process - the successive detachment of the deep lithosphere - enables the formation of 'Great Escarpments’, the uplift of plateaus and erosion in the interior of the continent, as well as the volcanism that brings diamonds to the Earth's surface. In southern Africa, these phenomena occur up to a thousand kilometres apart and are therefore not easy to link. According to the study, cratons are more dynamic than previously assumed.
To the original publication
GFZ Press Release
The picture shows the Drakensberg, part of the Great Escarpment in southern Africa. (Picture: Diriye Amey)
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