Scientists uncover hidden forces causing continents to rise - study

Scientists have answered 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.

They have found that when tectonic plates break apart, powerful waves are triggered deep within the Earth that can cause continental surfaces to rise by over a kilometre.

The experts’ findings help resolve a long-standing mystery about the dynamic forces that shape and connect some of the Earth’s most dramatic landforms – expansive topographic features called ‘escarpments’ and ‘plateaus’ that profoundly influence climate and biology.

Researchers from the Universities of Birmingham and Southampton joined counterparts at the University of Potsdam to examine the effects of global tectonic forces on landscape evolution over hundreds of millions of years. The findings are published in the journal Nature.

The vertical motions of the stable parts of continents, called cratons, remain one of the least understood aspects of plate tectonics. The researchers’ findings help explain why parts of the continents previously thought of as ‘stable’ experience substantial uplift and erosion, and how such processes can migrate hundreds or even thousands of kilometres inland, forming sweeping elevated regions known as plateaus, like the Central Plateau of South Africa.

Dr Steve Jones, Associate Professor in Earth Systems at the University of Birmingham, commented: “What we have here is a compelling argument that rifting can, in certain circumstances, directly generate long-lived continental scale upper mantle convection cells, and these rift-initiated convective systems have a profound effect on Earth’s surface topography, erosion, sedimentation and the distribution of natural resources.”

The team used advanced computer models and statistical methods to interrogate how the Earth’s surface has responded to the breakup of continental plates through time. They discovered that when continents split apart, the stretching of the continental crust causes stirring movements in Earth’s mantle (the convecting layer between the crust and the core).

Tom Gernon, Professor of Earth Science the University of Southampton and lead author of the study said: “Scientists have long suspected that steep kilometre-high topographic features called Great Escarpments – like the classic example encircling South Africa – are formed when continents rift and eventually split apart. However, explaining why the inner parts of continents, far from such escarpments, rise and become eroded has proven much more challenging. Is this process even linked to the formation of these towering escarpments? Put simply, we didn’t know.”

The scientists pieced together evidence to propose that the Great Escarpments originate at the edges of ancient rift valleys, much like the steep walls seen at the margins of the East African Rift today. Meanwhile, the rifting event also sets about a ‘deep mantle wave’ that travels along the continent’s base at about 15-20 kilometres per million years. They believe that this wave convectively removes layers of rock from the continental roots.

Building on this, the team modelled how landscapes respond to this mantle-driven uplift. They found that migrating mantle instabilities give rise to a wave of surface erosion that lasts tens of millions of years and moves across the continent at a similar speed. This intense erosion removes a huge weight of rock that causes the land surface to rise further, forming elevated plateaus.

The team’s study provides a new explanation for the puzzling vertical movements of cratons far from the edges of continents, where uplift is more common. Experts concluded that the same chain of mantle disturbances that provoke diamonds to quickly rise from Earth’s deep interior also fundamentally shape continental landscapes, influencing a host of factors from regional climates and biodiversity to human settlement patterns.