Earth's surface is the 'living skin' of our planet – it connects the physical, chemical, and biological systems.
frameborder="0″ allow="accelerometer; autoplay; clipboard-write; encrypted-media; gyroscope; picture-in-picture; web-share" allowfullscreen>, running on hundreds of computer processors. Each simulation took several days, building a complete picture to reconstruct the past 100 million years of Earth's surface evolution.
All of these fit well with existing geological observations. For instance, we combined data from present-dayOur main outputs are available as time-based global maps at five-million-year intervals fromOne of Earth's fundamental surface processes is erosion, a slow process in which materials like soil and rock are worn and carried away by wind or water. This results in sediment flows.
Investigating the way sediment flows have changed through space and time is crucial for our understanding of how Earth's climates have varied in the past. Our simulated past landscapes are fully integrated with the various processes at play, especially the hydrological system – the movement of water – providing a more robust and detailed view of Earth's surface.
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