Abstract
The quantitative understanding of processes operating in the earth system has advanced significantly over the last few decades. This has led to the realization that a close interaction between deep earth and surface processes is a key element in earth dynamics and its impact on geo-environment, geo-energy, geo-resources and geo-hazards in general. The European continent and its ocean-continent margins provide an excellent natural laboratory to examine the impact of geodynamics and climate on topography at the earth’s surface. The overview presented here demonstrates the need for a further understanding of the earth system across space and timescales. Cross-border scientific cooperation on a full pan-European scale, benefiting from funding opportunities offered by the European Commission and a pro-active role in bottom-up self-organization involving members of the Earth and Cosmic Sciences section of Academia Europaea, is needed more than ever.
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