CORDIS Project
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The project investigates how mountain ranges respond to tectonic uplift and climate change by measuring rock erosion rates over thousands to millions of years. It aims to clarify the dominant processes affecting erosion and their implications for global climate change using advanced techniques in thermochronology.
Mountain ranges evolve in response to tectonic uplift, erosion and climatic change, but decoupling the feedbacks between these processes remains one of the most active debates in Earth Science.
Resolving this debate is fundamental for successful projection of Earth’s surface response under a changing climate.
The Impact of ClimatE on mountain Denudation remains highly contested because no technique is available to resolve changes in erosion rates over the timescale of glacial-interglacial cycles…
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