Did Neogene climate change impact the mountain belts of Europe?
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If you have a question about this talk, please contact Christian Franzke.
Whether late Cenozoic climate change was a driver of apparent
‘uplift’ of mountain ranges remains a critical problem in the earth
sciences as it determines how anomalous modern landscapes are relative
to earth’s geological past. Have erosion rates dramatically increased
globally during the last few millions of years? What impact might this
have on mountain landscapes, foreland basins and sediment fluxes? These
questions are tested using a broad range of thermochronological and
sedimentological data from across Europe.
This talk is part of the British Antarctic Survey series.
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