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Q-MESA

Mechanisms of Evolution of Sandstone Areas, Central and Western Europe

The Q-MESA is a multidisciplinary collaboration led by Dr Duszyński (Wroclaw University), bringing together geomorphologists, heritage researchers, geochronologists, and mineralogists from Poland, UK, Italy, and USA to

It aims test factors controlling evolution and development of sandstone tablelands in Central and Western Europe. I support the project by using novel luminescence dating techniques to establish timing and rate of deposition.

Project is funded by the Polish National Science Centre.


Publications resulting from this research

Duszyński, F., Waroszewski, J., Fenn, K., Kacprzak, A., Jancewicz, K., Egli, M. (2024) Cliff-foot sandy cones: A proxy to study the time frames, patterns and rates of sandstone caprock decay? Catena, 247, 108529. https://doi.org/10.1016/j.catena.2024.108529

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