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Autor:
Etzelmüller, B. (Bernd), Patton, H. (Henry), Schomacker, A. (Anders), Czekirda, J. (Justyna), Girod, L. (Luc), Hubbard, A. (Alun), Lilleøren, K. S. (Karianne S.), Westermann, S. (Sebastian)
Iceland’s periglacial realm is one of the most dynamic on the planet, with active geomorphological processes and high weathering rates of young bedrock resulting in high sediment yields and ongoing mass movement. Permafrost is discontinuous in Icel
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2423::978e858cd3888d157a5bc8689dfa0bc2
http://urn.fi/urn:nbn:fi-fe2020091669748
http://urn.fi/urn:nbn:fi-fe2020091669748
