Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Max Boxleitner"'
Publikováno v:
Geomorphology. 340:15-31
In order to improve our understanding of the glacier development in central Switzerland after the Last Glacial Maximum (LGM) we have investigated moraine sequences of the Meiental (“Meien Valley”). After detailed field mapping, 34 rock samples fr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c0a87e5243030df1ec8c5a31230163fd
https://doi.org/10.1016/j.geomorph.2019.04.004
https://doi.org/10.1016/j.geomorph.2019.04.004
Autor:
Susan Ivy-Ochs, Markus Egli, Marcus Christl, Max Maisch, Max Boxleitner, Dagmar Brandová, Dennis Dahms
Publikováno v:
Boreas. 48:867-878
The Goschenertal (Goschenen valley) is the type locality of the so‐called Goschenen Cold Phases I (~3–2.3 ka) and II (~1.8–1.1 ka). According to earlier studies, these Late Holocene climatic cooling periods were characterized by changes in vege
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8c2d194d86216b3dcfd9b6e4ad1d438f
https://doi.org/10.1111/bor.12394
https://doi.org/10.1111/bor.12394
Publikováno v:
Geographica Helvetica, 73 (3)
Geographica Helvetica, Vol 73, Pp 241-252 (2018)
Geographica Helvetica, Vol 73, Pp 241-252 (2018)
Exposure dating has substantially improved our knowledge about glacier advances during the Younger Dryas (YD) and the early Holocene. The glacier development after the Last Glacial Maximum (LGM) and the timing of morphologically evidenced, earlier La
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::03ec6477d56a59c144399b8881d8f274
https://hdl.handle.net/20.500.11850/295636
https://hdl.handle.net/20.500.11850/295636
Autor:
Raquel de Castro Portes, Dagmar Brandová, Max Maisch, Dennis Dahms, Marcus Christl, Max Boxleitner, Markus Egli, Jarosław Waroszewski, Alessandra Musso, Małgorzata Malkiewicz
The European Alps are a geomorphologically active region and experience a number of gravity-driven hillslope processes. Soil and landscape formation in the Alps has consequently undergone several minor and major traceable changes of developmental tra
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::45882132c3583c31dcee9d476540c070
https://www.zora.uzh.ch/id/eprint/138336/
https://www.zora.uzh.ch/id/eprint/138336/