How the Paleoclimate of the Younger Dryas Stadial influenced Sand Deposition in Pingo Remnants in the Northern Netherlands.
dc.rights.license | CC-BY-NC-ND | |
dc.contributor.advisor | Hoek, Wim | |
dc.contributor.author | Bonanno, Leonardo | |
dc.date.accessioned | 2024-07-25T23:01:59Z | |
dc.date.available | 2024-07-25T23:01:59Z | |
dc.date.issued | 2024 | |
dc.identifier.uri | https://studenttheses.uu.nl/handle/20.500.12932/46939 | |
dc.description.sponsorship | Utrecht University | |
dc.language.iso | EN | |
dc.subject | Climate Reconstruction and Physical Geography | |
dc.title | How the Paleoclimate of the Younger Dryas Stadial influenced Sand Deposition in Pingo Remnants in the Northern Netherlands. | |
dc.type.content | Master Thesis | |
dc.rights.accessrights | Open Access | |
dc.subject.courseuu | Earth, Life and Climate | |
dc.thesis.id | 34913 |