The Tromsø-Lyngen glacier readvance (early Younger Dryas) at Hinnøya-Ofotfjorden, northern Norway: a reassessment

dc.contributor.author	Bergstrøm, Bjørn
dc.contributor.author	Sveian, Harald
dc.contributor.author	Olsen, Lars
dc.coverage.spatial	NORDLAND
dc.coverage.spatial	TROMS
dc.coverage.spatial	12312 Ulsvåg
dc.coverage.spatial	13323 Tjeldsundet
dc.date.accessioned	2020-08-26T09:05:45Z
dc.date.available	2020-08-26T09:05:45Z
dc.date.issued	2005
dc.identifier.uri	https://hdl.handle.net/11250/2674158
dc.description.abstract	Based on radiocarbon dates, marine seismic data, mapping of surficial deposits, observations of marine limits and shoreline correlations, we have documented a considerable glacier readvance during the Tromsø-Lyngen event in the early Younger Dryas Chron, reaching farther west and northwest in the Hinnøya-Ofjotfjorden area than previously suggested. The continental ice sheet advanced across Tjeldsundet and occupied parts of eastern Hinnøya where it coalesced with local glaciers.\r(Forkortet)
dc.language.iso	eng
dc.relation.ispartofseries	NGU Bulletin (445)
dc.rights	Navngivelse 4.0 Internasjonal
dc.rights.uri	http://creativecommons.org/licenses/by/4.0/deed.no
dc.subject	AVSETNING
dc.subject	BRE
dc.subject	BREBEVEGELSE
dc.subject	GLASIALGEOLOGI
dc.title	The Tromsø-Lyngen glacier readvance (early Younger Dryas) at Hinnøya-Ofotfjorden, northern Norway: a reassessment
dc.type	Journal article
dc.description.localcode	52671
dc.source.pagenumber	s.73-88

Except where otherwise noted, this item's license is described as Navngivelse 4.0 Internasjonal