http://hdl.handle.net/1956/1458 Search the Channel search http://bora.uib.no/simple-search http://hdl.handle.net/1956/2137 Title: New approaches to garden history; taxonomical, dendrological, pollen analytical and archaeological studies in a 17th century Renaissance garden at the Milde estate, Norway <br/> <br/>Authors: Moe, Dagfinn; Hufthammer, Ann-Karin; Indrelid, Svein; Salvesen, Per H. <br/> <br/>Description: In: The archaeology of crop fields and gardens - Proceedings of the 1st Conference on Crop Fields and Gardens Archaeology Barcelona (Spain), 1-3 June 2006. edited by Jean-Paul Morel, Jordi Tresserras Juan and Juan Carlos Matamala http://hdl.handle.net/1956/405 Title: Paleomagnetic correlations between scandinavian ice-sheet fluctuations and greenland dansgaard–oeschger events, 45,000–25,000 yr B.P. <br/> <br/>Authors: Mangerud, Jan; Løvlie, R.; Gulliksen, S.; Hufthammer, Ann-Karin; Larsen, E.; Valen, V. <br/> <br/>Abstract: Two paleomagnetic excursions, the Skjong correlated with the Laschamp (about 41,000 GISP2 yr B.P.) and the Valderhaug correlated with the Mono Lake (about 34,000 GISP2 yr B.P.), have been identified in stratigraphic superposition in laminated clay deposited in ice-dammed lakes in three large caves in western Norway. During both periods the margin of the Scandinavian Ice Sheet advanced and reached the continental shelf beyond the outermost coastline. The mild, 4000-yr-long Ålesund interstade, when the coast and probably much of the hinterland were ice-free, separated the two glacial advances. The two paleomagnetic excursions have also been indirectly identified as increased fluxes of http://hdl.handle.net/1956/405 Title: Paleomagnetic correlations between scandinavian ice-sheet fluctuations and greenland dansgaard–oeschger events, 45,000–25,000 yr B.P. <br/> <br/>Authors: Mangerud, Jan; Løvlie, R.; Gulliksen, S.; Hufthammer, Ann-Karin; Larsen, E.; Valen, V. <br/> <br/>Abstract: Two paleomagnetic excursions, the Skjong correlated with the Laschamp (about 41,000 GISP2 yr B.P.) and the Valderhaug correlated with the Mono Lake (about 34,000 GISP2 yr B.P.), have been identified in stratigraphic superposition in laminated clay deposited in ice-dammed lakes in three large caves in western Norway. During both periods the margin of the Scandinavian Ice Sheet advanced and reached the continental shelf beyond the outermost coastline. The mild, 4000-yr-long Ålesund interstade, when the coast and probably much of the hinterland were ice-free, separated the two glacial advances. The two paleomagnetic excursions have also been indirectly identified as increased fluxes of http://hdl.handle.net/1956/405 Title: Paleomagnetic correlations between scandinavian ice-sheet fluctuations and greenland dansgaard–oeschger events, 45,000–25,000 yr B.P. <br/> <br/>Authors: Mangerud, Jan; Løvlie, R.; Gulliksen, S.; Hufthammer, Ann-Karin; Larsen, E.; Valen, V. <br/> <br/>Abstract: Two paleomagnetic excursions, the Skjong correlated with the Laschamp (about 41,000 GISP2 yr B.P.) and the Valderhaug correlated with the Mono Lake (about 34,000 GISP2 yr B.P.), have been identified in stratigraphic superposition in laminated clay deposited in ice-dammed lakes in three large caves in western Norway. During both periods the margin of the Scandinavian Ice Sheet advanced and reached the continental shelf beyond the outermost coastline. The mild, 4000-yr-long Ålesund interstade, when the coast and probably much of the hinterland were ice-free, separated the two glacial advances. The two paleomagnetic excursions have also been indirectly identified as increased fluxes of