Zobrazeno 1 - 10
of 15
pro vyhledávání: '"Eivind Sønstegaard"'
Publikováno v:
Norwegian Journal of Geology (2022)
Externí odkaz:
https://doaj.org/article/c24c7fd5b21a454ea1163ebbc3b5daf0
Autor:
Asbjørn Rune Aa, Eivind Sønstegaard
Publikováno v:
The Holocene. 29:187-196
Marginal moraines on the northern side of Grovabreen, a plateau glacier in inner Sunnfjord, Western Norway, have been mapped and morphostratigraphically correlated with the Erdalen Event and possibly the Finse Event and the ‘Little Ice Age’. Schm
Autor:
Eivind Sønstegaard, John Inge Svendsen, Anna L.C. Hughes, Inge Aarseth, Jan Mangerud, Kåre Skår, Øystein S. Lohne
Publikováno v:
Quaternary Science Reviews. 132:175-205
Distinct Younger Dryas (YD) moraines are mapped more-or-less continuously around the Scandinavian Ice Sheet. In most areas there is no evidence to suggest that a glacial re-advance took place during the YD, either because it did not happen or because
Autor:
Jan Mangerud, Gifford H. Miller, Oddvar Longva, Steinar Gulliksen, Eiliv Larsen, Eivind Sønstegaard, Hans Petter Sejrup
Publikováno v:
Boreas. 10:447-462
Seven localities with fossil-bearing tills were found in the Alesund area. Fifteen radiocarbon dates of marine shells in the tills all gave ages between 28,000 and 38,000 years B.P. In spite of a general scepticism to shell dates giving high finite a
Publikováno v:
Boreas. 8:179-187
The deglaciation patterns of the Bergen and Nordfjord-Sunnmore areas in western Norway are described and correlated. In the Bergen area the coast was first deglaciated at 12,600 B.P., with a succeeding re-advance into the North Sea around 12,200 B.P.
Publikováno v:
Boreas. 10:369-379
Stratigraphical investigations of an inter-till peat in Brumunddal suggest a major interstadial of Early Weichselian age. The insect fauna and the pollen composition indicate a mean July temperature 2–3dC lower than today during the climatic optimu
Publikováno v:
Boreas. 10:137-208
A complete interglacial cycle, named the Fjosangerian and correlated with the Eemian by means of its pollen stratigraphy, is found in marine sediments just above the present day sea level outside Bergen, western Norway. At the base of the section the
Publikováno v:
The Holocene. 17:955-964
A number of large rock avalanches from the northern slope of the 1435 m high mountain of Vora in Breim, inner Nordfjord have been mapped. The avalanche tongues dam the 4 km long Sandalsvatnet, they cover an area of 3 km 2 and the volume exceeds 100 m
Publikováno v:
Norsk Geologisk Tidsskrift. 79:33-45
During the Younger Dryas, the Alfoten area was covered by ice caps separated from the continental Scandinavian inland ice. The local Younger Dryas glacier margins of two coalescing plateau glaciers, Alfotbreen and Davikbreen, have been reconstructed
Publikováno v:
Journal of Quaternary Science. 13:17-27
Younger Dryas cirque glaciers are known to have existed beyond the Scandinavian Ice Sheet in parts of western Norway. At Krakenes, on the outermost coast, a cirque glacier formed and subsequently wasted away during the Younger Dryas. No glacier exist