Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Asbjørn Rune Aa"'
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::95ebef96b6961764a6abfd29a5f483d9
https://doi.org/10.1177/0959683618810392
https://doi.org/10.1177/0959683618810392
Publikováno v:
Holocene. Nov2007, Vol. 17 Issue 7, p955-964. 10p. 3 Color Photographs, 1 Diagram, 2 Charts, 4 Graphs, 2 Maps.
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bb7f0aa5a1723c6341c414a934194ea3
https://doi.org/10.1177/0959683607082411
https://doi.org/10.1177/0959683607082411
Autor:
Jan Arne Sjåstad, Asbjørn Rune Aa
Publikováno v:
Norsk Geologisk Tidsskrift. 80:27-32
The entire moraine sequence in front of Boyabreen, a southern outlet of Jostedalsbreen in southern Norway, has until now been regarded as being made up of 'Little Ice Age' (LIA) moraines. As the historical evidence does not support a LIA date for the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8e3463e255552a8a91050f0b339bc6f7
https://doi.org/10.1080/002919600750042654
https://doi.org/10.1080/002919600750042654
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ee6f84736c18726cec9462b0cf38f5bd
https://doi.org/10.1080/002919699433898
https://doi.org/10.1080/002919699433898
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::63956834c184b63d9229cd83eb4a117e
https://doi.org/10.1002/(sici)1099-1417(199801/02)13:1<17::aid-jqs337>3.0.co
https://doi.org/10.1002/(sici)1099-1417(199801/02)13:1<17::aid-jqs337>3.0.co
Autor:
Asbjørn Rune Aa
Publikováno v:
The Holocene. 6:82-89
'Little Ice Age' marginal moraines in the Grovabreen area, inner Sunnfjord, are mapped and described. The modem and 'Little Ice Age' (mid-eighteenth century) equilibrium-line altitude (ELA) of the plateau glacier Grovabreen is calculated by the use o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b4d97b99b6aa997d559de49a2768520d
https://doi.org/10.1177/095968369600600110
https://doi.org/10.1177/095968369600600110