Blar i Artikler på emneord "ISAVSMELTING"
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A proposed deglaciation chronology for the Trondheimsfjord area, Central Norway.
(NGU (373), Journal article, 1982)Radiocarbon datings of the deglaciation of the Trondheimsfjord area strongly suggest that the coastal areas and the outer part of the fjord were deglaciated before 11000 B.P. During early Younger Dryas the inland ice ... -
Age of the Younger Dryas ice-marginal substages in Mid-Norway - Tautra and Hoklingen, based on a compilation of 14C-dates
(NGU Bulletin (454), Journal article, 2015)The ice-marginal Tautra and Hoklingen Substages in the Trøndelag counties, Mid-Norway, have for a long time been referred to as of early and late Younger Dryas (YD) age, respectively. The basis for this is the regional ... -
Deglaciation of the outermost Trondheimsfjord area, mid-Norway
(NGU Bulletin (427), Journal article, 1995) -
Deglaciation of the Trondheimsfjord area, Central Norway
(NGU Bulletin (427), Journal article, 1995) -
Development of minor late-glacial ice domes east of Oppdal, Central Norway
(NGU Bulletin (441), Journal article, 2003)Glacial striations and ice-marginal forms such as lateral moraines and meltwater channels show that a major north-westerly-directed ice flow invaded the Oppdal area prior to the Younger Dryas (YD) Chronozone. Through the ... -
En rekonstruksjon av isbevegelser under siste istid i Samnanger og Kvam, Hordaland, Vest-Norge.
(NGU (369), Journal article, 1981)The reconstructions are based mainly on analysis of glacial striae. The oldest striae indicate that the glacier flow, was influenced by the deep Hardangerfjord, even during the Weichselian maximum. Younger striae of assumed ... -
Glasialgeologi og vegetasjonsinnvandring i Indre Nordhordland, Vest-Norge.
(NGU (369), Journal article, 1981)In the area between Hardangerfjorden and Sognefjorden an oldest regional ice movement towards the west has been reconstructed. Younger regional ice movements were towards south-west in the southern parts. Therefore, an ... -
Isavsmelting i og omkring midtre Gudbrandsdalen.
(NGU (223), Journal article, 1963)Observed glacial striae showing direction of ice-movement during the last active stage of the inland-ice are shown in fig. 1. Supposed major directions of ice movement are also shown in fig. 3. In the mountain parts are ... -
Ljørdalen. Beskrivelse til kvartærgeologisk landgeneralkart.
(NGU (206), Journal article, 1958)The area is characterized by the melting in situ of stagnant glaciers. The glacial material of scree and stream deposits date from the dead-ice stage of the inland ice during which it left eskers of more or less sorted ... -
Løsmateriale og isavsmeltning i nedre Gudbrandsdalen og Gausdal.
(NGU (228), Journal article, 1964)In the present paper are published some preliminary results of a study on glacigene material in two strongly glaciated valleys in Central Norway, namely Gudbrandsdalen and Gausdal. Particular attention has been paid to ... -
Noen isavsmeltningsfenomener i Østerdalen.
(NGU (188), Journal article, 1954)Some features from the melting of the inland ice in Østerdalen: A few of the more large-scale features formed by melting water of the last ice sheet are described. The last part of the inland ice filled the valleys in the ... -
Sunndalsøra 1420 III. Beskrivelse til kvartærgeologisk kart - M 1 : 50 000 (med fargetrykt kart).
(Skrifter (79), Map, 1987)The superficial deposits within the map-sheet are described and genetically classified. Tills are the dominating sediments, but considerable amounts of glaciofluvial and fluvial deposits also occur. Slide and talus deposits ... -
The deglaciation and vegetational history of a former ice-damned lake area at Skåbu, Nord-Fron, Southern Norway.
(NGU (373), Journal article, 1982)Cores obtained from a small peat bog within the area of a former ice-dammed lake show that 1.7 m of silt were deposited during the ice lake phase. The pollen in the silt is dominated by grasses and other NAP. A small ... -
The deglaciation of the coastal area NW of Svartisen, northern Norway.
(NGU (369), Journal article, 1981)Late Weichselian glacial events, marine fauna and shore-lines in the coastalarea NW of Svartisen are described. During the oldest glacial event (Vassalevent), marginal moraines were deposited near the mouths of the fjords. ... -
The surface of the inland ice in the Atndalen valley, South-central Norway.
(NGU Bulletin (438), Journal article, 2001)On the basis of different field observations, several authors have discussed the form of the inland ice in southern Norway. In this work, lateral features indicating the upper limit of zones of meltwater drainage marked ... -
Trekk av isbevegelsen og isavsmeltningen i Nordre Gudbrandsdalens fjelltrakter.
(NGU (223), Journal article, 1963)Glacial striae and ice-moulded forms indicate that the earliest direction of glacial flow was towards E, and that the flow at the maximum was towards N or NW. The late-glacial movement, however, seems to have been towards ...