Blar i NGU Open Archive på emneord "ISAVSMELTING"
Viser treff 21-27 av 27
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Sedimentkjerner fra Barentshavet Øst tatt på MAREANO-tokt med G.O. Sars i 2014
(NGU-Rapport (2016.021), Report, 2016)På tokt MAREANO 2014-2016 med forskningsfartøyet G.O. Sars i 2014 ble det tatt sedimentkjerner med gravitasjonsprøvetaker (GC) på åtte stasjoner i Barentshavet Øst. Hensikten var i første rekke å få informasjon om mektighet ... -
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 ... -
Vinjeøra 1421 II, kvartærgeologisk kart M 1:50 000, beskrivelse med kartbilag
(NGU-Rapport (2004.034), Report, 2004)Den kvartærgeologiske kartleggingen av kartblad Vinjeøra ble foretatt i 1995 og 1996 som en del av den systematiske kartleggingen i M 1:50 000 som ble gjort av NGU. Beskrivelsen gir en kort omtale av geologiske hendelser ...