Blar i Artikler på emneord "GLASIALGEOLOGI"
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A Late Quaternary correlation chart for Norway.
(NGU (223), Journal article, 1963)A correlation chart is presented containing the stratigraphical results of some selected Norwegian studies in the wide field of Quaternary geology. Studies of plant remains in bogs, pollen investigations, evidence of ... -
Bidrag til Sørlandets kvartærgeologi
(NGU (55), Journal article, 1910)Forkortet: The present paper contains some glaciological observations made in Nedenes amt and Lista og Mandal amt (Sørlandet) in the Southernmost part of Norway. The observations in Lista and Mandal amt have confined to ... -
Bredemte sjøer eller subglaciale avsetninger?
(NGU (255), Journal article, 1968)The present paper is a criticism and a contradiction of J. Gjessing's theory (Gjessing, 1960, 1966) of a subglacial formation of deposits that are actually terraces and bottom sediments of a former glacial (ice-dammed) ... -
Brerandstadier og avsmeltingsforhold i Repparfjord-Stabbursdal- området, Vest-Finnmark. En deglaciasjonsprofil fra fjord til vidde.
(NGU (213), Journal article, 1961)The purpose of this article is given a description of two prominent active substages of the deglaciation period of the last ice-age in Finnmark, Northern Norway. The area concerned is situated on the peninsula between the ... -
C14-datings referring to shore lines, transgressions, and glacial substages in Northern Norway. (A supplement to papers of 1960 and 1961 by the author).
(NGU (215), Journal article, 1962)Denne publikasjonen er en foreløpig meddelelse som i det vesentlige dreier seg om en serie C14-dateringer utført av R. Nydal ved Laboratoriet for Radiologisk Datering i Trondheim. Dateringene synes å gi viktige opplysninger ... -
Deglasiasjonsforløpet i Aurlandsdalen og områdene omkring, Vest-Norge.
(NGU (317), Journal article, 1975)Ice movements and the course of deglatiation in the Aurland area are reconstructed. The oldest ice movement was from the SE-ESE and converged towards Aurlandsfjorden, while the younger movements were influenced by the local ... -
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 ... -
Dokka. Beskrivelse til kvartærgeologisk kart 1816 IV - M 1:50 000 (med fargetrykt kart).
(NGU; Skrifter (383; 41), Journal article, 1983)The superficial deposits and their morphological features within the map-sheet Dokka, 1816 IV, in central south-eastern Norway are classified and described. Ice movements and the course of deglaciation are reconstucted. ... -
Einergrein av Preboreal alder funnet i israndavsetning i Eidfjord, Vest-Norge.
(NGU (266), Journal article, 1970)In 1969 a branch of juniper (Juniperus communis) was found in a sand-pit on the ice marginal delta in Eidfjord, West-Norway. Radiocarbon dating gave an age of 9680\u00B190 years B.P., which means that the delta is Preboreal ... -
Elvdal. Beskrivelse til kvartærgeologisk kart 2018 III - M 1:50 000 (med fargetrykt kart)
(NGU; Skrifter (346 ; 27), Journal article, 1979)The superficial deposits consists mainly of sandy basal till\r and gravelly-sandy ablation till. The glaciofluvial and fluvial\rsediments are mainly gravelly. The lithology of the fine gravel and the\r mineralogy of sand ... -
En notis om istidsgruset ved Lysefjordens munding
(NGU (32), Journal article, 1901)Forkortet: The mouth of the Lysefjord is situated at 58\u00B0 52' n.l. to the SE of the town of Stavanger. The glacial deposits here are of interests in the history of geology Esmark found as far back as 1824 at this place ... -
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 ... -
Geometry and vertical extent of the late Weichselian ice sheet in northwestern Oppland County, Norway
(NGU Bulletin (451), Journal article, 2011)The position of the ice margin during the last deglaciation is well known in Scandinavia, in particular during the Younger Dryas (YD) chronozone from when large ice marginal deposits easily can be traced at or close to the ... -
Glacial geology of the area between Jostedalsbreen and Jotunheimen, South Norway.
(NGU (291), Journal article, 1973)Ice movement and the course of deglaciation are reconstructed. The age of and the climate during the deglaciation are discussed in the light of equilibrium line displacement, shoreline positions, pollen analysis and ... -
Glacial geology of Western Troms, North Norway.
(NGU (256), Journal article, 1968)A moraine chronology was established for western Troms. Altogether six main glacial phases were recognised. Several of the phases were radiocarbon dated. Observations were made of the corresponding shore lines, the marine ... -
Glacial stadials and interstadials of the Late Precambrian Smalfjord Tillite on Laksefjordvidda, Finnmark, North Norway.
(NGU (358), Journal article, 1980)Three glacial conglomerates and two intervening sandstones in the Smalfjord Formation on Laksefjordvidda were deposited during three glacial episodes and two interstadials, respectively. MOst of the sequence is preserved ... -
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 ... -
Hallingdal. Beskrivelse til kvartærgeologisk landgeneralkart.
(NGU (190), Journal article, 1955)(forkortet): The present map of the quaternary deposits of Hallingdal was prepared on the general principles reffered to in the summary of Oslo, NGU no. 16, the first map description published in this series and followed ... -
Har Jæren vært dekket av en Skagerak-bre? Er "Skagerak-morenen" en marin leire?
(NGU (228), Journal article, 1964)Jæren is a low plain on the coast of southwestern Norway. This plain is covered with relatively thick Quaternary deposits including a very bouldary W\u00CFrm till on top of calcareous clays and stratified sand and gravel. ... -
I. Rendalens bræsjø
(NGU (79), Journal article, 1916)The present paper forms a supplement to the author's: Ice-dammed lakes of Northern Østerdal, NGU nr. 73. The lowest sete-building lake in the Glommen valley has extended its branches into the valleys Rendalen, Tydalen and ...