Blar i Artikler på emneord "MORENE"
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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 ... -
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 ... -
Big boulders of tillite rock in Porsanger, Northern Norway.
(NGU (247), Journal article, 1967)In 1959 numerous erratic boulders of tillite rock were discovered at the head of Austerbotn, the eastern arm of the Porsangerfjord. Some of the boulders are very big, having volumes of up to 20m3. In 1965 another two ... -
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 ... -
De fem jordartsregioner i Norge.
(NGU (195), Journal article, 1956)The five soil regions of Norway: The greater part of the deposits covering the rock in Norway were placed in their present position during the melting period of the inland ice. In studying the formation of soils two different ... -
Distribution of rock fragments, grain size and chemical elements of tills in the Lake Mjøsa area, eastern Norway
(NGU Bulletin (453), Journal article, 2014)The Lake Mjøsa area in eastern Norway forms an interesting case to study glacial erosion, transport and deposition because bedrock lithology (source of till) is relatively well known and the Geological Survey of Norway ... -
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 ... -
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 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 geology,deglacition chronology and sea-level changes in the southern Telemark and Vestfold counties, Southeastern Norway
(NGU Bulletin (435), Journal article, 1999)A revised and more detailed deglaciation chronology is presented in the soputhern Telemark and Vestfold, southeastern Norway, based mainly on information and results from mapping projects on the superficial deposits carried ... -
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 ... -
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 der existeret store, isdæmmede indsjøer paa østsiden av Langfjeldene?
(NGU (14), Journal article, 1894)Langfjeldene is the great mountainridge, which runs through southern Norway. Mr.Andr.M.Hansen have forwarded the hypothesis, that in the region east of it (map p. 52) there existed at the end of the ice-age large lakes ... -
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 ... -
Iagttagelser fra bræer i Sogn og Fjordane
(NGU (34), Journal article, 1901)Forkortet: In the valleys in front of the Norwegian glaciers, there are nearly always great plains of sand and gravel, which the glacial streams have deposited. Om pp. 4 to 8, this is instanced by an account of the fluvial ... -
II. Kalkstenshuler i Ranen
(NGU (69), Journal article, 1914)Forkortet: In the district of Rana in Northern Norway (about 66 1\/2\u00B0 N) we have some of the most important layers of limestone and dolomitic limestone in Norway. Grønligrotten (the situation shown on map p.4) is ... -
Isbevegelse i Lillehammer-området, Sør-Norge, under siste nedising.
(NGU (378), Journal article, 1983)The ice movement from the last glaciation in the northern part of the lake Mjøsa district are presented in an ice phase model. Four main ice phases are reconstructed mainly based on striation, but fluted surfaces, poorly ... -
Isrand-dannelser ved Atnesjøen.
(NGU (183), Journal article, 1952)Atnesjø is a lake in Central Norway, 700 m above sea level just to the SE of the Rondane mountain group. The Atnariver enters the lake from the north, and leaves at the north end, forming an affluent to the great Glomma ...