Blar i Artikler på emneord "GEOMORFOLOGI"
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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 ... -
Dybderne i nogle indsjøer i Jotunfjeldene og Thelemarken
(NGU (14), Journal article, 1894)Many of our lakes are very deep; some of them are deeper than the bottom of the sea nearest to them. The depths are given in metres -
Echo-soundings in the Skagerrak. With remarks on the geomorphology.
(NGU (223), Journal article, 1963)Denne avhandling gir, først og fremst på plansjer og andre figurer, resultatet av ekko,lodninger som på foranledning av forfatteren, i tidsrommet 1953-60, er blitt utført i Skagerrak-området av en rekke fartøyer til belysning ... -
Evolution structurale de la region Nisser - Vråvatn (Norvege meredionale). (The precambrian rocks of the Telemark area in south central Norway no. VIII. Strucutral development of the Nisser-Vråvatn region.)
(NGU (266), Journal article, 1970)Tectonic and petrographic studies of the Precambrian rocks in the Nisser-Vråvatn region of Telemark have led to the recognition of the following principal features: (1) The basement of the \"Telemark suite\" does not appear ... -
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 ... -
IV. Litt om Jutulhugget
(NGU (79), Journal article, 1917)The Jutulhug (\"The big Troll's Notch\") is a cleft or canyon situated in the central part of Southern Norway under 62 degrees N. As our somewhat schematic drawing on p. 4 shows, it is situated in a wide saddle between the ... -
Karsthuler i Nordland.
(NGU (165), Journal article, 1947)The cave passages are mostly tunnel shaped, usually with a circular or elliptical section. These passages were formed when they were completely water-filled. Underground streams have later made cuts into the floor of some ... -
Litt om Mjøsjøkelen
(NGU (37), Journal article, 1903)Forkortet: To the East of lake Mjøsa is at Brummundal an isolated outcrop of \"rhombic-feldspar-porphyry\" accompanied by a red or yellowish sandstone quite unique in Norway. The joint occurrence of these exceptional rocks ... -
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 glasifluviale isrand-avsetninger i den sydlige del av Glomma- vassdragets (nåværende) dreneringsområde. Med en del berggeologisk-morfologiske data fra de nordlige Øyeren-traktene.
(NGU; Skrifter (306; 11), Journal article, 1974)The present paper represents more or less a continuation of the writer's publication from 1924, which mainly dealt with the northern Romerike district of southeastern Norway, from Jessheim to Lake MjThe present paper ... -
Nogle bidrag til forstaaelsen af, hvorledes Norges dale og fjelde er blevne til
(NGU (32), Journal article, 1901)Forkortet: Up to the present, the relief of Norway has not been understood sufficiently to allow of a satisfactory explanation being given of even the most salient features, such as the contrast between plateau and valley, ... -
North Sea troughs and plate tectonics.
(NGU (316), Journal article, 1975)Interlinked roughly trilete-shaped predominantly sub-Upper Cretaceous trough systems extending north-south for more than 1200 km are described for the North Sea basin and the Northeast Atlantic. Palimpsest tectonic controls ... -
Om elve-erosjon og en isdemt sjø i Birtavarre-området, Troms.
(NGU (184), Journal article, 1953)The geological survey in the Birtavarre region during the summer 1952 had as its main purpose the investigation of the copper ores of the district. However, some attention was also paid to geomorphological and quaternary ... -
Possible Mesozoic mantle plume activity beneath the continental margin of Norway.
(NGU (322), Journal article, 1975)Based on recent geological and geophysical information from the Norwegian\/Greenland Sea and North Sea areas, and on earlier geomorphological information interpreted in terms of regional drainage pattern evolution, it is ... -
Strandfladen, et nyt træk i Norges geografi
(NGU (14), Journal article, 1894)Forkortet: The western slopes of the Scandinavian peninsula do not generally extend quite to the sea; but we see there low almost level parts, which the author calls the Norwegian coast plain. The figures on pp. 1 and 2 ... -
Structure and evolution of the Atlantic floor between Northern Scotland and Iceland.
(NGU (316), Journal article, 1975)The continental shelf west of the Shetland and Orkney islands is a region of varied geology traversed by the Caledonian front, including some areas of shallow basement and some partially fault-bounded Mesozoic basins such ... -
The geology of the Leirpollen area, Tanafjord, Finnmark.
(NGU (247), Journal article, 1967)900 metres of sedimentary rocks, including Eocambrian tillits, have been mapped on 1:50 000 and 1:25 000 scales around Leirpollen and correlated with Vestertana Group which outcrops on the Digermul Peninsula. The rocks ... -
Vega. Beskrivelse til det geologiske generalkart
(NGU (80), Journal article, 1917)The region described is situated on the coast of Northern Norway between 65 and 66 dgrs. N. The coast is surrounded by a girdle of islands and skerries. This archipelago is up to 50 km broad. Here are the islands Leka, ... -
Voss. Fjeldbygningen inden rektangelkartet Voss's omraade
(NGU (40), Journal article, 1905)Forkortet:The Western gneiss region. The lightest red in the map is gneiss, the darkestred is an amphibole-bearing rock, the Evanger diorite, mostly made schistoseby compression; the middle red represents granite the ...