Browsing Artikler by Subject "BORING"
Now showing items 1-20 of 20
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En undersøkelse av kvartære, økostratigrafiske soner i Drammen, på grunnlag av foraminiferer.
(NGU (215), Journal article, 1962)1. The present paper is a report on a quantitative study of the fossil, benthonic foraminifera of Late- and Post-Galcial clay samples from Drammen, Norway. 2. On the basia of their content of foraminifera, it has been ... -
Grunnvann i Vestfold. Meddelelse fra Vannboringsarkivet nr. 11.
(NGU (213), Journal article, 1961)Drilling for water has become very common in the county of Vestfold since World War II. The water is mostly restricted to fractures, joints, fissures and solution openings in the rocks. The main rock-types found in Vestfold ... -
Grunnvatnet
(NGU (92), Journal article, 1922) -
Ingeniørgeologiske undersøkelser for anlegg i fjell.
(NGU; Skrifter (352; 30), Journal article, 1979)The purpose of this paper is to provide geologists with an outline of the procedures and methods used by engineering geologists in the planning and construction of underground openings in rock. Examples of different types ... -
Kulforekomsten paa Andøen
(NGU (4), Journal article, 1891)Forkortet: A map and section are given p. 132. \"Myr\" signifies peatmoss, \"sandsten\" sand- stone, \"lerjernsten\" clay ironstone, \"bitumines skifer\" bituminous shale, \"skjælmergel\" shell-marl, \"borhul\" borehole, ... -
Lerfall ved Roel, Innerøy.
(NGU (166), Journal article, 1946)Innerøy is situated on the South-Eastern shore of Borgenfjord, a branch of Trondheimsfjord. The slip occurred in the afternoon of the 24th of April 1937. A road near the beach was destroyed by the slide over a distance of ... -
Marine kvartær-fossiler fra Seimsjøen i Sør-Odal.
(NGU (205), Journal article, 1959)The locality is situated 67 km NE of Oslo centre, at the outlet of Seimsjøen, the southwestern extension of Storsjøen lake (water level 130 m above sea level). Borings were undertaken by the Norwegian Geotechnical Institute, ... -
Meddelelser fra Vannboringsarkivet nr. 2. Vannboringer utført i traktene omkring Mjøsa og Randsfjorden 1950-52.
(NGU (184), Journal article, 1953)A brief report is given on some water-borings carried out at Mjøsa and northern Randsfjord during the last few years. The rocks in the districts in question consist of Precambrian granite and gneiss. Eocambrian sandstone ... -
Meddelelser fra Vannboringsarkivet. Nr. 1. En orientering om arkivets arbeidsgrunnlag. Om samarbeide med boringsfirmaene. Den viktigste fennoskandiske faglitteratur.
(NGU (184), Journal article, 1953)The article is the first report from the sewly established archives for well drillings in Norwegian bedrock. The number of wells is estimated to about 1300. The data, obtained in cooperation with well-drillers, concern ... -
Om torvmyrer i Norge og deres tilgodegjørelse. Anden del
(NGU (24), Journal article, 1897)Forkortet: 1. The occurrence of peat-mosses. The peat occurs most abundantly in the neighbourhood of the coast line owing to the greater humidity of the climate there. The different kinds of mosses and their characetristics ... -
Om torvmyrer i Norge og deres tilgodegjørelse. Første del
(NGU (20), Journal article, 1896)Forkortet: 1. The method of investigation. Maps of the mosses are made to the scale of 1:5000 and printed in the scale of 1:20 000. The depths are stated by borings, and specimens from the different layers studied. The ... -
Om torvmyrer i Norge. Tredje del
(NGU (38), Journal article, 1904)Forkortet: The book is the third and concluding volume of the book, that has been printed as the numerous 20 and 24 of the publications of the Geological Survey of Norway. The volume contains detailed descriptions of mosses ... -
Orienterende undersøkelser vedrørende sprøhet og flisighet av bergarter.
(NGU (247), Journal article, 1967) -
Ras i Mikvoldmelen, Værdalsøren.
(NGU (166), Journal article, 1946)A river steep of considerable length and height is situated on the right hand of the Værdal river at its mouth in the Trondheim fjord. Consisting og loose materials, an upper layer of sand and a lower one of sandy clay, ... -
Ras ved Jonsrud på Feiringveien.
(NGU (166), Journal article, 1946)In the vicinity of Jonsrud on the beach of lake Mjøsa, the road is built in a steep slope about 30 m above the level. Here the road surveyor in the autumn of 1935 observed fissures through the ground. On the 23rd of September ... -
Results of recent geological and geophysical investigations in Moray Firth, Scotland.
(NGU (316), Journal article, 1975)Geophysical, shallow drilling and sea-bed sampling investigations have shown that the main sedimentary basin of the Moray Firth is separated by an ENE-trending, horst-like uplift zone from a secondary basin to the south. ... -
Terrænundersøgelser og jordboringer i Stjørdalen, Værdalen og Guldalen samt i Trondhjem i 1894, 95 og 96
(NGU (27), Journal article, 1898)Forkortet: The Norwegian valleys filled up at a large extent by gravel, sand and clay in the course of time been submitted to earthslips and sinking of the grounds, however more especially those of Gauldalen, Stjørdalen ... -
"Trysilhevningen". Kambro-ordovicisk stratigrafi i Femundtraktene.
(NGU (215), Journal article, 1962)Diamond drillings carried out 1960 in the vicinity of the lake Femund, near the Swedish border (fig. 1) gave new informations about the cambro-ordovician stratigraphy in the south-eastern miogeosynclinal belt of the ... -
Utgliding av jernbanefylling ved Kolbotn stasjon.
(NGU (166), Journal article, 1946)This station lies on the Østfold railway, 13 km from Oslo. One day in November 1936 a 4 m high newly built ballast with the rails on it suddenly sunk into a ground consisting of peat and a weak clayey deposit. Over a ... -
V. Om Andøens jurafelt, navnlig om landets langsomme nedsynken under juratiden og den senere hævning samt gravforkastning
(NGU (43), Journal article, 1905)Forkortet:Das Andøya Jurafeld, das auf der Strandebene (s. Fig.1,4 und Tafel I.Profil Fig.1 und 2) liegt, hat eine L\u00E4nge von ca. 8.4 Km und ein Areal auf festem Lande von etwa 10 km\u00B2; das Areal muss aber noch ...