Undersøkelser over norske lerer IV. Norske lerforekomster: B. Møre Sør-Trøndelag, Nord-Trøndelag, delvis Nordland samt resterende del av Akershus, Hedmark og Buskerud fylker.
The present paper is a sequel to the \"Norwegian Clay Deposits A\". Statens Raa- stofskomites Publikation No. 16 (The State Raw Material Commitee Publication No. 16) by the same author and is chiefly a description of the occurence of samples of clay collected during the summer of 1923. In...
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ftnorgesgu:oai:openarchive.ngu.no:11250/2674494 2023-05-15T17:24:36+02:00 Undersøkelser over norske lerer IV. Norske lerforekomster: B. Møre Sør-Trøndelag, Nord-Trøndelag, delvis Nordland samt resterende del av Akershus, Hedmark og Buskerud fylker. Dietrichson, Brynjulf 14204 Stangvik 13203 Åndalsnes 13202 Eresfjord 13201 Tingvoll RENNEBU ORKLAND MELHUS RINDAL MØRE OG ROMSDAL TRØNDELAG NORDLAND VIKEN INNLANDET RAUMA MOLDE TINGVOLL SURNADAL SYKKYLVEN 1924 application/pdf https://hdl.handle.net/11250/2674494 nor nor NGU (120) https://hdl.handle.net/11250/2674494 Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no CC-BY 52 LEIR KVARTÆRGEOLOGI AVSETNING SKREDAVSETNING SKREDFORM GLASIALGEOLOGI MORENE Journal article 1924 ftnorgesgu 2022-07-03T15:26:46Z The present paper is a sequel to the \"Norwegian Clay Deposits A\". Statens Raa- stofskomites Publikation No. 16 (The State Raw Material Commitee Publication No. 16) by the same author and is chiefly a description of the occurence of samples of clay collected during the summer of 1923. In Northern Norway the brick-making industry is less extended than in the districts described in the foregoing paper. In order to obtain a more extensive representation of existing clays, samples were taken, not only from the clay pits at brick fields, but also from clay deposits made accessible by the landslides and slips, that frequently occur in the Trøndelag district. In his introduction, the author points aout that the northernclys on the whole consits of a coarser material than the deposits in the south of the couuntry, and he presumes the cause of this to be that the material in the north has not suffered so many re-sedimentations. Beside mechanical sorting, the clay material suffers chemical changes when constantly under the influence of a large surplus of water. The author points out that there exists a connection between the moranic masses found within the draining districts of a river system and the marine clay deposits occurring at the bottom of the valley. 35532 Article in Journal/Newspaper Nordland Nordland Northern Norway Nordland NGU Open Archive (Geological Survey of Norway) Norway Viken ENVELOPE(19.395,19.395,69.232,69.232) Raa ENVELOPE(14.933,14.933,68.583,68.583) Molde ENVELOPE(7.159,7.159,62.738,62.738) Rauma ENVELOPE(7.717,7.717,62.550,62.550) Rindal ENVELOPE(9.211,9.211,63.051,63.051) Surnadal ENVELOPE(8.725,8.725,62.974,62.974) Tingvoll ENVELOPE(13.934,13.934,67.008,67.008) Åndalsnes ENVELOPE(7.687,7.687,62.567,62.567) Orkland ENVELOPE(9.693,9.693,63.230,63.230) |
institution |
Open Polar |
collection |
NGU Open Archive (Geological Survey of Norway) |
op_collection_id |
ftnorgesgu |
language |
Norwegian |
topic |
LEIR KVARTÆRGEOLOGI AVSETNING SKREDAVSETNING SKREDFORM GLASIALGEOLOGI MORENE |
spellingShingle |
LEIR KVARTÆRGEOLOGI AVSETNING SKREDAVSETNING SKREDFORM GLASIALGEOLOGI MORENE Dietrichson, Brynjulf Undersøkelser over norske lerer IV. Norske lerforekomster: B. Møre Sør-Trøndelag, Nord-Trøndelag, delvis Nordland samt resterende del av Akershus, Hedmark og Buskerud fylker. |
topic_facet |
LEIR KVARTÆRGEOLOGI AVSETNING SKREDAVSETNING SKREDFORM GLASIALGEOLOGI MORENE |
description |
The present paper is a sequel to the \"Norwegian Clay Deposits A\". Statens Raa- stofskomites Publikation No. 16 (The State Raw Material Commitee Publication No. 16) by the same author and is chiefly a description of the occurence of samples of clay collected during the summer of 1923. In Northern Norway the brick-making industry is less extended than in the districts described in the foregoing paper. In order to obtain a more extensive representation of existing clays, samples were taken, not only from the clay pits at brick fields, but also from clay deposits made accessible by the landslides and slips, that frequently occur in the Trøndelag district. In his introduction, the author points aout that the northernclys on the whole consits of a coarser material than the deposits in the south of the couuntry, and he presumes the cause of this to be that the material in the north has not suffered so many re-sedimentations. Beside mechanical sorting, the clay material suffers chemical changes when constantly under the influence of a large surplus of water. The author points out that there exists a connection between the moranic masses found within the draining districts of a river system and the marine clay deposits occurring at the bottom of the valley. 35532 |
format |
Article in Journal/Newspaper |
author |
Dietrichson, Brynjulf |
author_facet |
Dietrichson, Brynjulf |
author_sort |
Dietrichson, Brynjulf |
title |
Undersøkelser over norske lerer IV. Norske lerforekomster: B. Møre Sør-Trøndelag, Nord-Trøndelag, delvis Nordland samt resterende del av Akershus, Hedmark og Buskerud fylker. |
title_short |
Undersøkelser over norske lerer IV. Norske lerforekomster: B. Møre Sør-Trøndelag, Nord-Trøndelag, delvis Nordland samt resterende del av Akershus, Hedmark og Buskerud fylker. |
title_full |
Undersøkelser over norske lerer IV. Norske lerforekomster: B. Møre Sør-Trøndelag, Nord-Trøndelag, delvis Nordland samt resterende del av Akershus, Hedmark og Buskerud fylker. |
title_fullStr |
Undersøkelser over norske lerer IV. Norske lerforekomster: B. Møre Sør-Trøndelag, Nord-Trøndelag, delvis Nordland samt resterende del av Akershus, Hedmark og Buskerud fylker. |
title_full_unstemmed |
Undersøkelser over norske lerer IV. Norske lerforekomster: B. Møre Sør-Trøndelag, Nord-Trøndelag, delvis Nordland samt resterende del av Akershus, Hedmark og Buskerud fylker. |
title_sort |
undersøkelser over norske lerer iv. norske lerforekomster: b. møre sør-trøndelag, nord-trøndelag, delvis nordland samt resterende del av akershus, hedmark og buskerud fylker. |
publishDate |
1924 |
url |
https://hdl.handle.net/11250/2674494 |
op_coverage |
14204 Stangvik 13203 Åndalsnes 13202 Eresfjord 13201 Tingvoll RENNEBU ORKLAND MELHUS RINDAL MØRE OG ROMSDAL TRØNDELAG NORDLAND VIKEN INNLANDET RAUMA MOLDE TINGVOLL SURNADAL SYKKYLVEN |
long_lat |
ENVELOPE(19.395,19.395,69.232,69.232) ENVELOPE(14.933,14.933,68.583,68.583) ENVELOPE(7.159,7.159,62.738,62.738) ENVELOPE(7.717,7.717,62.550,62.550) ENVELOPE(9.211,9.211,63.051,63.051) ENVELOPE(8.725,8.725,62.974,62.974) ENVELOPE(13.934,13.934,67.008,67.008) ENVELOPE(7.687,7.687,62.567,62.567) ENVELOPE(9.693,9.693,63.230,63.230) |
geographic |
Norway Viken Raa Molde Rauma Rindal Surnadal Tingvoll Åndalsnes Orkland |
geographic_facet |
Norway Viken Raa Molde Rauma Rindal Surnadal Tingvoll Åndalsnes Orkland |
genre |
Nordland Nordland Northern Norway Nordland |
genre_facet |
Nordland Nordland Northern Norway Nordland |
op_source |
52 |
op_relation |
NGU (120) https://hdl.handle.net/11250/2674494 |
op_rights |
Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no |
op_rightsnorm |
CC-BY |
_version_ |
1766115696689807360 |