Fjeldstrøget mellem Saldalen og Dunderlandsdalen.
Forkortet:The region described is situated in the interior of Northern Norway between66\u00B0 30' and 67\u00B0N, and to the east of the Territory treated in The Geology ofNorthern Helgeland, NGU Nr.62.The stratified rocks, occurring here, are mica-schist, crystalline limestone,gneiss and schist...
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1913
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Online Access: | https://hdl.handle.net/11250/2675205 |
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ftnorgesgu:oai:openarchive.ngu.no:11250/2675205 2023-05-15T15:41:13+02:00 Fjeldstrøget mellem Saldalen og Dunderlandsdalen. Rekstad, Johan 20283 Blakkådal 20282 Bjøllådal 20181 Engerdal 20284 Arstaddalen 21283 Lønsdal 21284 Junkerdal SALTDAL RANA MELØY BEIARN GILDESKÅL 1913 application/pdf https://hdl.handle.net/11250/2675205 nor nor NGU (67) https://hdl.handle.net/11250/2675205 Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no CC-BY 1-65 STØRKNINGSBERGART OMDANNET BERGART MALMGEOLOGI KVARTÆRGEOLOGI KARTLEGGING PETROGRAFI Journal article 1913 ftnorgesgu 2022-07-03T15:26:14Z Forkortet:The region described is situated in the interior of Northern Norway between66\u00B0 30' and 67\u00B0N, and to the east of the Territory treated in The Geology ofNorthern Helgeland, NGU Nr.62.The stratified rocks, occurring here, are mica-schist, crystalline limestone,gneiss and schistose quartz-rock. Of these the mica-schist has the greatestextension (see annexted map). The direction of the strike is for the most partN-S to NNE-SSW or parallel with the mountain-range. But near to the borders ofthe great granitic intrusions, it bends along the border-lines of the eruptivesThe mica-schist is graylish and of pronounced, schistosity. It is speckled withbrown garnets, and in some places also with brown staurolite (see Fig.2,pl.VIand Fig.1,pl-VII). Crystalline limestone and marble cover a considerable area(see map). The limestone contains generally a small percentage of magnesia. Inseveral places also layers of dolomite are intercalated in the limestoneseries, mainly in its upper parts. Much of the limestone is gray-coloured andyields a fetid odour when blown. But here also occur white, yellow and redvarieties of the limestone. It contains in part argillaceous matter and passesinto a calcareous schist. The mineral of tremolite occurs often in the dolomite 35714 Article in Journal/Newspaper Beiarn Dunderlandsdalen Gildeskål Helgeland Northern Norway Saltdal NGU Open Archive (Geological Survey of Norway) Arstaddalen ENVELOPE(14.415,14.415,66.950,66.950) Beiarn ENVELOPE(14.572,14.572,67.006,67.006) Dunderlandsdalen ENVELOPE(14.823,14.823,66.447,66.447) Gildeskål ENVELOPE(14.026,14.026,67.034,67.034) Helgeland Junkerdal ENVELOPE(15.572,15.572,66.810,66.810) Lønsdal ENVELOPE(15.463,15.463,66.743,66.743) Meløy ENVELOPE(13.407,13.407,66.824,66.824) Norway Saltdal ENVELOPE(15.317,15.317,66.983,66.983) |
institution |
Open Polar |
collection |
NGU Open Archive (Geological Survey of Norway) |
op_collection_id |
ftnorgesgu |
language |
Norwegian |
topic |
STØRKNINGSBERGART OMDANNET BERGART MALMGEOLOGI KVARTÆRGEOLOGI KARTLEGGING PETROGRAFI |
spellingShingle |
STØRKNINGSBERGART OMDANNET BERGART MALMGEOLOGI KVARTÆRGEOLOGI KARTLEGGING PETROGRAFI Rekstad, Johan Fjeldstrøget mellem Saldalen og Dunderlandsdalen. |
topic_facet |
STØRKNINGSBERGART OMDANNET BERGART MALMGEOLOGI KVARTÆRGEOLOGI KARTLEGGING PETROGRAFI |
description |
Forkortet:The region described is situated in the interior of Northern Norway between66\u00B0 30' and 67\u00B0N, and to the east of the Territory treated in The Geology ofNorthern Helgeland, NGU Nr.62.The stratified rocks, occurring here, are mica-schist, crystalline limestone,gneiss and schistose quartz-rock. Of these the mica-schist has the greatestextension (see annexted map). The direction of the strike is for the most partN-S to NNE-SSW or parallel with the mountain-range. But near to the borders ofthe great granitic intrusions, it bends along the border-lines of the eruptivesThe mica-schist is graylish and of pronounced, schistosity. It is speckled withbrown garnets, and in some places also with brown staurolite (see Fig.2,pl.VIand Fig.1,pl-VII). Crystalline limestone and marble cover a considerable area(see map). The limestone contains generally a small percentage of magnesia. Inseveral places also layers of dolomite are intercalated in the limestoneseries, mainly in its upper parts. Much of the limestone is gray-coloured andyields a fetid odour when blown. But here also occur white, yellow and redvarieties of the limestone. It contains in part argillaceous matter and passesinto a calcareous schist. The mineral of tremolite occurs often in the dolomite 35714 |
format |
Article in Journal/Newspaper |
author |
Rekstad, Johan |
author_facet |
Rekstad, Johan |
author_sort |
Rekstad, Johan |
title |
Fjeldstrøget mellem Saldalen og Dunderlandsdalen. |
title_short |
Fjeldstrøget mellem Saldalen og Dunderlandsdalen. |
title_full |
Fjeldstrøget mellem Saldalen og Dunderlandsdalen. |
title_fullStr |
Fjeldstrøget mellem Saldalen og Dunderlandsdalen. |
title_full_unstemmed |
Fjeldstrøget mellem Saldalen og Dunderlandsdalen. |
title_sort |
fjeldstrøget mellem saldalen og dunderlandsdalen. |
publishDate |
1913 |
url |
https://hdl.handle.net/11250/2675205 |
op_coverage |
20283 Blakkådal 20282 Bjøllådal 20181 Engerdal 20284 Arstaddalen 21283 Lønsdal 21284 Junkerdal SALTDAL RANA MELØY BEIARN GILDESKÅL |
long_lat |
ENVELOPE(14.415,14.415,66.950,66.950) ENVELOPE(14.572,14.572,67.006,67.006) ENVELOPE(14.823,14.823,66.447,66.447) ENVELOPE(14.026,14.026,67.034,67.034) ENVELOPE(15.572,15.572,66.810,66.810) ENVELOPE(15.463,15.463,66.743,66.743) ENVELOPE(13.407,13.407,66.824,66.824) ENVELOPE(15.317,15.317,66.983,66.983) |
geographic |
Arstaddalen Beiarn Dunderlandsdalen Gildeskål Helgeland Junkerdal Lønsdal Meløy Norway Saltdal |
geographic_facet |
Arstaddalen Beiarn Dunderlandsdalen Gildeskål Helgeland Junkerdal Lønsdal Meløy Norway Saltdal |
genre |
Beiarn Dunderlandsdalen Gildeskål Helgeland Northern Norway Saltdal |
genre_facet |
Beiarn Dunderlandsdalen Gildeskål Helgeland Northern Norway Saltdal |
op_source |
1-65 |
op_relation |
NGU (67) https://hdl.handle.net/11250/2675205 |
op_rights |
Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no |
op_rightsnorm |
CC-BY |
_version_ |
1766374099515342848 |