Tysfjords geologi. Beskrivelse til det geologiske gradteigskart Tysfjord.
The situation of the map Tysfjord is shown on p. 10. It comprises a very rugged country between the coast and the frontier, with several glaciers and mountains up to 1744 meter. The present paper contains the geomorphology, general geology, tectonics and glacial geology of the district, further the...
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1941
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ftnorgesgu:oai:openarchive.ngu.no:11250/2674532 2023-05-15T16:32:48+02:00 Tysfjords geologi. Beskrivelse til det geologiske gradteigskart Tysfjord. Foslie, Steinar 13314 Evenes 13313 Kjøpsvik 13312 Frostisen 13311 Skjomen NARVIK HAMARØY 1941 application/pdf https://hdl.handle.net/11250/2674532 nor nor NGU (149) https://hdl.handle.net/11250/2674532 Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no CC-BY 1-298 + p STØRKNINGSBERGART KARTLEGGING SEDIMENTÆR BERGART KVARTÆRGEOLOGI PETROGRAFI OMDANNET BERGART Journal article 1941 ftnorgesgu 2022-07-03T15:26:43Z The situation of the map Tysfjord is shown on p. 10. It comprises a very rugged country between the coast and the frontier, with several glaciers and mountains up to 1744 meter. The present paper contains the geomorphology, general geology, tectonics and glacial geology of the district, further the history of mining, a full description of all the non-metallic mineral deposits and of those ore deposits, which are restricted to this map area. The petrology and the rock analyses (amounting to more than 30) are reserved however for a special paper dealing with a wider district. The same is the case with the main ore deposits in the northern part, extending outside the map area. A main feature of the geomorphology of the district is the extreme westerly position of the main Scandinavian watershed. Its distance from the head of some of the present fjords is only 3 km, and in late glacial time this distance in one place was only 1 km. From here the water runs 350 km eastwards to the Gulf of Bothnia. There is scarcely to be found a parallel elsewhere to such an extreme position. The sceneries on both sides of this watershed are widely different. 34900 Article in Journal/Newspaper Hamarøy Kjøpsvik Narvik Narvik Tysfjord NGU Open Archive (Geological Survey of Norway) Evenes ENVELOPE(16.699,16.699,68.460,68.460) Hamarøy ENVELOPE(15.638,15.638,68.084,68.084) Kjøpsvik ENVELOPE(16.374,16.374,68.097,68.097) Narvik ENVELOPE(17.427,17.427,68.438,68.438) Skjomen ENVELOPE(17.401,17.401,68.255,68.255) Tysfjord ENVELOPE(16.374,16.374,68.097,68.097) |
institution |
Open Polar |
collection |
NGU Open Archive (Geological Survey of Norway) |
op_collection_id |
ftnorgesgu |
language |
Norwegian |
topic |
STØRKNINGSBERGART KARTLEGGING SEDIMENTÆR BERGART KVARTÆRGEOLOGI PETROGRAFI OMDANNET BERGART |
spellingShingle |
STØRKNINGSBERGART KARTLEGGING SEDIMENTÆR BERGART KVARTÆRGEOLOGI PETROGRAFI OMDANNET BERGART Foslie, Steinar Tysfjords geologi. Beskrivelse til det geologiske gradteigskart Tysfjord. |
topic_facet |
STØRKNINGSBERGART KARTLEGGING SEDIMENTÆR BERGART KVARTÆRGEOLOGI PETROGRAFI OMDANNET BERGART |
description |
The situation of the map Tysfjord is shown on p. 10. It comprises a very rugged country between the coast and the frontier, with several glaciers and mountains up to 1744 meter. The present paper contains the geomorphology, general geology, tectonics and glacial geology of the district, further the history of mining, a full description of all the non-metallic mineral deposits and of those ore deposits, which are restricted to this map area. The petrology and the rock analyses (amounting to more than 30) are reserved however for a special paper dealing with a wider district. The same is the case with the main ore deposits in the northern part, extending outside the map area. A main feature of the geomorphology of the district is the extreme westerly position of the main Scandinavian watershed. Its distance from the head of some of the present fjords is only 3 km, and in late glacial time this distance in one place was only 1 km. From here the water runs 350 km eastwards to the Gulf of Bothnia. There is scarcely to be found a parallel elsewhere to such an extreme position. The sceneries on both sides of this watershed are widely different. 34900 |
format |
Article in Journal/Newspaper |
author |
Foslie, Steinar |
author_facet |
Foslie, Steinar |
author_sort |
Foslie, Steinar |
title |
Tysfjords geologi. Beskrivelse til det geologiske gradteigskart Tysfjord. |
title_short |
Tysfjords geologi. Beskrivelse til det geologiske gradteigskart Tysfjord. |
title_full |
Tysfjords geologi. Beskrivelse til det geologiske gradteigskart Tysfjord. |
title_fullStr |
Tysfjords geologi. Beskrivelse til det geologiske gradteigskart Tysfjord. |
title_full_unstemmed |
Tysfjords geologi. Beskrivelse til det geologiske gradteigskart Tysfjord. |
title_sort |
tysfjords geologi. beskrivelse til det geologiske gradteigskart tysfjord. |
publishDate |
1941 |
url |
https://hdl.handle.net/11250/2674532 |
op_coverage |
13314 Evenes 13313 Kjøpsvik 13312 Frostisen 13311 Skjomen NARVIK HAMARØY |
long_lat |
ENVELOPE(16.699,16.699,68.460,68.460) ENVELOPE(15.638,15.638,68.084,68.084) ENVELOPE(16.374,16.374,68.097,68.097) ENVELOPE(17.427,17.427,68.438,68.438) ENVELOPE(17.401,17.401,68.255,68.255) ENVELOPE(16.374,16.374,68.097,68.097) |
geographic |
Evenes Hamarøy Kjøpsvik Narvik Skjomen Tysfjord |
geographic_facet |
Evenes Hamarøy Kjøpsvik Narvik Skjomen Tysfjord |
genre |
Hamarøy Kjøpsvik Narvik Narvik Tysfjord |
genre_facet |
Hamarøy Kjøpsvik Narvik Narvik Tysfjord |
op_source |
1-298 + p |
op_relation |
NGU (149) https://hdl.handle.net/11250/2674532 |
op_rights |
Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no |
op_rightsnorm |
CC-BY |
_version_ |
1766022547618398208 |