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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Bibliographic Details
Main Author: Foslie, Steinar
Format: Article in Journal/Newspaper
Language:Norwegian
Published: 1941
Subjects:
Online Access:https://hdl.handle.net/11250/2674532
id ftnorgesgu:oai:openarchive.ngu.no:11250/2674532
record_format openpolar
spelling 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