Fra det indre af Finmarken
Forkortet: The solid rock. In the region between Bjørnstad (NW corner of the map) and the first geological boundary line (dotted on the map) there are mostly sheared, quartzitic, feldsparbearing sandstone, lying more or less horizontally. Near to Boiabeska is a declivity represented on figs.2 and 3,...
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1902
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ftnorgesgu:oai:openarchive.ngu.no:11250/2675101 2023-05-15T16:59:56+02:00 Fra det indre af Finmarken Reusch, Hans 19332 Gal'bajav'ri 19331 Suossjav'ri 20334 Iesjåkka 20333 Bæivasgiedde 20332 Galmatskai'di 20331 Karasjok TANA KAUTOKEINO 19333 Lappuluobbal 19334 Masi 19341 Cåkkaras'sa 19342 Iesjavri KARASJOK PORSANGER ALTA 1902 application/pdf https://hdl.handle.net/11250/2675101 nor nor NGU (36) https://hdl.handle.net/11250/2675101 Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no CC-BY 64 KVARTÆRGEOLOGI MALMGEOLOGI STØRKNINGSBERGART GULL PETROGRAFI Journal article 1902 ftnorgesgu 2022-07-03T15:26:27Z Forkortet: The solid rock. In the region between Bjørnstad (NW corner of the map) and the first geological boundary line (dotted on the map) there are mostly sheared, quartzitic, feldsparbearing sandstone, lying more or less horizontally. Near to Boiabeska is a declivity represented on figs.2 and 3, page 10. On fig.3, the numerals indicate 1. gray, compact, somewhat schistose h\u00E4lleflinta with some phyllite; 2. reddish-gray sparagmite of a gneissic appearance; 3. red phyllite; 4. quartzitic sandstone; gray or greenish gray; 5. greenish gray phyllite with a slight fissility. The rock of Ravna and the neighbourhood (between the dotted lines on the map) is gneiss-granite, very much the same as the Archaean granites with parallel structuer in Southern Norway. At Kara- sjok and to the South and West of it the predominant rocks are altered sandstones, partly pure quartz sandstone, now appearing as quartzite; partly feldspar-bearing sandstone, now looking like gneissic rocks. Basic rocks, altered gabbro, amphibolite and amphibole schists occur there also. The rock at the gold washings at Sargijokk is probably a sheared gneiss, it is a light, fine-grained greenish-gray schist, rich in muscovite and chlorite. The rock is very much contorted as it seen in fig.1 on page 19 which represents a rock-face l m long. 36054 Article in Journal/Newspaper Karasjok Kautokeino Masi NGU Open Archive (Geological Survey of Norway) Alta Karasjok ENVELOPE(25.519,25.519,69.472,69.472) Kautokeino ENVELOPE(23.048,23.048,69.003,69.003) Lappuluobbal ENVELOPE(23.756,23.756,69.216,69.216) Masi ENVELOPE(23.666,23.666,69.444,69.444) Norway Porsanger ENVELOPE(24.956,24.956,70.052,70.052) |
institution |
Open Polar |
collection |
NGU Open Archive (Geological Survey of Norway) |
op_collection_id |
ftnorgesgu |
language |
Norwegian |
topic |
KVARTÆRGEOLOGI MALMGEOLOGI STØRKNINGSBERGART GULL PETROGRAFI |
spellingShingle |
KVARTÆRGEOLOGI MALMGEOLOGI STØRKNINGSBERGART GULL PETROGRAFI Reusch, Hans Fra det indre af Finmarken |
topic_facet |
KVARTÆRGEOLOGI MALMGEOLOGI STØRKNINGSBERGART GULL PETROGRAFI |
description |
Forkortet: The solid rock. In the region between Bjørnstad (NW corner of the map) and the first geological boundary line (dotted on the map) there are mostly sheared, quartzitic, feldsparbearing sandstone, lying more or less horizontally. Near to Boiabeska is a declivity represented on figs.2 and 3, page 10. On fig.3, the numerals indicate 1. gray, compact, somewhat schistose h\u00E4lleflinta with some phyllite; 2. reddish-gray sparagmite of a gneissic appearance; 3. red phyllite; 4. quartzitic sandstone; gray or greenish gray; 5. greenish gray phyllite with a slight fissility. The rock of Ravna and the neighbourhood (between the dotted lines on the map) is gneiss-granite, very much the same as the Archaean granites with parallel structuer in Southern Norway. At Kara- sjok and to the South and West of it the predominant rocks are altered sandstones, partly pure quartz sandstone, now appearing as quartzite; partly feldspar-bearing sandstone, now looking like gneissic rocks. Basic rocks, altered gabbro, amphibolite and amphibole schists occur there also. The rock at the gold washings at Sargijokk is probably a sheared gneiss, it is a light, fine-grained greenish-gray schist, rich in muscovite and chlorite. The rock is very much contorted as it seen in fig.1 on page 19 which represents a rock-face l m long. 36054 |
format |
Article in Journal/Newspaper |
author |
Reusch, Hans |
author_facet |
Reusch, Hans |
author_sort |
Reusch, Hans |
title |
Fra det indre af Finmarken |
title_short |
Fra det indre af Finmarken |
title_full |
Fra det indre af Finmarken |
title_fullStr |
Fra det indre af Finmarken |
title_full_unstemmed |
Fra det indre af Finmarken |
title_sort |
fra det indre af finmarken |
publishDate |
1902 |
url |
https://hdl.handle.net/11250/2675101 |
op_coverage |
19332 Gal'bajav'ri 19331 Suossjav'ri 20334 Iesjåkka 20333 Bæivasgiedde 20332 Galmatskai'di 20331 Karasjok TANA KAUTOKEINO 19333 Lappuluobbal 19334 Masi 19341 Cåkkaras'sa 19342 Iesjavri KARASJOK PORSANGER ALTA |
long_lat |
ENVELOPE(25.519,25.519,69.472,69.472) ENVELOPE(23.048,23.048,69.003,69.003) ENVELOPE(23.756,23.756,69.216,69.216) ENVELOPE(23.666,23.666,69.444,69.444) ENVELOPE(24.956,24.956,70.052,70.052) |
geographic |
Alta Karasjok Kautokeino Lappuluobbal Masi Norway Porsanger |
geographic_facet |
Alta Karasjok Kautokeino Lappuluobbal Masi Norway Porsanger |
genre |
Karasjok Kautokeino Masi |
genre_facet |
Karasjok Kautokeino Masi |
op_source |
64 |
op_relation |
NGU (36) https://hdl.handle.net/11250/2675101 |
op_rights |
Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no |
op_rightsnorm |
CC-BY |
_version_ |
1766052563534217216 |