De alluviale gullforekomster i indre Finnmark.
The first find of alluvial gold in Finnmarken was made by inspector (bergmester) Tellef Dahll in 1866 in sand from a small river named Nitusjokka near Karasjok. During the following 5 years gold deposits were found in all the rivers of the Tana river systm and the Alta and Reisa rivers. Gold has bee...
Main Author: | |
---|---|
Format: | Article in Journal/Newspaper |
Language: | Norwegian |
Published: |
1966
|
Subjects: | |
Online Access: | https://hdl.handle.net/11250/2674832 |
id |
ftnorgesgu:oai:openarchive.ngu.no:11250/2674832 |
---|---|
record_format |
openpolar |
spelling |
ftnorgesgu:oai:openarchive.ngu.no:11250/2674832 2023-05-15T13:20:42+02:00 De alluviale gullforekomster i indre Finnmark. Bjørlykke, Harald 20334 Iesjåkka 20333 Bæivasgiedde 20332 Galmatskai'di 20331 Karasjok KAUTOKEINO KARASJOK 1966 application/pdf https://hdl.handle.net/11250/2674832 nor nor NGU (236) https://hdl.handle.net/11250/2674832 Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no CC-BY 1-66 AVSETNING ELVEAVSETNING MAGNETOMETRI MALMGEOLOGI GULL GEOLOGISK UNDERSØKELSE Journal article 1966 ftnorgesgu 2022-07-03T15:26:50Z The first find of alluvial gold in Finnmarken was made by inspector (bergmester) Tellef Dahll in 1866 in sand from a small river named Nitusjokka near Karasjok. During the following 5 years gold deposits were found in all the rivers of the Tana river systm and the Alta and Reisa rivers. Gold has been found in small amount in all kinds of sand- and gravel deposits and also in the unwashed moraine deposits. The gold fields which have been subject to production or prospection work are situated at the upper parts of the rivers. The occurrences of alluvial gold in Finnmark may be classified in The following way: 1. Preglacial accumulations undisturbed by ice erosion during the ice age. 2: Preglacial accumulations disturbed and redeposited in moraines and fluvioglacial deposits. 3. Accumulations in postglacial river beds. The gold in these deposits seems chiefly to have been washed out from the moraines. Mineralogical analyses of the mineral composition of the gold-bearing sand and gravel have been carried out. The minerals of the gold-bearing deposits may be divided in two groups: 1. Minerals belonging to the surrounding solid rock. 2. Minerals which do not seem to belong to the solid rock in the neighbourhood of the deposits. 35214 Article in Journal/Newspaper Alta Finnmark Karasjok Kautokeino Tana Finnmark NGU Open Archive (Geological Survey of Norway) Alta Kautokeino ENVELOPE(23.048,23.048,69.003,69.003) Karasjok ENVELOPE(25.519,25.519,69.472,69.472) Reisa ENVELOPE(8.414,8.414,63.433,63.433) Tana River ENVELOPE(28.395,28.395,70.503,70.503) |
institution |
Open Polar |
collection |
NGU Open Archive (Geological Survey of Norway) |
op_collection_id |
ftnorgesgu |
language |
Norwegian |
topic |
AVSETNING ELVEAVSETNING MAGNETOMETRI MALMGEOLOGI GULL GEOLOGISK UNDERSØKELSE |
spellingShingle |
AVSETNING ELVEAVSETNING MAGNETOMETRI MALMGEOLOGI GULL GEOLOGISK UNDERSØKELSE Bjørlykke, Harald De alluviale gullforekomster i indre Finnmark. |
topic_facet |
AVSETNING ELVEAVSETNING MAGNETOMETRI MALMGEOLOGI GULL GEOLOGISK UNDERSØKELSE |
description |
The first find of alluvial gold in Finnmarken was made by inspector (bergmester) Tellef Dahll in 1866 in sand from a small river named Nitusjokka near Karasjok. During the following 5 years gold deposits were found in all the rivers of the Tana river systm and the Alta and Reisa rivers. Gold has been found in small amount in all kinds of sand- and gravel deposits and also in the unwashed moraine deposits. The gold fields which have been subject to production or prospection work are situated at the upper parts of the rivers. The occurrences of alluvial gold in Finnmark may be classified in The following way: 1. Preglacial accumulations undisturbed by ice erosion during the ice age. 2: Preglacial accumulations disturbed and redeposited in moraines and fluvioglacial deposits. 3. Accumulations in postglacial river beds. The gold in these deposits seems chiefly to have been washed out from the moraines. Mineralogical analyses of the mineral composition of the gold-bearing sand and gravel have been carried out. The minerals of the gold-bearing deposits may be divided in two groups: 1. Minerals belonging to the surrounding solid rock. 2. Minerals which do not seem to belong to the solid rock in the neighbourhood of the deposits. 35214 |
format |
Article in Journal/Newspaper |
author |
Bjørlykke, Harald |
author_facet |
Bjørlykke, Harald |
author_sort |
Bjørlykke, Harald |
title |
De alluviale gullforekomster i indre Finnmark. |
title_short |
De alluviale gullforekomster i indre Finnmark. |
title_full |
De alluviale gullforekomster i indre Finnmark. |
title_fullStr |
De alluviale gullforekomster i indre Finnmark. |
title_full_unstemmed |
De alluviale gullforekomster i indre Finnmark. |
title_sort |
de alluviale gullforekomster i indre finnmark. |
publishDate |
1966 |
url |
https://hdl.handle.net/11250/2674832 |
op_coverage |
20334 Iesjåkka 20333 Bæivasgiedde 20332 Galmatskai'di 20331 Karasjok KAUTOKEINO KARASJOK |
long_lat |
ENVELOPE(23.048,23.048,69.003,69.003) ENVELOPE(25.519,25.519,69.472,69.472) ENVELOPE(8.414,8.414,63.433,63.433) ENVELOPE(28.395,28.395,70.503,70.503) |
geographic |
Alta Kautokeino Karasjok Reisa Tana River |
geographic_facet |
Alta Kautokeino Karasjok Reisa Tana River |
genre |
Alta Finnmark Karasjok Kautokeino Tana Finnmark |
genre_facet |
Alta Finnmark Karasjok Kautokeino Tana Finnmark |
op_source |
1-66 |
op_relation |
NGU (236) https://hdl.handle.net/11250/2674832 |
op_rights |
Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no |
op_rightsnorm |
CC-BY |
_version_ |
1766355165614440448 |