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THE ???? DATABASE | |||||
Occurence 0 - 000 FEIL | |||||
(Object Id: ) (Last updated: 26.04.2020) |
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Location |
County: | Municipality: | Mangler () |
Map 1:50000: | Astafjorden (1332-2) | Map 1:250000: | Narvik |
County: | UTM-Zone 33 - EUREF89/WGS84 |
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Resource |
Resource Type: | Ferrous metals(Fe, Mn, Ti) | Resource Subtype: | Iron | |
Element(s): | Fe |
Importance |
Raw material meaning: | Not Assessed (reg. 18.02.2015) |
Mineralization |
Genesis: | Form: | |||
Main texture: | Min. distribution: |
Main grain size: | Main alteration: |
Strike/Dip: | Direction: | |||
Plunge: |
Stratigraphic classification of host rock |
Era: | Period: |
Province: | ||
Geotec.unit: | ||
Tectonic complex: | ||
Igneous complex: |
Group: | Formation: |
Information(s) in free text format |
Free text |
A linear magnetic anomaly in Runddalen, SW of Skoddebergvatnet, appears to be the northwards continuation of the Kleven iron formation. The central part of the anomaly is covered by scree and glacial material, but minor outcrops along a stream show calcareous mica schist with disseminated magnetite. The iron formation is at least 2 m thick (Sample JSFE1418), and is situated above a 5 m thick marble on top of garnet mica schist. The strike is N-S with moderate dips towards west (185°/35°). |
Fieldsamples |
Sample No. | Sample type | Miscellanrous | |||||
JSFE1418 | Bedrock |
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NB! All analyse values are shown at the end of the printout.: |
The fact sheet was created on 03.05.2024 |
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