(Last updated: 15.01.2019)
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Norsk versjon | ||||
| THE INDUSTRIAL MINERAL DATABASE | |||||
| Occurence 1811 - 301 Søbergsli | |||||
| (Object Id: 7376) (Last updated: 15.01.2019) |
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| Location |
| County: | Nordland | Municipality: | Bindal (1811) |
| Map 1:50000: | Bindal (1825-3) | Map 1:250000: | Mosjøen |
| Coordinate system: | EU89-UTM Zone 33 | (Coordinates NOT confirmed) |
| East: | 392032 m. | North: | 7233298 m. |
| Longitude: | 12.6923290 | Latitude: | 65.2052050 |
| Show on map |
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| Resource |
| Resource Type: | Carbonates | Resource Subtype: | Limestone |
| Importance |
| Raw material meaning: | Not Assessed (reg. 18.02.2015) |
Products |
| Element/product | Crude ore grade or quality | Reg. date | |
| Limestone | % | 15.10.2024 |
Mineralization |
| Genesis: | Form: | |||
| Main texture: | Min. distribution: |
| Main grain size: |
| Strike/Dip: | Direction: | |||
| Plunge: |
| Stratigraphic classification of host rock |
| Era: | Paleozoic | Period: |
| Province: | Caledonides | |
| Geotec.unit: | Helgeland Nappe Complex | |
| Tectonic complex: | ||
| Igneous complex: |
| Group: | Formation: |
Information(s) in free text format |
| Free text |
| «Det er en grovkornig hvit marmor, som til dels indeholder grafitskjæl. Det i saltsyre uopløste er kun ubetydelig og bestaar av grafit og spor av kvarts. Denne marmor optræder i betydelige masser og gjennemsættes av spredte granitganger.» J. Rekstad, 1914 «III. Kalksten fra Nordland» |
Bibliography: |
| From NGU's Reference Archive: |
| Rekstad, Johan , 1914 |
| III. Kalksten fra Nordland |
| ;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.69;9 pages |
| Abstract: | |
| Some analyses of limestones from Northern Norway are given. They show that the percentage of carbonate of Magnesium (MgCO3) is small in several of these lime- stones. They may therefore be used in the industries of carbide and cellulose. The limestones of Northern Norway consist of varieties from almost pure carbo- nate of Calcium (CaCO3) to dolomite (CaCO3MgCO3). It was formerly a common belief that all the limestones of this region were too rich in carbonate of Magnesium for such uses, but that is not the case. |
| The fact sheet was created on 02.11.2025 |
| Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
| Copyright © 2025 Geological Survey of Norway |