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English version | ||||
| NATURSTEINSDATABASEN | |||||
| Forekomstområde 1824 - 608 | |||||
| (Sist oppdatert 05.mai.2010) | |||||
Navn på deposit area : Drevjadalen |
| (Objekt Id : 1824,608,00,00) |
| Lokalisering |
| Fylke : | Nordland (18) | Kommune : | Vefsn (1824) |
| Kart 1:50000: | Mosjøen (1826-1) | Kart 1:250000: | Mosjøen |
| Markeringspunkt: | Lengdegrad: | 13.0895820 | Breddegrad: | 65.8666710 |
| EU89-UTM Zone 33 | (Coordinates IS confirmed) |
| X-koord: | 412850 m. | Y-koord: | 7306375 m. |
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| Materialtype |
| Hovedtype: | Kleberstein og serpentinitt | Subtype: | Kleberstein | |
| Brickstone(Y/N): | N |
| Production |
| Activity: | Steinbrudd | Reserves: | ||
| Prod. method: | Dagbrudd | Production: | ||
| Prod. status: | Nedlagt | Volume of dump: |
| Betydning |
| Offentlig: | Not Assessed (reg. 18.02.2015) |
| Economical: | Ikke vurdert , (Confirmed 27.jun.2001 by Tom Heldal) |
Deposit rock |
| Lithology: | Weathering colour: | |||
| Era: | Period: | |||
| Dating: | Method: | |||
| Genesis: | Form: | |||
| Main texture: |
| 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: |
Opplysning(er) i fritekstformat |
| Fri tekst |
| Klebersteinen oppter som et linseformig legeme i glimmerskifer |
Bibliography: |
| From NGU's Reference Archive: |
| Nissen, August L. , 1974 |
| Mosjøen. Beskrivelse til det berggrunnssgeologiske gradteigskart I 17 1 : 100 000. |
| ;Norges geologiske undersøkelse;KARTBESKRIVELSE; TIDSSKRIFTARTIKKEL;NGU; Skrifter; No.307; 12;1 - 29 + pages |
| Abstract: | |
| Description are given of the various lithologies occurring within the map area. These mainly comprise Cambro - Silurian supracrustals and intrusive, as well as granitic basement rocks of supposed Precambrian age. The intrusive rocks are principally those of the Bindal (granitoid) and Mosjøen (gabbro) massifs. These bodies are younger than the supracrustals, but their mutual age relationship is uncertain. The Alsten granite, however, is thought to be older than the other massifs. Minerale assemblages present in the metasedimentary rocks denote that these lithologies have been metamorphosed in the almandine-amphibolite facies. Evidence of at least three Caledonian fold episodes is present in the area. |
Fieldsamples |
| Sample No. | Sample type | Miscellanrous | |||
| 110F | Bedrock |
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| Faktaarket ble generert 13.06.2026 |
| Spørsmål eller kommentarer vedrørende faktaarket kan mailes til: ressursdatabaser@ngu.no |
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