|
|
Norsk versjon | ||||
| THE INDUSTRIAL MINERAL DATABASE | |||||
| Deposit Area 1849 - 315 | |||||
| (Last updated 11.mar.2019) | |||||
Name of Deposit Area : Lilandsmarka |
| (Object Id : 1849,315,00,00) |
| Location |
| County : | Nordland (18) | Municipality : | Hamarøy (1849) |
| Map 1:50000: | Hamarøya (1231-3) | Map 1:250000: | Svolvær |
| Marking point: | Longitude: | 15.5076150 | Latitude: | 68.0901150 |
| EU89-UTM Zone 33 | (Coordinates IS confirmed) |
| X-coord: | 521137 m. | Y-coord: | 7552998 m. |
|
|
| Commodity |
| Main Type: | Feldspar | Sub Type: | Pegmatitic feldspar |
| Production |
| Activity: | Test mining | Reserves: | ||
| Prod. method: | Open pit mining | Production: | ||
| Prod. status: | Disused, closed | Volume of dump: |
| Importance |
| Public: | Not Assessed (reg. 18.02.2015) |
| Economical: | Not classified/evaluated |
Products |
| Element/product | Crude ore grade or quality | |
| CHERAM | ??? % |
Operations |
| From - To | Activity | Comments | |
| Test mining | Company/Institution :Hilling |
Mineralization |
| Era: | Period: | |||
| Dating: | Method: | |||
| Genesis: | Form: | Lens | ||
| Main texture: | Min. distribution: | Irregular (scattered) |
| Main grain size: | Coarse grained (> 3 mm) |
| Strike/Dip: | Direction: | |||
| Plunge: |
| Stratigraphic classification of host rock |
| Era: | Period: |
| Province: | ||
| Geotec.unit: | ||
| Tectonic complex: | ||
| Igneous complex: |
| Group: | Formation: |
Mineralogy |
| Relationship | Mineral | Amount | |
| Not defined | Potassic feldspar | Major mineral (>10%) | |
| Not defined | Quartz | Major mineral (>10%) | |
| Not defined | Plagioclase | Subordinate mineral (1-10%) |
Information(s) in free text format |
| Free text |
| Forekomsten ligger ca. 60 m opp fra veien utover til Skutvik, 2 km syd for Hamsund. Det er opparbetdet traktorvei frem til bruddet hvor kjøpmann Hilling, Innhavet, har tatt ut en prøvelass. Pegmatitten ligger i et sterkt overdekket område, i bruddveggen ses noen få tynne linser og ganger av kvarts. Feltspaten synes å være av meget god kvalitet. Irmdlertid ligger pegmatitten i sterkt stigende terreng med raskt påbyggende overfjell. |
| Photo(s) from the Deposit area: |
|
Fieldsamples |
| Sample No. | Sample type | Miscellanrous | ||
| Ø73-21 | Bedrock |
|
| The fact sheet was created on 17.05.2024 |
| Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
| Copyright © 2024 Geological Survey of Norway |