(Last updated: 29.05.2013)
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Norsk versjon | ||||
| THE NATURAL STONE DATABASE | |||||
| Occurence 5546 - 606 Morsoneset | |||||
| (Object Id: 12428) (Last updated: 29.05.2013) |
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| Location |
| County: | Troms | Municipality: | Kvænangen (5546) |
| Map 1:50000: | Kvænangen (1734-1) | Map 1:250000: | Nordreisa |
| Coordinate system: | EU89-UTM Zone 34 |
| East: | 540394 m. | North: | 7738365 m. |
| Longitude: | 22.0457770 | Latitude: | 69.7502250 |
| Show on map |
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| Resource |
| Resource Type: | Slate and schist | Resource Subtype: | Quartzitic flagstone | |
| Brickstone(Y/N): | Y |
| Importance |
| Raw material meaning: | Little Importance (reg. 18.02.2015) |
| Historical: | No , (Confirmed 22.sep.2012 by Bjørn Lund) |
| Resources and production |
| Activity: | Stone quarrying | Reserves: | ||
| Operating method: | Open pit mining | Historical production: |
Products |
| Commercial Name | Product description |
| Kvartsittskifer | Classification: Cleaved slabs | Colour: Grayish | |
| Play of colours : | Uniformity: | ||
| Lithology: Quartzrich flagstone | Grain size: Fine - medium grained (<1mm - 3 mm) |
Mineralogy: |
| Feldspar | Major mineral (>10%) | ||
| Quartz | Major mineral (>10%) | ||
| Mica | Subordinate mineral (1-10%) |
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Operations |
| From - To | Activity | Comments | |
| - 1939 | Regular production |
Deposit rock |
| Lithology: | Quartzrich flagstone | Weathering colour: | Gray | |
| Era: | Paleozoic | Period: | ||
| Genesis: | Form: | Layer | ||
| Main texture: | Schistose |
| Main grain size: | Fine - medium grained (<1mm - 3 mm) | Main alteration: |
| Strike/Dip: | 260 / 26 | Direction: | ||
| Plunge: |
| Stratigraphic classification of host rock |
| Era: | Paleozoic | Period: |
| Province: | ||
| Geotec.unit: | ||
| Tectonic complex: | ||
| Igneous complex: |
| Group: | Formation: |
Structures |
| Location: | Type: | Orientation(360 gr.): | Relation to min.: | |
| Not defined | Schistosity | Strike/Dip :260 / 26 |
Information(s) in free text format |
| Description |
| Over et område på 200 x 200 m ligger flere små kvartsittbrudd. Bruddene ble drevet til like før krigen (1940). Skiferen er en tyntspaltende kvartsittskifer og ble brukt hovedsakelig til takskifer. Området har også potensial til murestein. |
| Location |
| Bruddorådet ligger like ved sjøen, men er uten veiforbindelse. Nærmeste vei ligger ved Toppelbukt i en avstan av sc.1,5 km. |
| The fact sheet was created on 04.05.2024 |
| Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
| Copyright © 2024 Geological Survey of Norway |