Norsk versjon | |||||
THE NATURAL STONE DATABASE | |||||
Deposit Area 1621 - 601 | |||||
(Last updated 26.jan.2010) |
Name of Deposit Area : Ørland |
(Object Id : 1621,601,00,00) |
Location |
County : | Sør-Trøndelag (16) | Municipality : | Ørland (1621) |
Map 1:50000: | Ørland (1522-3) | Map 1:250000: | Trondheim |
Marking point: | Longitude: | 9.6742840 | Latitude: | 63.7119570 |
EU89-UTM Zone 32 | (Coordinates IS confirmed) |
X-coord: | 533319 m. | Y-coord: | 7065093 m. |
|
Commodity |
Main Type: | Gneiss | Sub Type: | Gneiss | |
Brickstone(Y/N): | N |
Production |
Activity: | Stone quarrying | Reserves: | ||
Prod. method: | Open pit mining | Production: | ||
Prod. status: | Disused, closed | Volume of dump: |
Importance |
Public: | Little Importance (reg. 18.02.2015) |
Economical: | Minor interest , (Confirmed 24.nov.2006 by Leif Furuhaug) |
Historical: | No , (Confirmed 12.jan.2010 by Leif Furuhaug) |
Products |
Commercial Name | Product description |
Ørland | Classification : | Colour : | |
Play of colours : | Uniformity : | ||
Lithology : | Grain size : |
Mineralogy: |
Plagioclase | Major mineral (>10%) | ||
Quartz | Major mineral (>10%) | ||
Potassic feldspar | Major mineral (>10%) | ||
Epidote | Accessory mineral (<1%) |
Deposit rock |
Lithology: | Tonalite | Weathering colour: | ||
Era: | Paleozoic | Period: | ||
Dating: | Method: | |||
Genesis: | Form: | |||
Main texture: |
Main grain size: | Main alteration: |
Strike/Dip: | Direction: | |||
Plunge: |
Stratigraphic classification of host rock |
Era: | Paleozoic | Period: |
Province: | ||
Geotec.unit: | ||
Tectonic complex: | ||
Igneous complex: |
Group: | Formation: |
Information(s) in free text format |
Description |
Forekomsten er egentlig en pukkforekomst. Detaljerte opplysninger er registrert i pukkdatabasen. Forekomsten ligger på militært område. Den var i drift som pukkforekomst i 1985, men er ikke i drift idag. |
The fact sheet was created on 19.05.2024 |
Questions or comments regarding the fact sheet can be emailed to: ressursdatabaser@ngu.no |
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