Norsk versjon
THE ORE DATABASE
Deposit Area 1149 - 020
(Last updated 22.mar.2013)

Name of Deposit Area : Feøy
(Object Id : 1149,020,00,00)
Drill Cores from the Deposit Area: See Borehole Area Feøy

Location
County : Rogaland (11) Municipality : Karmøy (1149)
Map 1:50000: Haugesund (1113-1) Map 1:250000: Haugesund
Marking point: Longitude: 5.1621680 Latitude: 59.3875360
EU89-UTM Zone 32
X-coord: 282068 m. Y-coord: 6589490 m.

Commodity
Main Type: Ferroalloys (Cr,Ni,Co,V,Mo,W) Sub Type: Nickel
Element(s): Ni Cu PGE
Production
Activity: Mining Reserves:
Prod. method: Production: 37 thousand tons
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
CU 2,69 %
NI 2,1 %
PD 4,4 ppm
PT 1,6 ppm

Operations
From - To Activity Comments
1896 - 1922 Regular production

Mineralization
Era: Paleozoic Period:
Dating: Method:
Genesis: Form: Lens
Main texture: Massive Min. distribution:
Main grain size: Medium grained (1-3 mm) Main alteration: Chloritisation
Strike/Dip: Direction:
Plunge:
Stratigraphic classification of host rock
Era: Paleozoic Period:
Province: Caledonides
Geotec.unit:
Tectonic complex:
Igneous complex: Karmøy Ophiolite Complex
Group: Formation:

Mineralogy
Relationship Mineral Amount
Ore mineral Pyrrhotite Major mineral (>10%)
Ore mineral Chalcopyrite Subordinate mineral (1-10%)
Ore mineral Pyrite Subordinate mineral (1-10%)
Ore mineral Pentlandite Subordinate mineral (1-10%)

Lithology:
Relationship Rock Origin
Host rock Gabbro Intrusive
Original rock :Gabbro
Host rock Sheeted dykes Intrusive
Original rock :Gabbro

Information(s) in free text format
Free text
The Feøy deposit is a minor Ni-Cu deposit, which is located in the sheeted-dyke complex of the Karmøy ophiolite complex. The deposit was mined between 1896 and 1922, and 37 000 t of ore was produced with 2.6 % Cu and 2.1 % Ni. The ore was quite rich in PGE, containing 4.4 ppm Pd, 1.6 ppm Pt and 0.2 ppm Rh. The ore was medium-grained, dominated by pyrrhotite, while chalcopyrite, pyrite and pentlandite were subordinate.

Bibliography:
From NGU's Reference Archive:
Boyd, R.; Nixon, F. , 1985
Norwegian nickel deposits: a review.
;Geologian Tutkimuskeskus / Geological Survey of Finland;ARTIKKEL;Bulletin; Nickel-copper deposits of the Baltic Shield and Scandinavian; Caledonides.; No.333;363-394 pages


The fact sheet was created on 18.05.2024

Questions or comments regarding the fact sheet can be emailed to:
ressursdatabaser@ngu.no
Copyright © 2024 Geological Survey of Norway