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THE ORE DATABASE
Occurence 5603 - 025 Porsa grube
(Object Id: 788)
(Last updated: 11.10.2017)

Location
County: Finnmark Municipality: Hammerfest (5603)
Map 1:50000: Vargsund (1935-4) Map 1:250000: Hammerfest
Coordinate system: EU89-UTM Zone 34
East: 601644 m. North: 7810501 m.
Longitude: 23.7130720 Latitude: 70.3798490
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Resource
Resource Type: Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) Resource Subtype: Copper
Element(s): Cu Fe
Importance
Raw material meaning: Little Importance (reg. 18.02.2015)

Resources and production
Activity: Mining Reserves: 66 thousand tons
Operating method: Underground mining Historical production: 60 thousand tons


Products
Element/product Crude ore grade or quality Reg. date
Cu 2 % 05.12.1996

Operations
From - To Activity Comments
1905 - 1918 Regular production

Mineralization
Era: Proterozoic Period: Paleoproterozoic
Genesis: Hydrothermal vein Form: Plate
Main texture: Porphyroblastic Min. distribution: Irregular (scattered)
Main grain size: Very unevenly grained Main alteration: No country rock alteration
Strike/Dip: 280 / 85 Direction:
Plunge:
Stratigraphic classification of host rock
Era: Proterozoic Period: Paleoproterozoic
Province: Caledonian Basement Province
Geotec.unit: Komagfjord-Repparfjord Greenstone Belt
Tectonic complex:
Igneous complex:
Group: Nussir Formation: Svartfjell

Mineralogy
Relationship Mineral Amount
Gangue mineral Quartz Major mineral (>10%)
Gangue mineral Calcite Major mineral (>10%)
Gangue mineral Plagioclase Subordinate mineral (1-10%)
Gangue mineral Chlorite Subordinate mineral (1-10%)
Gangue mineral Hornblende Subordinate mineral (1-10%)
Ore mineral Chalcopyrite Major mineral (>10%)
Ore mineral Pyrite Major mineral (>10%)
Ore mineral Hematite Subordinate mineral (1-10%)
Ore mineral Magnetite Subordinate mineral (1-10%)
Ore mineral Sphalerite Accessory mineral (<1%)

Lithology:
Relationship Rock Origin
Unknown Grønnstein Extrusive
Original rock :Basalt
Metamorphic facies :Greenschist

Structures
Location: Type: Orientation(360 gr.): Relation to min.:
Unknown Joints/Fractures Strike/Dip :280 / 85 Syn-mineralisation ;...Effect :Controls

Information(s) in free text format
Free text
The Porsa mine is located at Gruvevatn (Øvre Porsavatn), 4 km south-southeast of Porsa village in Kvalsund municipality. The mine is accessible by road with a gate. Key to the gate can be obtained from the neighbouring houses. The mine is situated close to the dam for the electrical power supply. The mining in the area started in 1900 by opening of the Bachke mine, nearly 3 km north of the Porsa mine. The company A/S Vesterdalen Kobbergruver (Copper Mines) commenced the investigations in Porsa in 1905. Porsa Copper Mines Ltd, under the leadership of Loius Greville and based on English investments, had then already conducted minor investigations in the area. The mining rights between the companies were not settled. A/S Vesterdalen was bankrupt by the end of 1905, and its properties was overtaken by the Swedish company Skandia. They conducted very limited investigations in the period 1906-07, and sold the rights to the English company Porsa Copper Mines Ltd. Test mining was carried out in Porsa in 1905 and the beginning of 1906. Ca. 600-700 tonnes of ore were sold to the Alten Kobberverk in Kåfjord and partly shipped to a smelter in Swansea in England. Porsa Copper Mines Ltd commenced further work in 1908 and the ore production was 3-4000 tonnes annually in the period 1909-1911. The reason for the closing of the mine in 1911 is not known. In 1918 the mine was reopened by A/S Porsa Kobbergruver, that carried out active mining until 1931. The mine was closed in due to lower copper prices. The mining has been carried out along two parallel, nearly east-west orientated carbonate+quartz veins in metabasalt. These veins are located about 150 m apart, and were named Greville in the south and Parallel (also Chr. Michelsen) in the north. The shafts are 76 m and 64 m, respectively. From an adit on the level ¿64 in the Parallel a shaft has been made down to 96 m below surface. Further mining has been carried out along adits and stopes on several levels. The entrances are today closed by concrete and steel covers and are not accessible. The ore-bearing veins are about 100 metres long. The thickness of the veins varies between 3 and 10 m and seems to decline along depth in the vertical veins. Steep dips, around 85° towards north are also found The deposit is located in Paleoproterozoic greenstones of the Svartfjell Formation in the Nussir Group, about 2 km northeast of the Caledonian Nappes. Well-preserved pillow lava structures occur in the greenstones in the area between the veins. The ore minerals consist of chalcopyrite and pyrite comprising aggregates and thin lenses and bands. Magnetite and hematite are also commonly found in the calcite dominated veins. Lensoide inclusions of the wall-rock commonly occur.

Bibliography:
From NGU's Reference Archive:
Bergen, A. M. , 1918
Porsa grube, daganlegg ved hovedgruvene 1:500.
;Norges geologiske undersøkelse;KART;Bergarkivet; No.K 989

Damm, C.O.B. , 1918
A/S Porsa kobbergruber.
;Norges geologiske undersøkelse;FAGRAPPORT;Bergarkivet; No.BA 3824;8 pages
Abstract:
Rapporten beskriver 2 dagers befaring av gruvene Greville og Chr. Mickelsen etter at de er lenset for vann. Beskrivelse av bergarter og mineraler i alle gruveganger samt i malmgangene i dagen gis. Eventuell gjenopptagelse av driften er ikke diskutert.

Geis, H.P. , 1967
Porsa Grube Kvalsund, Finnmark.
;Norges geologiske undersøkelse;FAGRAPPORT;Bergarkivet; No.BA 6618;1 pages
Abstract:
Rapporten konkluderer med at man anser A/S Porsa konsesjonsområde ikke drivverdig, - og Elkem - Spigerverket lar konsesjonen tilfalle Staten. Kartbilagene viser geologisk kartlegging med prøvetakingsprofiler i det mineraliserte feltet. Forekomstnr. forts.: 50076-84 og 50397. Forekomstens koordinater forts.: 35 6131 78251.

Krause, Michael , 1980
Some uranium mineralizations in the Raipas Suite of the Komagfjord tectonic window, Finnmark, Norway.
;Norges geologiske undersøkelse;TIDSSKRIFTARTIKKEL;NGU; No.355;49-52 pages
Abstract:
Uranium mineralizations have been discovered in the northwest part of the Komagfjord tectonic window. The mineralizations are found in two mines of the old Porsa-Neverfjord copper mining district. Pitchblende and brannerite occur as primary minerals. Black slates are considered to be the source rocks of the uranium-bearing fluids.

Reitan, P. H. , 1958
Forslag til videre undersøkelser i Porsa-området.
;Norges geologiske undersøkelse;FAGRAPPORT;Bergarkivet; No.BA 3941;3 pages
Abstract:
I rapporten foreslås geologisk kartlegging både i og utenfor de gamle gruvene i Porsa-området, med spesiell vekt på strukturer og sprekkesystemer. Dette anses nødvendig hvis det skal være mulig å finne mer malm i området. Rapporten skisserer bemannings- og utstyrsbehov for undersøkelsen.

Sandstad, Jan Sverre , 1981
Porsa malmfelt.
;Norges geologiske undersøkelse;FAGRAPPORT;NGU-rapport; No.1800/62A;20 pages
Abstract:
Rapporten er et sammendrag fra Michael Krauses rapporter og doktorgrad fra Mainz 1981: "Eine Schwermetallprospektion im alten Porsa Neverfjord-Grubenzirk von Nord-Norwegen". Krause har nylig påvist svake uran-mineraliseringer i forbindelse med kjente gangforekomster av kobbersulfider i Porsafeltet. Med bakgrunn i disse undersøkelsene har han benyttet geokjemiske prospekteringsmetoder i bekkesedimenter og bekkevann for om mulig å påvise nye mineraliseringer. Geologisk hører feltet inn under Komagfjord grunnfjellsvindu med lavmetamorfe suprakrustalbergarter. Geokjemiske anomalier skyldes hovedsakelig høy organisk andel i bekkesedimentene, utvasking fra gamle gruver og bergarter som dolomitt og skifer. Geofysiske helikoptermålinger utført av NGU ga ikke nye indikasjoner på malmmineraliseringer. De kjente reserver etter tidligere gruvedrift og påviste nye mineraliseringer av uran er for små til å være av økonomisk interesse i dag.

Fieldsamples
Sample No. Sample type Miscellanrous
FI0134.83-2 Dump
Sampler: Pratt & Nielsen
Comment: Kobbermineralisering i kvarts-karbonatgang
No. of registrated element analyses = 1
FI0134.83-3 Dump
Sampler: Pratt & Nielsen
Comment: Kobbermineralisering i kvarts-karbonatgang
No. of registrated element analyses = 1
FI0134.83-4 Dump
Sampler: Pratt & Nielsen
Comment: Kobbermineralisering i kvarts-karbonatgang
No. of registrated element analyses = 1
FI0134.83-5 Dump
Sampler: Pratt & Nielsen
Comment: Kobbermineralisering i kvarts-karbonatgang
No. of registrated element analyses = 1
FI0134.83-6 Dump
Sampler: Pratt & Nielsen
Comment: Kobbermineralisering i kvarts-karbonatgang
No. of registrated element analyses = 1
FI0134.83-7 Dump
Sampler: Pratt & Nielsen
Comment: Kobbermineralisering i kvarts-karbonatgang
No. of registrated element analyses = 1
FI0134.83-8 Dump
Sampler: Pratt & Nielsen
Comment: Kobbermineralisering i kvarts-karbonatgang
No. of registrated element analyses = 1
FI0134.83-9 Dump
Sampler: Pratt & Nielsen
Comment: Kobbermineralisering i kvarts-karbonatgang
No. of registrated element analyses = 1
HA-P-022 Bedrock
Sampler: KARLSTRØM/...Size(kg): 200
Comment: Store klyser av kobberkis omgitt av hematittutfellinger i kalkspatgang. Østlige tipp.
No. of registrated element analyses = 1
HA-P-023 Bedrock
Sampler: KARLSTRØM/...Size(kg): 200
Comment: Aggregater av cp. sammen med grønnsteinsfragmenter i kalkspatgang. Østlige tipp.
No. of registrated element analyses = 1
HA-P-024 Bedrock
Sampler: KARLSTRØM/...Size(kg): 200
Comment: Cp.-klyser i gang av perfekte kalkspatkrystaller og aktinolittnåler. Østlige tipp.
No. of registrated element analyses = 1
HA-P-025 Bedrock
Sampler: KARLSTRØM/...Size(kg): 200
Comment: Utfelling av hematitt med py.-korn og små cp.-klyser i kalkspatgang. En del serpentiniserte grønnsteinsfragmenter. Hovedtippen.
No. of registrated element analyses = 1
HA-P-026 Bedrock
Sampler: KARLSTRØM/...Size(kg): 200
Comment: Cp.-klyser i gangmasse av kalkspat (til dels rød) med omvandlete bergartsfragmenter og små mt.-krystaller. Hovedtipp.
No. of registrated element analyses = 1
83-1 Dump
Sampler: Pratt & Nielsen
Comment: Kobbermineralisering i kvarts-karbonatgang
No. of registrated element analyses = 1
NB! All analyse values are shown at the end of the printout.:

Name of Locality: Greville grube
(Object Id: 939 25,01,00)

Location
County: Finnmark Municipality: Hammerfest (5603)
Map 1:50000: Vargsund (1935-4) Map 1:250000: Hammerfest
Coordinate system: EU89-UTM Zone 34
East: 601694 m. North: 7810376 m.
Longitude: 23.7142570 Latitude: 70.3787090
Show on map

Resource
Resource Type: Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) Resource Subtype: Copper
Element(s): Cu
Resources and production
Activity: Pitting Reserves:
Operating method: Historical production:


Fieldsamples
Sample No. Sample type Miscellanrous
HA-P-027 Bedrock
Sampler: KARLSTRØM/...Size(kg): 200
Comment: Kraftige utfellinger av hematitt og svovelkis sammen med omv. grønnsteinsfragmenter i kalkspatgang. En del mindre cp.aggregater. Greville grube.
No. of registrated element analyses = 1
HA-P-028 Bedrock
Sampler: KARLSTRØM/...Size(kg): 200
Comment: Cp.-aggregater i kalkspatgang.
No. of registrated element analyses = 1
NB! All analyse values are shown at the end of the printout.:

Name of Locality: Skjerp 2
(Object Id: 940 25,02,00)

Location
County: Finnmark Municipality: Hammerfest (5603)
Map 1:50000: Vargsund (1935-4) Map 1:250000: Hammerfest
Coordinate system: EU89-UTM Zone 34
East: 601594 m. North: 7810241 m.
Longitude: 23.7114310 Latitude: 70.3775400
Show on map

Resource
Resource Type: Base metals (Cu,Zn,Pb,Fe sulphides, As,Sb,Bi,Sn) Resource Subtype: Copper
Element(s): Cu
Resources and production
Activity: Pitting Reserves:
Operating method: Historical production:


Fieldsamples
Sample No. Sample type Miscellanrous
HA-P-029 Dump
Sampler: Karlstrøm, H.
No. of registrated element analyses = 1
HA-P-030 Dump
Sampler: Karlstrøm, H.
No. of registrated element analyses = 1
NB! All analyse values are shown at the end of the printout.:


Analyse Results
from
Deposit Area 5603 - 025 Porsa grube

Element analyses

( *=parts pr. million, #=parts pr.billion, Negative values means below detection limit value.)
Sample No. Sample Type Cu* Zn* Pb* Co* Ni* Ag* Au#
FI0134.83-2 Dump 11756 1 2 117 125 .4 15.0
FI0134.83-3 Dump 1559 6 2 11 17 .1 5.0
FI0134.83-4 Dump 711 18 2 23 27 .3 16.0
FI0134.83-5 Dump 2957 3 2 50 33 .4 21.0
FI0134.83-6 Dump 14848 5 2 5 18 .8 26.0
FI0134.83-7 Dump 16195 21 2 398 50 .8 88.0
FI0134.83-8 Dump 3828 3 2 5 8 .4 8.0
FI0134.83-9 Dump 6086 1 4 283 83 .5 33.0
HA-P-022 Bedrock 23815 59 2 524 289 3.2 695.0
HA-P-023 Bedrock 50174 141 2 30 45 3.8 1449.0
HA-P-024 Bedrock 19059 45 2 11 8 .5 1120.0
HA-P-025 Bedrock 1698 8 2 568 134 .3 50.0
HA-P-026 Bedrock 30501 81 2 248 202 1.3 476.0
HA-P-027 Bedrock 5018 14 2 382 69 .2 97.0
HA-P-028 Bedrock 26454 66 4 192 175 .9 457.0
HA-P-029 Dump 99999 679 2 25 19 19.4 10.0
HA-P-030 Dump 34048 94 5 9 5 5.2 363.0
83-1 Dump 99999 1 9 95 113 2.4 526.0
------------------
Sample No. Pt# Pd# Rh# As* Cd* Ba* Mo* Sb* Bi*
FI0134.83-2 1.0 2.0 2.0 8 1.0 7 1.00 2 2
FI0134.83-3 14.0 15.0 2.0 2 1.0 11 1.00 3 3
FI0134.83-4 13.0 17.0 2.0 4 1.0 14 1.00 2 2
FI0134.83-5 1.0 2.0 2.0 6 1.0 5 1.00 2 2
FI0134.83-6 8.0 12.0 2.0 3 1.0 7 2.00 2 2
FI0134.83-7 1.0 3.0 2.0 18 5.0 2 1.00 2 2
FI0134.83-8 7.0 52.0 2.0 3 1.0 3 4.00 2 6
FI0134.83-9 1.0 9.0 2.0 10 3.0 5 1.00 2 2
HA-P-022 1.0 11.0 1.0 34 2.2 4 1.00 2 2
HA-P-023 1.0 19.0 1.0 2 5.1 5 1.00 2 18
HA-P-024 1.0 1.0 1.0 2 1.5 4 1.00 2 4
HA-P-025 1.0 17.0 1.0 10 .8 4 1.00 2 5
HA-P-026 1.0 83.0 1.0 42 2.5 11 1.00 2 18
HA-P-027 1.0 1.0 1.0 2 .8 3 2.00 2 7
HA-P-028 1.0 12.0 1.0 13 2.4 5 1.00 2 8
HA-P-029 1.0 1.0 1.0 4 17.9 3 1.00 2 2
HA-P-030 1.0 1.0 1.0 3 3.2 9 1.00 2 17
83-1 1.0 2.0 2.0 4 1.0 10 1.00 2 46
------------------
Sample No. S% V* Cr* Mn* Fe% Th* U* W* Sr*
FI0134.83-2 2.80 42 1 516 9.84 1.00 5.00 1 5.0
FI0134.83-3 .11 61 31 153 2.69 1.00 5.00 1 2.0
FI0134.83-4 .14 65 26 235 4.03 1.00 5.00 1 24.0
FI0134.83-5 .84 31 1 1244 4.86 2.00 6.00 1 29.0
FI0134.83-6 1.11 39 19 495 2.82 2.00 5.00 1 15.0
FI0134.83-7 5.63 25 1 1062 23.80 4.00 12.00 1 26.0
FI0134.83-8 .26 36 13 325 2.31 1.00 5.00 1 10.0
FI0134.83-9 5.23 87 1 570 33.49 4.00 7.00 2 12.0
HA-P-022 11.44 30 26 1826 19.72 1.00 5.00 1 28.0
HA-P-023 12.28 7 3 1933 10.50 1.00 5.00 1 44.0
HA-P-024 2.46 4 2 2416 2.78 1.00 5.00 1 57.0
HA-P-025 10.51 94 32 551 34.26 1.00 5.00 1 13.0
HA-P-026 7.83 54 20 523 14.20 1.00 5.00 1 14.0
HA-P-027 10.13 69 20 664 27.57 1.00 5.00 1 9.0
HA-P-028 9.16 12 10 2154 9.22 1.00 5.00 1 51.0
HA-P-029 39.69 2 1 195 27.93 1.00 5.00 1 1.0
HA-P-030 4.68 1 1 2419 3.98 1.00 5.00 1 79.0
83-1 26.10 8 1 213 21.06 2.00 5.00 1 2.0
------------------
Sample No. La* B* Na* Mg* Al* P* K * Ca* Ti*
FI0134.83-2 2.00 2 0 0 0 0 0 2 0
FI0134.83-3 4.00 2 0 0 0 0 0 1 0
FI0134.83-4 3.00 2 0 1 1 0 0 1 0
FI0134.83-5 2.00 2 0 0 0 0 0 14 0
FI0134.83-6 2.00 2 0 0 0 0 0 5 0
FI0134.83-7 2.00 2 0 0 0 0 0 11 0
FI0134.83-8 2.00 2 0 0 0 0 0 3 0
FI0134.83-9 2.00 4 0 0 0 0 0 4 0
HA-P-022 2.00 2 0 0 0 0 0 13 0
HA-P-023 2.00 3 0 0 0 0 0 18 0
HA-P-024 2.00 2 0 0 0 0 0 27 0
HA-P-025 2.00 2 0 0 0 0 0 4 0
HA-P-026 2.00 2 0 0 0 0 0 5 0
HA-P-027 2.00 2 0 0 0 0 0 3 0
HA-P-028 2.00 2 0 0 0 0 0 25 0
HA-P-029 2.00 2 0 0 0 0 0 0 0
HA-P-030 2.00 2 0 0 0 0 0 33 0
83-1 2.00 3 0 0 0 0 0 1 0


The fact sheet was created on 02.05.2024

Questions or comments regarding the fact sheet can be emailed to:
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