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Flåt Nickel Mines, Flåt, Evje og Hornnes, Agder, Norwayi
Regional Level Types
Flåt Nickel MinesGroup of Mines
FlåtFarm
Evje og HornnesMunicipality
AgderCounty
NorwayCountry

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PhotosMapsSearch
Latitude & Longitude (WGS84):
58° 35' 56'' North , 7° 52' 12'' East
Latitude & Longitude (decimal):
Type:
Group of Mines
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Byglandsfjord332 (2014)8.2km
Birkeland2,254 (2010)36.5km
Vennesla10,931 (2014)37.2km
Tveit1,397 (2010)43.2km
Justvik1,630 (2014)45.7km
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
ClubLocationDistance
Sørlandets GeologiforeningKristiansand50km
Mindat Locality ID:
32927
Long-form identifier:
mindat:1:2:32927:2
GUID (UUID V4):
0f82c0c6-36af-4447-ac81-6b6d9f828588
Other Languages:
Norwegian:
Flåt nikkelgruver, Flåt, Evje og Hornnes, Agder, Norge


INCREASING DEMAND FOR NICKEL

When the demand for nickel increased in the second half of the 19th century, several copper deposits hosted in amphibolite were tested for the presence of nickel.

In 1857 nickel was found in the copper ore of a small copper mine, locally called the Kobberhola, situated at the Myklåsen, not far from a tiny hamlet by the name of Evje. After three years of prospecting, starting in 1869, mining commenced in 1872. During three periods of mining, 2,8 million tonnes of ore were mined.

THE LARGEST IN EUROPE

During a short period the Flåt nickel mine was the largest in its kind in the world, and somewhat longer the largest in Europe. From this ore 20.000 tonnes of nickel and 14.500 tonnes of copper were extracted. In addition some cobalt, gold, silver, platinum and palladium were extracted. During the Second World War the German occupants exhausted the mine, and the mine was closed for good in 1946.

The mine reached a depth of 422 m, actually 20 m below the sea level. An extension of the ore body is present at greater depth, but it is not known if this deposit is economic.

THE EVJE NIKKELVERK SMELTER

The smelter near the Fennefossen waterfall near the centre of Evje produced an intermediate product, comprising a mix of nickel and copper. This was called "nikkelmatte". The "nikkelmatte" was sent to Kristiansand for further processing in a factory called Falconbridge, a Canadian company involved in the mining and processing of ore in the Sudbury area.

This factory still exists under the name Glencore Nikkel AS, and is a major producer of nickel in the world. However, all the ore is mined and processed elsewhere and the facty processes only the intermediate product, the "nikkelmatte", also called matte.

Here is a nice presentation of the refining processes: http://www.nikkelverk.no/no/OmOss/produksjon/Pages/flytskjema.aspx
Nickel, copper and cobalt are the main products, but additionally gold and platina group metals are produced.

THE FERTILIZER PLANT

During WW2 the Germans constructed a fertilizer plant to extract an apatite concentrate from the flotation tailings. With a newly developed flotation proces the apatite could be separated. These efforts were hampered by the availability and quality of the necessary chemicals. (Monen 2016, book 2, s. 99)

However, during two years, 200.000 tons of slam were processed, yielding 6000 tons of apatite concentrate with a 27,5% phospahte content. This concentrate was subsequently sent to the Lysaker Kjemiske Fabrikk for further processing.

This project was an economic failure and the plant was subsequently closed when the war ended.

THE START OF THE GOLDEN DAYS OF PEGMATITE MINING

The nickel mine is directly responable for the extensive mining of quartz, feldspar and other minerals in this municipality and neighbouring municipality Iveland. At first sand was used in the smelting processes, but in 1844 it was decided to use "krystallkvarts", in plain language quartz.

It was already known that in the area around the mine several pegmatites outcropped. Access to plentiful of quartz was thereby secured. The mining of feldspar was to begin with not economic, due to the high cost of transportation to the nearest harbour, Kristiansand. When in 1896 a railroad connection with Kristiansand was opened, the mining of feldspar became economic.

Around 150 feldspar/quartz quarries and mines have been in operation in the Evje og Hornnes municipality in the period from 1844 and now. Today only two quarries are in operation, mining small amounts of ultra pure feldspar for dental applications.

Thanks to the Flåt nickel mine and all the pegmatite quarries, Evje could grow out to become a regional center and a popular place for tourists.

During the period 2004-2012 the upper parts of the old mine were accessible for tourists, but due to high expenses the proprietor had to shut down the mine.

The mine is located near Evje Mineral Trail, and the road is signposted.

The coordinates are for the entrance of the old Flåt nickel mine. The new mine was 245 m SSW of this one.

For collectors who can read norwegian, there is a set of 3 books available about the history of this mine, written by local historian Sigmund Monen: Gruvedrift og Nikkelindustri i Setesdal - Arbeidsfolk fortell m.m.

All in all around 1500 pages and plenty of pictures! It can be obtained by contacting the Evje og Hornnes municipality at: post@e-h.kommune.no


Coordinates © Kartverket - https://www.kartverket.no

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Commodity List

This is a list of exploitable or exploited mineral commodities recorded at this locality.


Mineral List


20 valid minerals. 1 erroneous literature entry.

Rock Types Recorded

Note: data is currently VERY limited. Please bear with us while we work towards adding this information!

Select Rock List Type

Alphabetical List Tree Diagram

Detailed Mineral List:

'Amphibole Supergroup'
Formula: AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
'Apatite'
Formula: Ca5(PO4)3(Cl/F/OH)
Boothite
Formula: CuSO4 · 7H2O
Description: Boothite occured on the walls and in loose rocks inside on of the mining buildings, where a roof took in water. It was first identified at the Natural History Museum, Oslo, film 22215. Reinvestigation of the results showed that the film corresponded more with melanterite than boothite. (pers. Com Gunnar Raade 18.04.1988 (Interne Notater s 137)
Calcite
Formula: CaCO3
'Chabazite'
Chalcopyrite
Formula: CuFeS2
Cobaltite
Formula: CoAsS
Fluorapophyllite-(K)
Formula: KCa4(Si8O20)(F,OH) · 8H2O
'Garnierite'
Gold
Formula: Au
Gold var. Electrum ?
Formula: (Au,Ag)
Description: Six grains (to 0,1 mm) found by Schönwandt, and containing 16% Ag, and it s probably electrum (Neumann 1985).
Hematite
Formula: Fe2O3
Heulandite-Ca
Formula: (Ca,Na)5(Si27Al9)O72 · 26H2O
Ilmenite
Formula: Fe2+TiO3
Laumontite
Formula: CaAl2Si4O12 · 4H2O
Linnaeite ?
Formula: Co2+Co3+2S4
Description: The mineral is not investigated good enough to be shure it's linnaeite, but it belong to the linnaeite group.
Magnetite
Formula: Fe2+Fe3+2O4
Melanterite
Formula: Fe2+(H2O)6SO4 · H2O
Description: First descruibed as boothite, but reinvestigation of the results showed it to be melanterite
Millerite
Formula: NiS
Habit: Short prismatic
Description: Occure in zones close to younger pegmatites that have metamorphed the ore.
Pentlandite
Formula: (NixFey)Σ9S8
'Plagioclase'
Formula: (Na,Ca)[(Si,Al)AlSi2]O8
Pyrite
Formula: FeS2
Habit: (111), sometime corners cut of by (100).
Pyrrhotite
Formula: Fe1-xS
Quartz
Formula: SiO2
Sphalerite
Formula: ZnS
'Stilbite Subgroup'
Formula: M6-7[Al8-9Si27-28O72] · nH2O
Violarite
Formula: Fe2+Ni3+2S4
Vivianite
Formula: Fe2+Fe2+2(PO4)2 · 8H2O

Gallery:

(NixFey)Σ9S8 Pentlandite

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
Gold1.AA.05Au
var. Electrum ?1.AA.05(Au,Ag)
Group 2 - Sulphides and Sulfosalts
Pentlandite2.BB.15(NixFey)Σ9S8
Sphalerite2.CB.05aZnS
Chalcopyrite2.CB.10aCuFeS2
Pyrrhotite2.CC.10Fe1-xS
Millerite2.CC.20NiS
Linnaeite ?2.DA.05Co2+Co3+2S4
Violarite2.DA.05Fe2+Ni3+2S4
Pyrite2.EB.05aFeS2
Cobaltite2.EB.25CoAsS
Group 4 - Oxides and Hydroxides
Magnetite4.BB.05Fe2+Fe3+2O4
Hematite4.CB.05Fe2O3
Ilmenite4.CB.05Fe2+TiO3
Quartz4.DA.05SiO2
Group 5 - Nitrates and Carbonates
Calcite5.AB.05CaCO3
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
Melanterite7.CB.35Fe2+(H2O)6SO4 · H2O
Boothite ?7.CB.35CuSO4 · 7H2O
Group 8 - Phosphates, Arsenates and Vanadates
Vivianite8.CE.40Fe2+Fe2+2(PO4)2 · 8H2O
Group 9 - Silicates
Fluorapophyllite-(K)9.EA.15KCa4(Si8O20)(F,OH) · 8H2O
Laumontite9.GB.10CaAl2Si4O12 · 4H2O
Heulandite-Ca9.GE.05(Ca,Na)5(Si27Al9)O72 · 26H2O
Unclassified
'Plagioclase'-(Na,Ca)[(Si,Al)AlSi2]O8
'Garnierite'-
'Amphibole Supergroup'-AB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
'Stilbite Subgroup'-M6-7[Al8-9Si27-28O72] · nH2O
'Chabazite'-
'Apatite'-Ca5(PO4)3(Cl/F/OH)

List of minerals for each chemical element

HHydrogen
H Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
H BoothiteCuSO4 · 7H2O
H Fluorapophyllite-(K)KCa4(Si8O20)(F,OH) · 8H2O
H LaumontiteCaAl2Si4O12 · 4H2O
H MelanteriteFe2+(H2O)6SO4 · H2O
H Stilbite SubgroupM6-7[Al8-9Si27-28O72] · nH2O
H VivianiteFe2+Fe22+(PO4)2 · 8H2O
H Heulandite-Ca(Ca,Na)5(Si27Al9)O72 · 26H2O
H ApatiteCa5(PO4)3(Cl/F/OH)
CCarbon
C CalciteCaCO3
OOxygen
O Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
O BoothiteCuSO4 · 7H2O
O CalciteCaCO3
O Fluorapophyllite-(K)KCa4(Si8O20)(F,OH) · 8H2O
O HematiteFe2O3
O IlmeniteFe2+TiO3
O LaumontiteCaAl2Si4O12 · 4H2O
O MagnetiteFe2+Fe23+O4
O MelanteriteFe2+(H2O)6SO4 · H2O
O QuartzSiO2
O Stilbite SubgroupM6-7[Al8-9Si27-28O72] · nH2O
O VivianiteFe2+Fe22+(PO4)2 · 8H2O
O Heulandite-Ca(Ca,Na)5(Si27Al9)O72 · 26H2O
O Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
O ApatiteCa5(PO4)3(Cl/F/OH)
FFluorine
F Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
F Fluorapophyllite-(K)KCa4(Si8O20)(F,OH) · 8H2O
F ApatiteCa5(PO4)3(Cl/F/OH)
NaSodium
Na Heulandite-Ca(Ca,Na)5(Si27Al9)O72 · 26H2O
Na Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
AlAluminium
Al Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Al LaumontiteCaAl2Si4O12 · 4H2O
Al Stilbite SubgroupM6-7[Al8-9Si27-28O72] · nH2O
Al Heulandite-Ca(Ca,Na)5(Si27Al9)O72 · 26H2O
Al Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
SiSilicon
Si Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Si Fluorapophyllite-(K)KCa4(Si8O20)(F,OH) · 8H2O
Si LaumontiteCaAl2Si4O12 · 4H2O
Si QuartzSiO2
Si Stilbite SubgroupM6-7[Al8-9Si27-28O72] · nH2O
Si Heulandite-Ca(Ca,Na)5(Si27Al9)O72 · 26H2O
Si Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
PPhosphorus
P VivianiteFe2+Fe22+(PO4)2 · 8H2O
P ApatiteCa5(PO4)3(Cl/F/OH)
SSulfur
S BoothiteCuSO4 · 7H2O
S ChalcopyriteCuFeS2
S CobaltiteCoAsS
S LinnaeiteCo2+Co23+S4
S MelanteriteFe2+(H2O)6SO4 · H2O
S MilleriteNiS
S Pentlandite(NixFey)Σ9S8
S PyriteFeS2
S PyrrhotiteFe1-xS
S SphaleriteZnS
S ViolariteFe2+Ni23+S4
ClChlorine
Cl Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Cl ApatiteCa5(PO4)3(Cl/F/OH)
KPotassium
K Fluorapophyllite-(K)KCa4(Si8O20)(F,OH) · 8H2O
CaCalcium
Ca CalciteCaCO3
Ca Fluorapophyllite-(K)KCa4(Si8O20)(F,OH) · 8H2O
Ca LaumontiteCaAl2Si4O12 · 4H2O
Ca Heulandite-Ca(Ca,Na)5(Si27Al9)O72 · 26H2O
Ca Plagioclase(Na,Ca)[(Si,Al)AlSi2]O8
Ca ApatiteCa5(PO4)3(Cl/F/OH)
TiTitanium
Ti Amphibole SupergroupAB2C5((Si,Al,Ti)8O22)(OH,F,Cl,O)2
Ti IlmeniteFe2+TiO3
FeIron
Fe ChalcopyriteCuFeS2
Fe HematiteFe2O3
Fe IlmeniteFe2+TiO3
Fe MagnetiteFe2+Fe23+O4
Fe MelanteriteFe2+(H2O)6SO4 · H2O
Fe Pentlandite(NixFey)Σ9S8
Fe PyriteFeS2
Fe PyrrhotiteFe1-xS
Fe ViolariteFe2+Ni23+S4
Fe VivianiteFe2+Fe22+(PO4)2 · 8H2O
CoCobalt
Co CobaltiteCoAsS
Co LinnaeiteCo2+Co23+S4
NiNickel
Ni MilleriteNiS
Ni Pentlandite(NixFey)Σ9S8
Ni ViolariteFe2+Ni23+S4
CuCopper
Cu BoothiteCuSO4 · 7H2O
Cu ChalcopyriteCuFeS2
ZnZinc
Zn SphaleriteZnS
AsArsenic
As CobaltiteCoAsS
AgSilver
Ag Gold var. Electrum(Au,Ag)
AuGold
Au Gold var. Electrum(Au,Ag)
Au GoldAu

Other Regions, Features and Areas containing this locality


This page contains all mineral locality references listed on mindat.org. This does not claim to be a complete list. If you know of more minerals from this site, please register so you can add to our database. This locality information is for reference purposes only. You should never attempt to visit any sites listed in mindat.org without first ensuring that you have the permission of the land and/or mineral rights holders for access and that you are aware of all safety precautions necessary.

References

 
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