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Altenberg mine, Kelmis, Liège, Wallonia, Belgiumi
Regional Level Types
Altenberg mineOpen-Cast Mine (Backfilled)
KelmisMunicipality
LiègeProvince
WalloniaRegion
BelgiumCountry

This page kindly sponsored by François Wouters
PhotosMapsSearch
08236410014947039418787.jpg
View of the Altenberg zinc mining area, ca 1885.

Altenberg mine, Kelmis, Liège, Wallonia, Belgium
Latitude & Longitude (WGS84):
50° 42' 51'' North , 6° 0' 32'' East
Latitude & Longitude (decimal):
Type:
Open-Cast Mine (Backfilled) - last checked 2020
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
La Calamine10,232 (2011)0.4km
Lontzen4,862 (2011)3.7km
Plombières9,596 (2011)4.3km
Wolfhaag125 (2017)4.9km
Raren175 (2017)6.0km
Nearest Clubs:
Local clubs are the best way to get access to collecting localities
ClubLocationDistance
Vieille Montagne HeritageKelmis / La Calamine, Belgium0km
Mindat Locality ID:
304
Long-form identifier:
mindat:1:2:304:6
GUID (UUID V4):
1a833e58-80d5-4d44-924b-f235e9bf802f
Other/historical names associated with this locality:
Vieille Montagne Mine; Kelmisberg Mine; der Kull
Name(s) in local language(s):
der Kull


The Altenberg mine (Vieille Montagne) in Kelmis

In 1806, Jean-Jacques Daniel Dony was granted the concession for the Altenberg mine by Napoleon. In 1813, Dony sold the mine to François-Dominique Mosselman from Brussels. In 1837, the mine was incorporated into the newly created Société des Mines et Fonderies de Zinc de la Vieille Montagne with headquarters in Liège and Paris. By 1884 the mine was exhausted.

This ancient zinc mine was a metasomatic replacement deposit. The zinc ore occurs as the so-called “Galmei” or “Calamine” (an intergrowth of smithsonite, hemimorphite, and willemite). Only traces of sulfides occurred along the walls of the open pit.

01277380017072517266475.jpg
1855 Altenberg Zinc Mine Panorama

Altenberg mine, Kelmis, Liège, Wallonia, Belgium

Between 1837 and 1884 some 1,414,328 tonnes of calamine was produced, total production is uncertain due to the lack of production statistics before 1825.

The open cut mine Altenberg (Kelmisberg) mountain was located north of the road leading from Aachen to Liège. The mine was abandoned in 1884. Today the open cut is backfilled.

02295220015135535595282.jpg
1843 Altenberg Open Cut Zinc Mine.

Altenberg mine, Kelmis, Liège, Wallonia, Belgium

"Neutral-Moresnet", in Kelmis (La Calamine), was an independent state for a little over a century until, in 1920, there came an end to its independence, and it became a part of Belgium. An open cut zinc mine was located in Neutral-Moresnet that had been exploited for centuries for the production of “galmei”. The mine itself was named “Altenberg” in German and “Vieille-Montagne” in French.

09262890017056488701024.jpg
1875 Altenberg Zinc mine and associated zinc plant.

Altenberg mine, Kelmis, Liège, Wallonia, Belgium

"Galmei" or calamine is a mixture of zinc silicates and carbonates, smithsonite, hemimorphite, and willemite. It was used in the production of “brass”, which in turn is a mixture of copper and zinc.



The produced ores were roasted in local shaft furnaces, and then the zinc ore was converted into zinc metal by reduction with coal by muffle furnaces.

The old dumps and a settling pond are located opposite the open cut and south of the Aachen-Liège road. In this area, the former mineral processing plant was situated. Starting in 1900, the S.A. de la Vieille Montagne processed the tailings from the old Altenberg mine, ashes from the old zinc plant and hand-picked ores from other mines in this area (the Schmalgraf, Fossey, Welkenraedt, and Lontzen mines).

03489980015794611785645.jpg
1928 "Giftmühle" Zinc White plant Vieille Montagne

Altenberg mine, Kelmis, Liège, Wallonia, Belgium

Later, after these mines were abandoned (~1935), ores from Germany, Spain and from overseas were dressed. Consequently, minerals from different and even overseas localities may occur in the dumps.

The name "Altenberg" or “Moresnet” on old labels sometimes refers to the mining district, sometimes to the Altenberg mine. Both were used.

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


26 valid minerals. 3 (TL) - type locality of valid minerals.

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:

Allophane
Formula: (Al2O3)(SiO2)1.3-2 · 2.5-3H2O
Brianyoungite
Formula: Zn3(CO3,SO4)(OH)4
'Calamine'
Calcite
Formula: CaCO3
Cerussite
Formula: PbCO3
Dolomite
Formula: CaMg(CO3)2
Fraipontite (TL)
Formula: (Zn,Al)3((Si,Al)2O5)(OH)4
Type Locality:
Habit: thin layers of mica-like platelets filling veinlets in smithsonite
Colour: white
Galena
Formula: PbS
Goethite
Formula: α-Fe3+O(OH)
Goslarite
Formula: ZnSO4 · 7H2O
Greenockite
Formula: CdS
Gypsum
Formula: CaSO4 · 2H2O
Hematite
Formula: Fe2O3
Hemimorphite
Formula: Zn4Si2O7(OH)2 · H2O
Hopeite (TL)
Formula: ZnZn2(PO4)2 · 4H2O
Type Locality:
Description: "Reportedly found around 1820 (Des Cloizeaux, 1893) and never found again. The very few specimens from this locality are now in a number of museums." (Hatert et al., 2002)
References:
Hydrozincite
Formula: Zn5(CO3)2(OH)6
Kaolinite
Formula: Al2(Si2O5)(OH)4
Kolbeckite
Formula: ScPO4 · 2H2O
Habit: crystals of up to 1mm showing {110}, {011} and {154} (Schrauf, 1879)
Colour: very pale yellow
Description: on hemimorphite
'Limonite'
Marcasite
Formula: FeS2
'Moresnetite'
Pyrite
Formula: FeS2
Quartz
Formula: SiO2
Sauconite
Formula: Na0.3Zn3((Si,Al)4O10)(OH)2 · 4H2O
Siderite
Formula: FeCO3
Smithsonite
Formula: ZnCO3
Sphalerite
Formula: ZnS
Sulphur
Formula: S8
Willemite (TL)
Formula: Zn2SiO4
Type Locality:
Description: This is the type locality, not the Franklin, NJ, area. Named in 1830 by Serve-Dieu Abailard "Armand" Lévy in honor of Willem I (1772-1843), King (1813-1840) of the Netherlands, wherein the type locality was located at the time. It had been previously observed, but not described, from the Franklin District orebodies.

Gallery:

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
Sulphur1.CC.05S8
Group 2 - Sulphides and Sulfosalts
Sphalerite2.CB.05aZnS
Greenockite2.CB.45CdS
Galena2.CD.10PbS
Pyrite2.EB.05aFeS2
Marcasite2.EB.10aFeS2
Group 4 - Oxides and Hydroxides
Goethite4.00.α-Fe3+O(OH)
Hematite4.CB.05Fe2O3
Quartz4.DA.05SiO2
Group 5 - Nitrates and Carbonates
Smithsonite5.AB.05ZnCO3
Calcite5.AB.05CaCO3
Siderite5.AB.05FeCO3
Dolomite5.AB.10CaMg(CO3)2
Cerussite5.AB.15PbCO3
Hydrozincite5.BA.15Zn5(CO3)2(OH)6
Brianyoungite5.BF.30Zn3(CO3,SO4)(OH)4
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
Goslarite7.CB.40ZnSO4 · 7H2O
Gypsum7.CD.40CaSO4 · 2H2O
Group 8 - Phosphates, Arsenates and Vanadates
Hopeite (TL)8.CA.30ZnZn2(PO4)2 · 4H2O
Kolbeckite8.CD.05ScPO4 · 2H2O
Group 9 - Silicates
Willemite (TL)9.AA.05Zn2SiO4
Hemimorphite9.BD.10Zn4Si2O7(OH)2 · H2O
Sauconite9.EC.45Na0.3Zn3((Si,Al)4O10)(OH)2 · 4H2O
Kaolinite9.ED.05Al2(Si2O5)(OH)4
Fraipontite (TL)9.ED.15(Zn,Al)3((Si,Al)2O5)(OH)4
Allophane9.ED.20(Al2O3)(SiO2)1.3-2 · 2.5-3H2O
Unclassified
'Limonite'-
'Calamine'-
'Moresnetite'-

List of minerals for each chemical element

HHydrogen
H Allophane(Al2O3)(SiO2)1.3-2 · 2.5-3H2O
H BrianyoungiteZn3(CO3,SO4)(OH)4
H Fraipontite(Zn,Al)3((Si,Al)2O5)(OH)4
H Goethiteα-Fe3+O(OH)
H GoslariteZnSO4 · 7H2O
H GypsumCaSO4 · 2H2O
H HemimorphiteZn4Si2O7(OH)2 · H2O
H HydrozinciteZn5(CO3)2(OH)6
H HopeiteZnZn2(PO4)2 · 4H2O
H KaoliniteAl2(Si2O5)(OH)4
H KolbeckiteScPO4 · 2H2O
H SauconiteNa0.3Zn3((Si,Al)4O10)(OH)2 · 4H2O
CCarbon
C BrianyoungiteZn3(CO3,SO4)(OH)4
C CalciteCaCO3
C CerussitePbCO3
C DolomiteCaMg(CO3)2
C HydrozinciteZn5(CO3)2(OH)6
C SideriteFeCO3
C SmithsoniteZnCO3
OOxygen
O Allophane(Al2O3)(SiO2)1.3-2 · 2.5-3H2O
O BrianyoungiteZn3(CO3,SO4)(OH)4
O CalciteCaCO3
O CerussitePbCO3
O DolomiteCaMg(CO3)2
O Fraipontite(Zn,Al)3((Si,Al)2O5)(OH)4
O Goethiteα-Fe3+O(OH)
O GoslariteZnSO4 · 7H2O
O GypsumCaSO4 · 2H2O
O HematiteFe2O3
O HemimorphiteZn4Si2O7(OH)2 · H2O
O HydrozinciteZn5(CO3)2(OH)6
O HopeiteZnZn2(PO4)2 · 4H2O
O KaoliniteAl2(Si2O5)(OH)4
O KolbeckiteScPO4 · 2H2O
O QuartzSiO2
O SauconiteNa0.3Zn3((Si,Al)4O10)(OH)2 · 4H2O
O SideriteFeCO3
O SmithsoniteZnCO3
O WillemiteZn2SiO4
NaSodium
Na SauconiteNa0.3Zn3((Si,Al)4O10)(OH)2 · 4H2O
MgMagnesium
Mg DolomiteCaMg(CO3)2
AlAluminium
Al Allophane(Al2O3)(SiO2)1.3-2 · 2.5-3H2O
Al Fraipontite(Zn,Al)3((Si,Al)2O5)(OH)4
Al KaoliniteAl2(Si2O5)(OH)4
Al SauconiteNa0.3Zn3((Si,Al)4O10)(OH)2 · 4H2O
SiSilicon
Si Allophane(Al2O3)(SiO2)1.3-2 · 2.5-3H2O
Si Fraipontite(Zn,Al)3((Si,Al)2O5)(OH)4
Si HemimorphiteZn4Si2O7(OH)2 · H2O
Si KaoliniteAl2(Si2O5)(OH)4
Si QuartzSiO2
Si SauconiteNa0.3Zn3((Si,Al)4O10)(OH)2 · 4H2O
Si WillemiteZn2SiO4
PPhosphorus
P HopeiteZnZn2(PO4)2 · 4H2O
P KolbeckiteScPO4 · 2H2O
SSulfur
S BrianyoungiteZn3(CO3,SO4)(OH)4
S GalenaPbS
S GoslariteZnSO4 · 7H2O
S GreenockiteCdS
S GypsumCaSO4 · 2H2O
S MarcasiteFeS2
S PyriteFeS2
S SphaleriteZnS
S SulphurS8
CaCalcium
Ca CalciteCaCO3
Ca DolomiteCaMg(CO3)2
Ca GypsumCaSO4 · 2H2O
ScScandium
Sc KolbeckiteScPO4 · 2H2O
FeIron
Fe Goethiteα-Fe3+O(OH)
Fe HematiteFe2O3
Fe MarcasiteFeS2
Fe PyriteFeS2
Fe SideriteFeCO3
ZnZinc
Zn BrianyoungiteZn3(CO3,SO4)(OH)4
Zn Fraipontite(Zn,Al)3((Si,Al)2O5)(OH)4
Zn GoslariteZnSO4 · 7H2O
Zn HemimorphiteZn4Si2O7(OH)2 · H2O
Zn HydrozinciteZn5(CO3)2(OH)6
Zn HopeiteZnZn2(PO4)2 · 4H2O
Zn SauconiteNa0.3Zn3((Si,Al)4O10)(OH)2 · 4H2O
Zn SmithsoniteZnCO3
Zn SphaleriteZnS
Zn WillemiteZn2SiO4
CdCadmium
Cd GreenockiteCdS
PbLead
Pb CerussitePbCO3
Pb GalenaPbS

Other Databases

Wikipedia:https://en.wikipedia.org/wiki/Vieille_Montagne
Wikidata ID:Q947317

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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