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Dr. Geier mine (Amalienhöhe mine; Elisenhöhe mine), Waldalgesheim, Rhein-Nahe, Mainz-Bingen, Rhineland-Palatinate, Germanyi
Regional Level Types
Dr. Geier mine (Amalienhöhe mine; Elisenhöhe mine)Mine (Abandoned)
WaldalgesheimMunicipality
Rhein-NaheCollective Municipality
Mainz-BingenDistrict
Rhineland-PalatinateState
GermanyCountry

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Latitude & Longitude (WGS84):
49° 57' 33'' North , 7° 50' 18'' East
Latitude & Longitude (decimal):
Type:
Mine (Abandoned) - last checked 2023
Köppen climate type:
Nearest Settlements:
PlacePopulationDistance
Waldalgesheim3,676 (2011)1.1km
Weiler2,712 (2015)1.9km
Waldlaubersheim804 (2011)2.9km
Rümmelsheim1,435 (2011)3.3km
Warmsroth426 (2016)4.1km
Mindat Locality ID:
35660
Long-form identifier:
mindat:1:2:35660:1
GUID (UUID V4):
4a574ef0-e4dd-4a6b-91b2-b29475319049
Other Languages:
German:
Grube Dr. Geier (Grube Amalienhöhe; Grube Elisenhöhe), Waldalgesheim, Rhein-Nahe, Landkreis Mainz-Bingen, Rheinland-Pfalz, Deutschland


Geology
The iron and manganese ores of the Dr. Geier mine are hosted by Middle Devonian dolostones within an isoclinal through at the southern border of the variscan Rheinisches Schiefergebirge. Genetically they are related to the paleo-karst of the carbonate rocks overlain by marine sands of Oligocene age. Their formation is bound to cavities, caverns, sinkholes and dolines which formed within massive dolomite zones and zones with strong tectonic impact like fractures, joint-sets and bedding planes of the through structure during an uplift-period in the Eocene and the Lower Oligocene.

Up to 50 % of the doline fillings are Tertiary sands and clays. The ores are of mixed iron-manganese type with a Fe: Mn ratio of approx. 2:1. They contain variable amounts of muscovite (10–50%), goethite (30–50%), amorphous Mn oxides (20–30%) and manganite and pyrolusite ("Hartmanganerz", 0–22%). Their formation can be explained by a mixture of descendant colloidal solutions of Fe and Mn hydroxides under oxidizing conditions of the karst hydrography. The Mn and Fe can be deducted from weathered neighboring devonian shales of the Schiefergebirge and the dolomites. The ore grades were 12 – 20 wt.% Mn and averaging 29 wt.% Fe.

History
The oldest reports on manganese mining in the area date from the 17th century. At least since 1808 the Concordia mine near Seibersbach - a few km west of Waldalgesheim - was in operation. In 1832 the Sahler brothers were granted a concession to mine, followed by the Elisenhöhe claim in 1839 and the Waldalgesheim claim in 1840. Contineous mining began in 1880 by the Wandesleben brothers in open cuts. From 1885 Dr. Heinrich Claudius Geier of Mainz started extensive exploration works and sank the first shaft. These activities led to 12 concessions (mining claims) on manganese and iron. In 1904 the Gewerkschaft Braunsteinwerke Dr. Geier was founded and in 1911 all mines and concessions of the Gebr. Wandesleben GmbH (Concordia and Elisenhöhe mines, Waldalgesheim claim) were incorporated. A 7.5 km cableway to the river Rhine was built in 1912 to facilitate the ore transport to the shipping station. 1917 marks the year of the highest Mn ore production (240,853 t). At the same time the construction of the new main shaft was started (Straubenschacht). The ore was used for ironworks and partly as a pigment ore for ceramics. In 1918 673 of 1000 shares of the Gewerkschaft Braunsteinwerke Dr. Geier were acquired by Mannesmannröhren-Werke AG, Düsseldorf, followed by the purchase of another 27 shares in 1926. In 1939 all mining operations were mandated to Mannesmannröhren-Werke AG.
From 1945 to 1950 operations were controlled by the French military government, then management was mandated back to Mannesmann AG. In 1952 the Gewerkschaft Braunsteinwerke Dr. Geier was incorporated into the Gewerkschaft Mannesmann, Düsseldorf. The remaining mines Amalienhöhe, Elisenhöhe and Heerberg were modernized and extended. In the mid of the 1950s the exhaustion of the ore reserves became evident and in 1954 mining of the huge dolomite reserves started. Since 1964 a part of the dolomite was processed to dolomite sinter in rotary furnaces. The products were transported railway-bound via the Rheinstollen gallery to the shipping facility north of Bingen. During these years the mine increasingly suffered from high production costs compared to open pit dolomite mines and finally was not able to compete on the market so in 1971 the mine was closed. In total about 6.4 million tonnes Fe-Mn ore and about 2.5 million tonnes of dolomite had been recovered.

The surface installations of the Straubenschacht site are worth to be specially mentioned. The ensemble is considered to be a most important monument of mining related architecture in Germany. The impressive neo-baroque style site was planned by Markwort & Seibert from Darmstadt. Unfortunately the buildings partly are in a very bad shape today and one can only hope that there will be strong efforts to conserve and restore this outstanding cultural heritage in the near future.

[comp. Roger Lang 2009]

Select Mineral List Type

Standard Detailed Gallery Strunz Chemical Elements

Mineral List


14 valid minerals.

Detailed Mineral List:

Aragonite
Formula: CaCO3
Calcite
Formula: CaCO3
References:
Chalcopyrite
Formula: CuFeS2
Copper
Formula: Cu
Dolomite
Formula: CaMg(CO3)2
References:
Epsomite
Formula: MgSO4 · 7H2O
Description: Recent formation from mine waters
Gypsum
Formula: CaSO4 · 2H2O
'Limonite'
References:
Malachite
Formula: Cu2(CO3)(OH)2
Manganite
Formula: Mn3+O(OH)
Pyrite
Formula: FeS2
Pyrolusite
Formula: Mn4+O2
References:
Quartz
Formula: SiO2
Rhodochrosite
Formula: MnCO3
References:
Romanèchite
Formula: (Ba,H2O)2(Mn4+,Mn3+)5O10
References:

Gallery:

CaMg(CO3)2 Dolomite

List of minerals arranged by Strunz 10th Edition classification

Group 1 - Elements
Copper1.AA.05Cu
Group 2 - Sulphides and Sulfosalts
Chalcopyrite2.CB.10aCuFeS2
Pyrite2.EB.05aFeS2
Group 4 - Oxides and Hydroxides
Quartz4.DA.05SiO2
Pyrolusite4.DB.05Mn4+O2
Romanèchite4.DK.10(Ba,H2O)2(Mn4+,Mn3+)5O10
Manganite4.FD.15Mn3+O(OH)
Group 5 - Nitrates and Carbonates
Calcite5.AB.05CaCO3
Rhodochrosite5.AB.05MnCO3
Dolomite5.AB.10CaMg(CO3)2
Aragonite5.AB.15CaCO3
Malachite5.BA.10Cu2(CO3)(OH)2
Group 7 - Sulphates, Chromates, Molybdates and Tungstates
Epsomite7.CB.40MgSO4 · 7H2O
Gypsum7.CD.40CaSO4 · 2H2O
Unclassified
'Limonite'-

List of minerals for each chemical element

HHydrogen
H EpsomiteMgSO4 · 7H2O
H GypsumCaSO4 · 2H2O
H ManganiteMn3+O(OH)
H MalachiteCu2(CO3)(OH)2
H Romanèchite(Ba,H2O)2(Mn4+,Mn3+)5O10
CCarbon
C AragoniteCaCO3
C CalciteCaCO3
C DolomiteCaMg(CO3)2
C MalachiteCu2(CO3)(OH)2
C RhodochrositeMnCO3
OOxygen
O AragoniteCaCO3
O CalciteCaCO3
O DolomiteCaMg(CO3)2
O EpsomiteMgSO4 · 7H2O
O GypsumCaSO4 · 2H2O
O ManganiteMn3+O(OH)
O MalachiteCu2(CO3)(OH)2
O PyrolusiteMn4+O2
O QuartzSiO2
O RhodochrositeMnCO3
O Romanèchite(Ba,H2O)2(Mn4+,Mn3+)5O10
MgMagnesium
Mg DolomiteCaMg(CO3)2
Mg EpsomiteMgSO4 · 7H2O
SiSilicon
Si QuartzSiO2
SSulfur
S ChalcopyriteCuFeS2
S EpsomiteMgSO4 · 7H2O
S GypsumCaSO4 · 2H2O
S PyriteFeS2
CaCalcium
Ca AragoniteCaCO3
Ca CalciteCaCO3
Ca DolomiteCaMg(CO3)2
Ca GypsumCaSO4 · 2H2O
MnManganese
Mn ManganiteMn3+O(OH)
Mn PyrolusiteMn4+O2
Mn RhodochrositeMnCO3
Mn Romanèchite(Ba,H2O)2(Mn4+,Mn3+)5O10
FeIron
Fe ChalcopyriteCuFeS2
Fe PyriteFeS2
CuCopper
Cu ChalcopyriteCuFeS2
Cu CopperCu
Cu MalachiteCu2(CO3)(OH)2
BaBarium
Ba Romanèchite(Ba,H2O)2(Mn4+,Mn3+)5O10

Other Regions, Features and Areas containing this locality

Eurasian PlateTectonic Plate
EuropeContinent
Germany

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References

 
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