Emilie Shaft, Bülten-Adenstedt Mine, Ilsede, Peine District, Lower Saxony, Germanyi
Regional Level Types | |
---|---|
Emilie Shaft | Mine (Abandoned) |
Bülten-Adenstedt Mine | Mine (Abandoned) |
Ilsede | Municipality |
Peine District | District |
Lower Saxony | State |
Germany | Country |
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Latitude & Longitude (WGS84):
52° 16' 47'' North , 10° 12' 28'' East
Latitude & Longitude (decimal):
Type:
Mine (Abandoned) - last checked 2022
Köppen climate type:
Nearest Settlements:
Place | Population | Distance |
---|---|---|
Ilsede | 12,241 (2016) | 1.9km |
Peine | 49,953 (2014) | 4.8km |
Hohenhameln | 9,815 (2011) | 10.1km |
Söhlde | 8,361 (2015) | 10.2km |
Meerdorf | 1,140 (2015) | 10.5km |
Mindat Locality ID:
419945
Long-form identifier:
mindat:1:2:419945:1
GUID (UUID V4):
247e0481-a2ca-4313-b919-64ae1064b149
Other/historical names associated with this locality:
Schacht Emilie, Grube Emilie, Grube Bülten Adenstedt, Grube Gross-Bülten,
Translation of https://www.geolife.de/poi-948630090-9460.html :
The Emilie shaft was dug to a depth of 284 m between 1937 and 1939 and was considered one of the most modern mines for ore mining at the time.
Today, visitors can find essential information about the Emilie Shaft on an information board.
The cycle path that leads along the shaft was a track road for the transport of sand and mud and a connecting route to the train station in Vöhrum until ore mining stopped.
Today, visitors can find essential information about the Emilie Shaft on an information board.
The cycle path that leads along the shaft was a track road for the transport of sand and mud and a connecting route to the train station in Vöhrum until ore mining stopped.
Located between the villages of Bülten and Adenstedt, approx. 5.5 km SSE of Peine.
Outcrop description: First opencast mining, then mine (underground). Hermann-Schacht, Wilhelm-Schacht, Engelhard-Schacht, Gerhard-Schacht, Emilie-Schacht, Carl-Schacht (dewatering).
Start of mining: 3rd century, proven from 1858, end of mining in 1976.
Location type: Mine (abandoned/old)
Geology: Manganese and iron mineralization. Mn-containing ore shell pebbles date back to oolitic brown iron deposits from the Jurassic, which were shattered by repeated flooding of the Cretaceous Sea and deposited in halokinetic troughs.
Exquisite groutite crystals.
Select Mineral List Type
Standard Detailed Gallery Strunz Chemical ElementsDetailed Mineral List:
ⓘ Groutite Formula: Mn3+O(OH) References: Vik Vanrusselt collectionIdentification: Dealer/Collection Label |
ⓘ 'Limonite' References: https://www.mindat.org/photo-1321345.htmlIdentification: Visual Identification |
ⓘ Marcasite Formula: FeS2 References: https://www.mindat.org/photo-1321345.htmlIdentification: Visual Identification |
ⓘ Quartz Formula: SiO2 References: https://www.mindat.org/photo-1321345.htmlIdentification: Visual Identification |
Gallery:
List of minerals arranged by Strunz 10th Edition classification
Group 2 - Sulphides and Sulfosalts | |||
---|---|---|---|
ⓘ | Marcasite | 2.EB.10a | FeS2 |
Group 4 - Oxides and Hydroxides | |||
ⓘ | Quartz | 4.DA.05 | SiO2 |
ⓘ | Groutite | 4.FD.10 | Mn3+O(OH) |
Unclassified | |||
ⓘ | 'Limonite' | - |
List of minerals for each chemical element
H | Hydrogen | |
---|---|---|
H | ⓘ Groutite | Mn3+O(OH) |
O | Oxygen | |
O | ⓘ Groutite | Mn3+O(OH) |
O | ⓘ Quartz | SiO2 |
Si | Silicon | |
Si | ⓘ Quartz | SiO2 |
S | Sulfur | |
S | ⓘ Marcasite | FeS2 |
Mn | Manganese | |
Mn | ⓘ Groutite | Mn3+O(OH) |
Fe | Iron | |
Fe | ⓘ Marcasite | FeS2 |
Other Regions, Features and Areas containing this locality
Eurasian PlateTectonic Plate
EuropeContinent
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