Vote for your favorite mineral in #MinCup26! - Sphalerite vs. Anorthite
Both zinc ore Sphalerite and calcium plagioclase feldspar Anorthite have perfect cleavage that will split cleanly if you hit them with a hammer, but only one can claim a larger split of your votes!
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Stibnite from
Silbersand Mine, Sankt Johann, Vordereifel, Mayen-Koblenz, Rhineland-Palatinate, Germany


Locality type:Mine
Classification
Species:Stibnite
Formula:Sb2S3
Confirmation
Validity:Believed Valid
Data
Mineral Data:Click here to view Stibnite data
Locality Data:Click here to view Silbersand Mine, Sankt Johann, Vordereifel, Mayen-Koblenz, Rhineland-Palatinate, Germany
Data Identifiers
Mindat Occurrence Record ID:612600
Long-form Identifier:1:3:612600:1
GUID (UUID V4):0
Nearest other occurrences of Stibnite
20.4km (12.7 miles) ⓘHoffnung Mine (Spes Mine), Martinsknipp, Ahrbrück, Altenahr, Ahrweiler, Rhineland-Palatinate, Germany
23.7km (14.7 miles) ⓘSaarsegen Mine, Lind, Altenahr, Ahrweiler, Rhineland-Palatinate, Germany
33.3km (20.7 miles) ⓘGeorg Mine, Willroth, Altenkirchen-Flammersfeld, Altenkirchen, Rhineland-Palatinate, Germany
34.5km (21.4 miles) ⓘRosenberg Mine, Braubach, Loreley, Rhein-Lahn-Kreis, Rhineland-Palatinate, Germany
37.1km (23.0 miles) ⓘSilberwiese mine, Oberlahr, Altenkirchen-Flammersfeld, Altenkirchen, Rhineland-Palatinate, Germany
38.3km (23.8 miles) ⓘNeuhoffnung Mine, Bad Ems, Bad Ems-Nassau, Rhein-Lahn-Kreis, Rhineland-Palatinate, Germany
39.4km (24.5 miles) ⓘApollo Mine, Raubach, Puderbach, Neuwied, Rhineland-Palatinate, Germany
39.7km (24.7 miles) ⓘMorgenröthe Mine, Dahlheim, Loreley, Rhein-Lahn-Kreis, Rhineland-Palatinate, Germany
42.8km (26.6 miles) ⓘWerlau, Sankt Goar, Hunsrück-Mittelrhein, Rhein-Hunsrück-Kreis, Rhineland-Palatinate, Germany
52.1km (32.4 miles) ⓘWohlfahrt Mine, Rescheid, Hellenthal, Euskirchen, Cologne, North Rhine-Westphalia, Germany
References
Wagner, T., Cook, N. J. (2000) Late-Variscan antimony mineralisation in the Rheinisches Schiefergebirge, NW Germany: evidence for stibnite precipitation by drastic cooling of high-temperature fluid systems. Mineralium Deposita, 35 (2) 206-222 doi:10.1007/s001260050016
 
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