|
|
Welcome!
Quartz, Germany
Posted by Rock Currier
|
|
Quartz, Germany March 24, 2009 07:02PM |
Registered: 7 years ago Posts: 8,482 |
Click here to view Best Minerals Quartz and here for Best Minerals A to Z and here for Fast Navigation of Best Minerals articles.
Can you help make this a better article? What good localities have we missed? Can you supply pictures of better specimens than those we show here? Can you give us more and better information about the specimens from these localities? Can you supply better geological or historical information on these localities?
Quartz - Germany
SiO2 trigonal
Here will go an image of a quartz from Germany that will hopefully get users to more closely examine this thread and some introductry remarks about German quartzes.
Quartz
Germany
Baden-Württemberg, Black Forest, Pforzheim
![]() | |
| Quartz 1.4cm | © Stefan Koch |
Öschelbronn and Dietlingen near Pforzheim are localities known for smoky to almost black double terminated xls, usually 5 mm to 2 cm, rarely up to 4 cm (at least the biggest I've seen). Those are formed in dolomitic marls ("Mittlerer Muschelkalk", mid-triassic). They are double-layered with a crumbly and grainy quartz-anhydrite mixture in the core, covered by a well crystallized outer layer with inclucions of bituninous matter, colouring the xls (so not being a real smoky quartz). Those xls are unique and only known from te northern and northeastern rim of the Black Forest. They are called "Pforzheimer Stinkquarz" (the "stink" means smelling, because freshly broken xls smell burnt because of the bituminous matter). The xls can be collected on the fields after harvest.
[Sebastian Möller 2009]
Quartz
Germany
Baden-Württemberg, Black Forest, Wolfach, Oberwolfach, Rankach valley, Clara Mine
![]() | |
| Quartz FOV 6mm wide | © A. Bleeker |
Quartz
Germany
Bavaria, Franconia, Fichtelgebirge, Wunsiedel, Bernstein
![]() | |
| Quartz, FOV 2.2cm | © 2005 M. Kampf |
Quartz
Germany
Bavaria, Franconia, Fichtelgebirge, Wunsiedel, Göpfersgrün, Johannes Mine
![]() | |
| Quartz 9cm wide | © K.Gerl |
Quartz
Germany
Bavaria, Upper Palatinate, Schwandorf, Wölsendorf Fluorite mining District
![]() | |
| Quartz 10cm tall | © Rob Lavinsky |
![]() | |
| Quartz & Fluorite 6.5cm wide | © Joseph Polityka |
Quartz
Germany
Hesse, Odenwald, Bensheim, Reichenbach
![]() | |
| Quartz 14cm wide | © Christian Bracke |
Quartz
Germany
Hesse, Taunus Mts, Usingen, Usingen quartzite works
![]() | |
| Quartz 14.6cm tall | © Christian Bracke |
![]() | |
| Quartz 11.5cm tall | © J.N |
Quartz
Germany
Lower Saxony, Harz Mts, Bad Lauterberg, Charlotte Magdalena Mine
![]() | |
| Quartz 6.9cm wide | © Christian Bracke |
Quartz
Germany
Lower Saxony, Harz Mts, Clausthal-Zellerfeld, Hahnenklee, Töberschekopf hill
![]() | |
| Quartz 6.5cm wide | © G. van der Veldt |
![]() | |
| Quartz 10cm wide | © G. van der Veldt |
Quartz
Germany
Lower Saxony, Hildesheim
![]() | |
| Quartz after fossil 1.5cm | © Tamás Ungvári 2005 |
Quartz
Germany
Lower Saxony, Rinteln, Hohenrode, Rumbeck Mtn (Taubenberg Mtn)
![]() | |
| Quartz FOV 1.8cm wide | © 2006 M. Kampf |
![]() | |
| 6.5mm Quartz xl on matrix | © Chinellato Matteo |
Quartz
Germany
North Rhine-Westphalia, Niederberg area, Velbert, Wasserfall Quarry
![]() | |
| Quartz FOV 1.8cm | © 2005 M. Kampf |
![]() | |
| Quartz FOV 2.2cm | © 2005 M. Kampf |
Quartz
Germany
North Rhine-Westphalia, Niederberg area, Wülfrath, Rohdenhaus, Rohdenhaus Quarry (incl. Krieger Quarry)
![]() | |
| Quartz 7cm wide | © Harjo |
![]() | |
| Quartz 65cm tall | © Harjo |
Quartz
Germany
North Rhine-Westphalia, Sauerland, Brilon, Rösenbeck
![]() | |
| Quartz 10.2cm tall | © Christian Bracke |
Quartz
Germany
North Rhine-Westphalia, Sauerland, Meschede, Ramsbeck, Dörnberg Mine
![]() | |
| Quartz 4.7cm wide | © KrauklMinerals |
![]() | |
| Quartz 5.3cm wide | © KrauklMinerals |
![]() | |
| Quartz 4.5cm wide | © KrauklMinerals |
![]() | |
| Quartz on Dolomite 5.7cm wide | © KrauklMinerals |
![]() | |
| Quartz 6.8cm wide | © KrauklMinerals |
Quartz
Germany
North Rhine-Westphalia, Sauerland, Warstein, Kallenhardt, Brühne quarry
![]() | |
| Quartz FOV 1.5cm wide | © tho-thie@web.de |
[[b]Quartz[/b]
Germany
North Rhine-Westphalia, Sauerland, Warstein, Suttrop, Auf dem Stein quarry
![]() | |
| Quartz 2.9cm tall | © Rob Lavinsky |
![]() | |
| Largest Quartz is 3cm tall | © Rob Lavinsky |
![]() | |
| Quartz 3cm wide | © Rob Lavinsky |
Suttrop-Type Quartz
The "type locality" of these crystals is "Auf der Vogelstange", a street at Suttrop, where crystals could be found until the area was mostly overbuilt. They can also be found in nearby quarries. Similar quartz specimen can be found along a "belt" of Devonian and Carboniferous limestones at the northern end of the Sauerland, a low mountain range in Nordrhein-Westfalen, Germany. This belt extends over 150 km from Dornap near Wuppertal in the West to Wünneberg-Bleiwäsche south of Paderborn in the East and is about 20 km wide. Among the many other locations where Suttrop-type quartz can be found are quarries at Kallenhardt, Wünnenberg-Bleiwäsche, Warstein, Hagen-Hohenlimburg, Velbert-Rhodenhaus.
The crystals themselves are younger than the Devonian limestones and formed probably during the late Paleocoic age in a hydrothermal environment. The crystals can be up to 5cm long, but most are much smaller. The color of the translucent crystals is most commonly a creamy white to light brown. The crystals are characterized by a pseudohexagonal, double terminated habit and a zonar inner structure. Both geyser-like rhythmic movements of water and tectonic events have been discussed as a cause of the zonar pattern. The mineral anhydrite, CaSO4, was incorporated at relatively high temperatures; later some of it was dissolved at lower temperatures (anhydrite is more soluble at lower temperatures), leaving tiny cavities in the crystal that contribute to its white color. Interestingly, overall the temperature during crystal growth increased with time, starting at about 60-80°C and ending at above 120°C, perhaps even above 300°C (Behr et al., 1979), which is very different from the typical development of quartz from Alpine-type fissures, for example. The crystals have a very high number of fluid inclusions, consuming up to 10% of their volume. Accordingly, the crystals have a lower specific gravity than usual. They also never show any accessorial faces and are heavily twinned.
While single double-terminated crystals are most sought-after, the crystals usually occur in irregularly intergrown aggregates that may weigh many kilograms and sometimes accumulate in former karst cavities.
[Amir C. Akhavan 2009]
Quartz
Germany
Rhineland-Palatinate, Eifel Mts, Mayen, Ettringen, Ettringer Bellerberg Mt.
![]() | |
| Quartz, Tridymite FOV 3mm | © Stephan Wolfsried |
![]() | |
| Quartz FOV 3mm | © Stephan Wolfsried |
![]() | |
| Quartz FOV 3mm | © Stephan Wolfsried |
Quartz
Germany
Rhineland-Palatinate, Hunsrück Mts, Idar-Oberstein, Niederwörresbach, Juchem Quarry
![]() | |
| Quartz v. amethyst 11cm wide | © Harjo |
![]() | |
| Quartz v. amethyst FOV 15cm | © A. Bleeker |
![]() | |
| Quartz geode 17.8cm wide | © |
![]() | |
| Quartz v. amethyst 9.1cm tall | © Rob Lavinsky |
![]() | |
| Quartz v. amethyst 13.5cm tall | © Russell G. Rizzo |
Quartz
Germany
Rhineland-Palatinate, Hunsrück Mts, Idar-Oberstein, Steinkaulenberg
![]() | |
| Quartz v. amethyst geode 9cm tall | © Russell G. Rizzo |
Quartz
Germany
Rhineland-Palatinate, Hunsrück Mts, Kirschweiler, Katzenloch, Rösselhalde
![]() | |
| Quartz v. eisenkissel FOV 5cm wide | © A. Bleeker |
![]() | |
| Quartz v. eisenkissel FOV 5cm wide | © A. Bleeker |
Quartz
Germany
Rhineland-Palatinate, Hunsrück Mts, Monzingen, Langenthal, Basalt AG Quarry ("Ferdinand Kloos" Quarry)
![]() | |
| Quartz, FOV 2.5mm wide | © A. Bleeker |
Quartz
Germany
Rhineland-Palatinate, Hunsrück Mts, Stromberg, Limestone quarries
![]() | |
| Quartz 21cm wide | © Christian Bracke |
Quartz
Germany
Rhineland-Palatinate, Rockenhausen, Lenz Quarry
![]() | |
| Quartz v. amethyst 12.5cm tall | © Peter Haas |
![]() | |
| Quartz v. smoky 14cm wide | © R. lang 2006 |
Quartz
Germany
Rhineland-Palatinate, Taunus Mts, Kaub, Slate quarry
![]() | |
| Quartz 7cm tall | © michael berghäuser |
Quartz
Germany
Rhineland-Palatinate, Taunus Mts, Nastätten, Miehlen
![]() | |
| Quartz 7cm tall | © michael berghäuser |
![]() | |
| Quartz ~6cm wide | © michael berghäuser |
![]() | |
| Quartz 10cm wide | © www.mb-minerals.de |
Quartz
Germany
Rhineland-Palatinate, Taunus Mts, Singhofen, Jammertal
![]() | |
| Quartz 5cm tall | © Volker Betz |
![]() | |
| Quartz 3cm tall | © Volker Betz |
![]() | |
| Quartz 4.8cm tall | © Volker Betz |
Quartz
Germany
Rhineland-Palatinate, Taunus Mts, St Goarshausen, Forstbach valley
![]() | |
| Quartz 7cm tall | © www.mb-minerals.de |
Quartz
Germany
Rhineland-Palatinate, Taunus Mts, St Goarshausen, Nochern
![]() | |
| Quartz 7cm tall | © michael berghäuser |
![]() | |
| Quartz 7cm tall | © michael berghäuser |
Quartz
Germany
Saxony, Erzgebirge, Annaberg-Buchholz, Dörfel, Dörfel Quarry (Bögl Quarry)
![]() | |
| Quartz 5cm tall | © RK |
![]() | |
| Quartz 2.5cm tall | © RK |
![]() | |
| Quartz 7cm wide | © RK |
Quartz
Germany
Saxony, Erzgebirge, Annaberg-Buchholz, Wiesenbad
![]() | |
| Quartz v. amethyst FOV 4cm wide | © 2006 RK |
Quartz
Germany
Saxony, Erzgebirge, Aue, Hakenkrümme Quarry
![]() | |
| Quartz 10cm wide | © M. Adelt |
Quartz
Germany
Saxony, Erzgebirge, Ehrenfriedersdorf, Sauberg Mine
![]() | |
| Quartz 4cm tall | © RK |
Quartz
Germany
Saxony, Erzgebirge, Freiberg District, Halsbrücke, Beihilfe Mine
![]() | |
| Quartz 11.5cm wide | © Rob Lavinsky |
Quartz
Germany
Saxony, Erzgebirge, Glashütte, Schlottwitz
![]() | |
| Quartz v. amethyst 17cm wide | © Petr Fuchs |
Quartz
Germany
Saxony, Erzgebirge, Schwarzenberg District, Bockau, Fahsel quarry
![]() | |
| Quartz v. jasper 10cm wide | © M. Adelt |
![]() | |
| Quartz v. smoky 8cm wide | © M. Adelt |
Quartz
Germany
Saxony, Oberlausitz, Kamenz, Oßling Quarry
![]() | |
| Quartz 20cm wide | © RK |
Quartz
Germany
Saxony, Vogtland, Bad Brambach
![]() | |
| Quartz 2cm wide | © RK |
![]() | |
| Quartz 7cm wide | © RK |
![]() | |
| Quartz 7cm wide | © M. Adelt |
![]() | |
| Quartz v. smoky 14cm wide | © M. Adelt |
![]() | |
| Quartz 4cm tall | © M. Adelt |
Click here to view Best Minerals Quartz and here for Best Minerals A to Z and here for Fast Navigation of Best Minerals articles.
Rock Currier
Crystals not pistols.
Edited 13 time(s). Last edit at 09/26/2011 08:48PM by Harjo Neutkens.
|
Re: Quartz, Germany March 27, 2009 07:51PM |
Registered: 4 years ago Posts: 1,425 |
Auf dem Stein quarry, Suttrop, Warstein, Sauerland, North Rhine-Westphalia, Germany
Suttrop-Type Quartz
The "type locality" of these crystals is "Auf der Vogelstange", a street at Suttrop, where crystals could be found until the area was mostly overbuilt. They can also be found in nearby quarries.
Similar quartz specimen can be found along a "belt" of Devonian and Carboniferous limestones at the northern end of the Sauerland, a low mountain range in Nordrhein-Westfalen, Germany. This belt extends over 150 km from Dornap near Wuppertal in the West to Wünneberg-Bleiwäsche south of Paderborn in the East and is about 20 km wide.
Among the many other locations where Suttrop-type quartz can be found are quarries at Kallenhardt, Wünnenberg-Bleiwäsche, Warstein, Hagen-Hohenlimburg, Velbert-Rhodenhaus.
The crystals themselves are younger than the Devonian limestones and formed probably during the late Paleocoic age in a hydrothermal environment.
The crystals can be up to 5cm long, but most are much smaller. The color of the translucent crystals is most commonly a creamy white to light brown. The crystals are characterized by a pseudohexagonal, double terminated habit and a zonar inner structure. Both geyser-like rhythmic movements of water and tectonic events have been discussed as a cause of the zonar pattern. The mineral anhydrite, CaSO4, was incorporated at relatively high temperatures; later some of it was dissolved at lower temperatures (anhydrite is more soluble at lower temperatures), leaving tiny cavities in the crystal that contribute to its white color. Interestingly, overall the temperature during crystal growth increased with time, starting at about 60-80°C and ending at above 120°C, perhaps even above 300°C (Behr et al., 1979), which is very different from the typical development of quartz from Alpine-type fissures, for example. The crystals have a very high number of fluid inclusions, consuming up to 10% of their volume. Accordingly, the crystals have a lower specific gravity than usual. They also never show any accessorial faces and are heavily twinned.
While single double-terminated crystals are most sought-after, the crystals usually occur in irregularly intergrown aggregates that may weigh many kilograms and sometimes accumulate in former karst cavities.
Edited 1 time(s). Last edit at 03/28/2009 10:26AM by Amir C. Akhavan.
Suttrop-Type Quartz
The "type locality" of these crystals is "Auf der Vogelstange", a street at Suttrop, where crystals could be found until the area was mostly overbuilt. They can also be found in nearby quarries.
Similar quartz specimen can be found along a "belt" of Devonian and Carboniferous limestones at the northern end of the Sauerland, a low mountain range in Nordrhein-Westfalen, Germany. This belt extends over 150 km from Dornap near Wuppertal in the West to Wünneberg-Bleiwäsche south of Paderborn in the East and is about 20 km wide.
Among the many other locations where Suttrop-type quartz can be found are quarries at Kallenhardt, Wünnenberg-Bleiwäsche, Warstein, Hagen-Hohenlimburg, Velbert-Rhodenhaus.
The crystals themselves are younger than the Devonian limestones and formed probably during the late Paleocoic age in a hydrothermal environment.
The crystals can be up to 5cm long, but most are much smaller. The color of the translucent crystals is most commonly a creamy white to light brown. The crystals are characterized by a pseudohexagonal, double terminated habit and a zonar inner structure. Both geyser-like rhythmic movements of water and tectonic events have been discussed as a cause of the zonar pattern. The mineral anhydrite, CaSO4, was incorporated at relatively high temperatures; later some of it was dissolved at lower temperatures (anhydrite is more soluble at lower temperatures), leaving tiny cavities in the crystal that contribute to its white color. Interestingly, overall the temperature during crystal growth increased with time, starting at about 60-80°C and ending at above 120°C, perhaps even above 300°C (Behr et al., 1979), which is very different from the typical development of quartz from Alpine-type fissures, for example. The crystals have a very high number of fluid inclusions, consuming up to 10% of their volume. Accordingly, the crystals have a lower specific gravity than usual. They also never show any accessorial faces and are heavily twinned.
While single double-terminated crystals are most sought-after, the crystals usually occur in irregularly intergrown aggregates that may weigh many kilograms and sometimes accumulate in former karst cavities.
Edited 1 time(s). Last edit at 03/28/2009 10:26AM by Amir C. Akhavan.
|
|
Re: Quartz, Germany March 27, 2009 11:07PM |
Registered: 7 years ago Posts: 8,482 |
|
|
Re: Quartz, Germany September 16, 2009 11:54AM |
|
Registered: 5 years ago Posts: 718 |
Hello.
There are quite a lot of localities in Germany.
Some really should be mentioned. Sorry, if some are already listed.
Baden-Württemberg:
Öschelbronn and Dietlingen near Pforzheim
known localities for smoky to almost black double terminated xls, usually 5 mm to 2 cm, rarely up to 4 cm (at least the biggest I've seen). Those are formed in dolomitic marls ("Mittlerer Muschelkalk", mid-triassic). They are double-layered with a crumbly and grainy quartz-anhydrite mixture in the core, covered by a well crystallized outer layer with inclucions of bituninous matter, colouring the xls (so not being a real smoky quartz). Those xls are unique and only known from te northern and northeastern rim of the Black Forest. They are called "Pforzheimer Stinkquarz" (the "stink" means smelling, because freshly broken xls smell burnt because of the bituminous matter). The xls can be collected on the fields after harvest.
Im Gehn Quarry, Bramsche, North Rhine-Westphalia
Nice Rock Crystals.
Amethyst locations in saxony (Erzgebirge Mts.) which have produced nice specimen include Seidelgrund Amethyst vein, Wiesenbad and Gebirge near Marienberg.
Smoky Quartz xls up to 12 cm have been found in Granulitgebirge Mts., Saxony (near Chemnitz).
There, at Mühlau a bigger pocket had been hit when a pipeline or cable trench had been built. The xls are prismatic, brown with white rim (partly and thin). Nice ones up to dm in length are from Elzing Quarry, Limbach-Oberfrohna. I've seen a cavity (xls already removed, but a friend told me they were up to at least 50 cm) I could nearly go into. Those are cavities in pegmatite veins, usually accompanied by feldspar xls (orthoclase) and Schorl xls.
Then there are lots of agate localities in Germany.
Regards,
Sebastia Möller
There are quite a lot of localities in Germany.
Some really should be mentioned. Sorry, if some are already listed.
Baden-Württemberg:
Öschelbronn and Dietlingen near Pforzheim
known localities for smoky to almost black double terminated xls, usually 5 mm to 2 cm, rarely up to 4 cm (at least the biggest I've seen). Those are formed in dolomitic marls ("Mittlerer Muschelkalk", mid-triassic). They are double-layered with a crumbly and grainy quartz-anhydrite mixture in the core, covered by a well crystallized outer layer with inclucions of bituninous matter, colouring the xls (so not being a real smoky quartz). Those xls are unique and only known from te northern and northeastern rim of the Black Forest. They are called "Pforzheimer Stinkquarz" (the "stink" means smelling, because freshly broken xls smell burnt because of the bituminous matter). The xls can be collected on the fields after harvest.
Im Gehn Quarry, Bramsche, North Rhine-Westphalia
Nice Rock Crystals.
Amethyst locations in saxony (Erzgebirge Mts.) which have produced nice specimen include Seidelgrund Amethyst vein, Wiesenbad and Gebirge near Marienberg.
Smoky Quartz xls up to 12 cm have been found in Granulitgebirge Mts., Saxony (near Chemnitz).
There, at Mühlau a bigger pocket had been hit when a pipeline or cable trench had been built. The xls are prismatic, brown with white rim (partly and thin). Nice ones up to dm in length are from Elzing Quarry, Limbach-Oberfrohna. I've seen a cavity (xls already removed, but a friend told me they were up to at least 50 cm) I could nearly go into. Those are cavities in pegmatite veins, usually accompanied by feldspar xls (orthoclase) and Schorl xls.
Then there are lots of agate localities in Germany.
Regards,
Sebastia Möller
|
|
Re: Quartz, Germany November 07, 2009 10:36AM |
Registered: 7 years ago Posts: 8,482 |
Copyright © Jolyon Ralph and Ida Chau 1993-2013. Site Map.
Locality, mineral & photograph data are the copyright of the individuals who submitted them. Site hosted & developed by Jolyon Ralph.
Mindat.org is an online information resource dedicated to providing free mineralogical information to all. Mindat relies on the contributions of thousands of members and supporters. Mindat does not offer minerals for sale. If you would like to add information to improve the quality of our database, then click here
to register.
Current server date and time: 22nd May 2013 03:56:12
Current server date and time: 22nd May 2013 03:56:12
Mindat Lightbox
Options| Fade toolbar when not in focus | Fix toolbar to bottom of page | ||
|---|---|---|---|
| Hide Social Media Links | |||
| Slideshow frame delay | seconds | ||





























































































