Quartz-Fluorite-40064
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
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Relevante Bilder
![](https://upload.wikimedia.org/wikipedia/commons/thumb/a/a7/Chalcopyrite-Quartz-Rhodochrosite-hbru-07a.jpg/250px-Chalcopyrite-Quartz-Rhodochrosite-hbru-07a.jpg)
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
![](https://upload.wikimedia.org/wikipedia/commons/thumb/7/72/Cuprite-Malachite-m06-12a.jpg/125px-Cuprite-Malachite-m06-12a.jpg)
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
![](https://upload.wikimedia.org/wikipedia/commons/thumb/5/50/Copper-Azurite-49067.jpg/250px-Copper-Azurite-49067.jpg)
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
![](https://upload.wikimedia.org/wikipedia/commons/thumb/6/68/Gypsum-Glauberite-172282.jpg/125px-Gypsum-Glauberite-172282.jpg)
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
![](https://upload.wikimedia.org/wikipedia/commons/thumb/e/ee/Azurite-Malachite-173855.jpg/125px-Azurite-Malachite-173855.jpg)
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
![](https://upload.wikimedia.org/wikipedia/commons/thumb/0/0a/Bayldonite-Mimetite-rare08-2-52a.jpg/250px-Bayldonite-Mimetite-rare08-2-52a.jpg)
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
![](https://upload.wikimedia.org/wikipedia/commons/thumb/6/60/Ferberite%2C_Scheelite-352361.jpg/125px-Ferberite%2C_Scheelite-352361.jpg)
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
![](https://upload.wikimedia.org/wikipedia/commons/thumb/e/eb/Azurite-Malachite-rh3-24a.jpg/250px-Azurite-Malachite-rh3-24a.jpg)
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
![](https://upload.wikimedia.org/wikipedia/commons/thumb/b/ba/Goethite-Pyrite-162480.jpg/125px-Goethite-Pyrite-162480.jpg)
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
![](https://upload.wikimedia.org/wikipedia/commons/thumb/6/6c/Rhodochrosite-Serandite-34724.jpg/125px-Rhodochrosite-Serandite-34724.jpg)
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
![](https://upload.wikimedia.org/wikipedia/commons/thumb/7/7c/Aragonite-Copper-236750.jpg/250px-Aragonite-Copper-236750.jpg)
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
![](https://upload.wikimedia.org/wikipedia/commons/thumb/9/92/Fluorite-197984.jpg/125px-Fluorite-197984.jpg)
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
![](https://upload.wikimedia.org/wikipedia/commons/thumb/8/8f/Goethite-Gypsum-3d20a.jpg/125px-Goethite-Gypsum-3d20a.jpg)
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
![](https://upload.wikimedia.org/wikipedia/commons/thumb/1/1f/Perimorphose_Calcite-Sphalerite-Siderite_-_Aggeneys%2C_Orange_River_Area%2C_Southafrica.jpg/250px-Perimorphose_Calcite-Sphalerite-Siderite_-_Aggeneys%2C_Orange_River_Area%2C_Southafrica.jpg)
![](https://upload.wikimedia.org/wikipedia/commons/thumb/0/0e/Bayldonite-t08-69a.jpg/250px-Bayldonite-t08-69a.jpg)
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
![](https://upload.wikimedia.org/wikipedia/commons/thumb/e/e9/Aragonite-Sulphur-35879.jpg/250px-Aragonite-Sulphur-35879.jpg)
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
![](https://upload.wikimedia.org/wikipedia/commons/thumb/f/fd/Perimorphose_Calcit-Sphalerit-Siderit_inside_-_Aggeneys%2C_Orange_River_Area%2C_Southafrica.jpg/250px-Perimorphose_Calcit-Sphalerit-Siderit_inside_-_Aggeneys%2C_Orange_River_Area%2C_Southafrica.jpg)
![](https://upload.wikimedia.org/wikipedia/commons/thumb/8/8b/Scheelite-rare08-2-25a.jpg/250px-Scheelite-rare08-2-25a.jpg)
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
![](https://upload.wikimedia.org/wikipedia/commons/thumb/e/e6/Glauberite-172284.jpg/125px-Glauberite-172284.jpg)
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
![](https://upload.wikimedia.org/wikipedia/commons/thumb/c/cc/Azurite-146904.jpg/250px-Azurite-146904.jpg)
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
![](https://upload.wikimedia.org/wikipedia/commons/thumb/9/94/Ferberite-166632.jpg/125px-Ferberite-166632.jpg)
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
![](https://upload.wikimedia.org/wikipedia/commons/thumb/b/b8/Azurite-114364.jpg/250px-Azurite-114364.jpg)
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
![](https://upload.wikimedia.org/wikipedia/commons/thumb/f/f9/Quartz-174553.jpg/250px-Quartz-174553.jpg)
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
![](https://upload.wikimedia.org/wikipedia/commons/thumb/1/1b/Malachite-132181.jpg/250px-Malachite-132181.jpg)
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
![](https://upload.wikimedia.org/wikipedia/commons/thumb/5/5b/Quartz-139259.jpg/250px-Quartz-139259.jpg)
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
![](https://upload.wikimedia.org/wikipedia/commons/thumb/f/f4/Mimetite-280322.jpg/125px-Mimetite-280322.jpg)
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
![](https://upload.wikimedia.org/wikipedia/commons/thumb/d/de/Quartz-163758.jpg/250px-Quartz-163758.jpg)
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
![](https://upload.wikimedia.org/wikipedia/commons/thumb/2/27/Cuprite-ww12b.jpg/125px-Cuprite-ww12b.jpg)
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
![](https://upload.wikimedia.org/wikipedia/commons/thumb/5/55/Goethite-226303.jpg/250px-Goethite-226303.jpg)
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
![](https://upload.wikimedia.org/wikipedia/commons/thumb/3/36/Goethite-169735.jpg/250px-Goethite-169735.jpg)
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
![](https://upload.wikimedia.org/wikipedia/commons/thumb/8/8c/Pyrite-214678.jpg/125px-Pyrite-214678.jpg)
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
![](https://upload.wikimedia.org/wikipedia/commons/thumb/1/1a/Copper-65560.jpg/125px-Copper-65560.jpg)
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
![](https://upload.wikimedia.org/wikipedia/commons/thumb/3/3d/Copper-72284.jpg/125px-Copper-72284.jpg)
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
![](https://upload.wikimedia.org/wikipedia/commons/thumb/4/46/Gypsum-251119.jpg/250px-Gypsum-251119.jpg)
(c) Rob Lavinsky, iRocks.com – CC-BY-SA-3.0
![](https://upload.wikimedia.org/wikipedia/commons/thumb/3/30/Glendonite.jpg/125px-Glendonite.jpg)
![](https://upload.wikimedia.org/wikipedia/commons/thumb/0/0a/Gypsum_kapnik.jpg/250px-Gypsum_kapnik.jpg)
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PseudomorphosePseudomorphose ist ein Begriff aus der Mineralogie und bezeichnet ein Mineral, das nicht seine typische Eigengestalt (Kristallsystem) zeigt, sondern die äußere Form einer anderen Mineralart angenommen hat. Pseudomorphosen entstehen beispielsweise dadurch, dass zuerst Mineral A in einem Gestein kristallisiert, später weggelöst wird und der Hohlraum durch Mineral B verfüllt wird. .. weiterlesen