Mineralienatlas (name for mineral atlas) is the platform for people interested in mineralogy, geology, palaeontology and mining since 2001. We operate a significant database for minerals, fossils, rocks and their localities. Mineralienatlas is not limited to a section. We bring together information and inform comprehensive.

To complete our information constantly, we need your support. With us, everyone can and should participate. Currently Mineralienatlas is used and expanded by 10586 members. Every month hundreds of thousands of visitors use our website as an information source.
 
Geolitho Foundation non-profit GmbH
Geolitho Foundation non-profit GmbH is the non-profit supporter of the Mineral Atlas (Mineralienatlas), the Lithotheque, the Geolitho Collection Management and the Marketplace and Store by collectors for collectors. The Foundation promotes public education in the field of mineralogy, geology, paleontology and mining by operating, maintaining and further expanding earth science projects.
 
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https://vfmg.de/der-aufschluss/
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https://www.chiemgauer-mineralien-fossiliensammler.de/
https://www.juwelo.de
https://fossilsworldwide.de/
 
The min­er­al fair end­ed suc­cess­ful­ly and the au­thor of this ar­ti­cle re­ceived on­ly pos­i­tive feed­back. Many deal­ers were ex­treme­ly sat­is­fied. Ac­cord­ing to the or­ganiz­er, 18,000 guests visit­ed the halls on Sa­t­ur­day alone. Both days were a hive of ac­tiv­i­ty and the nu­mer­ous chil­dren's at­trac­tions were wel ... moreThe mineral fair ended successfully and the author of this article received only positive feedback. Many dealers were extremely satisfied. According to the organizer, 18,000 guests visited the halls on Saturday alone. Both days were a hive of activity and the numerous children's attractions were well received. Parents were everywhere with their children to complete the geo-rally.

For mineral collectors, the usual dealers were on site, although some tables remained empty. There were no highlights from the scene or overflowing tables with identical material from new finds. However, one stand with an impressive selection of Germanite chunks was a welcome novelty.

The special exhibition “The Impossible Crystal” was a success. Even if not all the exhibits could be described as “impossible crystal”, all the pieces were of the best quality and well worth seeing. In the B halls, the author visited the “Young Designers”, including a student who presented cast silver jewelry in an organic design that showed off the embedded stones to their best advantage - an impressive piece of work...

Translated with DeepL.com (free version)
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This is the most com­pre­hen­sive syn­op­sis re­lat­ed to the his­to­ry, the min­er­al­o­gy, the ex­ploi­ta­tion and the most ac­tu­al eco­nom­ic and po­lit­i­cal re­sumé on rare earth el­e­ments and their min­er­als to be found in the in­ter­net. REE be­long to the most im­por­tant raw ma­te­rials of the 21st cen­tu­ry, which are used ... moreThis is the most comprehensive synopsis related to the history, the mineralogy, the exploitation and the most actual economic and political resumé on rare earth elements and their minerals to be found in the internet. REE belong to the most important raw materials of the 21st century, which are used in a large number of key technologies. However, due to the fact that almost 97% of the world's REE are mined and produced in China, REE have become an ongoing political issue, mainly amongst technology providing countries like the US, Japan and Western Europe.

This portrait tries to explain the characteristics of REE and their role for our modern world. Written and investigated by Peter Seroka. (Article in german)
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... Der gewöhn­liche Habi­tus des Ana­tas ist dipyra­mi­dal, wobei die Dop­pelpyra­mide {111} spitz­er als die Dop­pelpyra­mide {112} ist und der Form nach einem Ok­taed­er gleichkommt (aber auch rundlich oder flachdipyra­mi­dal). Die En­den der Kris­talle sind un­ter­schiedlich, oft nur an den Kris­tallen eine Dipyra ... more... Der gewöhnliche Habitus des Anatas ist dipyramidal, wobei die Doppelpyramide {111} spitzer als die Doppelpyramide {112} ist und der Form nach einem Oktaeder gleichkommt (aber auch rundlich oder flachdipyramidal). Die Enden der Kristalle sind unterschiedlich, oft nur an den Kristallen eine Dipyramide ohne weitere Flächen. Dies ist der am häufigst vorkommende Habitus. Weniger, jedoch nicht selten, treten Dipyramiden mit abgestumpften Spitzen auf, bzw. auch durch eine Basisfläche angeschnitten, welche wiederum von Flächen weiterer Dipyramiden begleitet sein kann. Stumpfere Dipyramidern können ... Ein Beitrag von Peter Seroka
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