Blog der Deutschen Gemmologischen Gesellschaft

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Herausgeber: 
Deutsche Gemmologische Gesellschaft e.V.
Prof.-Schlossmacher-Str. 1
D-55743 Idar-Oberstein

 

Copyright:
Für alle Beiträge behält sich die Deutsche Gemmologische Gesellschaft (Deutsche Gesellschaft für Edelsteinkunde) e.V. sämtliche Rechte vor, insbesondere die des Nachdrucks, der Übersetzung in andere Sprachen und der photomechanischen Wiedergabe. Die veröffentlichten Beiträge stellen – soweit namentlich bezeichnet – die Auffassung der Autoren dar und geben nicht notwendig die Meinung von Herausgeber und Schriftleitung wieder. (Content of this journal may not be reproduced in any form without the permission of the German Gemmological Association. Opinions expressed do not necessarily reflect the views of the Association.)

The typical inclusion pattern in Moldavite: Round to oval gas bubbles, as well as straight or curved swirls (flow structures) and elongated lechatelierite inclusions showing high relief (x40, photo: T. Stephan).

One of the most well known and popular natural glasses is moldavite, which formed during a meteorite impact about 14.8 million years ago. Today, moldavite is mainly obtained from the Czech Republic. In spring 2022, the authors visited the largest mine currently in operation, a sand-and-gravel quarry near the small village of Chlum in the southern Czech Republic, where moldavite is found as a by-product. This article reviews the formation and distribution of moldavite, gives an overview of current mining activities and reports the gemmological characteristics of samples collected by the authors.

 

This article was first published in The Journal of Gemmology, 38(7), 2023, pp. 696-707. A pdf-file of this article is available here.

 

Authors

Dr. Tom Stephan, DGemG,
Štěpán Jaroměřský, Faculty of Science, Charles University, Prague, Czech Republic
Lukáš Zahradníček, National Museum, Prague, Czech Republic &
Stefan Müller, DSEF


© 2023 by Gem-A

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