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Granulite outcrop, Waldheim, Döbeln, Saxony, Germany
Outcrop of a hydrothermally altered granulite, located just east of the Waldheim freight depot. Today inaccessible.
Located about 10 km SW of Döbeln.
Prismatine from this locality was considered as kornerupine for a long time, before it was eventually recognised as a new mineral. Older specimens, therefore, may still be labelled as kornerupine. The latter, however, does not occur here.
Mineral List
| Corundum var: Ruby | Dumortierite 'Kryptotile' | Prismatine (TL) Sapphirine | Schorl Spinel |
8 entries listed. 6 valid minerals. 1 type locality (valid mineral).
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References
- SAUER, A. (1886): (Über eine eigentümliche Granulitart als Muttergestein zweier neuer Mineralspecies). Zeitschrift der Deutschen Geologischen Gesellschaft 38, 704-705.
- UHLIG, J. (1910): Über Prismatin und Kryptotil von Waldheim in Sachsen.- Zeitschrift für Kristallographie und Mineralogie 47, 215-213.
- Grew, E.S., M.A. Cooper & F.C. Hawthorne (1996): Prismatine: Revalidation for boron-rich compositions in the kornerupine group. Mineralogical Magazine 60, 483-491.
- UHLIG, J. (1910): Über Prismatin und Kryptotil von Waldheim in Sachsen.- Zeitschrift für Kristallographie und Mineralogie 47, 215-213.
- Grew, E.S., M.A. Cooper & F.C. Hawthorne (1996): Prismatine: Revalidation for boron-rich compositions in the kornerupine group. Mineralogical Magazine 60, 483-491.
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