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Schlattain-Clavadatsch-Padella-Schuppen
- Origine del nome
- Rango
- scaglia tettonica
- Statuto
- termine locale (informale)
- In breve
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The Schlattain-Clavadatsch-Padella Slices form small isolated klippes, located in the core of the synclinorium of the “Samedan Zone” and composed of Triassic to Late Cretaceous sediments. They were thrust onto the cover of the Err Nappe and therefore attributed to the Bernina Nappe Complex.
- Nota sul nome
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Trais-Fluors-Schuppe p.p. (Cornelius ----)