-
Schlattain-Clavadatsch-Padella-Schuppen
- Origin of the Name
- Rank
- tectonic slice
- Status
- local name (informal)
- In short
-
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.
- Nomenclatorial Remarks
-
Trais-Fluors-Schuppe p.p. (Cornelius ----)
- Skip to home page (press enter)
- Skip to main navigation (press enter)
- Skip to main content (press enter)
- Skip to contact page (press enter)
- Skip to search page (press enter)